Wikipédia jvwiki https://jv.wikipedia.org/wiki/Wikip%C3%A9dia:Pendhapa MediaWiki 1.45.0-wmf.7 first-letter Médhia Mirunggan Parembugan Naraguna Parembugan Naraguna Wikipédia Parembugan Wikipédia Barkas Parembugan Barkas MédhiaWiki Parembugan MédhiaWiki Cithakan Parembugan Cithakan Pitulung Parembugan Pitulung Kategori Parembugan Kategori Gapura Parembugan Gapura TimedText TimedText talk Modhul Parembugan Modhul Acara Pembicaraan Acara 5 9411 1731259 1556253 2025-06-29T16:17:59Z 202.145.5.46 /* Kurangi lindungi */ pérangan anyar 1731259 wikitext text/x-wiki Nyuwun pangapura banget aku prei suwe, saiki molai aktif maneh. Mas Meursault kaya sopir metromini ngejar setoran, ati-ati mas aja nganti ngganggu urusan sing luwih utama, [[Panganggo:Slamet Serayu|Slamet Serayu]] 00:50, 23 Januari 2007 (UTC) :Suwun mas. Aku kebeneran lagi kegandrungan ya péngin nulis-nulis artikel ing jv: kéné! Soalé wis suwé ora aktif. Préi sedélok saka id:. ''Garis mati'' tanggal 8 Maret 2007, soalé dina iku jv: umuré telung taun. Oh iya wingi Siji Sura ya! [[User:Meursault2004|Meursault2004]]^{[[User_talk:Meursault2004|ngobrol]]} 05:28, 23 Januari 2007 (UTC) Mas, jenengé kok garis mati dudu ulang taun? nek ulang taun kan iso tumpengan, lha nek garis mati kok dadi medéni [[Panganggo:Slamet Serayu|Slamet Serayu]] 06:50, 23 Januari 2007 (UTC) == Pengunduran diri == Rekan-rekan pengurus Wikipedia bahasa Jawa, dengan ini saya ingin mengajukan pengunduran diri saya sebagai pengurus/opsis di Wikipedia bahasa Jawa dengan alasan saya tidak bisa memenuhi kewajiban pengurus di Wikipedia ini (tidak aktif di sini), selain daripada itu saya tidak merasa kompeten sebagai pengurus karena tidak bisa berbahasa Jawa (kan aneh, masak pengurus tidak bisa bahasanya). Mohon agar dapat dimaklumi. Terima kasih. [[:id:User:Borgx|borgx]]^{([[:id:User_talk:Borgx|kirim pesan]])} 03:16, 20 Januari 2008 (UTC) ===Agree=== # '''Agree''' - Wah sayang sekali. Tapi kami harapkan kalau ada apa-apa masih tetap dibantu ya:-) [[User:Meursault2004|Meursault2004]]^{[[User_talk:Meursault2004|ngobrol]]} 14:05, 20 Januari 2008 (UTC) #* Tentu saja saya akan bantu kalau bisa. [[:id:User:Borgx|borgx]]^{([[:id:User_talk:Borgx|kirim pesan]])} 00:05, 21 Januari 2008 (UTC) # '''Agree''' - tapi berat dan sangat-sangat disayangkan, [[Panganggo:Slamet Serayu|Slamet Serayu]] 04:32, 23 Januari 2008 (UTC) # '''Agree''' - memang sayang sekali, yang penting masih bisa dihubungi/ditanya-tanya. [[User:TracySurya|Tracy]]^{[[User_talk:TracySurya|gunemanku]]} 10:20, 27 Januari 2008 (UTC) ===Disagree=== == Seneng sanget == Atiku lega, pak Pras karo mbak Tracy dadi Pengurus neng jv:, slamet ya, [[Panganggo:Slamet Serayu|Slamet Serayu]] 03:46, 23 Januari 2008 (UTC) :Pengunduran Bung Borgx aku sejatine ora setuju ning arep konsultasi mas Meursault ndise', muga-muga molai saiki aku isa melu aktif maneh, [[Panganggo:Slamet Serayu|Slamet Serayu]] 03:46, 23 Januari 2008 (UTC) :Syukur mas, nanging ya wis bèn borgx amerga dhèwèké tugasé wis akèh lan bisa nulung tanpa dadi pangurus. Ing sisi liya Wikipedia Jawa isih cilik dadi yèn pangurusé kakèhan mengko bisa disrengeni Wikimedia Pusat. [[User:Meursault2004|Meursault2004]]^{[[User_talk:Meursault2004|ngobrol]]} 08:12, 23 Januari 2008 (UTC) Matur nuwun mas Slamet, semoga kehadiran kami ada manfaatnya, ayo sama-sama kita ramaikan, kalau bukan kita siapa lagi? Kanggo Mas Meursault, bab pangunduran dhiri mas Borgx jané aku ya kurang sarujuk, apa pancèn cacahing pangurus kuwi ana wates utawa ''ratio''né? Tinimbang mas Borgx mundur jané aluwung aku ora usah dadi pangurus waé, nanging tetep waé aku bakal aktif (gak ngaruh nèk cara cah saiki). [[panganggo:Pras|Pras]] [[User_talk:Pras|^{<small>Kothak pesen</small>}]] 11:25, 23 Januari 2008 (UTC) :Wah, menawi Pak Pras ingkang badhé ''mengundurkan diri'', kula ingkang mboten sarujuk. [[User:TracySurya|Tracy]]^{[[User_talk:TracySurya|gunemanku]]} 10:20, 27 Januari 2008 (UTC) Ya apa boleh buat ... soalnya Borgx sendiri sibuk dan kurang paham bahasa Jawa :-) Tetapi untungnya masih bisa ditanya-tanya. [[User:Meursault2004|Meursault2004]]^{[[User_talk:Meursault2004|ngobrol]]} 12:36, 27 Januari 2008 (UTC) == Pengunduran diri == Halo rekan-rekan pengurus, saya telah [http://meta.wikimedia.org/w/index.php?title=Steward_requests/Permissions&oldid=3012575 mengundurkan diri] dari kepengurusan karena (memang) bukan pengguna aktif di Wikipedia bahasa Jawa ini. Terima kasih :D. [[Panganggo:Hayabusa future|Hayabusa future]] ^{[[Dhiskusi Panganggo:Hayabusa future|pirembagan]]} 24 Oktober 2011 14.37 (UTC) == Kurangi lindungi == {{Pp}}{{Pp-semi-protected}} [[Mirunggan:Pasumbanging naraguna/202.145.5.46|202.145.5.46]] 29 Juni 2025 16.17 (UTC) 889cotf2e58h79sdoo70g42woq88kcq 0 17481 1731260 1715575 2025-06-29T17:15:29Z -Lemmy- 23684 1731260 wikitext text/x-wiki {{Football club infobox | clubname = Eintracht Frankfurt | image = | fullname = Eintracht Frankfurt | nickname = SGE, Die Adler | founded = [[1899]] | ground = [[Deutsche Bank Park]], [[Frankfurt am Main]] | capacity = 58.000 | chairman = [[Mathias Beck]] | manager = [[Dino Toppmöller]]| league = [[Bundesliga]] | season = 2024/25 | position = 3. | | pattern_la1 = _frankfurt2425h | pattern_b1 = _frankfurt2425h | pattern_ra1 = _frankfurt2425h | pattern_sh1 = | pattern_so1 = | leftarm1 = FF0000 | body1 = FFFFFF | rightarm1 = FF0000 | shorts1 = 000000 | socks1 = FFFFFF | pattern_la2 = _frankfurt2425a | pattern_b2 = _frankfurt2425a | pattern_ra2 = _frankfurt2425a | pattern_sh2 = | pattern_so2 = | leftarm2 = 000000 | body2 = 000000 | rightarm2 = 000000 | shorts2 = 000000 | socks2 = 000000 | pattern_la3 = _frankfurt2425t | pattern_b3 = _frankfurt2425t | pattern_ra3 = _frankfurt2425t | pattern_sh3 = | pattern_so3 = | leftarm3 = FF6600 | body3 = FF6600 | rightarm3 = FF6600 | shorts3 = 000000 | socks3 = FF6600 }} [[File:Commerzbank-Arena (Haupttribüne).JPG|250px|right|thumb|Deutsche Bank Park Kandhang Eintracht Frankfurt]] [[Gambar:Eintrachtadler.JPG|thumb|right|260px|Ultras Frankfurt]] '''Eintracht Frankfurt''', uga dikenal minangka ''SGE'' utawa sadurungé ''Die Adler'', yakuwi salah siji klub bal-balan utawa [[bal-balan]] [[Jerman]] sing main ing [[Bundesliga]] lan duwé markas ing kutha [[Frankfurt am Main]]. Didegaké ing [[8 Maret]] [[1899]]. == Prestasi == * '''[[Piala UEFA]]: 2''' ** 1979/80, 2021/22 * '''[[Liga Jerman]]: 1''' ** 1958/59 * '''[[Piala DFB]]: 5''' ** 1973/74; 1974/75; 1980/81; 1987/88; 2017/18 == Pratélan juru main 2024/25 == === Skuad utama === {{updated|5 Fèbruari 2025}}<ref>[https://en.eintracht.de/2024-2025/squad/ eintracht.de] </ref> {{Fs start}} {{Fs player|no=1|nat=GER|pos=GK||name=[[Kevin Trapp]]|other=Kapten}} {{Fs player|no=3|nat=BEL|pos=DF|name=[[Arthur Theate]]}} {{Fs player|no=4|nat=GER|pos=DF|name=[[Robin Koch]]|other=wakil kapten}} {{Fs player|no=5|nat=SUI|pos=DF|name=[[Aurèle Amenda]]}} {{Fs player|no=6|nat=DEN|pos=MF|name=[[Oscar Højlund]]}} {{Fs player|no=8|nat=ALG|pos=FW|name=[[Farès Chaïbi]]}} {{Fs player|no=9|nat=CRO|pos=FW|name=[[Igor Matanović]]}} {{Fs player|no=11|nat=FRA|pos=FW|name=[[Hugo Ekitike]]}} {{Fs player|no=13|nat=DEN|pos=DF|name=[[Rasmus Kristensen]]}} {{Fs player|no=15|nat=TUN|pos=MF|name=[[Ellyes Skhiri]]}} {{Fs player|no=16|nat=SWE|pos=MF|name=[[Hugo Larsson]]}} {{Fs player|no=17|nat=FRA|pos=FW|name=[[Elye Wahi]]}} {{Fs player|no=18|nat=GER|pos=MF|name=[[Mahmoud Dahoud]]}} {{Fs player|no=19|nat=FRA|pos=FW|name=[[Jean-Mattéo Bahoya]]}} {{Fs player|no=20|nat=TUR|pos=MF|name=[[Can Uzun]]}} {{Fs player|no=21|nat=GER|pos=DF|name=[[Nathaniel Brown]]}} {{Fs player|no=22|nat=USA|pos=DF|name=[[Timothy Chandler]]}} {{Fs player|no=23|nat=HUN|pos=MF|name=[[Krisztián Lisztes]]}} {{fs mid}} {{Fs player|no=26|nat=FRA|pos=MF|name=[[Éric Junior Dina Ebimbe]]}} {{Fs player|no=27|nat=GER|pos=MF|name=[[Mario Götze]]}} {{Fs player|no=28|nat=GER|pos=MF|name=[[Marcel Wenig]]}} {{Fs player|no=29|nat=FRA|pos=DF|name=[[Niels Nkounkou]]}} {{Fs player|no=30|nat=BEL|pos=FW|name=[[Michy Batshuayi]]}} {{Fs player|no=33|nat=GER|pos=GK|name=[[Jens Grahl]]}} {{Fs player|no=34|nat=GER|pos=DF|name=[[Nnamdi Collins]]}} {{Fs player|no=35|nat=BRA|pos=DF|name=[[Tuta]]}} {{Fs player|no=36|nat=GER|pos=FW|name=[[Ansgar Knauff]]}} {{Fs player|no=38|nat=GER|pos=MF|name=[[Ebu Bekir Is]]}} {{Fs player|no=40|nat=BRA|pos=GK|name=[[Kauã Santos]]}} {{Fs player|no=44|nat=ECU|pos=DF|name=Davis Bautista}} {{Fs player|no=45|nat=GER|pos=MF|name=Mehdi Loune}} {{Fs player|no=47|nat=HUN|pos=MF|name=Noah Fenyő}} {{Fs player|no=48|nat=ESP|pos=FW|name=Junior Awusi}} {{Fs player|no=49|nat=MAR|pos=FW|name=Anas Alaoui}} <!-- {{Fs player|no=|nat=USA|pos=MF|name=[[Paxten Aaronson]]}} {{Fs player|no=|nat=GER|pos=DF|name=[[Elias Baum]]}} {{Fs player|no=|nat=POR|pos=DF|name=[[Aurélio Buta]]}} {{Fs player|no=|nat=ESP|pos=FW|name=[[Nacho Ferri]]}} {{Fs player|no=|nat=GER|pos=FW|name=[[Jessic Ngankam]]}} {{Fs player|no=|nat=ALB|pos=GK|name=[[Simon Simoni]]}} {{Fs player|no=|nat=CRO|pos=DF|name=[[Hrvoje Smolčić]]}} Joining in 2025-26 --> {{Fs end}} == Pranala njaba == * [http://www.eintracht.de Situs web resmi] * [http://www.sge4ever.de Situs Fans Eintracht] {{Bundesliga}} [[Kategori:Tim bal-balan Jerman]] [[Kategori:Jerman]] [[Kategori:Frankfurt am Main]] {{jerman-sb-stub}} eec85yh9ukw7ex43529scb6cxxwfjci 0 24265 1731270 1632412 2025-06-30T10:00:32Z InternetArchiveBot 48188 Rescuing 1 sources and tagging 0 as dead.) #IABot (v2.0.9.5 1731270 wikitext text/x-wiki {| border=1 cellpadding="2" cellspacing="0" width="300px" align="right" style="margin: 0 0 1em 1em; background: #f9f9f9; border: 1px #aaaaaa solid; border-collapse: collapse; font-size: 95%;" |+<span style="font-size:large;">'''Gemeente Utrecht'''</span> |- |style="background:#efefef;" align="center" colspan=2| {| |- |align="center" width="140px"|[[Gambar:Flag of Utrecht city.svg|120px]] |align="center" width="140px"|[[Gambar:Utrecht gemeente wapen.svg|120px]] |- |align="center" width="140px"|<small>Gendéra {{PAGENAME}}</small> |align="center" width="140px"|<small>Lambang {{PAGENAME}}</small> |} |- |align=center colspan=2| <br />[[Gambar:LocatieUtrecht.png|240px]]<br /><br /><div class="center">{{PAGENAME}} ing Walanda</div><br /> |- ! colspan="2" | Katrangan cekak |- style="background: #ffffff;" | [[Provinsi ing Walanda|Provinsi]]: || [[Provinsi Utrecht|Utrecht]] |- style="background: #ffffff;" | Jembar: || 99,32 [[kilometer persegi|km²]] |- style="background: #ffffff;" | [[Padunung]]: || 293.854 <small>(1 November 2007)</small> |- style="background: #ffffff;" | Situs wèb resmi: || http://www.utrecht.nl {{Webarchive|url=https://web.archive.org/web/20110204030348/http://www.utrecht.nl/ |date=2011-02-04 }} |- ! colspan="2" | Pulitik |- style="background: #ffffff;" | ''Burgemeester'' (Walikutha): || Aleid Wolfsen |} '''Utrecht''' iku siji ''[[gemeente]]'' lan uga kutha krajan [[Provinsi Utrecht]] ing [[Walanda]]. Kutha iki sing ndunungi ana 293.854 jiwa (1 November 2007) lan ambané ana 99,32&nbsp;km². Sajarah kutha Utrecht iki wis lawas banget. Kutha iki diadegaké déning bangsa Romawi ing kiwa-tengené taun [[50 SM]] ing pinggir [[Kali Rijn]] lan diwèhi jeneng ''Traiectum ad Rhenum''. Jeneng ing [[basa Latin]] iki tegesé: "papan panyabrangan kali Rijn". Jeneng iki pungkasané dicekak ing [[basa Walanda]] dadi ''Utrecht'' lan dienggo nganti sepréné. Kutha Utrecht uga nduwé siji univèrsitas nagari sing diarani ''[[Univèrsitas Utrecht|Universiteit Utrecht]]''. {{GemeentenUtrecht}} [[Kategori:Gemeente ing Walanda]] 1dc5xiy8vuvjcma5nq4p39yvrae27ey 0 42511 1731262 1641432 2025-06-30T01:41:12Z InternetArchiveBot 48188 Rescuing 1 sources and tagging 0 as dead.) #IABot (v2.0.9.5 1731262 wikitext text/x-wiki {{Taxobox | color = lightgreen | name = ''Sorgum'' | image = Sorghum.jpg | image_width = 250px | regnum = [[Plantae]] | divisio = [[Magnoliophyta]] | classis = [[Liliopsida]] | ordo = [[Poales]] | familia = [[Poaceae]] | genus = '''''Sorghum''''' | genus_authority = [[Carolus Linnaeus|L.]] | subdivision_ranks = Spesies | subdivision = Dumadi saka 30 spésies, pirsani teks }} '''Sorgum''' utawa '''canthèl''' (''Sorghum'' spp.) iku [[tetuwuhan]] serbaguna sing bisa kanggo sumber [[pangan]], [[pakan kéwan]] lan bahan baku [[indhustri]]. Minangka bahan pangan angka 5, sorgum ana ing urutan angka 5 sawisé [[gandum]], [[jagung]], [[pari]], lan [[jawawut|jelai]]. Sorgum minangka panganan pokok wigati ing [[Asia Kidul]] lan [[Afrika]] sub-sahara. == Spesies == * ''[[Sorghum almum]]'' * ''[[Sorghum amplum]]'' * ''[[Sorghum angustum]]'' * ''[[Sorghum arundinaceum]]'' * ''[[Sorghum bicolor]]'' * ''[[Sorghum brachypodum]]'' * ''[[Sorghum bulbosum]]'' * ''[[Sorghum burmahicum]]'' * ''[[Sorghum controversum]]'' * ''[[Sorghum drummondii]]'' * ''[[Sorghum ecarinatum]]'' * ''[[Sorghum exstans]]'' * ''[[Sorghum grande]]'' * ''[[Johnson grass|Sorghum halepense]]'' * ''[[Sorghum interjectum]]'' * ''[[Sorghum intrans]]'' * ''[[Sorghum laxiflorum]]'' * ''[[Sorghum leiocladum]]'' * ''[[Sorghum macrospermum]]'' * ''[[Sorghum matarankense]]'' * ''[[Sorghum miliaceum]]'' * ''[[Sorghum nitidum]]'' * ''[[Sorghum plumosum]]'' * ''[[Sorghum propinquum]]'' * ''[[Sorghum purpureosericeum]]'' * ''[[Sorghum stipoideum]]'' * ''[[Sorghum timorense]]'' * ''[[Sorghum trichocladum]]'' * ''[[Sorghum versicolor]]'' * ''[[Sorghum virgatum]]'' * ''[[Sorghum vulgare]]'' * ''[[Andropogon sorghum]]'' == Pranala njaba == {{Commons category|Sorghum}} * [http://www.fao.org/docrep/T0818e/T0818E00.HTM FAO Report (1995) "Sorghum and millets in human nutrition"] * [http://www.fao.org/inpho/content/compend/toc_main.htm#TopOfPage FAO "Compendium on post-harvest operations" — Contains discussion on origin, processing and uses of sorghum] * [http://www.hort.purdue.edu/newcrop/afcm/sorghum.html Alternative Field Crops] * [http://www.itis.usda.gov/servlet/SingleRpt/SingleRpt?search_topic=TSN&search_value=42106 ITIS 42106] {{Webarchive|url=https://web.archive.org/web/20051129020415/http://www.itis.usda.gov/servlet/SingleRpt/SingleRpt?search_topic=TSN&search_value=42106 |date=2005-11-29 }} 2002-09-22 * [http://www.icrisat.org/text/research/grep/homepage/sorghum/sorghumhomepage.htm ICRISAT] {{Webarchive|url=https://web.archive.org/web/20050324042221/http://www.icrisat.org/text/research/grep/homepage/sorghum/sorghumhomepage.htm |date=2005-03-24 }} * [http://amarillo.tamu.edu/programs/irrigtce/publications/Grain%20Sorghum%20Irrigation%20B-6152.pdf Grain Sorghum Irrigation] {{Webarchive|url=https://web.archive.org/web/20090911064046/http://amarillo.tamu.edu/programs/irrigtce/publications/Grain%20Sorghum%20Irrigation%20B-6152.pdf |date=2009-09-11 }} *[http://www.grains.org/page.ww?section=Barley%2C+Corn+%26+Sorghum&name=Sorghum Sorghum on US Grains Council Web Site] *[http://www.sorghumgrowers.com National Grain Sorghum Producers] *[http://www.ca.uky.edu/nssppa/production.html National Sweet Sorghum Producers and Processors Association] *[http://www.grains.org/galleries/default-file/Sorghum%20Handbook.pdf] {{Webarchive|url=https://web.archive.org/web/20071202074553/http://www.grains.org/galleries/default-file/Sorghum%20Handbook.pdf |date=2007-12-02 }} - Sorghum Handbook *[http://weedsoft.unl.edu/documents/GrowthStagesModule/Sorghum/Sorg.htm Sorghum Growth Stages] {{Webarchive|url=https://web.archive.org/web/20070429022343/http://weedsoft.unl.edu/documents/GrowthStagesModule/Sorghum/Sorg.htm |date=2007-04-29 }} * [http://biology.plosjournals.org/perlserv/?request=get-document&doi=10.1371/journal.pbio.0030013 Sequencing of the Sorghum Genome by Methylation Filtration] *[http://www2.dpi.qld.gov.au/health/11762.html Risk management of cyanide (prussic acid) and nitrates in sorghum crops] *[http://www.phytozome.net/sorghum Preliminary assembly and annotation of sorghum bicolor genome] [[Kategori:Poaceae]] [[Kategori:Serealia]] {{botani-stub}} egne2cm2hzdpqndk6ayud36pifk30hg 0 43471 1731250 1731237 2025-06-29T12:05:23Z Henri Aja 45299 Reverted 2 edits by [[Special:Contributions/182.1.178.229|182.1.178.229]] ([[User talk:182.1.178.229|talk]]) (TwinkleGlobal) 1731250 wikitext text/x-wiki {{Infobox TV channel | Name = sapta ksvara kusbini | Image = TVRILogo2019.svg | Image size = 200px | Launch = [[24 Agustus]] [[1962]] ing Jakarta | Owner = [[Pamaréntah Indonésia]] | Sister channel = [[TPI]] ([[1991]]-[[1997]])<br />[[QTV]] ([[2000]]-[[2011]])<br />[[Swara]] ([[2000]]-[[2011]])<br />[[TV Edukasi|Televisi Edukasi]] ([[2004]]-[[2014]]) | Website = www.tvri.go.id | terr serv 1 = [[Daerah Khusus Ibukota Jakarta|Jakarta]] | terr chan 1 = 31 UHF (TVRI Jakarta, analog)<br />39 UHF (TVRI Nasional, analog) <br/>42 UHF (TVRI Jakarta dan Nasional, digital [[DVB-T2]])| terr serv 2 = [[Kota Bandung|Bandung]] | terr chan 2 = 7 VHF (TVRI Bandung)<br />40 UHF (TVRI Nasional) | terr serv 3 = [[Kota Bogor|Bogor]] | terr chan 3 = 7 VHF (TVRI Bandung)<br />34 UHF (TVRI Nasional) | terr serv 4 = [[Kota Tanjung Pinang|Tanjung Pinang]] | terr chan 4 = 6 (1) UHF (TVRI Nasional)<br />6 (2) UHF (TVRI Batam) | terr serv 5 = [[Kota Semarang|Semarang]] | terr chan 5 = 5 VHF (TVRI Semarang)<br /> 23 UHF (TVRI Nasional) | terr serv 6 = [[Pulau Bintan|Bintan]] | terr chan 6 = 6 (1) UHF (TVRI Nasional)<br />6 (2) UHF (TVRI Batam) | terr serv 7 = [[Kota Surabaya|Surabaya]] | terr chan 7 = 10 VHF (TVRI Surabaya)<br />26 UHF (TVRI Nasional) | terr serv 8 = [[Makassar]] | terr chan 8 = 5 VHF (TVRI Makassar)<br />37 UHF (TVRI Nasional)| terr serv 9 = [[Kota Banda Acèh|Banda Acèh]] | terr chan 9 = 36 UHF (TVRI Nasional & TVRI Acèh & TVRI Langsa) | terr serv 10 = [[Kota Medan|Medan]] | terr chan 10 = 6 VHF (TVRI Medan)<br />47 UHF (TVRI Nasional) | terr serv 11 = [[Kota Batam|Batam]] ([[Pulau Batam]]) | terr chan 11 = 6 (1) UHF (TVRI Nasional)<br />6 (2) UHF (TVRI Batam) | terr serv 12 = [[Kota Yogyakarta|Yogyakarta]] | terr chan 12 = 9 VHF (TVRI Yogyakarta)<br />22 UHF (TVRI Nasional) | terr serv 13 = [[Kota Denpasar|Denpasar]] ([[Bali]]) | terr chan 13 = 9 VHF (TVRI Bali)<br />29 UHF (TVRI Nasional) | terr serv 14 = [[Kota Bandar Lampung|Bandar Lampung]] | terr chan 14 = 40 UHF (TVRI Bandar Lampung)<br />50 UHF (TVRI Nasional) | terr serv 15 = [[Kota Palembang|Palembang]] | terr chan 15 = 10 VHF (TVRI Palembang)<br />40 UHF (TVRI Nasional) | terr serv 16 = [[Kota Padang|Padang]] | terr chan 16 = 7 VHF (TVRI Padang)<br />25 UHF (TVRI Nasional) | terr serv 17 = [[Kota Pekanbaru|Pekanbaru]] | terr chan 17 = 8 VHF (TVRI Riau)<br />50 UHF (TVRI Nasional) | terr serv 18 = [[Kota Pontianak|Pontianak]] | terr chan 18 = 8 VHF (TVRI Pontianak)<br />50 UHF (TVRI Nasional) | terr serv 19 = [[Kota Banjarmasin|Banjarmasin]] | terr chan 19 = 4 VHF (TVRI Banjarmasin) sampai [[2014]]<br />40 UHF (TVRI Nasional & TVRI Kalimantan Selatan) | terr serv 20 = [[Kota Malang|Malang]] | terr chan 20 = 3 VHF (TVRI Malang)<br />42 UHF (TVRI Nasional) | terr serv 21 = [[Kota Manado|Manado]] | terr chan 21 = 10 VHF (TVRI Manado)<br />45 UHF (TVRI Nasional) | terr serv 22 = [[Kota Kediri|Kediri]] | terr chan 22 = 32 UHF (TVRI Kediri)<br />61 UHF (TVRI Nasional) | terr serv 23 = [[Kota Mataram|Mattaram, Lombok]] | terr chan 23 = 7 VHF (TVRI Lombok)<br />12 UHF (TVRI Nasional) | terr serv 24 = [[Kota Makassar|Makassar]] | terr chan 24 = 5 VHF (TVRI Makassar)<br />20 UHF (TVRI Nasional) | terr serv 25 = [[Kota Pematangsiantar|Pematang Siantar]] | terr chan 25 = 6 VHF (TVRI Medan)<br />47 UHF (TVRI Nasional) | terr serv 26 = [[Rantau Prapat, Labuhanbatu|Rantau Parapat]] | terr chan 26 = 6 VHF (TVRI Medan)<br />47 UHF (TVRI Nasional) | terr serv 27 = [[Kota Binjai|Binjai]] | terr chan 27 = 6 VHF (TVRI Medan)<br />47 UHF (TVRI Nasional) | terr serv 28 = [[Kota Sibolga|Sibolga]] | terr chan 28 = 6 VHF (TVRI Medan)<br />47 UHF (TVRI Nasional) | terr serv 29 = [[Kota Tanjungbalai|Tanjung Balai]] | terr chan 29 = 6 VHF (TVRI Medan)<br />47 UHF (TVRI Nasional) | terr serv 30 = [[Kota Tebing Tinggi|Tebing Tinggi]] | terr chan 30 = 6 VHF (TVRI Medan)<br />47 UHF (TVRI Nasional) | terr serv 31 = [[Boyolangu, Tulungagung|Boyolangu]] | terr chan 31 = 10 VHF (TVRI Surabaya)<br />26 UHF (TVRI Nasional) | terr serv 32 = [[Kota Jambi|Jambi]] | terr chan 32 = 27 UHF (TVRI Nasional) | terr serv 33 = [[Kota Surakarta|Sala]] | terr chan 33 = 10 VHF (TVRI Surabaya)<br />26 UHF (TVRI Nasional) | terr serv 34 = [[Kota Atambua|Atambua]] | terr chan 34 = 10 VHF (TVRI Nasional)<br />20 VHF (TVRI Nasional) | terr serv 35 = [[Kabupatèn Kebumen|Kebumen]] | terr chan 35 = 47 UHF (melalui [[Ratih TV]]) (TVRI Nasional) | }} '''TVRI''' (singkatan teka '''Televisi Republik Indonesia''') iku [[stasiun televisi]] pisanan ing Indonésia, sing anggegana wiwit taun [[1962]] ing [[Jakarta]]<ref>{{Cite web |url=http://www.tvri.co.id/sejarah.php |title=Sejarah TVRI |access-date=2020-10-31 |archive-date=2008-08-03 |archive-url=https://web.archive.org/web/20080803193106/http://www.tvri.co.id/sejarah.php |url-status=dead }}</ref>. Siaran perdanané giaran Upacara Pèngetan Dina Kamardikan [[Républik Indonésia]] angka 17 saka [[Pura Negara]] [[Jakarta]]. Siaran iki isih wujud giaran ireng-putih. TVRI sabanjuré ngliput [[Asian Games]] sing dianakaké ing Jakarta. == Gladri logo == {{Logo saluran televisi}} <gallery> Gambar:TVRILogo1962.svg|Logo kapisan TVRI (24 Agustus 1962-24 Agustus 1974). Gambar:TVRILogo1974.png|Logo kaloro TVRI (24 Agustus 1974-24 Agustus 1982). Gambar:TVRILogo2001.svg|Logo kalima TVRI (1 Agustus 2001-1 Agustus 2003). Gambar:TVRILogo2003.svg|Logo kaenem TVRI (1 Agustus 2003-30 Maret 2007). Gambar:TVRILogo2006.svg|Logo kapitu TVRI (1 April 2007-29 Maret 2019). Gambar:TVRILogo2019.svg|Logo kawolu TVRI, sing dinggo wiwit 29 Maret 2019. </gallery> == Pranala njaba == * [http://www.tvri.co.id Situs resmi] {{Webarchive|url=https://web.archive.org/web/20150706064944/http://www.tvri.co.id/ |date=2015-07-06 }} * [http://produksi-tvrikalsel.blogspot.com Weblog TVRI Kalsel] == Réferènsi == {{reflist}} {{Televisi ing Indonésia}} [[Kategori:Stasiun televisi Indonésia]] [[Kategori:Stasiun televisi sing madeg taun 1962]] {{Tv-stub}} d9l1hh4bylmel4xbozycrub1oxfnibf 0 71392 1731255 1688927 2025-06-29T12:10:19Z Bebasnama 44025 1731255 wikitext text/x-wiki {{multiscript|Gendéra|ꦒꦼꦤ꧀ꦢꦺꦫ}} [[Barkas:ASEAN Nations Flags in Jakarta 3.jpg|jmpl|Gendéra nagara-nagara [[ASEAN]] kumlèbèt ing [[Jakarta]].]] '''Gendéra''' utawa '''klèbèt''' yaiku pralambang saka kain utawa kertas segi papat utawa segitelu (kang ditaleni ana ing ujung tongkat, saka, lan saperangané) kang didadèkaké [[lambang]] saka [[Nagara]].<ref>[http://pusatbahasa.diknas.go.id/kbbi/index.php pusatbahasa.diknas.go.id] {{Webarchive|url=https://web.archive.org/web/20090805021214/http://pusatbahasa.diknas.go.id/kbbi/index.php |date=2009-08-05 }}.</ref>, lembaga, organisasi, utawa minangka pratandha. Kerepé gendéra iku dikèberaké ana ing saka lan umumé dianggo kanthi simbolis gawé menèhi sinyal utawa identifikasi. Gendéra kerep uga dianggo gawé nglambangaké negara gawé nunjukaké kadaulatané. == Cathetan suku == {{reflist}} {{Pratélan Gendéra}} {{Kategori:Piranti}} {{Stub}} mua5wk9wbf4mk33svfl1cwrunv1k9na 0 75231 1731263 1708641 2025-06-30T02:07:46Z InternetArchiveBot 48188 Rescuing 1 sources and tagging 0 as dead.) #IABot (v2.0.9.5 1731263 wikitext text/x-wiki {{artikel ing krama}} {{Infobox Officeholder |name = Christine Lagarde |image = Lagarde.jpg |office = Direktur [[Dana Moneter Internasional]]<br /> |deputy = [[John Lipsky]] |term_start = 5 Juli 2011 |term_end = |succeeding = [[John Lipsky]] <small>(Penjabat)</small> |predecessor = [[John Lipsky]] <small>(Penjabat)</small> |successor = |office2 = [[Mantri Ékonomi, Perindustrian dan Tenaga Kerja (Prancis)|Mantri Keuangan]] |primeminister2 = [[François Fillon]] |term_start2 = 19 Juni 2007 |term_end2 = <!-- 29 June 2011 --> |predecessor2 = [[Jean-Louis Borloo]] |successor2 = dèrèng wonten |office3 = [[Kementerian Pertanian (Prancis)|Mantri Pertanian]] |primeminister3 = [[François Fillon]] |term_start3 = 18 Mèi 2007 |term_end3 = 19 Juni 2007 |predecessor3 = [[Dominique Bussereau]] |successor3 = [[Michel Barnier]] |office4 = [[Mantri Perdagangan dan Perindustrian (Prancis)|Mantri Perdagangan lan Perindustrian]] |primeminister4 = [[Dominique de Villepin]] |term_start4 = 31 Mèi 2005 |term_end4 = 18 Mèi 2007 |predecessor4 = [[Christian Jacob (pulitikus Prancis)|Christian Jacob]] |successor4 = Jabatan dibusakake |birth_date = {{birth date and age|1956|1|1|df=y}} |birth_place = {{flagicon|Prancis}} [[Paris]], [[Républik Prancis Keempat|Prancis]] |death_date = |death_place = |party = [[Uni Gerakan Rakyat]] |alma_mater = [[Universitas Paris Barat Nanterre La Défense]]<br />[[Institut d'études politiques d'Aix-en-Provence|Institut Ilmu Pulitik, Aix-en-Provence]] |religion = [[Gréja Katulik Roma|Katulik Roma]] }} '''Christine Madeleine Odette Lagarde''' ({{lahirmati||1|1|1956}}) <ref name="internet1">[http://www.nouveleconomiste.fr/Portraits/1230-Lagarde.html Le Nouvel Economiste] {{Webarchive|url=https://web.archive.org/web/20110828092934/http://www.nouveleconomiste.fr/Portraits/1230-Lagarde.html |date=2011-08-28 }} dipunundhuh tanggal 27 Juni 2011)</ref> sapunika panjenenganipun dados mantri kauangan, mantri urusan ékonomi, lan perindhustrian [[Perancis]]. Sapunika Lagarde ugi dados dhirektur kapilih [[Dana Moneter Internasional]]. Panjenenganipun nembé badhé njabat kalungguhan punika mangke tanggal [[5 Juli]] [[2011]]. Lagarde dipunangkat mantri keuangan déning présidhèn [[Perancis]], [[Nicolas Sarkozy]] ing sasi Juni [[2007]]. Saderengipun Lagarde dados mantri pertanian Perancis lan mantri perdagangan wekdal papréntahanipun [[Dominique de Villepin]]. Lagarde dados tiyang èstri ingkang wiwitan dados mantri urusan ékonomi wonten ing golongan ékonomi [[G8]], ugi dados tiyang èstri pertama ingkang dados pandheganipun [[IMF]].<ref name="internet2">[http://www.imf.org/external/np/sec/pr/2011/pr11259.htm ''IMF Executive Board Selects Christine Lagarde as Managing Director''] dipunundhuh tanggal 28 Juni 2011)</ref> Lagarde dados tiyang èstri ingkang pertama ingkang njabat dhirektur salah satunggalipun perusahaan konsultan hukum internasional Baker & McKenzie.<ref name="internet3">[http://www.ft.com/cms/s/0/3f36c9c4-d2d0-11de-af63-00144feabdc0.html?nclick_check=1 Financial Times] dipunundhuh tanggal 29 Juni 2011)</ref> 16 November 2009 ''The Financial Times'' milih Migarde minangka mantri keuangan ingkang saé piyambak wonten ing nagari-nagari ingkang ngagem mata uang [[Euro]]. Panjenenganipun ugi mlebet urutan kaping 17 tiyang èstri ingkang paling gadhah prabawa ing donya miturut majalah ''Forbes''.<ref name="internet4"/> Tanggal 28 Juni 2011, panjenenganipun dipunparingi amanah minangka dhirektur kepala [[Dana Moneter Internasional]], ingkang gadhah wekdal kalungguhan sadangunipun gangsal taun, kalungguhan punika dipunwwiwiti tanggal 5 Juli 2011 lan panjenenganipun minangka gantosipun [[Dominique Strauss-Kahn]] ingkang sampun lengser. <ref name="internet4">[http://www.forbes.com/lists/2009/11/power-women-09_The-100-Most-Powerful-Women_Rank.html « The 100 Most Powerful Women »] dipunundhuh tanggal 29 Juni 2011)</ref> == Cathetan suku == {{reflist}} == Pranala njawi == {{commons}} * [http://www.project-syndicate.org/contributor/1564 Column archives] {{Webarchive|url=https://web.archive.org/web/20110727071021/http://www.project-syndicate.org/contributor/1564 |date=2011-07-27 }} at [[Project Syndicate]] [[Kategori:Artikel mawa basa krama]] [[Kategori:Lair 1956]] {{stub}} ezsmot7ps7mpxwgh08zw134xkmu9b8j 0 107690 1731249 1731243 2025-06-29T11:59:36Z Henri Aja 45299 Reverted 2 edits by [[Special:Contributions/182.2.46.136|182.2.46.136]] ([[User talk:182.2.46.136|talk]]) to last revision by AvichayBoo (TwinkleGlobal) 1731249 wikitext text/x-wiki '''Benjamin " Bibi " Netanyahu''' ([[Ibrani]]: בִּנְיָמִין " בִּיבִּי " נְתַנְיָהוּ, basa [[Arab]]: ﻧﺘﻨﻴﺎﻫﻮ ﺑﻨﻴﺎﻣﻴﻦ, Binyyameen Natayahu; lair ana [[Tel Aviv]], Israèl, 21 Oktober 1949 ; umur 75 taun) ya iku [[Mahamantri Israèl]].<ref name="BN bc">{{cite web|url=https://www.britannica.com/biography/Benjamin-Netanyahu|title=Benjamin Netanyahu: Prime Minister of Israel|last1=The Editors of Encyclopædia Britannica|first1=|date=13 Mèi 2015|work=|publisher=britannica.com|access-date=13 Sèptèmber 2016}}</ref> Tiyangé punika mangku kalungguhan dados [[Parté Likud]], uga dados anggota [[Knesset]], uga dados Mantri Kasarasan [[Israèl]], uga dados Mantri Urusan Pènsiunan [[Israèl]], saha dados Mantri Strategi Ékonomi ing nagara [[Israèl]].<ref name="BN bc"/> Netanyahu ya iku Mantri kapisan uga ora ana liyané dhèwèké [[Mahamantri]] [[Israèl]] kang lair ana [[Israèl]] sabanjuré tata nagara [[Israèl]]. Netanyahu dapthar ing Angkatan Pertahanan [[Israèl]] nalika taun 1967.<ref name="BN bc"/> Nalika iku, tiyangé mangku kalungguhan dados komandan ana ing unit komando èlit arané [[Sayeret Matkal]], mundhut babagan manéka warna misi mau, salah sawijiné ya iku misi nylametaké sandra saka [[Sabena Penerbangan 571]] dibajak ana taun 1972 (untungna ana ngisor pimpinan [[Ehud Barak]]). Dhèwèké juang ana [[Perang Yom Kippur]] ing taun 1973 uga éntuk pangkat kaptèn sadurungé rampung. Netanyahu njabat dadi [[Duta Besar]] [[Israèl]] kanggo [[Perserikatan Bangsa-bangsa]] 1984-1988, anggota [[Parté Likud]], uga [[Mahamantri]] saka sasi Juni 1996 nganti Juli 1999. Netanyahu Mantri Luar Negeri (2002-2003) uga Mantri Keuangan (2003-Agustus 2005) ana pamréntahan [[Ariel Sharon]], nanging dhèwèké tindak béda penemu ana rencana pisahan [[Jalur Gaza]]. Dhèwèké ngrebut bali kapemimpinan [[Likud]] ing tanggal 20 Dhésèmber 2005. Ana pemilu 2006, [[Likud]] ora ala, menangaké 12 (rolas) kursi. Ing sasi Dhésèmber 2006, Netanyahu dadi pejabat Pemimpin Oposisi ana [[Knesset]] uga Ketua [[Parté Likud]]. Ing sasi Agustus 2007, dhèwèké mertahanake kapemimpinan [[Likud]] nganggo ngalahaké [[Moshe Feiglin]] ana pemilihan parté. Sawisé pemilihan parlemèn 10 Fèbruari 2009, [[Likud]] diwènèhake pihak karo uga sayap tengen menang mayoritas, Netanyahu mbentuk pamréntahan koalisi.<ref name="BN b">{{cite web|url=http://www.biography.com/people/benjamin-netanyahu-9421908#political-success|title=Benjamin Netanyahu Biography|last1=Biography.com Editors|first1=|date=24 Maret 2015|work=|publisher=A&E Television Networks|access-date=13 Sèptèmber 2016}}</ref> Dhèwèké ya iku tunggalé Komandan Pasukan Khusus [[Israèl]] [[Yonatan Netanyahu]], kang séda ana misi nylametaké sandera, uga [[Ido Netanyahu]], penulis [[Israèl]] uga dramawan. Ing taun 2010, majalah [[Inggris]] [[New Statesman]] ndaptaraké Benjamin Netanyahu ana 11 ing pratélan "50 Donya Angka Paling Ngaruhi 2010". == Pranala njaba == *[http://www.bbc.com/indonesia/berita_indonesia/2016/03/160329_indonesia_israel_netanyahu_diplomatik Laman web BBC] *[http://www.biography.com/people/benjamin-netanyahu-9421908#political-success Biografi ana biography.com] *[http://www.haaretz.com/misc/tags/1.476753-1.476753 laman web Hareetz] *[http://www.netanyahu.org.il/en/news/1198-statements-by-prime-minister-benjamin-netanyahu-and-president-of-cyprus-nicos-anastasiades Laman web official Netanyahu.org.il] *[https://www.britannica.com/biography/Benjamin-Netanyahu Biografi ana britannica.com] [[Kategori:Artikel Wiki Mrebawani]] [[Kategori:Tokoh Israèl]] [[Kategori:Lair 1949]] 31icb293gutihn990dzuj0b6nl787xn 0 173608 1731264 1540570 2025-06-30T02:45:20Z InternetArchiveBot 48188 Rescuing 1 sources and tagging 0 as dead.) #IABot (v2.0.9.5 1731264 wikitext text/x-wiki [[Barkas:Hackfleisch-1.jpg|ka|jmpl| Daging sapi giling]] '''Daging sapi giling''' '''daging sapi cincang''' utawa '''daging sapi cincang''' yaiku [[Pérangan daging sapi|daging sapi]] sing wis disigar nganggo piso utawa [[Panggiling daging|penggiling daging]] (Inggris Inggris) utawa [[Panggiling daging|mesin cincang]] (Inggris Inggris). Iki digunakake ing resep-resep kalebu [[hamburger]] lan [[Saos bolognese|spaghetti Bolognese]] . Ing pirang-pirang negara, undang-undang panganan nemtokake kategori daging sapi ing ngisor lan apa sing bisa dikandung. Contone, ing [[Amérika Sarékat|Amerika Serikat]], lemak daging sapi bisa ditambahake ing hamburger nanging ora kanggo daging sapi sing digoreng yen daging digiling lan dikemas ing tanduran sing diidentifikasi USDA . <ref group="note">These rules only apply to meat being sold across state lines. In the U.S., much ground beef is produced at local grocery stores and is not sold across state lines. In these cases, the laws of the local state apply; state laws may have different requirements.</ref> Ing AS, maksimal 30% lemak miturut bobot diidini ing hamburger utawa daging sapi sing digiling. Jumlah sing diidini ing Prancis yaiku 5 nganti 20% (15% digunakake dening umume rantai panganan). Ing Jerman, daging sapi biasa bisa uga ngemot lemak nganti 15%, nanging "Tatar" khusus kanggo ''steak tartare'' bisa ngemot kurang saka 5% lemak. Kalor hamburger lan daging sapi ing ngisor iki bisa nambah bumbu, [[fosfat]], penyambung, utawa pengikat sing ditambahake; nanging ora diidini banyu tambahan. Daging sapi ing lemah asring dipasarake ing pirang-pirang isi lemak sing beda-beda kanggo cocog karo pilihan pelanggan. Daging sapi ing lemah biasane digawe saka potongan daging sapi sing kurang alus lan kurang populer. Trimings saka potongan tender bisa uga digunakake. <ref>{{Cite web|url=http://www.fsis.usda.gov/wps/portal/fsis/topics/food-safety-education/get-answers/food-safety-fact-sheets/meat-preparation/ground-beef-and-food-safety/CT_Index|title=Ground Beef and Food Safety|date=August 6, 2013|publisher=Fsis.usda.gov|access-date=2015-11-11|archive-date=2015-11-14|archive-url=https://web.archive.org/web/20151114234645/http://www.fsis.usda.gov/wps/portal/fsis/topics/food-safety-education/get-answers/food-safety-fact-sheets/meat-preparation/ground-beef-and-food-safety/ct_index|url-status=dead}}</ref> == Cathetan == [[Kategori:Daging sapi]] aseicu3f8ivg22vu3a1e1d4pwcxs2gr 0 173964 1731252 1720419 2025-06-29T12:09:01Z Manggisjeruk 65009 Manggisjeruk ngalih kaca [[Angabar]] menyang [[Panambayangan]] 1720419 wikitext text/x-wiki [[Barkas:Nickelocen_an_einem_Kühlfinger.jpg|ka|jmpl| [[Kristal]] ijo peteng saka nickelocene, sublim lan anyar disimpen ing driji sing adhem]] '''Angabar''' minangka transisi zat langsung saka padatan menyang negara [[gas]], tanpa ngliwati negara cair.<ref>{{Cite book|url=https://archive.org/details/generalchemistry00whit_0|title=General chemistry|last=Whitten|first=Kenneth W.|last2=Gailey|first2=Kenneth D.|last3=Davis|first3=Raymond E.|date=1992|publisher=Saunders College Publishing|isbn=0-03-072373-6|edition=4th|page=[https://archive.org/details/generalchemistry00whit_0/page/475 475]|url-access=registration}}</ref> Sublimasi minangka proses endotermik sing ana ing suhu lan tekanan ing sangisore titik triple zat ing diagram fase, sing cocog karo tekanan paling ngisor ing bahan kasebut bisa dadi cairan. Proses mbalikke sublimasi yaiku déposisi utawa desublimasi, ing endi zat kasebut langsung pindhah saka gas menyang fase padat.<ref name="DepositionDef">{{Cite journal|last=Boreyko|first=Jonathan B.|last2=Hansen|first2=Ryan R.|last3=Murphy|first3=Kevin R.|last4=Nath|first4=Saurabh|last5=Retterer|first5=Scott T.|last6=Collier|first6=C. Patrick|year=2016|title=Controlling condensation and frost growth with chemical micropatterns|journal=Scientific Reports|volume=6|pages=19131|bibcode=2016NatSR...619131B|doi=10.1038/srep19131|pmc=4726256|pmid=26796663}}</ref> Sublimasi uga digunakake minangka istilah umum kanggo njlentrehake transisi solid-to-gas (sublimasi) banjur transisi gas-to-solid ( déposisi ). Nalika penguapan saka cairan menyang gas ana [[Panguapan|penguapan]] saka permukaan yen ana ing sangisore titik didih saka cairan kasebut, lan nalika [[Umub|nggodhok]] kanthi pembentukan gelembung ing njero cairan kasebut yen ana ing titik didih, ora ana bedane kanggo transisi solid-to-gas sing mesthi ana sublimasi saka permukaan. Ing [[Kondisi standar kanggo suhu lan tekanan|tekanan normal]], umume [[Senyawa Kimia|senyawa]] lan [[Anasir kimiah|unsur]] [[Senyawa Kimia|kimia]] duwe telung negara sing beda-beda ing [[Suhu|suhu sing]] beda. Ing kasus kasebut, transisi saka solid menyang [[Gas|negara gas]] mbutuhake negara cair menengah. Tekanan sing diarani yaiku ''[[tekanan parsial]]'' zat, dudu tekanan ''total'' (kaya ta atmosfer) kanggo kabeh sistem. Dadi, kabeh padatan sing duwe [[Penetan uwab|tekanan uap sing apik]] ing suhu tartamtu bisa kaluhur ing udhara (kaya ta es banyu ing sangisore 0&nbsp;°C). Kanggo sawetara zat, kaya ta [[karbon]] lan [[Arsènik|arsenik]], sublimasi luwih gampang tinimbang [[Panguapan|penguapan]] saka leleh, amarga tekanan [[Titik telu|telung titik kasebut]] dhuwur banget, lan angel dipikolehi minangka cairan. [[Barkas:Ferrocen.jpg|ka|jmpl| Kristal ferrocene sawise dimurnekake kanthi sublimasi vakum]] == Referensi == [[Kategori:Gas]] q63spfa5ichhccfwxjnuax11sgf4d1e 1731254 1731252 2025-06-29T12:09:21Z Manggisjeruk 65009 1731254 wikitext text/x-wiki [[Barkas:Nickelocen_an_einem_Kühlfinger.jpg|ka|jmpl| [[Kristal]] ijo peteng saka nickelocene, sublim lan anyar disimpen ing driji sing adhem]] '''Panambayangan''' minangka transisi zat langsung saka padatan menyang negara [[gas]], tanpa ngliwati negara cair.<ref>{{Cite book|url=https://archive.org/details/generalchemistry00whit_0|title=General chemistry|last=Whitten|first=Kenneth W.|last2=Gailey|first2=Kenneth D.|last3=Davis|first3=Raymond E.|date=1992|publisher=Saunders College Publishing|isbn=0-03-072373-6|edition=4th|page=[https://archive.org/details/generalchemistry00whit_0/page/475 475]|url-access=registration}}</ref> Sublimasi minangka proses endotermik sing ana ing suhu lan tekanan ing sangisore titik triple zat ing diagram fase, sing cocog karo tekanan paling ngisor ing bahan kasebut bisa dadi cairan. Proses mbalikke sublimasi yaiku déposisi utawa desublimasi, ing endi zat kasebut langsung pindhah saka gas menyang fase padat.<ref name="DepositionDef">{{Cite journal|last=Boreyko|first=Jonathan B.|last2=Hansen|first2=Ryan R.|last3=Murphy|first3=Kevin R.|last4=Nath|first4=Saurabh|last5=Retterer|first5=Scott T.|last6=Collier|first6=C. Patrick|year=2016|title=Controlling condensation and frost growth with chemical micropatterns|journal=Scientific Reports|volume=6|pages=19131|bibcode=2016NatSR...619131B|doi=10.1038/srep19131|pmc=4726256|pmid=26796663}}</ref> Sublimasi uga digunakake minangka istilah umum kanggo njlentrehake transisi solid-to-gas (sublimasi) banjur transisi gas-to-solid ( déposisi ). Nalika penguapan saka cairan menyang gas ana [[Panguapan|penguapan]] saka permukaan yen ana ing sangisore titik didih saka cairan kasebut, lan nalika [[Umub|nggodhok]] kanthi pembentukan gelembung ing njero cairan kasebut yen ana ing titik didih, ora ana bedane kanggo transisi solid-to-gas sing mesthi ana sublimasi saka permukaan. Ing [[Kondisi standar kanggo suhu lan tekanan|tekanan normal]], umume [[Senyawa Kimia|senyawa]] lan [[Anasir kimiah|unsur]] [[Senyawa Kimia|kimia]] duwe telung negara sing beda-beda ing [[Suhu|suhu sing]] beda. Ing kasus kasebut, transisi saka solid menyang [[Gas|negara gas]] mbutuhake negara cair menengah. Tekanan sing diarani yaiku ''[[tekanan parsial]]'' zat, dudu tekanan ''total'' (kaya ta atmosfer) kanggo kabeh sistem. Dadi, kabeh padatan sing duwe [[Penetan uwab|tekanan uap sing apik]] ing suhu tartamtu bisa kaluhur ing udhara (kaya ta es banyu ing sangisore 0&nbsp;°C). Kanggo sawetara zat, kaya ta [[karbon]] lan [[Arsènik|arsenik]], sublimasi luwih gampang tinimbang [[Panguapan|penguapan]] saka leleh, amarga tekanan [[Titik telu|telung titik kasebut]] dhuwur banget, lan angel dipikolehi minangka cairan. [[Barkas:Ferrocen.jpg|ka|jmpl| Kristal ferrocene sawise dimurnekake kanthi sublimasi vakum]] == Referensi == [[Kategori:Gas]] 8ivd57996zap0q134f8vddji4kflzsc 0 177988 1731261 1563395 2025-06-29T18:09:38Z InternetArchiveBot 48188 Rescuing 1 sources and tagging 0 as dead.) #IABot (v2.0.9.5 1731261 wikitext text/x-wiki [[Barkas:Acorns_small_to_large.jpg|jmpl| Acorns wiwit cilik nganti gedhe saka Willow Oak, ''Quercus phellos'' (cilik banget, ing tengah); ing Oak Abang Kidul, ''Quercus falcata'' ; the White Oak, ''Quercus alba'' ; the Scarlet Oak, ''Quercus rosalia'' ; saka kidul Greenville County, SC, USA. Baris skala ing sisih tengen ndhuwur yaiku 1&nbsp;cm.]] '''Acorn''', utawa '''oaknut''', minangka [[Kacang woh|kacang]] ing [[Wit èk|wit oak]] lan sedulure (genera ''[[Wit èk|Quercus]]'' lan ''Lithocarpus'', ing kulawarga Fagaceae ). Biasane ngemot siji [[wiji]] (sok-sok rong wiji), ditutup ing [[Kulit kacang|cangkang]] kulit sing angel lan kulit ing cangkir sing bentuk cangkir . Acorns yaiku {{Convert|1–6|cm|in|abbr=off}} dawane lan {{Convert|0.8–4|cm|in|abbr=on}} ing sisih lemu. Acorns njupuk antara 6 lan 24 wulan (gumantung saka spesies) kanggo diwasa; deleng dhaptar spesies <nowiki><i id="mwKg">Quercus</i></nowiki> kanggo rincian klasifikasi oak, ing endi morfologi lan fenologi akorn minangka faktor penting. == Peran ekologis == Acorns duwe peran penting ing ekologi alas nalika wit ek minangka spesies sing dominan utawa akeh. <ref name="USDA">{{Cite book|url=http://www.fs.fed.us/psw/publications/documents/psw_gtr044/psw_gtr044.pdf|title=Proceedings of the symposium on the ecology, management, and utilization of California oaks, June 26–28|publisher=USDA Forest Service General Technical Report PSW-044|year=1980|editor-last=Plumb, Timothy R.|pages=1 to 368|asin=B000PMY1P8}}</ref> Volume panen akorn bisa beda-beda beda-beda, nggawe akeh utawa stres gedhe kanggo akeh kewan sing gumantung karo acorn lan predator kewan kasebut. <ref name="NYT">{{Cite news|url=https://www.nytimes.com/2011/12/03/nyregion/boom-and-bust-in-acorns-will-affect-many-creatures-including-humans.html|title=After Lean Acorn Crop in Northeast, Even People May Feel the Effects|last=King, Richie S.|date=2 December 2011|work=The New York Times|access-date=4 December 2011|quote=there is nothing unusual about large fluctuations in the annual number of acorns.}}</ref> Acorn, uga kacang-kacangan liyane, diarani mast . Margasatwa sing ngonsumsi acorn minangka bagean penting saka panganan kalebu manuk, kayata [[Jay|jays]], [[Dara|pigeons]], sawetara [[Bèbèk|bebek]], lan sawetara spesies [[Pelatuk kayu|pelatuk]] . [[Mamalia|Mamalia cilik]] sing mangan acorn kalebu [[Cindhil|tikus]], [[Cuwut|bajing]] lan sawetara [[Kéwan kekrikitan|tikus]] liyane. Acorn duweni pengaruh gedhe marang [[Kéwan kekrikitan|rodent]] cilik ing [[Habitat|papane]], amarga panen biji gedhe mbantu populasi tikus tuwuh . <ref>{{Cite web|url=https://www.srs.fs.usda.gov/uplandhardwood/research/article/acorn-study|title=Acorn Study {{!}} Research {{!}} Upland Hardwood Ecology and Management {{!}} SRS|website=www.srs.fs.usda.gov|access-date=2020-09-04|archive-date=2020-11-30|archive-url=https://web.archive.org/web/20201130213203/https://www.srs.fs.usda.gov/uplandhardwood/research/article/acorn-study|url-status=dead}}</ref> [[Barkas:Quercus_robur_-_sprouting_acorn.jpg|kiri|jmpl| Sprouting acorn saka ''Quercus robur'' .]] == Referensi == [[Kategori:Kacang]] 1g9lspfue24kxhfrvpao2svxc16tw9x 0 197482 1731251 1731218 2025-06-29T12:06:01Z Henri Aja 45299 Reverted 4 edits by [[Special:Contributions/149.108.179.161|149.108.179.161]] ([[User talk:149.108.179.161|talk]]) (TwinkleGlobal) 1731251 wikitext text/x-wiki [[Barkas:Black_hole_-_Messier_87.jpg|jmpl|350x350px| Luwang ireng gedhe pol ing inti galaksi elips [[Galaksi tipe cD|raksasa]] Messier 87 ing rasi [[Virgo]] . Massané kira-kira milyaran massané Srengéngé ( {{Val|7.22|0.34|0.40}}<nowiki></br></nowiki> {{Val|7.22|0.34|0.40}} M ) ing taun 2016. <ref> {{Cite journal|last=Oldham, L. J.|last2=Auger, M. W.|date=March 2016|title=Galaxy structure from multiple tracers - II. M87 from parsec to megaparsec scales|journal=Monthly Notices of the Royal Astronomical Society|volume=457|issue=1|pages=421–439|arxiv=1601.01323|bibcode=2016MNRAS.457..421O|doi=10.1093/mnras/stv2982}} </ref> Gambar iki dirilis déning proyèk Event Horizon Telescope ing April 2019. ]] '''Luwang ireng mahaagung'''(ing basa Inggris: '''''Supermassive black holes''''') iku jinis [[luwang ireng]] paling gedhé, kanthi massa saka atusan èwu nganti milyaran massané srengéngé. Umume utawa malah kabèh [[galaksi]] dianggep duwé luwang ireng mahaagung ing tengahé. Ing tengah [[Punjering Galaksi|galaksi]] [[Bimasekti]] dipitayani ana luwang ireng mahaagung Sagittarius A* . == Sajarah panemon == Luwang ireng mahaagung awalé dihipotesisaké déning [[Donald Lynden-Bell]] lan Martin Rees ing taun 1971 sing ngira yen pusat galaksi Bimasakti nduwèni luwang ireng mahaagung. Luwang ireng mahaagung tengah Bima Sakti ditemokaké tanggal 13 lan 15 Februari 1974, dening astronom Bruce Balick lan interferometer garis dhasar Robert Brown saka Observatorium Astronomi Radio Nasional lan dijenengi Sagittarius A*. Dheweke nemokaké sumber radio sing ngetokaké radiasi sinkroton, sing ditemokaké kandhel lan ora obah amarga gravitasi. Mulane, iki minangka indikasi pisanan yèn ana luwang ireng mahaagung ing inti Bima Sakti. == Proses pambentukan == [[Barkas:Supermassiveblackhole_nasajpl.jpg|ka|jmpl| Gambaran luwang ireng mahaagung lan cakra akresi.]] == Luwang ireng ing tengah Bima Sakti == Para astronom pitaya yèn Galaksi [[Bimasekti|Bima Sakti]] duwé luwang ireng mahaagung ing tengahé, 26.000 [[taun cahya]] saka [[Tata Surya]], ing wilayah sing diarani Sagittarius A* <ref name="Henderson">{{Cite news|url=http://www.timesonline.co.uk/tol/news/uk/science/article5316001.ece|title=Astronomers confirm black hole at the heart of the Milky Way|last=Henderson|first=Mark|date=December 9, 2008|access-date=2009-05-17|publisher=Times Online|location=London|archive-date=2008-12-16|archive-url=https://web.archive.org/web/20081216235509/http://www.timesonline.co.uk/tol/news/uk/science/article5316001.ece|url-status=dead}}</ref> amarga: * Lintang [[S2 (bintang)|S2]] ngetutaké ideran lonjong kanthi periode orbit 15,2 taun. Jarak paling cedhak 17 [[Jam cahaya|jam cahya]] ( {{Val|1.8}} utawa 120 AU) saka obyèk tengah. <ref>{{Cite journal|last=Schödel|first=R.|last2=et al.|date=17 October 2002|title=A star in a 15.2-year orbit around the supermassive black hole at the centre of the Milky Way|url=https://archive.org/details/sim_nature-uk_2002-10-17_419_6908/page/694|journal=Nature|volume=419|issue=6908|pages=694–696|arxiv=astro-ph/0210426|bibcode=2002Natur.419..694S|doi=10.1038/nature01121|pmid=12384690}} </ref> * Saka pengamatan obahé lintang S2, massa obyèk kasebut bisa dikira-kira 4,1 yuta massané surya, <ref name="Ghez08">{{Cite journal|last=Ghez, A. M.|last2=et al.|year=December 2008|title=Measuring Distance and Properties of the Milky Way's Central Supermassive Black Hole with Stellar Orbits|journal=Astrophysical Journal|volume=689|issue=2|pages=1044–1062|arxiv=0808.2870|bibcode=2008ApJ...689.1044G|doi=10.1086/592738}}</ref> <ref>{{Cite web|url=http://www.skyandtelescope.com/news/27621359.html|title=Milky Way's Central Monster Measured|archive-url=https://archive.today/20120910010925/www.skyandtelescope.com/news/27621359.html|archive-date=2012-09-10|dead-url=yes|access-date=2014-09-25}}</ref> utawa kira-kira {{Val|8.2}} . * Radius obyek tengah ora luwih saka 17 jam cahya, yen luwih gedhé, S2 bakal tabrakan karo. Nyatane, pengamatan anyar <ref>{{Cite journal|last=Ghez|first=A. M.|author-link=Andrea Ghez|last2=Salim, S.|last3=Hornstein, S. D.|last4=Tanner, A.|last5=Lu, J. R.|last6=Morris, M.|last7=Becklin, E. E.|last8=Duchêne, G.|date=May 2005|title=Stellar Orbits around the Galactic Center Black Hole|journal=The Astrophysical Journal|volume=620|issue=2|pages=744–757|arxiv=astro-ph/0306130|bibcode=2005ApJ...620..744G|doi=10.1086/427175}}</ref> nuduhaké radius awak tengah ora luwih saka 6,25 jam cahya, kira-kira padha karo ideran planit [[Uranus]] . == Luwang ireng mahaagung ing njaba Bima Sakti == [[Barkas:Double_Nucleus_of_the_Andromeda_Galaxy_(M31).tif|ka|jmpl| Inti Galaksi Andromeda, panggonan kang para astronom pitaya ana luwang ireng mahaagung ing njeroné. Gambar dijupuk déning [[Teleskop Hubble|Teleskop Angkasa Hubble]] . ''[[NASA]] / ESA .'']] Galaksi Andromeda (M31), adohe 2,5 yuta taun cahya, ana luwang ireng mahaagung ing tengahé kanthi (1,1–2,3) × ¹⁰⁸ (110–230 yuta) massané surya, ingkang luwih gedhé tinimbang Bimasekti. <ref name="Bender"> {{Cite journal|last=Bender|first=Ralf|last2=et al.|date=2005-09-20|title=HST STIS Spectroscopy of the Triple Nucleus of M31: Two Nested Disks in Keplerian Rotation around a Supermassive Black Hole|journal=[[The Astrophysical Journal]]|volume=631|issue=1|pages=280–300|arxiv=astro-ph/0509839|bibcode=2005ApJ...631..280B|doi=10.1086/432434}}</ref> == Deleng uga == * Dhaftar uwangireng paling gedhé * Lintang neutron * [[Luwang ireng]] * [[Galaksi]] * [[Punjering Galaksi|Pusat galaksi]] * Kuasar * Semburan sinar gamma == Referensi == {{Reflist|colwidth=30em}} qqtrw9c04q8u5sjjwfno5t902y69atu 0 198577 1731266 1729316 2025-06-30T08:19:47Z Sam Hidayat 33992 1731266 wikitext text/x-wiki '''Masjid Pathok Nagara Mlangi''' ya iku salah siji saka patang Masjid Pathok Nagara [[Kasultanan Ngayogyakarta]] kang ngubengi wewengkon kasultanan.<ref name=":0">{{Cite web|url=https://budaya.jogjaprov.go.id/artikel/detail/Rekonstruksi-Masjid-Pathok-Negara-Mlangi-di-Tahun-2012|title=Rekonstruksi Masjid Pathok Negara Mlangi di Tahun 2012|website=budaya.jogjaprov.go.id|language=id|access-date=2025-05-16}}</ref> Masjid iki mapan ana ing Dhusun Mlangi, Nagatirta, Kapanéwon Gamping, Slèman.<ref>{{Cite book|title=Masjid Bersejarah Provinsi Daerah Istimewa Yogyakarta|first=Tim Penyusun|publisher=Sholahuddin Offset|year=2007|location=Yogyakarta}}</ref> [[Barkas:Mlangi Pathok Nagara Mosque.jpg|jmpl|Fasad ngarep Masjid Pathok Nagara Mlangi]] Masjid Pathok Nagara iki ora mung kanggo papan ibadah lan panyebaran agama Islam. Nanging, masjid iki uga duwèni fungsi dadi tiyang nagara, wates wewengkon, lan pertahanan rakyat. Masjid Pathok Nagara Mlangi iki dadi bangunan masjid kapisan saka [[Masjid Pathok Nagara]] liyané.<ref name=":1">{{Cite web|url=https://wisatabudayaku.sv.ugm.ac.id/2020/01/23/masjid-pathok-negoro-mlangi/|title=Masjid Pathok Negoro Mlangi – Wisata Budayaku, Istimewa Jogjaku!|date=2020-01-23|language=id-ID|access-date=2025-05-16}}</ref> [[File:Denah Masjid Mlangi.jpg|thumb|Denah Masjid Mlangi]] == Sajarah == Jeneng Mlangi dijupuk saka tembung 'mulangi' kang tegesé mulang utawa ngajar. Jeneng kuwi dijupuk saka pangarep-arep Kyai Nur Iman kanggo ngembangaké ajaran Islam wiwit dhèwèké isih nom. Nanging, Kyai Nur Iman ora nginceng tahta dadi raja ing Karaton Ngayogyakarta.<ref name=":1" /> Masjid iki didadèkaké salah sawijining masjid pathok nagara wiwit taun 1758 nalika [[Perang Dipanegara]]. Wewengkon masjid iki kanggo markas rembugan nyiapaké strategi perang.<ref name=":0" /> Ing taun 1985, masyarakat ngreksa Masjid Pathok Nagara Mlangi dadi wangunan masjid kang duwèni arsitèktur modèren. Nanging, renovasi kuwi ngilangaké ciri khas saka Masjid Pathok Nagara.<ref name=":1" /> == Rujukan == {{reflist|1}} [[Kategori:Adipusaka Project]] [[Kategori:Cagar budaya ing Sléman]] 4jm876tf02vdxk3nuea2he22y3b5sg6 1731267 1731266 2025-06-30T08:20:12Z Sam Hidayat 33992 1731267 wikitext text/x-wiki '''Masjid Pathok Nagara Mlangi''' ya iku salah siji saka patang Masjid Pathok Nagara [[Kasultanan Ngayogyakarta]] kang ngubengi wewengkon kasultanan.<ref name=":0">{{Cite web|url=https://budaya.jogjaprov.go.id/artikel/detail/Rekonstruksi-Masjid-Pathok-Negara-Mlangi-di-Tahun-2012|title=Rekonstruksi Masjid Pathok Negara Mlangi di Tahun 2012|website=budaya.jogjaprov.go.id|language=id|access-date=2025-05-16}}</ref> Masjid iki mapan ana ing Dhusun Mlangi, Nagatirta, Kapanéwon Gamping, Slèman.<ref>{{Cite book|title=Masjid Bersejarah Provinsi Daerah Istimewa Yogyakarta|first=Tim Penyusun|publisher=Sholahuddin Offset|year=2007|location=Yogyakarta}}</ref> [[Barkas:Mlangi Pathok Nagara Mosque.jpg|jmpl|Fasad ngarep Masjid Pathok Nagara Mlangi]] Masjid Pathok Nagara iki ora mung kanggo papan ibadah lan panyebaran agama Islam. Nanging, masjid iki uga duwèni fungsi dadi tiyang nagara, wates wewengkon, lan pertahanan rakyat. Masjid Pathok Nagara Mlangi iki dadi bangunan masjid kapisan saka [[Masjid Pathok Nagara]] liyané.<ref name=":1">{{Cite web|url=https://wisatabudayaku.sv.ugm.ac.id/2020/01/23/masjid-pathok-negoro-mlangi/|title=Masjid Pathok Negoro Mlangi – Wisata Budayaku, Istimewa Jogjaku!|date=2020-01-23|language=id-ID|access-date=2025-05-16}}</ref> [[File:Denah Masjid Mlangi.jpg|thumb|Denah Masjid Mlangi]] == Sajarah == Jeneng Mlangi dijupuk saka tembung 'mulangi' kang tegesé mulang utawa ngajar. Jeneng kuwi dijupuk saka pangarep-arep Kyai Nur Iman kanggo ngembangaké ajaran Islam wiwit dhèwèké isih nom. Nanging, Kyai Nur Iman ora nginceng tahta dadi raja ing Karaton Ngayogyakarta.<ref name=":1" /> Masjid iki didadèkaké salah sawijining masjid pathok nagara wiwit taun 1758 nalika [[Perang Dipanegara]]. Wewengkon masjid iki kanggo markas rembugan nyiapaké strategi perang.<ref name=":0" /> Ing taun 1985, masyarakat ngreksa Masjid Pathok Nagara Mlangi dadi wangunan masjid kang duwèni arsitèktur modèren. Nanging, renovasi kuwi ngilangaké ciri khas saka Masjid Pathok Nagara.<ref name=":1" /> == Rujukan == {{reflist|1}} [[Kategori:Adipusaka Project]] [[Kategori:Cagar budaya ing Sléman]] 13zrsokdgvvee9inn6qt8rd021sxz8t 1731268 1731267 2025-06-30T08:20:52Z Sam Hidayat 33992 1731268 wikitext text/x-wiki '''Masjid Pathok Nagara Mlangi''' (Carakan: ꦩꦱ꧀ꦗꦶꦢ꧀ꦥꦛꦺꦴꦏ꧀ꦤꦒꦫꦩ꧀ꦭꦔꦶ) ya iku salah siji saka patang Masjid Pathok Nagara [[Kasultanan Ngayogyakarta]] kang ngubengi wewengkon kasultanan.<ref name=":0">{{Cite web|url=https://budaya.jogjaprov.go.id/artikel/detail/Rekonstruksi-Masjid-Pathok-Negara-Mlangi-di-Tahun-2012|title=Rekonstruksi Masjid Pathok Negara Mlangi di Tahun 2012|website=budaya.jogjaprov.go.id|language=id|access-date=2025-05-16}}</ref> Masjid iki mapan ana ing Dhusun Mlangi, Nagatirta, Kapanéwon Gamping, Slèman.<ref>{{Cite book|title=Masjid Bersejarah Provinsi Daerah Istimewa Yogyakarta|first=Tim Penyusun|publisher=Sholahuddin Offset|year=2007|location=Yogyakarta}}</ref> [[Barkas:Mlangi Pathok Nagara Mosque.jpg|jmpl|Fasad ngarep Masjid Pathok Nagara Mlangi]] Masjid Pathok Nagara iki ora mung kanggo papan ibadah lan panyebaran agama Islam. Nanging, masjid iki uga duwèni fungsi dadi tiyang nagara, wates wewengkon, lan pertahanan rakyat. Masjid Pathok Nagara Mlangi iki dadi bangunan masjid kapisan saka [[Masjid Pathok Nagara]] liyané.<ref name=":1">{{Cite web|url=https://wisatabudayaku.sv.ugm.ac.id/2020/01/23/masjid-pathok-negoro-mlangi/|title=Masjid Pathok Negoro Mlangi – Wisata Budayaku, Istimewa Jogjaku!|date=2020-01-23|language=id-ID|access-date=2025-05-16}}</ref> [[File:Denah Masjid Mlangi.jpg|thumb|Denah Masjid Mlangi]] == Sajarah == Jeneng Mlangi dijupuk saka tembung 'mulangi' kang tegesé mulang utawa ngajar. Jeneng kuwi dijupuk saka pangarep-arep Kyai Nur Iman kanggo ngembangaké ajaran Islam wiwit dhèwèké isih nom. Nanging, Kyai Nur Iman ora nginceng tahta dadi raja ing Karaton Ngayogyakarta.<ref name=":1" /> Masjid iki didadèkaké salah sawijining masjid pathok nagara wiwit taun 1758 nalika [[Perang Dipanegara]]. Wewengkon masjid iki kanggo markas rembugan nyiapaké strategi perang.<ref name=":0" /> Ing taun 1985, masyarakat ngreksa Masjid Pathok Nagara Mlangi dadi wangunan masjid kang duwèni arsitèktur modèren. Nanging, renovasi kuwi ngilangaké ciri khas saka Masjid Pathok Nagara.<ref name=":1" /> == Rujukan == {{reflist|1}} [[Kategori:Adipusaka Project]] [[Kategori:Cagar budaya ing Sléman]] oi4c1762nopf96n7awhih49ouc12xfk 1731269 1731268 2025-06-30T08:22:12Z Sam Hidayat 33992 1731269 wikitext text/x-wiki [[Barkas:Mlangi Pathok Nagara Mosque.jpg|jmpl|Fasad ngarep Masjid Pathok Nagara Mlangi]]'''Masjid Pathok Nagara Mlangi''' (Carakan: ꦩꦱ꧀ꦗꦶꦢ꧀ꦥꦛꦺꦴꦏ꧀ꦤꦒꦫꦩ꧀ꦭꦔꦶ) ya iku salah siji saka patang Masjid Pathok Nagara [[Kasultanan Ngayogyakarta]] kang ngubengi wewengkon kasultanan.<ref name=":0">{{Cite web|url=https://budaya.jogjaprov.go.id/artikel/detail/Rekonstruksi-Masjid-Pathok-Negara-Mlangi-di-Tahun-2012|title=Rekonstruksi Masjid Pathok Negara Mlangi di Tahun 2012|website=budaya.jogjaprov.go.id|language=id|access-date=2025-05-16}}</ref> Masjid iki mapan ana ing Dhusun Mlangi, Nagatirta, Kapanéwon Gamping, Slèman.<ref>{{Cite book|title=Masjid Bersejarah Provinsi Daerah Istimewa Yogyakarta|first=Tim Penyusun|publisher=Sholahuddin Offset|year=2007|location=Yogyakarta}}</ref> Masjid Pathok Nagara iki ora mung kanggo papan ibadah lan panyebaran agama Islam, nanging uga nduwèni fungsi dadi cagaking nagara, wates wewengkon, lan pertahanan rakyat. Masjid Pathok Nagara Mlangi iki dadi bangunan masjid kapisan saka patang [[Masjid Pathok Nagara]] liyané.<ref name=":1">{{Cite web|url=https://wisatabudayaku.sv.ugm.ac.id/2020/01/23/masjid-pathok-negoro-mlangi/|title=Masjid Pathok Negoro Mlangi – Wisata Budayaku, Istimewa Jogjaku!|date=2020-01-23|language=id-ID|access-date=2025-05-16}}</ref> [[File:Denah Masjid Mlangi.jpg|thumb|Denah Masjid Mlangi]] == Sajarah == Jeneng Mlangi dijupuk saka tembung 'mulangi' kang tegesé mulang utawa ngajar. Jeneng kuwi dijupuk saka pangarep-arep Kyai Nur Iman kanggo ngembangaké ajaran Islam wiwit dhèwèké isih nom. Nanging, Kyai Nur Iman ora nginceng tahta dadi raja ing Karaton Ngayogyakarta.<ref name=":1" /> Masjid iki didadèkaké salah sawijining masjid pathok nagara wiwit taun 1758 nalika [[Perang Dipanegara]]. Wewengkon masjid iki kanggo markas rembugan nyiapaké strategi perang.<ref name=":0" /> Ing taun 1985, masyarakat ngreksa Masjid Pathok Nagara Mlangi dadi wangunan masjid kang duwèni arsitèktur modèren. Nanging, renovasi kuwi ngilangaké ciri khas saka Masjid Pathok Nagara.<ref name=":1" /> == Rujukan == {{reflist|1}} [[Kategori:Adipusaka Project]] [[Kategori:Cagar budaya ing Sléman]] grgbqm0dgzbjnwwp40yo07uow28ab0w 0 198811 1731253 2025-06-29T12:09:01Z Manggisjeruk 65009 Manggisjeruk ngalih kaca [[Angabar]] menyang [[Panambayangan]] 1731253 wikitext text/x-wiki #ALIH [[Panambayangan]] onm81mcj68lc833noomagd5brv4ltz5 0 198812 1731256 2025-06-29T12:20:11Z Manggisjeruk 65009 Digawé kanthi mertal kaca "[[:en:Special:Redirect/revision/1292106749|Water cycle]]" 1731256 wikitext text/x-wiki == Referensi == [[Barkas:USGS_WaterCycle_English_ONLINE_20221013.png|jmpl| Cecarihan remit kang ngenthani jantran banyu sajagat. Purug obahe banyu ing antarane pabanyon aniling nginger munggah liwat kanthi ngriwe lan nguwab banjur nginger mudhun kanthi katarik kihaling [[Gravitasi|bebyutan]] . Cecarihan kasebut uga nuduhake kepiye panggunaan banyu manungsa lan ing endi banyu kasimpen lan kepiye inger-ingerane. <ref>{{Cite web|url=https://www.usgs.gov/media/images/water-cycle-png|title=The Water Cycle (PNG) {{!}} U.S. Geological Survey|date=13 October 2022|website=www.usgs.gov|access-date=2024-04-24}}</ref>]] '''Jantran banyu''' kuwi [[Dhaur Biogéokimia|jantraning urip-tanah-kimiya]] kang nyakup inger-inger manggehe [[banyu]], ing ndhuwur lan ing ngisor lumahing [[bumi]] ngliwati pabanyon kang beda-beda. Gunggunge banyu ing Bumi tetep ajeg sajrone wektu masiya manggeh dipigunakake. <ref>{{Cite web|url=https://ny1.com/nyc/all-boroughs/weather/2021/11/19/the-water-cycle-|title=Water may change phases, but the amount always remains constant|website=ny1.com|language=en|access-date=2025-05-01}}</ref> Nanging, mbabare banyu dadi pabanyon kayata [[Ès|es]], [[banyu tawa]], banyu asin lan banyu tetawangan iku maneka warna lan gumantung marang [[Iklim|rupaning iklim]] . Banyu pindhah saka siji pabanyon menyang liyane, kayata saka kali menyang [[Samodra|segara]], utawa saka segara menyang tawang-panawang amarga macem-macem prakara wadhag lan kimiya. Perkara sing ndadékaké nginger yaiku [[Panguwaban|nguwab]], [[Transpirasi|ngriwe]], [[Kondensasi|ngawun]], [[udan]], [[Angabar|nambayang]] ,[[Infiltrasi|ngirig]], [[bedhahan palumahan]], lan ilet ngisor palumahan. Kanthi mengkono, banyu ngliwati macem-macem wujud: cuweram, padhet ( [[Ès|es]] ) lan [[Uwab banyu|uwab]] . Samudra nduweni piguna wigati ing jantraning banyu amarga minangka sumber 86% panguwabane sajagat.<ref name=":4">{{Cite web|url=https://science.nasa.gov/earth-science/oceanography/ocean-earth-system/ocean-water-cycle|title=Water Cycle {{!}} Science Mission Directorate|website=science.nasa.gov|language=en|archive-url=https://web.archive.org/web/20180115065559/https://science.nasa.gov/earth-science/oceanography/ocean-earth-system/ocean-water-cycle|archive-date=2018-01-15|access-date=2018-01-15}}</ref> Jantraning banyu kadedel dening ijol-ijolan gandra ing wujud palintiran panas antarane wangun kang beda. Gandra sing kaenthi utawa rumangsuk sajrone owah-owahing wujud banyu uga isa nyebabake owah-owahan [[suhu]] . <ref>{{Cite web|url=https://www.ebsco.com/research-starters/chemistry/endothermic-and-exothermic-processes|title=Endothermic and exothermic processes {{!}} EBSCO Research Starters|website=www.ebsco.com|language=en|access-date=2025-05-01}}</ref> Panas rumangsuk minangka malihe banyu saka cuweran menyang wujud uwab liwat panguwaban. Panas iki uga dikenal minangka panas selaping panguwaban. <ref>{{Citation|last=Kirkham|first=M. B.|title=Chapter 3 - Structure and Properties of Water|date=2014-01-01|url=https://linkinghub.elsevier.com/retrieve/pii/B9780124200227000033|pages=27–40|editor-last=Kirkham|editor-first=M. B.|periodical=Principles of Soil and Plant Water Relations (Second Edition)|place=Boston|publisher=Academic Press|doi=10.1016/b978-0-12-420022-7.00003-3|isbn=978-0-12-420022-7|access-date=2025-05-01}}</ref> Kosok baline, nalika banyu ngawun utawa ajer saka es padhet, mula ngeculake gandra lan panas. Ing gegedhen sajagat, banyu nduweni piguna wigati kanggo mindhah panas saka wilayah tropis menyang kutub liwat indering segara. <ref>{{Cite web|url=https://www.bbc.co.uk/bitesize/guides/zpykxsg/revision/2#:~:text=Heat%20is%20transferred%20by%20warm,with%20the%20general%20atmospheric%20circulation.|title=Ocean currents - Atmosphere and climate - Edexcel - GCSE Geography Revision - Edexcel|website=BBC Bitesize|language=en-GB|access-date=2025-05-01}}</ref> == Referensi == [[Kategori:Banyu]] [[Kategori:Hidrologi]] ms42npl1rioqvc76042ry7dgs2v0ykr 1731257 1731256 2025-06-29T12:20:46Z Manggisjeruk 65009 1731257 wikitext text/x-wiki [[Barkas:USGS_WaterCycle_English_ONLINE_20221013.png|jmpl| Cecarihan remit kang ngenthani jantran banyu sajagat. Purug obahe banyu ing antarane pabanyon aniling nginger munggah liwat kanthi ngriwe lan nguwab banjur nginger mudhun kanthi katarik kihaling [[Gravitasi|bebyutan]] . Cecarihan kasebut uga nuduhake kepiye panggunaan banyu manungsa lan ing endi banyu kasimpen lan kepiye inger-ingerane. <ref>{{Cite web|url=https://www.usgs.gov/media/images/water-cycle-png|title=The Water Cycle (PNG) {{!}} U.S. Geological Survey|date=13 October 2022|website=www.usgs.gov|access-date=2024-04-24}}</ref>]] '''Jantran banyu''' kuwi [[Dhaur Biogéokimia|jantraning urip-tanah-kimiya]] kang nyakup inger-inger manggehe [[banyu]], ing ndhuwur lan ing ngisor lumahing [[bumi]] ngliwati pabanyon kang beda-beda. Gunggunge banyu ing Bumi tetep ajeg sajrone wektu masiya manggeh dipigunakake. <ref>{{Cite web|url=https://ny1.com/nyc/all-boroughs/weather/2021/11/19/the-water-cycle-|title=Water may change phases, but the amount always remains constant|website=ny1.com|language=en|access-date=2025-05-01}}</ref> Nanging, mbabare banyu dadi pabanyon kayata [[Ès|es]], [[banyu tawa]], banyu asin lan banyu tetawangan iku maneka warna lan gumantung marang [[Iklim|rupaning iklim]] . Banyu pindhah saka siji pabanyon menyang liyane, kayata saka kali menyang [[Samodra|segara]], utawa saka segara menyang tawang-panawang amarga macem-macem prakara wadhag lan kimiya. Perkara sing ndadékaké nginger yaiku [[Panguwaban|nguwab]], [[Transpirasi|ngriwe]], [[Kondensasi|ngawun]], [[udan]], [[Angabar|nambayang]] ,[[Infiltrasi|ngirig]], [[bedhahan palumahan]], lan ilet ngisor palumahan. Kanthi mengkono, banyu ngliwati macem-macem wujud: cuweram, padhet ( [[Ès|es]] ) lan [[Uwab banyu|uwab]] . Samudra nduweni piguna wigati ing jantraning banyu amarga minangka sumber 86% panguwabane sajagat.<ref name=":4">{{Cite web|url=https://science.nasa.gov/earth-science/oceanography/ocean-earth-system/ocean-water-cycle|title=Water Cycle {{!}} Science Mission Directorate|website=science.nasa.gov|language=en|archive-url=https://web.archive.org/web/20180115065559/https://science.nasa.gov/earth-science/oceanography/ocean-earth-system/ocean-water-cycle|archive-date=2018-01-15|access-date=2018-01-15}}</ref> Jantraning banyu kadedel dening ijol-ijolan gandra ing wujud palintiran panas antarane wangun kang beda. Gandra sing kaenthi utawa rumangsuk sajrone owah-owahing wujud banyu uga isa nyebabake owah-owahan [[suhu]] . <ref>{{Cite web|url=https://www.ebsco.com/research-starters/chemistry/endothermic-and-exothermic-processes|title=Endothermic and exothermic processes {{!}} EBSCO Research Starters|website=www.ebsco.com|language=en|access-date=2025-05-01}}</ref> Panas rumangsuk minangka malihe banyu saka cuweran menyang wujud uwab liwat panguwaban. Panas iki uga dikenal minangka panas selaping panguwaban. <ref>{{Citation|last=Kirkham|first=M. B.|title=Chapter 3 - Structure and Properties of Water|date=2014-01-01|url=https://linkinghub.elsevier.com/retrieve/pii/B9780124200227000033|pages=27–40|editor-last=Kirkham|editor-first=M. B.|periodical=Principles of Soil and Plant Water Relations (Second Edition)|place=Boston|publisher=Academic Press|doi=10.1016/b978-0-12-420022-7.00003-3|isbn=978-0-12-420022-7|access-date=2025-05-01}}</ref> Kosok baline, nalika banyu ngawun utawa ajer saka es padhet, mula ngeculake gandra lan panas. Ing gegedhen sajagat, banyu nduweni piguna wigati kanggo mindhah panas saka wilayah tropis menyang kutub liwat indering segara. <ref>{{Cite web|url=https://www.bbc.co.uk/bitesize/guides/zpykxsg/revision/2#:~:text=Heat%20is%20transferred%20by%20warm,with%20the%20general%20atmospheric%20circulation.|title=Ocean currents - Atmosphere and climate - Edexcel - GCSE Geography Revision - Edexcel|website=BBC Bitesize|language=en-GB|access-date=2025-05-01}}</ref> == Referensi == [[Kategori:Banyu]] [[Kategori:Hidrologi]] ld3emds44voecq02e5cj5ayu33845pv 1731258 1731257 2025-06-29T12:21:48Z Manggisjeruk 65009 1731258 wikitext text/x-wiki [[Barkas:USGS_WaterCycle_English_ONLINE_20221013.png|jmpl| Cecarihan remit kang ngenthani jantran banyu sajagat. Purug obahe banyu ing antarane pabanyon aniling nginger munggah liwat kanthi ngriwe lan nguwab banjur nginger mudhun kanthi katarik kihaling [[Gravitasi|bebyutan]] . Cecarihan kasebut uga nuduhake kepiye panggunaan banyu manungsa lan ing endi banyu kasimpen lan kepiye inger-ingerane. <ref>{{Cite web|url=https://www.usgs.gov/media/images/water-cycle-png|title=The Water Cycle (PNG) {{!}} U.S. Geological Survey|date=13 October 2022|website=www.usgs.gov|access-date=2024-04-24}}</ref>]] '''Jantran banyu''' kuwi [[Dhaur Biogéokimia|jantraning urip-tanah-kimiya]] kang nyakup inger-inger manggehe [[banyu]], ing ndhuwur lan ing ngisor lumahing [[bumi]] ngliwati pabanyon kang beda-beda. Gunggunge banyu ing Bumi tetep ajeg sajrone wektu masiya manggeh dipigunakake. <ref>{{Cite web|url=https://ny1.com/nyc/all-boroughs/weather/2021/11/19/the-water-cycle-|title=Water may change phases, but the amount always remains constant|website=ny1.com|language=en|access-date=2025-05-01}}</ref> Nanging, mbabare banyu dadi pabanyon kayata [[Ès|es]], [[banyu tawa]], banyu asin lan banyu tetawangan iku maneka warna lan gumantung marang [[Iklim|rupaning iklim]] . Banyu pindhah saka siji pabanyon menyang liyane, kayata saka kali menyang [[Samodra|segara]], utawa saka segara menyang tawang-panawang amarga macem-macem prakara wadhag lan kimiya. Perkara sing ndadékaké nginger yaiku [[Panguwaban|nguwab]], [[Transpirasi|ngriwe]], [[Kondensasi|ngawun]], [[udan]], [[Angabar|nambayang]] ,[[Infiltrasi|ngirig]], mbedah saka palumahan, lan mili ngisor palumahan. Kanthi mengkono, banyu ngliwati macem-macem wujud : cuweran, padhet ( [[Ès|es]] ) lan [[Uwab banyu|uwab]] . Samudra nduweni piguna wigati ing jantraning banyu amarga minangka sumber 86% panguwabane sajagat.<ref name=":4">{{Cite web|url=https://science.nasa.gov/earth-science/oceanography/ocean-earth-system/ocean-water-cycle|title=Water Cycle {{!}} Science Mission Directorate|website=science.nasa.gov|language=en|archive-url=https://web.archive.org/web/20180115065559/https://science.nasa.gov/earth-science/oceanography/ocean-earth-system/ocean-water-cycle|archive-date=2018-01-15|access-date=2018-01-15}}</ref> Jantraning banyu kadedel dening ijol-ijolan gandra ing wujud palintiran panas antarane wangun kang beda. Gandra sing kaenthi utawa rumangsuk sajrone owah-owahing wujud banyu uga isa nyebabake owah-owahan [[suhu]] . <ref>{{Cite web|url=https://www.ebsco.com/research-starters/chemistry/endothermic-and-exothermic-processes|title=Endothermic and exothermic processes {{!}} EBSCO Research Starters|website=www.ebsco.com|language=en|access-date=2025-05-01}}</ref> Panas rumangsuk minangka malihe banyu saka cuweran menyang wujud uwab liwat panguwaban. Panas iki uga dikenal minangka panas selaping panguwaban. <ref>{{Citation|last=Kirkham|first=M. B.|title=Chapter 3 - Structure and Properties of Water|date=2014-01-01|url=https://linkinghub.elsevier.com/retrieve/pii/B9780124200227000033|pages=27–40|editor-last=Kirkham|editor-first=M. B.|periodical=Principles of Soil and Plant Water Relations (Second Edition)|place=Boston|publisher=Academic Press|doi=10.1016/b978-0-12-420022-7.00003-3|isbn=978-0-12-420022-7|access-date=2025-05-01}}</ref> Kosok baline, nalika banyu ngawun utawa ajer saka es padhet, mula ngeculake gandra lan panas. Ing gegedhen sajagat, banyu nduweni piguna wigati kanggo mindhah panas saka wilayah tropis menyang kutub liwat indering segara. <ref>{{Cite web|url=https://www.bbc.co.uk/bitesize/guides/zpykxsg/revision/2#:~:text=Heat%20is%20transferred%20by%20warm,with%20the%20general%20atmospheric%20circulation.|title=Ocean currents - Atmosphere and climate - Edexcel - GCSE Geography Revision - Edexcel|website=BBC Bitesize|language=en-GB|access-date=2025-05-01}}</ref> == Referensi == [[Kategori:Banyu]] [[Kategori:Hidrologi]] 2s6te7weqvb0pxx0z9n4dd0efilz0v9 1731272 1731258 2025-06-30T11:42:17Z Manggisjeruk 65009 1731272 wikitext text/x-wiki [[Barkas:USGS_WaterCycle_English_ONLINE_20221013.png|jmpl| Cecarihan remit kang ngenthani jantran banyu sajagat. Purug obahe banyu ing antarane pabanyon aniling nginger munggah liwat kanthi ngriwe lan nguwab banjur nginger mudhun kanthi katarik kihaling [[Gravitasi|bebyutan]] . Cecarihan kasebut uga nuduhake kepiye panggunaan banyu manungsa lan ing endi banyu kasimpen lan kepiye inger-ingerane. <ref>{{Cite web|url=https://www.usgs.gov/media/images/water-cycle-png|title=The Water Cycle (PNG) {{!}} U.S. Geological Survey|date=13 October 2022|website=www.usgs.gov|access-date=2024-04-24}}</ref>]] '''Jantran banyu''' kuwi [[Dhaur Biogéokimia|jantraning urip-tanah-kimiya]] kang nyakup inger-inger manggehe [[banyu]], ing ndhuwur lan ing ngisor lumahing [[bumi]] ngliwati pabanyon kang beda-beda. Gunggunge banyu ing Bumi tetep ajeg sajrone wektu masiya manggeh dipigunakake. <ref>{{Cite web|url=https://ny1.com/nyc/all-boroughs/weather/2021/11/19/the-water-cycle-|title=Water may change phases, but the amount always remains constant|website=ny1.com|language=en|access-date=2025-05-01}}</ref> Nanging, mbabare banyu dadi pabanyon kayata [[Ès|es]], [[banyu tawa]], banyu asin lan banyu tetawangan iku maneka warna lan gumantung marang [[Iklim|rupaning iklim]] . Banyu pindhah saka siji pabanyon menyang liyane, kayata saka kali menyang [[Samodra|segara]], utawa saka segara menyang tawang-panawang amarga macem-macem prakara wadhag lan kimiya. Perkara sing ndadékaké nginger yaiku [[Panguwaban|nguwab]], [[Transpirasi|ngriwe]], [[Kondensasi|ngawun]], [[udan]], [[Angabar|nambayang]] ,[[Infiltrasi|ngirig]], mbedah saka palumahan, lan mili ngisor palumahan. Kanthi mengkono, banyu ngliwati macem-macem wujud : cuweran, padhet ( [[Ès|es]] ) lan [[Uwab banyu|uwab]] . Samudra nduweni piguna wigati ing jantraning banyu amarga minangka sumber 86% panguwabane sajagat.<ref name=":4">{{Cite web|url=https://science.nasa.gov/earth-science/oceanography/ocean-earth-system/ocean-water-cycle|title=Water Cycle {{!}} Science Mission Directorate|website=science.nasa.gov|language=en|archive-url=https://web.archive.org/web/20180115065559/https://science.nasa.gov/earth-science/oceanography/ocean-earth-system/ocean-water-cycle|archive-date=2018-01-15|access-date=2018-01-15}}</ref> Jantraning banyu kadedel dening ijol-ijolan gandra ing wujud palintiran panas antarane wangun kang beda. Gandra sing kaenthi utawa rumangsuk sajrone owah-owahing wujud banyu uga isa nyebabake owah-owahan [[suhu]] . <ref>{{Cite web|url=https://www.ebsco.com/research-starters/chemistry/endothermic-and-exothermic-processes|title=Endothermic and exothermic processes {{!}} EBSCO Research Starters|website=www.ebsco.com|language=en|access-date=2025-05-01}}</ref> Panas rumangsuk minangka malihe banyu saka cuweran menyang wujud uwab liwat panguwaban. Panas iki uga dikenal minangka panas selaping panguwaban. <ref>{{Citation|last=Kirkham|first=M. B.|title=Chapter 3 - Structure and Properties of Water|date=2014-01-01|url=https://linkinghub.elsevier.com/retrieve/pii/B9780124200227000033|pages=27–40|editor-last=Kirkham|editor-first=M. B.|periodical=Principles of Soil and Plant Water Relations (Second Edition)|place=Boston|publisher=Academic Press|doi=10.1016/b978-0-12-420022-7.00003-3|isbn=978-0-12-420022-7|access-date=2025-05-01}}</ref> Kosok baline, nalika banyu ngawun utawa ajer saka es padhet, mula ngeculake gandra lan panas.<ref>{{Cite web|url=https://www.bbc.co.uk/bitesize/guides/zpykxsg/revision/2#:~:text=Heat%20is%20transferred%20by%20warm,with%20the%20general%20atmospheric%20circulation.|title=Ocean currents - Atmosphere and climate - Edexcel - GCSE Geography Revision - Edexcel|website=BBC Bitesize|language=en-GB|access-date=2025-05-01}}</ref> == Referensi == [[Kategori:Banyu]] [[Kategori:Hidrologi]] 1k2p213hnt46g73v9vr4gp001w78ctx 1731273 1731272 2025-06-30T11:45:21Z Manggisjeruk 65009 /* Referensi */ 1731273 wikitext text/x-wiki [[Barkas:USGS_WaterCycle_English_ONLINE_20221013.png|jmpl| Cecarihan remit kang ngenthani jantran banyu sajagat. Purug obahe banyu ing antarane pabanyon aniling nginger munggah liwat kanthi ngriwe lan nguwab banjur nginger mudhun kanthi katarik kihaling [[Gravitasi|bebyutan]] . Cecarihan kasebut uga nuduhake kepiye panggunaan banyu manungsa lan ing endi banyu kasimpen lan kepiye inger-ingerane. <ref>{{Cite web|url=https://www.usgs.gov/media/images/water-cycle-png|title=The Water Cycle (PNG) {{!}} U.S. Geological Survey|date=13 October 2022|website=www.usgs.gov|access-date=2024-04-24}}</ref>]] '''Jantran banyu''' kuwi [[Dhaur Biogéokimia|jantraning urip-tanah-kimiya]] kang nyakup inger-inger manggehe [[banyu]], ing ndhuwur lan ing ngisor lumahing [[bumi]] ngliwati pabanyon kang beda-beda. Gunggunge banyu ing Bumi tetep ajeg sajrone wektu masiya manggeh dipigunakake. <ref>{{Cite web|url=https://ny1.com/nyc/all-boroughs/weather/2021/11/19/the-water-cycle-|title=Water may change phases, but the amount always remains constant|website=ny1.com|language=en|access-date=2025-05-01}}</ref> Nanging, mbabare banyu dadi pabanyon kayata [[Ès|es]], [[banyu tawa]], banyu asin lan banyu tetawangan iku maneka warna lan gumantung marang [[Iklim|rupaning iklim]] . Banyu pindhah saka siji pabanyon menyang liyane, kayata saka kali menyang [[Samodra|segara]], utawa saka segara menyang tawang-panawang amarga macem-macem prakara wadhag lan kimiya. Perkara sing ndadékaké nginger yaiku [[Panguwaban|nguwab]], [[Transpirasi|ngriwe]], [[Kondensasi|ngawun]], [[udan]], [[Angabar|nambayang]] ,[[Infiltrasi|ngirig]], mbedah saka palumahan, lan mili ngisor palumahan. Kanthi mengkono, banyu ngliwati macem-macem wujud : cuweran, padhet ( [[Ès|es]] ) lan [[Uwab banyu|uwab]] . Samudra nduweni piguna wigati ing jantraning banyu amarga minangka sumber 86% panguwabane sajagat.<ref name=":4">{{Cite web|url=https://science.nasa.gov/earth-science/oceanography/ocean-earth-system/ocean-water-cycle|title=Water Cycle {{!}} Science Mission Directorate|website=science.nasa.gov|language=en|archive-url=https://web.archive.org/web/20180115065559/https://science.nasa.gov/earth-science/oceanography/ocean-earth-system/ocean-water-cycle|archive-date=2018-01-15|access-date=2018-01-15}}</ref> Jantraning banyu kadedel dening ijol-ijolan gandra ing wujud palintiran panas antarane wangun kang beda. Gandra sing kaenthi utawa rumangsuk sajrone owah-owahing wujud banyu uga isa nyebabake owah-owahan [[suhu]] . <ref>{{Cite web|url=https://www.ebsco.com/research-starters/chemistry/endothermic-and-exothermic-processes|title=Endothermic and exothermic processes {{!}} EBSCO Research Starters|website=www.ebsco.com|language=en|access-date=2025-05-01}}</ref> Panas rumangsuk minangka malihe banyu saka cuweran menyang wujud uwab liwat panguwaban. Panas iki uga dikenal minangka panas selaping panguwaban. <ref>{{Citation|last=Kirkham|first=M. B.|title=Chapter 3 - Structure and Properties of Water|date=2014-01-01|url=https://linkinghub.elsevier.com/retrieve/pii/B9780124200227000033|pages=27–40|editor-last=Kirkham|editor-first=M. B.|periodical=Principles of Soil and Plant Water Relations (Second Edition)|place=Boston|publisher=Academic Press|doi=10.1016/b978-0-12-420022-7.00003-3|isbn=978-0-12-420022-7|access-date=2025-05-01}}</ref> Kosok baline, nalika banyu ngawun utawa ajer saka es padhet, mula ngeculake gandra lan panas.<ref>{{Cite web|url=https://www.bbc.co.uk/bitesize/guides/zpykxsg/revision/2#:~:text=Heat%20is%20transferred%20by%20warm,with%20the%20general%20atmospheric%20circulation.|title=Ocean currents - Atmosphere and climate - Edexcel - GCSE Geography Revision - Edexcel|website=BBC Bitesize|language=en-GB|access-date=2025-05-01}}</ref> == Pratelan == Siklus air didukung oleh energi yang dipancarkan matahari. Ada beberapa cara untuk melakukannya, salah satu cara pertama adalah melalui penguapan , di mana energi dari matahari memanaskan air di samudra, danau, sungai, laut, kolam, dll., dan air tersebut mengalami perubahan fase menjadi gas (uap air) yang naik ke atmosfer. Dua cara lain air masuk ke atmosfer adalah melalui salju dan es yang menyublim menjadi uap air dan melalui evapotranspirasi , yaitu air yang ditranspirasi dari tanaman dan diuapkan dari tanah. == Referensi == [[Kategori:Banyu]] [[Kategori:Hidrologi]] np0iglp0nua3k56xetolnb5ahab8jsd 1731274 1731273 2025-06-30T11:46:13Z Manggisjeruk 65009 1731274 wikitext text/x-wiki [[Barkas:USGS_WaterCycle_English_ONLINE_20221013.png|jmpl| Cecarihan remit kang ngenthani jantran banyu sajagat. Purug obahe banyu ing antarane pabanyon aniling nginger munggah liwat kanthi ngriwe lan nguwab banjur nginger mudhun kanthi katarik kihaling [[Gravitasi|bebyutan]] . Cecarihan kasebut uga nuduhake kepiye panggunaan banyu manungsa lan ing endi banyu kasimpen lan kepiye inger-ingerane. <ref>{{Cite web|url=https://www.usgs.gov/media/images/water-cycle-png|title=The Water Cycle (PNG) {{!}} U.S. Geological Survey|date=13 October 2022|website=www.usgs.gov|access-date=2024-04-24}}</ref>]] '''Jantran banyu''' kuwi [[Dhaur Biogéokimia|jantraning urip-tanah-kimiya]] kang nyakup ingêr-ingêr manggêhè[[banyu]], ing ndhuwur lan ing ngisor lumahing [[bumi]] ngliwati pabanyon kang beda-beda. Gunggunge banyu ing Bumi tetep ajeg sajrone wektu masiya manggeh dipigunakake. <ref>{{Cite web|url=https://ny1.com/nyc/all-boroughs/weather/2021/11/19/the-water-cycle-|title=Water may change phases, but the amount always remains constant|website=ny1.com|language=en|access-date=2025-05-01}}</ref> Nanging, mbabare banyu dadi pabanyon kayata [[Ès|es]], [[banyu tawa]], banyu asin lan banyu tetawangan iku maneka warna lan gumantung marang [[Iklim|rupaning iklim]] . Banyu pindhah saka siji pabanyon menyang liyane, kayata saka kali menyang [[Samodra|segara]], utawa saka segara menyang tawang-panawang amarga macem-macem prakara wadhag lan kimiya. Perkara sing ndadékaké nginger yaiku [[Panguwaban|nguwab]], [[Transpirasi|ngriwe]], [[Kondensasi|ngawun]], [[udan]], [[Angabar|nambayang]] ,[[Infiltrasi|ngirig]], mbedah saka palumahan, lan mili ngisor palumahan. Kanthi mengkono, banyu ngliwati macem-macem wujud : cuweran, padhet ( [[Ès|es]] ) lan [[Uwab banyu|uwab]] . Samudra nduweni piguna wigati ing jantraning banyu amarga minangka sumber 86% panguwabane sajagat.<ref name=":4">{{Cite web|url=https://science.nasa.gov/earth-science/oceanography/ocean-earth-system/ocean-water-cycle|title=Water Cycle {{!}} Science Mission Directorate|website=science.nasa.gov|language=en|archive-url=https://web.archive.org/web/20180115065559/https://science.nasa.gov/earth-science/oceanography/ocean-earth-system/ocean-water-cycle|archive-date=2018-01-15|access-date=2018-01-15}}</ref> Jantraning banyu kadedel dening ijol-ijolan gandra ing wujud palintiran panas antarane wangun kang beda. Gandra sing kaenthi utawa rumangsuk sajrone owah-owahing wujud banyu uga isa nyebabake owah-owahan [[suhu]] . <ref>{{Cite web|url=https://www.ebsco.com/research-starters/chemistry/endothermic-and-exothermic-processes|title=Endothermic and exothermic processes {{!}} EBSCO Research Starters|website=www.ebsco.com|language=en|access-date=2025-05-01}}</ref> Panas rumangsuk minangka malihe banyu saka cuweran menyang wujud uwab liwat panguwaban. Panas iki uga dikenal minangka panas selaping panguwaban. <ref>{{Citation|last=Kirkham|first=M. B.|title=Chapter 3 - Structure and Properties of Water|date=2014-01-01|url=https://linkinghub.elsevier.com/retrieve/pii/B9780124200227000033|pages=27–40|editor-last=Kirkham|editor-first=M. B.|periodical=Principles of Soil and Plant Water Relations (Second Edition)|place=Boston|publisher=Academic Press|doi=10.1016/b978-0-12-420022-7.00003-3|isbn=978-0-12-420022-7|access-date=2025-05-01}}</ref> Kosok baline, nalika banyu ngawun utawa ajer saka es padhet, mula ngeculake gandra lan panas.<ref>{{Cite web|url=https://www.bbc.co.uk/bitesize/guides/zpykxsg/revision/2#:~:text=Heat%20is%20transferred%20by%20warm,with%20the%20general%20atmospheric%20circulation.|title=Ocean currents - Atmosphere and climate - Edexcel - GCSE Geography Revision - Edexcel|website=BBC Bitesize|language=en-GB|access-date=2025-05-01}}</ref> == Pratelan == Siklus air didukung oleh energi yang dipancarkan matahari. Ada beberapa cara untuk melakukannya, salah satu cara pertama adalah melalui penguapan , di mana energi dari matahari memanaskan air di samudra, danau, sungai, laut, kolam, dll., dan air tersebut mengalami perubahan fase menjadi gas (uap air) yang naik ke atmosfer. Dua cara lain air masuk ke atmosfer adalah melalui salju dan es yang menyublim menjadi uap air dan melalui evapotranspirasi , yaitu air yang ditranspirasi dari tanaman dan diuapkan dari tanah. == Referensi == [[Kategori:Banyu]] [[Kategori:Hidrologi]] 08mc15p1v5a6nnzppg7mp6zcl5ag5ec 0 198813 1731265 2025-06-30T04:55:14Z 71.35.4.111 Kaca anyar: {{Infobox artis indonesia | name = Squire Fridell | image = Squire Fridell.jpg | caption = Fridell, [[1977]] | birth_name = | birth_date = {{birth date and age|1943|2|9}} | birth_place = {{Flagicon|USA}} [[Oakland]], [[California]], [[Amérika Sarékat]] | death_date = | death_place = | death_cause = | body_discovered = | resting_place = | nationality = [[Americans|American]] | ethnicity = [[Caucasian people|Caucasian]] | othername = | years_active = 1968-1996 | occupatio... 1731265 wikitext text/x-wiki {{Infobox artis indonesia | name = Squire Fridell | image = Squire Fridell.jpg | caption = Fridell, [[1977]] | birth_name = | birth_date = {{birth date and age|1943|2|9}} | birth_place = {{Flagicon|USA}} [[Oakland]], [[California]], [[Amérika Sarékat]] | death_date = | death_place = | death_cause = | body_discovered = | resting_place = | nationality = [[Americans|American]] | ethnicity = [[Caucasian people|Caucasian]] | othername = | years_active = 1968-1996 | occupation = [[pembawa acara]] | spouse = {{marriage|Suzanne McDermaid|1977}} | partner = | children = 1 | parents = | influences = | influenced = | website = }} '''Squire Fridell''' ({{lahirmati|[[Amérika Sarékat]]|9|2|1943}})) ya iku sawijining pelawak, [[aktor]], lan [[pembawa acara]] saka [[Amérika Sarékat|Amérika]]. ==Cathetan suku== {{commons|Squire Fridell}} [[Kategori:Lair 1943]] [[Kategori:Wong urip]] {{AS-bio-stub}} l5u6w02iw8ftovtcw9rjpiav8p2tgls 0 198814 1731271 2025-06-30T10:50:52Z 178.168.84.189 Kaca anyar: {{Taxobox|domain=[[Eukaryota]]|regnum=[[Animalia]]|phylum=[[Chordata]]|classis=[[Aves]]|superordo=[[Neognathae]]|ordo=[[Trogoniformes]]|familia=[[Trogonidae]]|genus=''[[Pharomachrus]]''|species=''Pharomachrus mocinno''|image=File:Quetzal01.jpg}} '''Quetzal''' (''Pharomachrus mocinno'') iku spesies [[manuk]] tropis gedhé saka kulawarga [[Trogonidae]] lan ordo [[Trogoniformes]]. Iku urip ing alas [[Amérikah Tengah|Amérika Tengah]]. Quetzal lanang dikenal duwe wulu buntut sing... 1731271 wikitext text/x-wiki {{Taxobox|domain=[[Eukaryota]]|regnum=[[Animalia]]|phylum=[[Chordata]]|classis=[[Aves]]|superordo=[[Neognathae]]|ordo=[[Trogoniformes]]|familia=[[Trogonidae]]|genus=''[[Pharomachrus]]''|species=''Pharomachrus mocinno''|image=File:Quetzal01.jpg}} '''Quetzal''' (''Pharomachrus mocinno'') iku spesies [[manuk]] tropis gedhé saka kulawarga [[Trogonidae]] lan ordo [[Trogoniformes]]. Iku urip ing alas [[Amérikah Tengah|Amérika Tengah]]. Quetzal lanang dikenal duwe wulu buntut sing dawa banget, nganti siji meter. {{Stub}} [[Kategori:Manuk]] [[Kategori:Manuk Amérika Kidul]] a271mll39mty6nbp7g4nd24zsq2e4bw