Abin da ke faruwa a Geyser

Lamarin Geyser yana nufin abin da ke faruwa sakamakon fashewar ruwa da ke haifar da cryogenic da ake jigilar shi ta hanyar bututun dogon tsaye (yana nufin rabon tsayi-diamita ya kai wani ƙima) saboda kumfa da tururin ruwa ya samar, kuma polymerization tsakanin kumfa zai faru tare da ƙaruwar kumfa, kuma a ƙarshe za a juya ruwan cryogenic daga ƙofar bututun.

Geysers na iya faruwa ne lokacin da yawan kwararar ruwa a cikin bututun ya yi ƙasa, amma ya kamata a lura da su ne kawai lokacin da kwararar ruwa ta tsaya.

Lokacin da ruwa mai hana ruwa gudu ya sauka a cikin bututun tsaye, yana kama da tsarin sanyaya. Ruwan mai hana ruwa gudu zai tafasa ya kuma yi tururi saboda zafi, wanda ya bambanta da tsarin sanyaya ruwa! Duk da haka, zafi galibi yana fitowa ne daga ƙaramin mamayewar zafi na yanayi, maimakon babban ƙarfin dumama tsarin a cikin tsarin sanyaya ruwa. Saboda haka, layin iyaka na ruwa mai zafin jiki mai zafi yana samuwa kusa da bangon bututu, maimakon fim ɗin tururi. Lokacin da ruwan ke gudana a cikin bututun tsaye, saboda mamayewar zafi na muhalli, yawan zafin da ke cikin layin iyaka na ruwa kusa da bangon bututu yana raguwa. A ƙarƙashin aikin buoyancy, ruwan zai juya kwararar sama, yana samar da layin iyaka na ruwan zafi, yayin da ruwan sanyi a tsakiya ke gudana ƙasa, yana samar da tasirin convection tsakanin su biyun. Layin iyaka na ruwan zafi yana kauri a hankali tare da alkiblar babban har sai ya toshe ruwan tsakiya gaba ɗaya kuma ya dakatar da convection. Bayan haka, saboda babu convection don ɗaukar zafi, zafin ruwan a yankin zafi yana tashi da sauri. Bayan zafin ruwan ya kai zafin da ke cikewa, sai ya fara tafasa ya kuma samar da kumfa. Bam ɗin iskar gas na zingle yana rage yawan kumfa.

Saboda kasancewar kumfa a cikin bututun tsaye, amsawar ƙarfin ƙurar da ke cikin kumfa zai rage matsin lamba mai tsauri a ƙasan kumfa, wanda hakan zai sa sauran ruwan ya yi zafi sosai, don haka yana samar da ƙarin tururi, wanda hakan zai sa matsin lamba mai tsauri ya ragu, don haka haɓaka juna, zuwa wani mataki, zai samar da tururi mai yawa. Abin da ke faruwa na geyser, wanda yake kama da fashewa, yana faruwa ne lokacin da ruwa, ɗauke da walƙiyar tururi, ya sake fitowa cikin bututun. Wani adadin tururi da ke biyo baya tare da fitar da ruwa zuwa sararin sama na tankin zai haifar da canje-canje masu ban mamaki a cikin zafin jiki na sararin tankin, wanda ke haifar da canje-canje masu ban mamaki a cikin matsin lamba. Lokacin da canjin matsin lamba ya kasance a cikin kololuwa da kwarin matsin lamba, yana yiwuwa a sanya tankin cikin yanayin matsin lamba mara kyau. Tasirin bambancin matsin lamba zai haifar da lalacewar tsarin.

Bayan fashewar tururin, matsin lamba a cikin bututun yana raguwa da sauri, kuma ana sake saka ruwan cryogenic a cikin bututun tsaye saboda tasirin nauyi. Ruwan mai saurin gudu zai haifar da girgizar matsin lamba kamar guduma ruwa, wanda ke da babban tasiri ga tsarin, musamman akan kayan aikin sararin samaniya.

Domin kawar ko rage illar da abin da ke faruwa a geyser ke haifarwa, a gefe guda, ya kamata mu kula da tsarin rufe bututun, domin mamayewar zafi shine tushen abin da ke faruwa a geyser; A gefe guda kuma, ana iya nazarin tsare-tsare da dama: allurar iskar gas mara narkewa, ƙarin allurar ruwa mai narkewa da bututun zagayawa. Ma'anar waɗannan tsare-tsaren shine a canja wurin zafin ruwan da ya wuce kima, a guji taruwar zafi mai yawa, don hana faruwar abin da ke faruwa a geyser.

Ga tsarin allurar iskar gas mai inert, yawanci ana amfani da helium azaman iskar gas mai inert, kuma ana allurar helium a ƙasan bututun. Bambancin matsin lamba tsakanin ruwa da helium za a iya amfani da shi don yin canja wurin tururin samfurin daga ruwa zuwa taro na helium, don tururi wani ɓangare na ruwa mai cryogenic, sha zafi daga ruwa mai cryogenic, da kuma samar da tasirin sanyaya sama, don haka hana taruwar zafi mai yawa. Ana amfani da wannan tsarin a wasu tsarin cike gurɓataccen iska. Ciko na ƙarin shine don rage zafin ruwan cryogenic ta hanyar ƙara ruwa mai cryogenic mai sanyi sosai, yayin da tsarin ƙara bututun zagayawa shine don kafa yanayin zagayawa na halitta tsakanin bututun da tanki ta hanyar ƙara bututun, don canja wurin zafi mai yawa a yankunan gida da lalata yanayin samar da geysers.

Ku biyo mu a labarin na gaba don wasu tambayoyi!

Kayan Aikin HL Cryogenic

Kamfanin HL Cryogenic Equipment wanda aka kafa a shekarar 1992, wani kamfani ne da ke da alaƙa da Kamfanin HL Cryogenic Equipment Company. Kamfanin HL Cryogenic Equipment ya himmatu wajen ƙira da ƙera Tsarin Bututun Tsabtace ...

Jerin samfuran bututun Vacuum Jacketed Pipe, Vacuum Jacketed Hose, Vacuum Jacketed Valve, da Phase Separator a Kamfanin Kayan Aikin HL Cryogenic, waɗanda suka wuce ta cikin jerin hanyoyin magance fasaha masu tsauri, ana amfani da su don canja wurin iskar oxygen mai ruwa, nitrogen mai ruwa, argon mai ruwa, hydrogen mai ruwa, helium mai ruwa, LEG da LNG, kuma ana ba da sabis ga waɗannan samfuran don kayan aikin cryogenic (misali tankunan cryogenic, dewars da akwatunan sanyi da sauransu) a cikin masana'antar rabuwar iska, iskar gas, jiragen sama, kayan lantarki, superconductor, kwakwalwan kwamfuta, haɗa kai ta atomatik, abinci da abin sha, kantin magani, asibiti, biobank, roba, sabbin injinan sinadarai na kera kayan aiki, ƙarfe da ƙarfe, da binciken kimiyya da sauransu.