yintoni i-condensation

yintoni i-condensation

Siyazi ukuba amanzi aneendawo ezintathu ezisisiseko: okuqinileyo, ulwelo kunye negesi. Iinkqubo zokutshintsha kombuso zibalulekile kwaye akufanele zibhideke. Kule meko, siza kuthetha ngayo yintoni i-condensation nokubaluleka enako.

Ngenxa yesi sizathu, kweli nqaku siza kuhlolisisa ukuba yintoni i-condensation, iimpawu zayo, ukuba kwenzeka njani kunye nokubaluleka kwayo.

yintoni i-condensation

ukufuma ngokujiya

Icondensation yinkqubo yokutshintsha imeko apho amalungu akwimeko yegesi abe lulwelo. Le yinkqubo ebuyela umva yokwenziwa ngumphunga, apho izinto ezikwimeko yolwelo ziba yigesi.

Ukujiya kwenzeka ngokwemvelo, nangona kunjalo inokwenziwa ngokwenziwa kwilabhoratri ngesixhobo esibizwa ngokuba yicondenser. Kufuneka kuqatshelwe ukuba ngexesha le nkqubo, into etshintsha kuphela isimo. Nangona kunjalo, endaweni yokuba ibe yenye into, ihlala injalo, kuphela imeko yayo yenyama eguqukayo.

Le nkqubo sinokuyibona kwiindawo ezininzi zobomi bethu bemihla ngemihla, nokuba kuxa sisenza imisebenzi efana nokuhlamba okanye ukupheka emakhayeni ethu, okanye kwindalo. Iimeko ezithile zobushushu kunye noxinzelelo ziyimfuneko ukuze inkqubo yokudibanisa yenzeke kunye nokutshintshwa kwezinto ezivela kwizinto zegesi ukuya kwizinto zolwelo.

Xa iimeko zisenzeka kuxinzelelo olukufutshane ne-ambient, ibizwa ngokuba yi-transit condensation. Xa le nkqubo inyanzeliswa ngu ukusetyenziswa koxinzelelo oluphezulu, kubizwa ngokuba yi-liquefaction.

Ukujiya kwenzeka ngokwendalo xa irhasi iphola iye kutsho kumbethe, itshintsha ukusuka kwimo yerhasi ukuya kulwelo. Oku kunokufezekiswa ngokutshintsha uxinzelelo kwi element. Ukufezekisa i-condensation eyenziweyo, inokwenziwa ngokusebenzisa isixhobo esibizwa ngokuba yi-condenser, esetyenziswa ngokubanzi kwiinkqubo zoshishino okanye iibhubhoratri.

ukujiya kwendalo

I-Condensation yinkqubo yemihla ngemihla kwindalo. Oku kuyenzeka kwaye kulula ukukubona, ngakumbi ngamaxesha abandayo afana nobusika okanye amaqondo obushushu aphantsi. Umzekelo wokujiya kwindalo ngumbethe wasekuseni.

Umphunga wamanzi ujiya kuphela kumphezulu omnye, apho ubushushu bomphezulu ingaphantsi kobushushu bobushushu boxinzelelo olukhoyo kumphunga. Ebudeni bale nkqubo, iimolekyuli zamanzi zikhupha amandla ngendlela yobushushu, nto leyo enika ingcamango yokuba ubushushu be-ambient buphezulu kunokuba bunjalo ngokwenene kwindawo eshushu kakhulu nefumileyo.

Oku ngandlela thile kuqhatha ulusu kunye nomzimba wethu ekufumaneni ubushushu obuphezulu kunoko bukhoyo kwindawo ethile. Oku kubizwa ngokuba kukuva ubushushu okanye bubushushu.

Kwindalo, sinokubona inkqubo yokudibanisa ngeendlela ezahlukeneyo. Kwi-biosphere, le nkqubo yenzeka kakhulu ngamaxesha okuhla kweqondo lobushushu le-atmospheric, kwaye ibonakala kakhulu ngexesha lemozulu efana nombethe wasekuseni okanye imvula. Kukho ukuhlukahluka okubanzi kunye okukhethekileyo kweefom ze-condensation kwindalo.

Iintlobo zokuxinana

yintoni i-condensation ekhaya

Iintlobo zokujiya ziindidi zemozulu ethi izazinzulu zemozulu zizichaza ngokusekelwe kwiimpawu zendalo ezikhoyo kwindawo ethile. Ezinye zazo zinokubonwa kubomi bemihla ngemihla ziqhuba inkqubo ezivelisayo. Ezi ntlobo ze-condensation zihlelwa ngolu hlobo lulandelayo:

  • Umphunga: Umphunga uya kuxinana kumphezulu kuphela ukuba ubushushu bomphezulu bungaphantsi kobushushu kunye noxinzelelo lomphunga.
  • Iqabaka kunye nombethe: Ebusuku kunye namaqondo obushushu aphantsi, sinokubona iimeko ezimbini zokujiya okwenzeka ngokwemvelo. Xa le nkqubo iqhutyelwa xa ubushushu be-ambient budlula i-0 ° C, sinokubona amaconsi amancinci amanzi: amazolo. Ukuba i-condensation yenzeke xa ubushushu be-ambient bungaphantsi kwe-0 ° C, sibona umaleko omncinci we-crystalline ice: iqabaka.
  • Strata: I-strata yenziwe kwiindawo ezinobude obuthile. Ngumaleko omkhulu wamafu one-tint engwevu exineneyo kunenkungu kwaye ibonakala kwindawo enkulu.
  • I-Nimbus: I-Nimbus lilifu elifumaneka kwiindawo eziphakamileyo phakathi kwe-800 kunye ne-1000 yeemitha eziqulethe ubuninzi bokufuma kwaye ngoko umbala omnyama. Bangunobangela wemvula.
  • Cumulus: Amafu aphakathi kwe-2000 yeemitha kunye ne-6000 yeemitha ukuphakama abizwa ngokuba ngamafu e-cumulus. Zine-tint emhlophe kakhulu kwaye zinkulu. Ungayibona xa imozulu intle.
  • Amafu e-Cirrus: Amafu e-Cirrus ngamafu amancinci kakhulu abekwe ngaphezu kwe-7.000 yeemitha ngaphezu komphakamo wolwandle. Ukwakheka kwazo kwahlukile kwezinye ngenxa yokuba zenziwe ngeekristale ezintle kakhulu zomkhenkce ngenxa yobushushu obuphantsi obukhoyo kwiindawo eziphakamileyo apho zivela khona, ngoko ke azinayo i-liquid-gaseous composition ngokupheleleyo.

Usetyenziso lwe-Condensation

umjikelo wamanzi

I-condensation yinkqubo eyenzeka ngokwemvelo kwaye ngoko inokusetyenziswa kwiindawo ezahlukeneyo. Enye yezona zinto ziphambili kukufumana amanzi kwiindawo ezomileyo ngakumbi okanye ezomileyo ukugcina ukufuma kumhlaba wakuloo ndawo.

Iinkqubo ezifana namachibi ombethe zisetyenziselwa oku. (embiwe emhlabeni ukuvumela ukufumba kombethe), izinto zokuphelisa inkungu kunye nezinye iinkqubo zokufumana amanzi.

Uninzi lwale misebenzi lwenziwa ngenkxaso yemibutho ethile enika iingcebiso kunye noqeqesho kubahlali bale mimandla ukuphumeza nokugcina ezi nkqubo. I-condensation iyasetyenziswa nakwintsimi yamazinyo. Phakathi kwezinye izinto ezisetyenziswayo, I-silicone ejikisiweyo ingasetyenziselwa ukubhaliswa kwesigulane. Yenziwa ngenani leenkqubo zeekhemikhali, enye yazo yi-condensation yegesi ye-ethanol.

Olunye usetyenziso lwale nkqubo lubalulekile kwinkalo ye-chemical distillation nakwiilabhoratri zokusetyenziswa kwemizi-mveliso.

Iimbangela zokufuma ngokujiya

Xa umphunga wamanzi usemoyeni udibana nomhlaba obandayo, ukujiya kuyabumba, ukuze lo mphunga ujike ube lulwelo ngaphezulu. Umzekelo, xa sizigalela iglasi yamanzi abandayo. ubushushu beglasi buyafana nobushushu bamanzi ekuwo.

Ngokuqhelekileyo sithetha ukuba iglasi "iyabila", nangona oku kungenakwenzeka kuba ukubila yinkqubo yokupholisa eyenzeka emzimbeni okanye kwiindawo ezinamaqhekeza afana nolusu lwethu. Iicrystals azinayo imingxuma kwisakhiwo sazo. Enyanisweni, into ebizwa ngokuba "ngumbilo" kukufuma okuveliswa ngenxa yokuxinana, kuba umphunga wamanzi okhoyo kwindawo udibana nomphezulu onomkhenkce weglasi, uwunyakamise..

Ezindlini nakwiindawo ezivaliweyo, ukufuma okujiyileyo kuzibonakalisa kwiindawo ezahlukeneyo kuba ubushushu bangaphakathi kwezi ndawo buphezulu kunobushushu bangaphandle. Inokubonwa kwiisilingi kunye neesilingi, iindonga, iiglasi kunye neefestile, ngakumbi apho ibekwe elubala okanye kwindawo ebandayo.

Imisebenzi yabantu yemihla ngemihla kunye nokungenwa komoya okungahambi kakuhle kwiindawo zangaphakathi yenye yezona zinto zibangela ukufuma. Phekela ngaphakathi, uhlambe, womise iimpahla kwaye ufudumale kwaye uthethe.

Ezi ntshukumo zidala umphunga, kwaye umphunga esiwudalayo uhamba emoyeni ukuya kwindawo yokuhluma apho uhlala kwindawo epholileyo, ehlala ityhilekile imiphezulu efana neesilingi, iifestile, okanye iindonga. Ngelixa ingeyiyo kuphela into eyenziwayo okanye imiba yabantu enokudala ukufuma ngokuxinana, iimpazamo okanye iingxaki kulwakhiwo lwezindlu zethu okanye okusingqongileyo kwangaphakathi nako kunokuwenza mandundu.

Ndiyathemba ukuba ngolu lwazi unokufunda ngakumbi malunga nokuba yintoni i-condensation kunye neempawu zayo.


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