Siyazi ukuthi amanzi anezimo ezintathu eziyisisekelo: okuqinile, uketshezi kanye negesi. Izinqubo zokushintsha isimo zibalulekile futhi akufanele zidideke. Kulokhu, sizokhuluma ngakho yini i-condensation kanye nokubaluleka enakho.
Ngenxa yalesi sizathu, kulesi sihloko sizohlola ukuthi kuyini ukufingqa, izici zayo, ukuthi kwenzeka kanjani kanye nokubaluleka kwakho.
yini i-condensation
I-Condensation inqubo yokuguqula isimo sendaba lapho izingxenye ezisesimweni segesi ziba uketshezi. Lena inqubo ehlehlayo yokuhwamuka, lapho izakhi ezisesimweni esiwuketshezi ziba igesi.
Ukujiya kwenzeka ngokwemvelo, nakuba futhi ingenziwa ngokwenziwa elabhorethri ngomshini okuthiwa i-condenser. Kumele kuqashelwe ukuthi phakathi nale nqubo, isici sishintsha isimo kuphela. Nokho, esikhundleni sokuba enye into, ihlala injalo, isimo sayo somzimba kuphela esishintshayo.
Le nqubo singayibona ezindaweni eziningi zokuphila kwethu kwansuku zonke, kungakhathaliseki ukuthi lapho senza imisebenzi efana nokugeza noma ukupheka ezindlini zethu, noma ngokwemvelo. Izimo ezithile zokushisa nengcindezi ziyadingeka ukuze inqubo yokufingqa yenzeke kanye nokushintshwa kwezinto ezisuka ku-gaseous kuya kweziwuketshezi.
Uma izimo zenzeka ezingcindezini eziseduze ne-ambient, kubizwa ngokuthi i-condensation yezokuthutha. Lapho le nqubo iphoqelelwa ngu ukusetshenziswa kwe-overpressure ephezulu, kubizwa ngokuthi i-liquefaction.
Ukujiya kwenzeka ngokwemvelo lapho igesi iphola ifika endaweni yawo yamazolo, ishintsha isuka esimweni esinegesi iye esimweni soketshezi. Lokhu kungafezwa futhi ngokushintsha ingcindezi kusici. Ukuze kufinyelelwe ukufingqa ngokwenziwa, kungenziwa kusetshenziswa ithuluzi elibizwa ngokuthi i-condenser, elisetshenziswa kakhulu ezinqubweni zezimboni noma zaselabhorethri.
ukujiya kwemvelo
Ukufingqa kuyinqubo yansuku zonke emvelweni. Lokhu kwenzeka futhi kulula ukukubona, ikakhulukazi ngezikhathi ezibandayo njengobusika noma amazinga okushisa aphansi. Isibonelo sokujiya emvelweni amazolo asekuseni.
Umhwamuko ujiya endaweni eyodwa kuphela, lapho izinga lokushisa elingaphezulu likhona ingaphansi kwezinga lokushisa lokugcwala kwengcindezi ekhona kusitimu. Phakathi nale nqubo, ama-molecule amanzi akhulula amandla ngendlela yokushisa, okunikeza umbono wokuthi izinga lokushisa lendawo liphakeme kunalokho eliyikho ngempela endaweni eshisa kakhulu futhi enomswakama.
Lokhu ngandlela-thile kukhohlisa isikhumba nomzimba wethu ekutholeni izinga lokushisa eliphakeme kunalelo elikhona endaweni ethile. Lokhu kubizwa ngokuthi ukuzwa ukushisa noma ukuzwa ukushisa.
Emvelweni, singabona inqubo yokufingqa ngezindlela ezihlukahlukene. Ku-biosphere, le nqubo yenzeka ikakhulukazi ngezikhathi zokwehla kwezinga lokushisa lomoya, futhi ibonakala kakhulu ngezikhathi zezulu ezifana namazolo asekuseni noma imvula. Kukhona ukuhlukahluka okubanzi futhi okuyingqayizivele kwamafomu e-condensation emvelweni.
Izinhlobo ze-condensation
Izinhlobo zokujiya ziyizinhlobo zezimo zezulu ezichazwa yizazi zezulu ngokususelwa kuzici zemvelo ezikhona endaweni ethile. Ezinye zazo zingabonakala ekuphileni kwansuku zonke zenza inqubo ezizikhiqizayo. Lezi zinhlobo ze-condensation zihlukaniswa kanje:
- Umusi: Umhwamuko uzojiya endaweni engaphezulu kuphela uma izinga lokushisa lendawo liphansi kunezinga lokushisa nokucindezela komhwamuko.
- Isithwathwa namazolo: Ebusuku kanye namazinga okushisa aphansi, singabona izimo ezimbili zokufingqa okwenzeka ngokwemvelo. Uma le nqubo yenziwa lapho izinga lokushisa elizungezile lidlula i-0 ° C, singabona amaconsi amancane amanzi: amazolo. Uma ukuminyana kwenzeka lapho izinga lokushisa lendawo lingaphansi kuka-0°C, sibona ungqimba oluncane lweqhwa elicwebezelayo: isithwathwa.
- I-Strata: I-strata yakheka ezindaweni ezinobude obuthile. Kuwungqimba olukhulu lwamafu olunombala ompunga ominyene kunenkungu futhi ovela endaweni enkulu.
- I-Nimbus: I-Nimbus iyifu elitholakala ezindaweni eziphakeme phakathi kwamamitha angu-800 no-1000 eliqukethe umswakama omningi ngakho-ke linombala omnyama. Bayimbangela yemvula.
- I-Cumulus: Amafu aphakathi kwamamitha angu-2000 kanye namamitha angu-6000 ukuphakama abizwa ngokuthi amafu e-cumulus. Zinombala omhlophe qwa futhi zinkulu. Ungayibona uma isimo sezulu sisihle.
- Amafu e-Cirrus: Amafu e-Cirrus amafu azacile kakhulu atholakala ngaphezu kwamamitha ayi-7.000 ngaphezu kwezinga lolwandle. Ukwakheka kwazo kuhlukile kwezinye ngoba zenziwe ngamakristalu eqhwa amahle kakhulu ngenxa yezinga eliphansi lokushisa ezilethwa ezindaweni eziphakeme lapho zivela khona, ngakho azinakho ukubunjwa kwe-liquid-gaseous ngokuphelele.
Izicelo zokufingqa
Ukufingqa kuyinqubo eyenzeka ngokwemvelo ngakho-ke ingasetshenziswa emikhakheni ehlukene. Okunye okubalulekile wukuthola amanzi ezindaweni ezomile ikakhulukazi noma ezomile ukuze kugcinwe umswakama enhlabathini kuleyo ndawo.
Izindlela ezinjengamachibi amazolo zisetshenziselwa lokhu. (embiwe phansi ukuze kuqoqwe amazolo), izinto zokuqeda inkungu nezinye izinhlelo zokuthola amanzi.
Eminingi yale misebenzi yenziwa ngokwesekwa yizinhlangano ezithile ezihlinzeka ngezeluleko nokuqeqeshwa kubahlali balezi zindawo ukuze kuqaliswe futhi kugcinwe lezi zinhlelo. I-Condensation nayo isetshenziswa emkhakheni wamazinyo. Phakathi kokunye ukusetshenziswa, I-silicone ejiyile ingasetshenziselwa ukubhaliswa kokulunywa kwesiguli. Yenziwa ngezinqubo eziningi zamakhemikhali, enye yazo ukufiphala kwegesi ye-ethanol.
Okunye ukusetshenziswa kwale nqubo kuyisisekelo emkhakheni wokukhishwa kweziphuzo ngamakhemikhali nasezilabhorethri zokufaka izicelo zezimboni.
Izimbangela zomswakama ngokufingqa
Lapho umhwamuko osemoyeni uhlangana nendawo ebandayo, kuyakha ukujiya, ngakho lo mhwamuko uphenduka ube uketshezi ngaphezulu. Ngokwesibonelo, lapho sizithela ingilazi yamanzi abandayo. izinga lokushisa lengilazi liyafana nezinga lokushisa lamanzi eliwaqukethe.
Sivame ukusho ukuthi ingilazi "iyajuluka", nakuba lokhu kungenakwenzeka ngoba ukujuluka kuyinqubo yokupholisa eyenzeka emzimbeni noma ezindaweni ezinama-porous ezifana nesikhumba sethu. Amakristalu awanawo ama-pores esakhiweni sawo. Eqinisweni, lokho okubizwa ngokuthi "umjuluko" umswakama okhiqizwa ngenxa yokufingqa, ngoba umhwamuko okhona endaweni uhlangana nendawo eyiqhwa yengilazi, uyimanzise..
Ezindlini nasezindaweni ezivaliwe, umswakama ojiyile uzibonakalisa ezindaweni ezahlukahlukene ngenxa yokuthi izinga lokushisa lasendlini kulezi zindawo lingaphezulu kwezinga lokushisa langaphandle. Ingabonakala ophahleni nophahla, izindonga, ingilazi namafasitela, ikakhulukazi lapho ibekwe obala noma ezindaweni ezibandayo.
Imisebenzi yabantu yansuku zonke kanye nokungangeni kahle komoya endaweni yasendlini kungenye yezimbangela eziyinhloko zomswakama. Phekela ngaphakathi, ugeze, womise izingubo futhi ufudumale futhi ukhulume.
Lezi zenzo zidala isitimu, futhi isitimu esisidalayo sihamba emoyeni siye endaweni lapho sihlala khona endaweni epholile, evame ukuvezwa indawo efana nosilingi, amawindi, noma izindonga. Nakuba kungewona umsebenzi kuphela noma izici zomuntu ezingadala umswakama ngokujiya, amaphutha noma izinkinga ezakhiweni zezindlu zethu noma indawo yangaphakathi nakho kungakwandisa.
Ngithemba ukuthi ngalolu lwazi ungafunda kabanzi mayelana nokuthi kuyini ukufiphala kanye nezici zayo.