Izinga lomswakama elikhona emkhathini linganqunywa ngokukala umhwamuko wamanzi. Umswakama ohlobene, ngakolunye uhlangothi, ulinganisa ingxenye yamanzi asemoyeni maqondana nomthamo omkhulu womhwamuko wamanzi. Njengoba izinga lokushisa likhuphuka, umoya unamandla okugcina inani elikhulu lomhwamuko wamanzi. Uma kukhulunywa ngesimo sezulu, uhlobo oluthile lokuswakama okukhulunywa ngalo umswakama olinganiselwe.
Yini umswakama
Ukuba khona komhwamuko wamanzi emoyeni kunomthelela ngokwemvelo kumswakama, okuwuphawu lwemvelo lomkhathi. Ubuso bomhlaba, okuhlanganisa amachibi, izilwandle, nolwandle, kukhiphela umhwamuko wamanzi emkhathini ngenqubo yokuhwamuka.
Isici esiphawulekayo phakathi kwazo umkhathi omkhulu wolwandle, oqukethe ama-97% amangalisayo wamanzi aphelele eMhlabeni. Umjikelezo we-hydrological uncike kumswakama, njengoba umhwamuko ukhiqizwa njalo ngokuhwamuka bese ukhishwa ngokujiya. Njengoba amazinga okushisa enyuka, umoya unamandla okugcina inani elikhulu lomhwamuko wamanzi. Lokhu kusho ukuthi ezindaweni ezifudumele, amazinga omswakama angafinyelela amaphuzu aphezulu.
Ukuthi umswakama uhluka kanjani nezinga lokushisa
Umthelela wezinga lokushisa kumazinga womswakamo wasendlini ungabonakala ngesibonelo sokugcwala komoya. Ku-30°C, i-cubic meter eyodwa yomoya ominyene ingaqukatha amagremu angu-28 amanzi.. Nokho, uma izinga lokushisa lehla liye ku-8°C, amandla ehla abe amagremu angu-8 kuphela.
Umoya oshisayo unokubekezelela okuphezulu umswakama uma kuqhathaniswa nomoya obandayo. Indima yamazinga okushisa ekulawuleni amazinga okuswakama ibalulekile, ikakhulukazi uma sicabangela ukuthi isikhathi sethu esiningi sisichitha sisendlini. Ngokwesibonelo, ake sicabangele usuku lwasebusika. Umoya wangaphandle ungaba nomswakama ohlobene ongu-100% ku-5°C, ocishe ulingane namagremu angu-6,8 wamanzi. Nokho, eyodwa izinga lokushisa elingu-5°C ezindaweni ezivaliwe lingase lingakhululeki, ngakho-ke kuyadingeka ukulikhulisa. Njengoba umoya wangaphandle ungena endaweni engaphakathi endlini futhi ufudumala ufike ku-23 ° C, inani eliphelele lamanzi emoyeni lihlala lingashintshile. Kodwa-ke, ngenxa yomthamo omkhulu wokubamba amanzi womoya oshisayo, umswakama ohlobene wehla ufike ku-33%.
Kubalulekile ukucabangela ukuthi umoya oshisayo unokubekezelela okukhulu umswakama uma kuqhathaniswa nomoya obandayo. Isibonelo, phakathi nehlobo elishisayo, elinomswakama lapho umswakama ungama-80% futhi izinga lokushisa lingu-30°C, umoya wangaphandle ungaqukatha ama-24 amagremu/m3 wamanzi. Ezindlini zethu, izinga lokushisa elingu-30 ° C lingase lingakhululeki, ngakho-ke kuyadingeka ukusebenzisa isimo somoya ukuze wehlise. Nokho, Uma lo moya upholiswe ezingeni lokushisa elingaphansi kuka-26°C, Umswakama ohlobene uzofinyelela ku-100% futhi amanzi azoncipha, okuholela ekwakhekeni kwamazolo. Ngenxa yalesi sizathu, izinhlelo zokupholisa umoya ngokuvamile zihlanganisa i-dehumidifier. Ngaphandle kwale divayisi, izindonga zendlu yakho beziyogcwala umswakama ngokuphelele ehlobo.
Lapho umswakama ohlobene ufinyelela ku-100%, Kusho ukuthi umkhathi ugcwele umhwamuko wamanzi ngokuphelele.. Ngenxa yalokho, umoya awukwazi ukugcina umswakama owengeziwe, okuholela ekwakhekeni kwemvula.
Isimo sezulu sinesibopho sokushintshashintsha kwamazinga omswakamo. Ezindaweni ezibandayo, kuvamile ukuthola amazinga omswakama aphansi uma kuqhathaniswa nezimo zezulu ezifudumele. Lokhu kungenxa yokuthi umoya obandayo awukwazi ukubamba umswakama omningi njengowomoya ofudumele. Ngaphezu kwalokho, umswakama uvame ukwehla phakathi nenkathi yasebusika. Kunalokho, phakathi nezinyanga zasehlobo, amazinga omswakamo ayanda njengoba umoya unamandla okugcina umhwamuko omningi wamanzi ngokukhuphuka kwamazinga okushisa. Ukuze uthole ulwazi olwengeziwe lokuthi kanjani ukuthi umswakama uhluka kanjani nezinga lokushisa nezimo zomkhathi, ungathintana nesigaba sethu esinikezelwe kumswakama.
Umswakama wasendlini
Amazinga womswakamo wasendlini angathinteka ngisho nayimisebenzi emincane yansuku zonke. Izenzo ezehlukene esizenzayo ngaphakathi kwamakhaya ethu, njengokupheka, ukuhlanza, ukuwasha izitsha, ukuphefumula, ukuwasha, nokugeza, kunamandla okunyusa amazinga womswakamo. Ukugcina amazinga womswakamo angaphakathi endlini ebangeni elingama-30 kuya ku-60% kubalulekile ukuze kuqinisekiswe indawo enempilo.
Ukuba khona kokuswakama kanye nesikhunta ezindlini kunomthelela cishe ku-21% wesibalo sezifo zesifuba somoya minyaka yonke, okulinganiselwa ezigidini ezingama-21,8. Izimo ezifanele zokukhula kwebhaktheriya kanye nokwakheka kwesikhunta zidalwa amazinga aphezulu omswakama. Umswakama owedlulele ngaphakathi kwezakhiwo ungabangelwa izici eziningana, njengokuvuza, ukungena kwamanzi emvula ngamafasitela nangaphansi, noma ngisho nokukhuphuka okungokwemvelo komswakama ovela ezitezi eziphansi zesakhiwo. Izifo zokuphefumula njengesifuba somoya, i-allergies nezinye izifo ezihlobene nazo.
Kanye umswakama udlula umkhawulo onconywayo ongu-50%, umoya uqala ukuthatha ikhwalithi esindayo, enomswakama. Ukwenyuka okwengeziwe ngale kwaleli phuzu kungaholela ezinkingeni ezihlukahlukene. Izidalwa ezincane ezaziwa ngokuthi izibungu zothuli ziyimbangela yokungezwani komzimba nezinto eziningi kanye nezinkinga zokuphefumula.
Kuyathakazelisa ukuqaphela ukuthi izimbuzane zithembele kakhulu kumswakama womoya ukuze ziphile. Lezi zilwane ezincane ziphila kahle endaweni enamazinga okushisa aphakathi nendawo nomswakama ophezulu, njengoba kuzivumela ukuba zimunce amanzi. Ngakho-ke, izindawo ezinomswakama ophezulu zinikeza izimo ezifanele zokuhluma kwezimbuzane. Kubalulekile ukuqaphela ukuthi lezi zinambuzane ezincane zingabhebhethekisa ukungezwani komzimba nesifuba somoya, okugcizelela ukubaluleka kokugcina amazinga omswakamo asezingeni eliphezulu ezindlini zethu. Ngokwenza kanjalo, singanciphisa ngempumelelo ukuba khona kwezibungu futhi sinciphise imiphumela emibi enayo empilweni yethu.
