1.Isizukulwane sombani Umbani yinto ye-atmospheric photoelectric ekhiqizwa esimweni sezulu esinamandla. Ukubaneka kombani okunamandla okuhambisana nokukhipha amashaji kagesi ahlukahlukene efwini, phakathi kwamafu noma phakathi kwamafu nomhlaba kuyadonsana futhi kubizwa ngokuthi umbani, futhi umsindo wegesi okhula ngokushesha eduze nomgudu wombani yilokho abantu abakubiza ngokuthi ukuduma. Ngokuvumelana nezakhiwo zokushaja zokunyanyiswa kwabantu bobulili obufanayo kanye nokukhangwa kwabobulili obuhlukile, lapho amandla enkambu kagesi phakathi kwamabhulokhi amafu ngamashaja abobulili obuhlukile noma phakathi kwamabhulokhi wamafu nomhlaba akhuphuka aze afike ezingeni elithile (cishe 25-30 kV/cm) , izodiliza umoya futhi ikhiqize ukukhanya kwe-arc okunamandla Ukukhipha, lokhu yilokho esivame ukukubiza ngokuthi umbani. Ngesikhathi esifanayo, umoya esiteshini sokukhipha ushiswa ekushiseni okuphezulu (kufika ku-20,000 degrees) futhi ukhula ngokushesha ngenxa yomphumela oshisayo owenziwe umbane onamandla, okwenza umsindo wokuqhuma oqinile, okudumayo. Umbani nokuduma kubizwa ngokuthi izenzakalo zombani. 2. Ukuhlukaniswa nomphumela olimazayo wombani Umbani uhlukaniswe waba umbani oqondile, umbani wokungeniswa kanye nombani oyindilinga. Sekuyisikhathi eside ukuduma nombani kulethe imivimbo eyinhlekelele kubantu, izidalwa ezisemhlabeni kanye nempucuko yabantu ngendlela yokushaya kombani oqondile. Izinhlekelele ezinjengokulimala nokucekelwa phansi kwezakhiwo zivame ukubangelwa. 3, isimiso sokuvikela umbani Esimeni sezulu sokuduma kwezulu, ngezinye izikhathi sibona izihlahla ezinde ziwiswa umbani, kuyilapho ezinye izakhiwo ezizungezile eziphakeme njengemibhoshongo nezakhiwo eziphakeme ziphephile futhi ziphilile. Siyini isizathu salokhu? Lezi zihlahla eziphakeme nazo zikhokhiswa inani elikhulu lokushaja kagesi ngenxa yokungeniswa kongqimba lwamafu ngenani elikhulu lokushaja kagesi. Uma ishaja kagesi eqoqiwe isiningi kakhulu, isihlahla sizowiswa phansi. Ngaphansi kwezimo ezifanayo, ukuphepha kwezakhiwo eziphakeme kungase kuthiwe yizinduku zombani. Emibhoshongweni eminingi, kunento eyenziwe ngensimbi, emise okwenaliti efekethisiwe, futhi inaliti iqondile. Induku yombani lena. Ngakho-ke, kungani le nto ebukeka njengenaliti yokufekethisa futhi engamangalisa ngokubukeka inomphumela omuhle kangaka futhi "ingagwema umbani"? Eqinisweni, induku yombani kufanele ibizwe ngokuthi "induku yombani". Esimeni sezulu sokuduma kwezulu, lapho amafu anamandla avela phezu kwezakhiwo ezinde, kokubili induku yombani nesiphezulu sezakhiwo ezinde kubangelwa inani elikhulu lokushaja, futhi umoya phakathi kwenduku yombani namafu uphuka kalula bese uba umqhubi. . Ngale ndlela, ungqimba lwamafu olushajiwe lwakha indlela ngenduku yombani, futhi induku yombani iphansi. Induku yombani ingaqondisa ukushaja kwefu emhlabeni, ukuze ingabi yingozi ezakhiweni eziphakeme futhi iqinisekise ukuphepha kwayo. Ukuvikelwa kombani okuphelele kuhlukaniswe ngokuvikela umbani wangaphandle kanye nokuvikela umbani wangaphakathi. Ukuvikela umbani wangaphandle ngokuyinhloko ukuvimbela ukushaya kombani oqondile, futhi ukuvikela umbani wangaphakathi ngokuyinhloko ukuvimbela umbani wokungeniswa.

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Isikhathi sokuthunyelwe: May-07-2022