Iinzuzo zombane ebantwiniXa kuthethwa ngombane, abantu bazi ngakumbi ngeentlekele ezibangelwa ngumbane kubomi nakwimpahla yabantu. Ngenxa yesi sizathu, abantu aboyiki kuphela umbane, kodwa baphapheme kakhulu. Ngoko ukongezelela ekubangeleni iintlekele ebantwini, ngaba usazi ukuba iindudumo nemibane? Kuthekani ngeenzuzo ezinqabileyo zombane. Umbane nawo uneemfanelo zawo ezingacimekiyo ebantwini, kodwa asazi ngokwaneleyo ngawo. Umsebenzi wendudumo kunye nombane sisipho esingenaxabiso esivela kwindalo esiya ebantwini.Umbane uvelisa umlilo, oxhokonxa ukuqonda komntu nokusebenza komliloUmbane ubetha ihlathi ngokuphindaphindiweyo, ubangela imililo, kwaye imizimba yezilwanyana ezitshiswa ngomlilo ngokucacileyo inencasa ngakumbi kunezilwanyana ezikrwada, nto leyo eyaphefumlela ngokufanelekileyo ukuqonda nokusetyenziswa komlilo ngookhokho abangabantu. Ibutho labantu laqalisa ukutya ukutya okuphekiweyo okutyebileyo kangangexesha elide. Iphucula uphuhliso lwengqondo yomntu kunye nezihlunu, yandisa ubomi bomntu, kwaye ikhuthaza uphuhliso lwempucuko yabantu.Umbane unokuxela kwangaphambili imozulu.Abantu banamava amaninzi okusebenzisa iindudumo nemibane ukuqikelela utshintsho lwemozulu. Ngokomzekelo, ukuba ubona umbane entshona okanye emantla, ilifu lendudumo elavelisa umbane lisenokufudukela kummandla wasekuhlaleni ngokukhawuleza; ukuba kukho umbane empuma okanye ngasezantsi, kubonisa ukuba ilifu lendudumo lihambile kwaye imozulu yendawo iya kuphucula.Ukuvelisa i-oxygen ion negative, uhlambulule indawo ye-atmosphericUmbane unokuvelisa iiyoni zeoksijini ezingakhiyo. Ii-ion zeoksijini ezingalunganga, ezaziwa ngokuba ziivithamini zomoya, zinokucolisa kwaye zicoce umoya. Emva kwesiphango, ukuxinana okuphezulu kwee-ion zeoksijini ezingalunganga emoyeni kwenza umoya uhlaziyeke ngokungaqhelekanga kwaye abantu bazive bekhululekile kwaye bonwabile. Iimvavanyo zibonise ukuba i-ion ye-oksijini engalunganga, ebizwa ngokuthi "iivithamini zomoya", ziluncedo kakhulu kwimpilo yabantu. Xa umbane usenzeka, isenzo esinamandla sefotochemical siya kubangela ukuba inxalenye yeoksijini esemoyeni isabele ukuvelisa i-ozone nge-bleaching kunye ne-sterilizing effects. Emva kwesiphango, iqondo lobushushu liyehla, i-ozone esemoyeni iyanda, namathontsi emvula akhukulise uthuli olusemoyeni, abantu baya kuva umoya uhlaziyeke ngendlela engaqhelekanga. Esinye isizathu esibangela ukuba umbane ucoce imo engqongileyo yomoya okufuphi kumphezulu kukuba unako ukusasaza izinto ezingcolisa umoya. Uhlaziyo olukhatshwa ngumbane lunokuzisa umoya ongcolileyo ukuba umile ngaphantsi kwetroposphere ukuya kumphakamo ongaphezu kweekhilomitha ezili-10.Ukwenziwa kwezichumiso zenitrogenEyona nto ibaluleke kakhulu kaRaiden kukwenza isichumiso senitrogen. Inkqubo yombane ayinakwahlulwa kumbane. Ubushushu bombane buphakame kakhulu, ngokuqhelekileyo bungaphezulu kwama-30,000 degrees celcius, nto leyo ebuphinda kahlanu ubushushu bomhlaba welanga. Umbane nawo ubangela amandla ombane aphezulu. Ngaphantsi kobushushu obuphezulu kunye neemeko zombane ophezulu, iimolekyuli zomoya ziya kuba yi-ionized, kwaye xa ziphinda zidibanisa, i-nitrogen kunye ne-oksijini kuzo ziya kudibaniswa zibe yi-nitrite kunye ne-nitrate iialekyuli, eziya kunyibilika emanzini emvula kunye nomhlaba emhlabeni ukuba ube ngumanyolo we-nitrogen wendalo. Kuqikelelwa ukuba kukho i-400 yezigidi zeetoni zesichumiso senitrogen eziwela emhlabeni ngenxa yombane wodwa minyaka le. Ukuba zonke ezi zichumisi zenitrogen ziwela emhlabeni, kufana nokugalela malunga neekhilogram ezimbini zesichumiso senitrogen kwimu nganye yomhlaba, elingana neekhilogram ezilishumi zeammonium sulfate.Ukukhuthaza ukukhula kwebhayolojiUmbane unokukhuthaza ukukhula kwebhayoloji. Xa umbane usenzeka, amandla ebala lombane emhlabeni nasesibhakabhakeni anokufikelela ngaphezu kweshumi lamawaka evolthi ngesentimitha. Ukuchatshazelwa ngumahluko onjalo onamandla, iphotosynthesis kunye nokuphefumla kwezityalo kuyaphuculwa. Ke ngoko, ukukhula kwezityalo kunye nemetabolism yomelele ngakumbi phakathi kweentsuku ezimbini ukuya kweyesiphango. Abanye abantu bavuselela izityalo ngombane, kwaye bafumanisa ukuba i-peas i-branched ngaphambili, kwaye inani lamasebe landa, kwaye ixesha leentyantyambo laliyisiqingatha senyanga ngaphambili; umbona obukhwelwe kwiintsuku ezisixhenxe ngaphambili; kwaye ikhaphetshu inyuke nge-15% ukuya kwi-20%. Ayisiyiyo loo nto kuphela, ukuba kukho iindudumo ezintlanu ukuya kwezintandathu ngexesha lokukhula kwesityalo, ukuvuthwa kwaso kuya kuqhubela phambili malunga neveki.amandla angenalungcolisekoUmbane ngumthombo wamandla ongangcolisi. Iyakwazi ukukhupha i-1 ukuya kwi-1 yeebhiliyoni ze-joules ngexesha, kwaye izifundo ziqinisekisile ukuba ukukhankanya ngokuthe ngqo i-pulse yangoku kumbane kunokuvelisa amandla empembelelo amakhulu amawaka amaxesha oxinzelelo lwe-atmospheric. Ukusebenzisa le mpembelelo inkulu, umhlaba othambileyo unokudityaniswa, ngaloo ndlela ulondoloze amandla amaninzi kwiiprojekthi zokwakha. Ngokomgaqo wokufudumeza kwe-high-frequency induction, ubushushu obuphezulu obuveliswa ngumbane bunokwenza amanzi asematyeni ande ukuze afezekise injongo yokwaphula ilitye kunye nentsimbi ekrwada yasezimayini. Ngelishwa, abantu okwangoku abakwazi ukusebenzisa eli thuba.Ukushwankathela, umbane uneempembelelo ezininzi ezintle ekuphuhliseni uluntu. Ukongezelela, umbane ucebile kumandla aphezulu, kodwa uchaphazeleka kuphela kwinqanaba lobugcisa langempela, kwaye la mandla akanakusetyenziswa ngabantu. Mhlawumbi kwixesha elizayo elingekude, ngophuhliso lwenzululwazi nobuchwepheshe, iindudumo nemibane nazo ziya kuba ngamandla abantu abanokuwalawula.

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Ixesha lokuposa: Jun-02-2022