Air bokwakha

Inxalenye bume, leyo kufuphi Umhlaba kwaye, ngokulandelelana, ukuphefumla umntu, ebizwa ngokuba eziFihliweyo. I-ntathu eziFihliweyo lunobude ukususela km ezilithoba ukuya elinanye kwaye umxube ngomatshini yeegesi ezahlukeneyo.

air Ukwakhiwa akukho njalo. Kuxhomekeka sendawo, indlela esemanzini, iimeko zemozulu, nengxinano yabemi, umoya unokuba isakhiwo eyahlukileyo kunye neempawu ezahlukeneyo. Umoya angasuswa okanye gassy, okanye enzima amatsha - konke oku kuthetha ukuba kukho ubumdaka ethile.

Nangona kunjalo, oku kulandelayo uthathwa ukuba ube yinxalenye umgangatho zezulu njengepesenti:

- nitrogen - 78,9 ekhulwini;

- mpilo - 20,95 ekhulwini;

- carbon dioxide - 0.3 ekhulwini.

Ngapha koko, zikhona nezinye iigesi esesibhakabhakeni (helium, argon, neon, xenon, Interface, hydrogen, radon, ozone), kunye oxide kunye nomphunga wamanzi. Umdibaniso kancinane ngaphantsi kwesinye ekhulwini.

Kwakhona kubalulekile isalatha ubukho emoyeni ezinye izinto ezingcolisa ezingisileyo imvelaphi zendalo, ingakumbi, ezinye iimveliso sukube wabumba ngenxa zombini iinkqubo yebhayoloji nemichiza. singakhankanya ngokukhethekileyo phakathi kwabo bafanelwe ammonia (composition zezulu kude kwiindawo ezihlala abantu kuquka kumawaka malunga ezintathu ukuya ezintlanu milligrams nge-cubic meter), methane (inqanaba layo alinganayo kwi-avareji milligrams amabini amawaka alishumi nge-cubic meter), kwenitrojeni (uyaphakama esesibhakabhakeni yoxinaniso milligrams malunga neshumi elinesihlanu-ezilishumi nge-cubic meter), hydrogen emanzini, kunye nezinye iimveliso sukube.

Ngaphandle ubuthi anomoya sukube, ukwakhiwa eekhemikhali umoya ngokuqhelekileyo luquka uthuli imvelaphi isithuba lowo uwe phezu kweli gada lomhlaba imali iitoni ezisixhenxe sewaka square kilometre nganye ngexesha lonyaka, kwakunye amasuntswana uthuli ukufika mlilo.

Nakuba kunjalo, utshintsho kakhulu (hayi eyona) ubume zezulu ziyihlambele eziFihliweyo ukuze ngokuba komhlaba (izityalo, umhlaba) uthuli kunye umsi imililo yehlathi. Ingakumbi eninzi uthuli kwi khona umoya lizwekazi avela ezinkqantosini of Central Asia and Afrika. Yiloo nto umntu uthi ngokuqinisekileyo ukuba okusingqongileyo umoya ngokugqibeleleyo ecocekileyo nje ayikho, kwaye yingcamango obukhoyo kuphela theory.

air Ukwakhiwa lidla ukutshintsha rhoqo, yaye iinguqulelo zayo zendalo ngokuqhelekileyo umdlalo ezaneleyo indima minor, ingakumbi xa kuthelekiswa neziphumo zazo zonke ezi ngxushungxushu zakhe zokufakelwa kunokwenzeka. izifo ezinjalo ezinxulumene kukhethwa kunye nemisebenzi mveliso yabantu, esebenzisa izixhobo ukuba umsebenzi wasendlini, kwakunye nezithuthi. Ezi ukuphazamiseka leswikulu, kuquka umoya kunye nokuguqulwa, okt umahluko iqapheleka yokutshintsha amalungu kunye neepropati kwabo emoyeni.

Le neminye imisebenzi emininzi yabantu kwaye kwakhokelela ekubeni kwindawo engundoqo ye zezulu ukuba bangenele utshintsho ecothayo singabalulekanga, kodwa kunjalo ngokupheleleyo vuhlayiseki. Ngokomzekelo, izazinzulu ziqikelela ukuba kwiminyaka engamashumi amahlanu edlulileyo, abantu iye yasetyenziswa malunga isixa ofanayo umoya kule minyaka izizigidi edlulileyo, njengepesenti - amabini ekhulwini imfuyo yayo iyonke emoyeni. Ngoko ngokufanelekileyo ukwanda ukukhutshwa kwekharbon diokside emoyeni umhlaba esingxotyeni. Kolu khutsho lwe idatha yakutshanje sele ifikelele phantse amakhulu amane billion iitoni kwiminyaka elikhulu edluleyo.

Ngenxa yoko, ukwakhiwa umoya iyatshintsha zambi kakhulu, kwaye kunzima ukuyiqonda indlela iya kuba kwamashumi ambalwa.