Iibhaluni zemozulu, njengesithuthi esiqhelekileyo sokubona imozulu yobude obuphezulu, zifuna umthwalo othile kunye nesantya sokunyuka kwamaxabiso.Ngoko ke, iimpawu zayo eziphambili zezi zilandelayo:
(1) Ubume bejometri bungcono.Ukuze kuncitshiswe impembelelo yokuchasana komoya kunye nokuhamba komoya ngexesha lokunyuka kweebhaluni zemozulu (ingakumbi iibhaluni ezikhalayo), imilo yejometri yebhaluni iyadingeka ukuba ifane nesimo esilungelelanisiweyo, kwaye ibhaluni yomsindo ayifanele ibe isangqa esigqibeleleyo okanye iellipse.Kwibhola ekhangayo, isibambo kufuneka sikwazi ukumelana namandla okutsala ama-200N ngaphandle kokulimala.Ukuze kuncitshiswe amathuba okuba umqheba ukrazulwe, ubukhulu bebhola kufuneka bunyuswe ngokuthe chu ukuya kumqheba.
(2) Ulusu lwebhola kufuneka lulingane kwaye lube mcaba.Indawo apho ubungqingqwa buba buthathaka ngequbuliso kunokwenzeka ukuba kubangele iingxaki.Ke ngoko, ukuhlolwa kwenkangeleko kunye nokulinganisa ubukhulu beebhaluni zemozulu kubaluleke kakhulu.Ibhaluni kufuneka ingabi nobukhulu obungalinganiyo, amaqamza, ukungcola, njl. njl. ezichaphazela ukwandiswa okufanayo, kwaye akukho mingxunya, iintanda, njl njl.
(3) Ukumelana nokubanda kungcono.Ibhaluni yemozulu kufuneka idlule kwindawo ebanda kakhulu engaphantsi kwe -80 ° C ngexesha lenkqubo yokuphakamisa.Ukusebenza kwe-inflation yebhaluni kule ndawo imisela ukuphakama kokugqibela kokuthunyelwa kwebhaluni.Okukhona uphezulu umlinganiselo wobude bebhaluni kwiqondo lobushushu eliphantsi, kokukhona umlinganiselo wokwandiswa okukhulu.Ukuphakama kwebhaluni kuya kuba phezulu.Ke ngoko, kuyimfuneko ukongeza isithambiso ekuveliseni iibhaluni ze-latex ukwenzela ukuba ulusu lwebhaluni lungabi ngumkhenkce kwaye lube lukhuni xa ibhaluni idibana namaqondo obushushu aphantsi kufutshane ne-tropopause, ukuze kwandiswe ubude kunye nokuqhuma kwebhaluni kumaqondo obushushu aphantsi. , ngaloo ndlela kwandisa ukunyuswa kwebhaluni.ukuphakama.
(4) Ukumelana okuqinileyo nokuguga kwemitha kunye nokuguga kwe-ozone.Iibhaluni zemozulu zisetyenziswa xa i-ozone concentration iphezulu.I-concentration ye-ozone ifikelela kwinqanaba eliphezulu kwi-20000 ~ 28000 yeemitha ukusuka emhlabeni.Imitha ye-ultraviolet enamandla iya kubangela ukuba ifilimu iqhube, kwaye ukukhanya kwexesha elide ekukhanyeni kwelanga kuya kukhawuleza ifilimu.Ibhaluni iyanda njengoko ukuxinana kweatmosfera kuncipha ngexesha lenkqubo yokuphakanyiswa.Xa inyuka ibe malunga ne-30,000 yeemitha, ububanzi bayo buya kwanda ukuya ku-4.08 ngokuphindwe kabini, indawo engaphezulu iyanda ukuya ku-16 ngokuphindwe kabini, kwaye ubukhulu buyancipha ukuya ngaphantsi kwe-0.005mm., Ngoko ke, ukuchasana kwebhaluni ukuguga kwe-radiation Kwaye ukumelana nokuguga kwe-ozone kukwayona ntsebenzo iphambili yebhaluni.
(5) Ukusebenza kokugcina kungcono.Ukusuka kwimveliso ukuya ekusebenziseni, iibhaluni zemozulu zihlala zithatha unyaka omnye ukuya kwemi-2 okanye nangaphezulu.Ukusebenza okuphambili kweebhaluni akunakuncitshiswa kakhulu ngeli xesha.Ngoko ke, iibhaluni zemozulu zifuneka ukuba zibe nokusebenza kakuhle kokugcinwa kunye nomxholo oseleyo we-calcium chloride kumphezulu webhaluni.Kufuneka ibe phantsi kangangoko kunokwenzeka ukuphepha ukunamathela kwesikhumba sebhola kwiimeko zemozulu ezimanzi.Kwiindawo ezishushu (okanye amanye amaqondo obushushu aphezulu), kufuneka ikwazi ukugcina iminyaka emi-4.Ngoko ke, iibhaluni kufuneka zipakishwe kwiphakheji yobungqina bokukhanya ukuze kugwenywe ukukhanya (ingakumbi ukukhanya kwelanga), umoya okanye ubushushu obugqithisileyo.Ukuthintela ukusebenza kwebhaluni ukuba yehle ngokukhawuleza.
Ixesha lokuposa: Jun-13-2023