>ning ookeani tagasi pöörduv vesi on väga kõrge soolasisaldusega. Tulevikus sama protsessi läbiviimine on seetõttu aga kulukam
for real? ma küll arvutusi ei tea, aga olen päris kindel, et sellise meetodiga suudab inimene mõjutada ookeanivee soolsust nii umbes 0,0000001% ulatuses
Aga samas muidugi kui ajalukku tagasi vaadata, siis heeringas ka elas kuival maal, kuni kaljas, kahe mastiga, läks põhja soolalastiga
Aga samas muidugi kui ajalukku tagasi vaadata, siis heeringas ka elas kuival maal, kuni kaljas kahe mastiga läks põhja soolalastiga
Riskid võivad mitmetest asjaoludest sõltudes erineda ja õhku jääb ka küsimus pikaajalise mõju kohta, mida on vähe uuritud
The few studies available indicate that the ecological impacts of brine discharge vary widely
and are a function of several factors, including the characteristics of the brine, the discharge
method, the rate of dilution and dispersal, and the sensitivity of organisms. For example, brine discharge can cause widespread changes in the benthic community in shallow and/or semienclosed bays, whereas impacts can be undetectable in areas with heavy wave activity or significant flushing. http://pacinst.org/wp-content/uploads/2013/12/desal-marine-imapcts-full-report.pdf
The few studies available indicate that the ecological impacts of brine discharge vary widely
and are a function of several factors, including the characteristics of the brine, the discharge
method, the rate of dilution and dispersal, and the sensitivity of organisms. For example, brine discharge can cause widespread changes in the benthic community in shallow and/or semienclosed bays, whereas impacts can be undetectable in areas with heavy wave activity or significant flushing. http://pacinst.org/wp-content/uploads/2013/12/desal-marine-imapcts-full-report.pdf