Subject | English | Estonian |
environ., UN | 1999 Gothenburg Protocol to Abate Acidification, Eutrophication and Ground-level Ozone | protokoll hapestumise, eutrofeerumise ja troposfääriosooni vähendamise kohta |
environ., UN | 1999 Gothenburg Protocol to Abate Acidification, Eutrophication and Ground-level Ozone | aasta piiriülese õhusaaste kauglevi konventsiooni protokoll hapestumise, eutrofeerumise ja troposfääriosooni vähendamise kohta |
environ., UN | 1999 Gothenburg Protocol to Abate Acidification, Eutrophication and Ground-level Ozone | Göteborgi protokoll |
environ., UN | Protocol to Abate Acidification, Eutrophication and Ground-level Ozone | Göteborgi protokoll |
environ., UN | Protocol to Abate Acidification, Eutrophication and Ground-level Ozone | protokoll hapestumise, eutrofeerumise ja troposfääriosooni vähendamise kohta |
environ., UN | Protocol to Abate Acidification, Eutrophication and Ground-level Ozone | aasta piiriülese õhusaaste kauglevi konventsiooni protokoll hapestumise, eutrofeerumise ja troposfääriosooni vähendamise kohta |
environ., UN | Protocol to the 1979 Convention on Long-Range Transboundary Air Pollution to abate Acidification, Eutrophication and Ground-Level Ozone | protokoll hapestumise, eutrofeerumise ja troposfääriosooni vähendamise kohta |
environ., UN | Protocol to the 1979 Convention on Long-Range Transboundary Air Pollution to abate Acidification, Eutrophication and Ground-Level Ozone | Göteborgi protokoll |
environ., UN | Protocol to the 1979 Convention on Long-Range Transboundary Air Pollution to abate Acidification, Eutrophication and Ground-Level Ozone | aasta piiriülese õhusaaste kauglevi konventsiooni protokoll hapestumise, eutrofeerumise ja troposfääriosooni vähendamise kohta |
environ. | soil acidification A naturally occurring process in humid climates that has long been the subject of research, whose findings suggest acid precipitation effects. The generally accepted impact of soil acidification on the productivity of terrestrial plants is summarised as follows: as soil becomes more acidic the basic cations (Ca, Mg) on the soil exchange are replaced by hydrogen ions or solubilized metals. The basic cation, now in solution, can be leached through the soil. As time progresses the soil becomes less fertile and more acidic. Resultant decreases in soil pH cause reduced, less-active population of soil microorganisms, which in turn slow decomposition of plant residues and cycling of essential plant nutrients | mulla hapestumine |