Anthropogenic influences on riverine fluxes of dissolved inorganic carbon to the oceans

Bicarbonate (HCO3−), the predominant form of dissolved inorganic carbon in natural waters, originates mostly from watershed mineral weathering. On time scales of decades to centuries, riverine fluxes of HCO3− to the oceans and subsequent reactions affect atmospheric CO2, global climate and ocean pH....

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Vydané v:	Limnology and oceanography letters Ročník 3; číslo 3; s. 143 - 155
Hlavní autori:	Raymond, Peter A., Hamilton, Stephen K.
Médium:	Journal Article
Jazyk:	English
Vydavateľské údaje:	Hoboken John Wiley & Sons, Inc 01.06.2018 Wiley
Predmet:	Acidification Acids Alkalinity Anthropogenic factors Aquatic ecosystems Biogeochemistry Calcification Carbon cycle Carbon dioxide Chemistry Climate change Dissolved inorganic carbon Global warming Hydrologic cycle Liming Minerals Mining Natural waters Oceans Precipitation River systems Rivers Seawater Sediments Water treatment Watersheds Weathering Weathering zone
ISSN:	2378-2242, 2378-2242
On-line prístup:	Získať plný text
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