Nature, Količina 450Sir Norman Lockyer Macmillan Journals Limited, 2007 |
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Zadetki 1–3 od 86
Stran 277
... carbon than is present in biomass and n the atmosphere ' . Little is known , however , about the factors ontrolling the stability of soil organic carbon stocks2 and the esponse of the soil carbon pool to climate change remains uncer ...
... carbon than is present in biomass and n the atmosphere ' . Little is known , however , about the factors ontrolling the stability of soil organic carbon stocks2 and the esponse of the soil carbon pool to climate change remains uncer ...
Stran 407
... carbon load capacity of the sediments and organic carbon oxidation in continental nargins . At the global scale , previous studies have suggested that bout 70 per cent of riverine organic carbon is returned to the itmosphere , such as ...
... carbon load capacity of the sediments and organic carbon oxidation in continental nargins . At the global scale , previous studies have suggested that bout 70 per cent of riverine organic carbon is returned to the itmosphere , such as ...
Stran 545
... carbon dioxide after the atmosphere itself . CO2 entering the ocean alters the seawater carbonate equilibrium , decreasing pH and shifting dissolved inorganic carbon away from carbonate ( CO3 ) towards more bicarbonate ( HCO3 ) and CO2 ...
... carbon dioxide after the atmosphere itself . CO2 entering the ocean alters the seawater carbonate equilibrium , decreasing pH and shifting dissolved inorganic carbon away from carbonate ( CO3 ) towards more bicarbonate ( HCO3 ) and CO2 ...
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