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Soil organic carbon biomass mineralization

As decomposition proceeds, the C N ratio declines as organic carbon is lost from the system as CO2, and the C N ratio of stabilized SOM approaches the C N ratio of the microbial biomass. In a forest soil, Scheu and Parkinson (1995) found that the C N ratio dropped from 37.5 in fresh litter to 20.7 in the organic horizons and to 9.3 in the first mineral horizon. [Pg.4143]

See other pages where Soil organic carbon biomass mineralization is mentioned: [Pg.189] [Pg.145] [Pg.263] [Pg.309] [Pg.354] [Pg.123] [Pg.168] [Pg.229] [Pg.360] [Pg.191] [Pg.192] [Pg.206] [Pg.334] [Pg.712] [Pg.189] [Pg.265] [Pg.403] [Pg.4203] [Pg.4933] [Pg.921] [Pg.231] [Pg.145] [Pg.43] [Pg.190] [Pg.205] [Pg.208] [Pg.921] [Pg.150] [Pg.156] [Pg.297] [Pg.302] [Pg.116] [Pg.116] [Pg.266] [Pg.243] [Pg.30] [Pg.60] [Pg.348] [Pg.90] [Pg.90] [Pg.367] [Pg.808] [Pg.60] [Pg.33] [Pg.67] [Pg.331] [Pg.176] [Pg.4100] [Pg.4926] [Pg.81]

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Biomass carbon

Carbon mineral carbonation

Carbonate mineral

Carbonate mineralization

Carbonates soils

Mineral carbon

Mineral carbonation

Mineralization, biomass

Minerals soils

Organic mineralization

Organic soils

Soils carbon