Lesson 32 Mineral Cycling - Alaska Geobotany Center
Lesson 32 Mineral Cycling - Alaska Geobotany Center
Lesson 32 Mineral Cycling - Alaska Geobotany Center
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Carbon and nitrogen cycling in terrestrial ecosystems are<br />
tightly linked: Terrestrial Ecosystem Model<br />
From McGuire, Melilllo, and Joyce 1995<br />
Carbon<br />
• C enters the vegetation pool (C v ). as<br />
gross primary production (GPP).<br />
• Transfers either to the atmosphere as<br />
autotrophic plant respiration (R A )orto<br />
the soil pool ( C S ) as litter (L C ).<br />
• Leaves the soil pool as soil<br />
heterotrophic respiration (R H ).<br />
Nitrogen<br />
• N enters the vegetation pool (N V )from<br />
the inorganic N pool of the soil (N AV )as<br />
NUPTAKE.<br />
• Transfers from the vegetation to the<br />
organic soil pool (N S ) in litter production<br />
as the flux (L N ).<br />
• Net nitrogen mineralization (NETNMIN)<br />
accounts for nitrogen exchanged<br />
between the organic and inorganic<br />
nitrogen pool of the soil through<br />
decomposition.<br />
• NINPUT and NLOST are the inputs<br />
and outputs of N to and from the<br />
system.<br />
Other nutrients are linked to this cycle as<br />
they become needed for<br />
photosynthesis, metabolism, or<br />
structural plant tissues.