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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.

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