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drivers of soil respiration of root and microbial ... - Unitus DSpace

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14<br />

Reducing this uncertainties will required more robust estimate <strong>of</strong> the pool size <strong>and</strong> rates <strong>and</strong><br />

fluxes through the <strong>soil</strong> C pool.<br />

Estimates <strong>of</strong> the size <strong>of</strong> the global pool <strong>of</strong> SOC have ranged between 700 Pg (Bolin, 1970)<br />

<strong>and</strong> 2946 Pg (Bohn, 1976), with the value <strong>of</strong> around 1500 Gt now generally accepted as the most<br />

appropriate (Table 1).<br />

Study Soil C (Pg)<br />

Bolin (1970) 700<br />

Bohn (1976) 2946<br />

Baes et al. (1977) 1080<br />

Basilevich (1974) 1392<br />

Schlesinger (1977) 1456<br />

Aitjay et al. (1979) 2070<br />

Post et al. (1982) 1395<br />

Eswaran et al.(1993) 1576<br />

Batjes (1996) 1500<br />

Jacobson et al. (2000) 1500<br />

Table 1. Estimate <strong>of</strong> the size <strong>of</strong> the global SOC pool to 100cm.<br />

From the underst<strong>and</strong>ing <strong>of</strong> the behaviour <strong>of</strong> the SOC pool, models such as Rothamsted<br />

(Jenkinson <strong>and</strong> Rayner, 1977) <strong>and</strong> Century (Parton et al., 1993) have been developed <strong>and</strong> allow the<br />

results from the regional validation studies to be extrapolated to a global scale (Schimel et al.,<br />

1994). Such models divide the SOC pool into three to five pools with different turnover times<br />

ranging from tens to thous<strong>and</strong>s <strong>of</strong> years, <strong>and</strong> the sizes <strong>of</strong> these pools for a given <strong>soil</strong> texture are<br />

determined climate-driven interactions between plant C inputs, nutrients, <strong>microbial</strong> <strong>respiration</strong>,<br />

<strong>and</strong> leaching <strong>of</strong> dissolved organic carbon (DOC) (Fig.3).

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