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a Pacific Northwest National Laboratories, 901 D Street S.W., Ste. 900, Washington, DC 20024-2115
b Dep. of Renewable Resources, University of Alberta, 4-42 Earth Sciences Bldg., Edmonton, AB T6G 2E3, Canada
Corresponding author (cesar.izaurralde{at}pnl.gov)
We related C input and management to soil organic C (SOC) dynamics over 51 yr (19391990). We used two rotations from the Breton Classical Plots at Breton, Canada, on a Typic Cryoboralf: (i) wheat (Triticum aestivum L.)fallow (WF) and (ii) wheatoat (Avena sativa L.)barley (Hordeum vulgare L.)hay (primarily alfalfa, Medicago sativa L.)hay (WOBHH), in factorial combination with three fertility levels: no added fertilizer [Nil], N-P-K-S fertilizers [F], and farmyard manure [M]. Net aboveground C productivity (NAGCP, kg ha-1 yr-1) averaged 576 in WFNil and 1078 in WFF and SOC decreased in both, but NAGCP averaged 1208 in WFM, where SOC increased. A NAGCP of 853 in WOBHHNil maintained SOC, while both 1831 in WOBHHF and 1714 in WOBHHM increased SOC. After 51 yr, WOBHHM had 25 Mg ha-1 more SOC than did WFNil. Because of contrasting decay rates and root/shoot ratios, C input needed to maintain the original SOC was twofold greater in WF than in WOBHH, which required a fourfold increase in NAGCP to attain these inputs. A three-compartment model fitted to the data suggested loss of C from the active compartments and gain of C by the passive compartments. Inputs of C that maintained SOC over 51 yr would lead to a steady state of 2.9 times more C than in 1939, and 26% higher than the native SOC content. Return of 30% of the crop C as manure would sustain SOC sequestration in all WOBHH rotations with NAGCP > 400 kg ha-1 yr-1 and in those WF rotations with NAGCP > 1000 kg ha-1 yr-1.
Abbreviations: F, N-P-K-S fertilizers treatment M, farmyard manure treatment NAGCP, net aboveground C productivity Nil, no fertilizer treatment WF, wheatfallow WOBHH, wheatoatbarleyhayhay
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