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Title: Carbon Balance of the Breton Classical Plots over Half a Century

Journal Article · · Soil Science Society of America Journal

We related C input and management to soil organic C (SOC) dynamics over 51 yr (1939-1990). 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) wheat-oat (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 WF-Nil and 1078 in WF-F and SOC decreased in both, but NAGCP averaged 1208 in WF-M, where SOC increased. A NAGCP of 853 in WOBHH-Nil maintained SOC, while both 1831 in WOBHH-F and 1714 in WOBHH-M increased SOC. After 51 yr, WOBHH-M had 25 Mg ha-1 more SOC than did WF-Nil. 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 in crease 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, an d26% 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.

Research Organization:
Pacific Northwest National Lab., Richland, WA (US)
Sponsoring Organization:
US Department of Energy (US)
DOE Contract Number:
AC06-76RL01830
OSTI ID:
15005738
Report Number(s):
PNNL-SA-34781; KP1202020; TRN: US200324%%179
Journal Information:
Soil Science Society of America Journal, Vol. 65, Issue 2; Other Information: PBD: 1 Feb 2001
Country of Publication:
United States
Language:
English

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