4.7 Article

Influence of earthworm activity on aggregate-associated carbon and nitrogen dynamics differs with agroecosystem management

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SOIL BIOLOGY & BIOCHEMISTRY
卷 39, 期 5, 页码 1014-1022

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PERGAMON-ELSEVIER SCIENCE LTD
DOI: 10.1016/j.soilbio.2006.11.011

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aggregates; agricultural management; Aporrectodea rosea; earthworms; soil organic matter

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Earthworms are known to be important regulators of soil structure and soil organic matter (SOM) dynamics, however, quantifying their influence on carbon (C) and nitrogen (N) stabilization in agroecosystems remains a pertinent task. We manipulated population densities of the earthworm Aporrectodea rosea in three maize-tomato cropping systems [conventional (i.e., mineral fertilizer), organic (i.e., composted manure and legume cover crop), and an intermediate low-input system (i.e., alternating years of legume cover crop and mineral fertilizer)] to examine their influence on C and N incorporation into soil aggregates. Two treatments, no-earthworm versus the addition of five A. rosea adults, were established in paired microcosms using electro-shocking. A C-13 and N-15 labeled cover crop was incorporated into the soil of the organic and low-input systems, while N-15 mineral fertilizer was applied in the conventional system. Soil samples were collected during the growing season and wet-sieved to obtain three aggregate size classes: macroaggregates (> 250 mu m), microaggregates (53-250 mu m) and silt and clay fraction (< 53 mu m). Macroaggregates were further separated into coarse particulate organic matter (cPOM), microaggregates and the silt and clay fraction. Total C, C-13, total N and N-15 were measured for all fractions and the bulk soil. Significant earthworm influences were restricted to the low-input and conventional systems on the final sampling date. In the low-input system, earthworms increased the incorporation of new C into microaggregates within macroaggregates by 35% (2.8 g m(-2) increase; P = 0.03), compared to the no-earthworm treatment. Within this same cropping system, earthworms increased new N in the cPOM and the silt and clay fractions within macroaggregates, by 49% (0.21 g m-2; P < 0.01) and 38% (0.19 g m(-2); P = 0.02), respectively. In the conventional system, earthworms appeared to decrease the incorporation of new N into free microaggregates and macroaggregates by 49% (1.38 g m(-2); P = 0.04) and 41% (0.51 g m(-2); P = 0.057), respectively. These results indicate that earthworms can play an important role in C and N dynamics and that agroecosystem management greatly influences the magnitude and direction of their effect. (c) 2006 Elsevier Ltd. All rights reserved.

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