The effects of organic inputs over time on soil aggregate stability - A literature analysis

被引:569
作者
Abiven, Samuel [1 ]
Menasseri, Safya [2 ,3 ]
Chenu, Claire [4 ]
机构
[1] Univ Zurich, Dept Geog, CH-8057 Zurich, Switzerland
[2] Soil Agro & HydroSyst, UMR 1069, Agrocampus Rennes, F-35000 Rennes, France
[3] Soil Agro & HydroSyst, UMR 1069, INRA, F-35000 Rennes, France
[4] INRA UPMC CNRS ENSCP AgroParisTech ENS, UMR BIOEMCO, F-78850 Thiverval Grignon, France
关键词
Soil aggregate stability; Organic inputs; Aggregative factors; Review; STRUCTURAL STABILITY; SANDY-LOAM; MICROBIAL BIOMASS; SEWAGE-SLUDGE; ROOT MUCILAGE; MATTER; MANURE; CARBON; DECOMPOSITION; DYNAMICS;
D O I
10.1016/j.soilbio.2008.09.015
中图分类号
S15 [土壤学];
学科分类号
0903 ; 090301 ;
摘要
Since the beginning of the last century, many studies have reported evidence describing the effects of organic inputs on soil aggregate stability. In 1965, Monnier proposed a conceptual model that considers different patterns of temporal effects on aggregate stability depending on the nature of the organic inputs: easily decomposable products have an intense and transient effect on aggregate stability while more recalcitrant products have a lower but longer term effect. We confronted this conceptual model with a literature review of experimental data from laboratory and field experiments. This literature analysis validated the conceptual model proposed by Monnier and pointed out gaps in our current knowledge concerning the relationships between aggregate stability and organic inputs. Noticeably, the experimental dataset confirmed the biological and temporal effects of organic inputs on aggregate stability as proposed in the model. Monnier's model also related the evolution of aggregate stability to different microbial decomposing agents, but this relationship was not made clear in this literature analysis. No direct or universal relationship was found between the aggregative factors induced by organic input decomposition (binding molecules or decomposers of biomass) and temporal aggregate stability dynamics. This suggests the existence of even more complex relationships. The model can be improved by considering (i) the direct abiotic effect of some organic products immediately after the inputs, (ii) the initial biochemical characteristics of the organic products and (iii) the effects of organic products on the various mechanisms of aggregate breakdown. For now, no trend is evident in the effect of the rate of organic inputs or the effect of the soil characteristics (essentially carbon and clay contents) on aggregate stability. (c) 2008 Elsevier Ltd. All rights reserved.
引用
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页码:1 / 12
页数:12
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