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Factors affecting aggregate stability and water dispersible clay of recently cultivated semiarid soils of Argentina

机译:影响阿根廷新近种植的半干旱土壤团聚体稳定性和水分散性粘土的因素

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The aggregate stability and water dispersible clay of 18 surface soils ranging from 0 to 32 years of soybean monoculture after clearance from alarm of approximately 5000 ha in the semiarid Chacopampeana plain (Argentina) was studied. Both stabilityvariables were correlated with soil properties influencing aggregate stability. Aggregate stability and water dispersible clay were correlated with the length of agricultural use, organic carbon (OC) content, cation exchange capacity, free Al oxides andhydroxides to clay ratio, exchangeable Ca~(2+) content and exchangeable Na~+ percentage. A synergistic effect was observed between OC and free Al oxides and hydroxides. Clay content and electrolyte concentration of the saturation extract had no effect onaggregate stability and on water dispersible clay. From the results of this study it was concluded that the changing factors along agricultural use that affect water aggregate stability and water dispersible clay were exchangeable Ca~(2+) content and OCcontent.
机译:研究了半干旱Chacopampeana平原(阿根廷)从大约5000公顷的警报清除后,大豆单作0至32年间的18种表层土壤的团聚体稳定性和水分散性粘土。两个稳定性变量都与影响骨料稳定性的土壤特性相关。骨料的稳定性和水分散性粘土与农业使用时间,有机碳(OC)含量,阳离子交换能力,游离的氧化铝和氢氧化物与粘土的比例,可交换的Ca〜(2+)含量和可交换的Na〜+百分比相关。在OC与游离的Al氧化物和氢氧化物之间观察到协同作用。饱和提取物的粘土含量和电解质浓度对骨料稳定性和水分散性粘土没有影响。从研究结果可以得出结论,农业使用过程中影响水团聚体稳定性和水分散性粘土的变化因素是可交换的Ca〜(2+)含量和OC含量。

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