Aggregate Stability and Its Relationship with Some Chemical Properties of Red Soils in Subtropical China  

作　　者：LIZhao-Xia CAIChong-Fa SHIZhi-Hua WANGTian-Wei 

机构地区：[1]CollegeofResourcesandEnvironment,HuazhongAgriculturalUniversity,Wuhan430070China

出　　处：《Pedosphere》2005年第1期129-136,共8页土壤圈（英文版）

基　　金：ProjectsupportedbytheNationalKeyBasicResearchSupportFoundation(NKBRSF)ofChina(No.G1999011801)theNationalNaturalScienceFoundationofChina(No.4401034).

摘　　要：The stability of aggregates in the surface soil is crucial to soil erosion and runoff generation. Thus, to understand the stability and the breakdown mechanisms of soil aggregates as well as the relationship between aggregate stability and selected soil chemical properties, such as different forms of Fe and Al oxides, organic matter, CEC and clay content, the aggregates of slightly and severely eroded red soils derived from Quaternary red clay in subtropical China were analyzed using the routine wet sieving…The stability of aggregates in the surface soil is crucial to soil erosion and runoff generation. Thus, to understand the stability and the breakdown mechanisms of soil aggregates as well as the relationship between aggregate stability and selected soil chemical properties, such as different forms of Fe and Al oxides, organic matter, CEC and clay content, the aggregates of slightly and severely eroded red soils derived from Quaternary red clay in subtropical China were analyzed using the routine wet sieving and the Le Bissonnais methods. The results indicated that the aggregates of the severely eroded soils were more stable than those of the slightly eroded soils. Different aggregate breakdown mechanisms resulted in different particle size distribution. The slaking from entrapped air in aggregates severely destroyed the soil aggregates,especially in the slightly eroded soils. Meanwhile, mechanical breakdown and microcracking had little effect on the aggregates compared to slaking. The fragments resulting from slaking were mainly microaggregates that increased in size with increasing clay content. The main fragment size of the slightly eroded soils was 1.0-0.2 mm, while for the severely eroded soils it was 5.0-2.0 mm and 1.0-0.5 mm. Overall, more than 20% of the fragments were smaller than 0.2 mm.In addition, aggregate stability was positively and often significantly correlated with Fed, Ald, Feo and clay content, but significantly and negatively correlated to SOC.

关 键 词：ORGANIC-MATTER IRON-OXIDE INFILTRATION ERODIBILITY MECHANISMS BREAKDOWN ALUMINUM CLAY 

分 类 号：P642.132[天文地球—工程地质学] S152.9[天文地球—地质矿产勘探]