曹丽花, 赵世伟, 梁向锋, 刘合满, 杨永辉, 赵勇钢. PAM对黄土高原主要土壤类型水稳性团聚体的改良效果及机理研究[J]. 农业工程学报, 2008, 24(1): 45-49.
    引用本文: 曹丽花, 赵世伟, 梁向锋, 刘合满, 杨永辉, 赵勇钢. PAM对黄土高原主要土壤类型水稳性团聚体的改良效果及机理研究[J]. 农业工程学报, 2008, 24(1): 45-49.
    Cao Lihua, Zhao Shiwei, Liang Xiangfeng, Liu Heman, Yang Yonghui, Zhao Yonggang. Improvement effects of PAM on soil water-stable aggregates and its mechanisms in different soils in the Loess Plateau[J]. Transactions of the Chinese Society of Agricultural Engineering (Transactions of the CSAE), 2008, 24(1): 45-49.
    Citation: Cao Lihua, Zhao Shiwei, Liang Xiangfeng, Liu Heman, Yang Yonghui, Zhao Yonggang. Improvement effects of PAM on soil water-stable aggregates and its mechanisms in different soils in the Loess Plateau[J]. Transactions of the Chinese Society of Agricultural Engineering (Transactions of the CSAE), 2008, 24(1): 45-49.

    PAM对黄土高原主要土壤类型水稳性团聚体的改良效果及机理研究

    Improvement effects of PAM on soil water-stable aggregates and its mechanisms in different soils in the Loess Plateau

    • 摘要: 通过室内土柱培养,研究PAM对黑垆土、黄绵土、风沙土水稳性团聚体的改良效果,并探讨其作用机理和合理的施用浓度。结果表明,在浓度为0.05%~0.4%,PAM均可促进3种土壤>0.25 mm水稳性团聚体的形成,并有效降低3种土壤团聚体分形维数,改善土壤结构;方差分析表明,PAM改良3种土壤结构的机理是一致的,将<1 mm的水稳性团聚体聚合为更大粒径的水稳性团聚体,使>1 mm的水稳性团聚体含量增加。PAM改良黑垆土、黄绵土和风沙土土壤水稳性团聚体达到显著水平时的浓度也不相同,其适宜浓度分别为0.2%~0.4%,0.05%,0.05%。3种土壤的黏粒含量和有机质含量的差异,可能是影响PAM对不同土壤的水稳性团聚体的改良效果差异的主要原因。

       

      Abstract: In this paper, PAM was used and trained in soil column to study the effects of PAM on soil water stable aggregates of the dark loessial soil, loessial soil, aeolian sandy soil. In addition, the mechanisms of the effects of PAM and its optimal concentrations were offered. The results show that PAM could promote the formation of the > 0.25 mm water stable aggregates within the concentration of 0.05%~0.4% and reduced the fractal dimension of aggregates effectively in the studied soils. The results of variance analysis indicate that PAM has the similar mechanisms in improving three types of soil, the application of PAM makes <1 mm aggregates into bigger aggregates and increases the content of >1 mm aggregates. However, the concentrations are different for improving studied soils and achieving the remarkable effects because the clay and organic matter contents are different in the studied soils, which indicate that clay and organic matter contents are probably the major factors influencing the effects of PAM. The effective concentrations of PAM for the dark loessial soil, loessial soil, aeolian sandy soil are 0.2%~0.4%, 0.05%, 0.05%, respectively.

       

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