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    黄土高原土壤团聚体胶结物质的分布及作用综述

    Distribution and function of cementing materials of soil aggregates on the Loess Plateau, western China

    • 摘要: 胶结物质是土壤团聚体形成与稳定的基础和核心。以黄土高原团聚体胶结物质的区域特点为基础,对已有的团聚体形成理论及各胶结物质在团聚体形成过程中的作用特点等相关研究成果进行综述,分析总结出黄土高原土壤团聚体胶结物质的分布具有典型的区域特性:黏粒质量分数较低且空间分布差异大,随土壤剖面加深而降低;碳酸钙质量分数整体为10%左右,随土壤剖面加深先升高后降低;有机碳质量分数从东南向西北逐渐降低,且随土壤剖面加深而降低。主要存在问题包括:胶结剂类型在团聚体形成过程的差异、具体作用方式、强度和机理方面缺乏针对性系统研究;因此提出了相应的研究方向:根据胶结物质在土壤剖面的规律性变化,针对土壤腐殖质层、过渡层、碳酸钙淀积层胶结剂分布特征,分别开展有机碳为主、有机碳和碳酸钙交互作用、碳酸钙为主3 种类型下的团聚体胶结过程、强度及机制研究。

       

      Abstract: Cementing materials are the foundation and key component of the formation and stability of soil aggregates. Combining with the regional characteristics of cementing materials of soil aggregates on theLoess Plateau, western China, this paper reviews the existing aggregates forming theory and the functions of cementing materials in the process of aggregate formation. The typically regional characteristics of the cementing materials distribution in the soil aggregates of the Loess Plateau are summarized. The clay content is rare with considerably different spatial distribution, and decreases as it goes deeper along the soil profile. The calcium carbonate content, which is around 10% in most area, increases at first and then decreases as it goes deeper along the soil profile. The organic carbon content decreases when it goes from the southeast to the northwest and from the surface to deeper inside. The main problems include: the differences of the cement type in the process of aggregates formation,and the lack of systematic and targeted research on the specific mode and intensity of action of different cements as well as the bonding mechanism of cementing materials. Therefore, the corresponding research directions are proposed.According to the regularity of the cementing materials in the soil profile, future researches should be focused on cementing process, strength and mechanism of three kinds of soil aggregates,which are organic carbon as the main cementing materials on the humus layer, the interaction of organic carbon and calcium carbonate cementing material on the transition layer, and calcium carbonate as the main cementing materials on the illuvial layer.

       

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