阚晓晴, 程金花, 王葆, 等. 基于工业CT扫描的不同类型土壤孔隙结构研究[J]. 西南林业大学学报(自然科学), 2021, 41(4): 25–34 . DOI: 10.11929/j.swfu.202007062
引用本文: 阚晓晴, 程金花, 王葆, 等. 基于工业CT扫描的不同类型土壤孔隙结构研究[J]. 西南林业大学学报(自然科学), 2021, 41(4): 25–34 . DOI: 10.11929/j.swfu.202007062
Kan Xiaoqing, Cheng Jinhua, Wang Bao, Zheng Xin. Soil Structural Pore Network Under Different Soil Types by Industrial Computed Tomography[J]. Journal of Southwest Forestry University, 2021, 41(4): 25-34. DOI: 10.11929/j.swfu.202007062
Citation: Kan Xiaoqing, Cheng Jinhua, Wang Bao, Zheng Xin. Soil Structural Pore Network Under Different Soil Types by Industrial Computed Tomography[J]. Journal of Southwest Forestry University, 2021, 41(4): 25-34. DOI: 10.11929/j.swfu.202007062

基于工业CT扫描的不同类型土壤孔隙结构研究

Soil Structural Pore Network Under Different Soil Types by Industrial Computed Tomography

  • 摘要: 本研究从3个土壤类型样地中采集11个原状土柱,进行CT断层扫描,结合结构方程模型定量分析土壤大孔隙特征参数与土壤含水量间关系。结果表明:不同土壤类型的大孔隙累积弯曲度可抑制土壤含水量的增加,褐土区的大孔隙垂直连续性强,喀斯特人工恢复林地区的大孔隙水平发育度高,且破碎程度高。不同植被类型条件下的林地总孔隙体积较大,乔木群落土壤大孔隙平均直径分别是灌木和草本的1.33倍和1.87倍,灌木的弯曲度高于林地;大孔隙的弯曲度可促进土壤大孔隙表面积的增加。本研究可为后续定量化分析大孔隙三维特征及其对水分运移的贡献等内容提供基础支撑,为不同地区人工林有效恢复及管理、林地土壤营养物质运移及滞留、土壤水分运移机制等提供参考。

     

    Abstract: In this study, 11 undisturbed soil columns were collected from 3 types of soil samples, and the relationship between soil macropore characteristic parameters and soil water content was quantitatively analyzed by using structural equation model(SEM). The results show that the cumulative curvature of macropores in different soil types can inhibit the increase of soil water content, the vertical continuity of macropores in cinnamon soil area is strong, and the horizontal development and fragmentation degree of macropores in karst artificial restoration forest areas are higher. The total macropores volume of forest areas are larger. The average diameter of soil macropores in forest community was 1.33 and 1.87 times of shrub and herb, respectively. And the curvature of shrub was higher than that of forest areas. The curvature of macropores can increase the surface area of macropores. This study can provide basic support for the subsequent quantitative analysis of the three-dimensional characteristics of macropores and their contribution to water transport, and provide reference for the effective restoration and management of plantations in different areas, the movement and retention of soil nutrients in forest land, and the mechanism of soil water transport.

     

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