Pore Size Distribution of Clayey Soils and Its Correlation with Soil Organic Matter  

作　　者：Malik ZAFFAR LU Sheng-Gao 

机构地区：[1]Zhejiang Provincial Key Laboratory of Subtropical Soil and Plant Nutrition,College of Environmental and Resource Sciences,Zhejiang University [2]Ministry of Education Key Laboratory of Environmental Remediation and Ecosystem Health,College of Environmental and Resource Sciences,Zhejiang University

出　　处：《Pedosphere》2015年第2期240-249,共10页土壤圈（英文版）

基　　金：supported by the National Key Basic Research Program(973 Program) of China (No.2011CB100502)

摘　　要：Soil pore size distribution(PSD) directly influences soil physical,chemical,and biological properties,and further knowledge of soil PSD is very helpful for understanding soil functions and processes.In this study,PSD of three clayey soils collected from the topsoil(0-20 cm) of Vertisols in Northern China was analyzed using the N_2 adsorption(NA) and mercury intrusion porosimetry(MIP) methods.The effect of soil organic matter(SOM) on the PSD of clayey soils was also evaluated.The differential curves of pore volume of clayey soils by the NA method exhibited that the pores with diameter < 0.01 μm accounted for more than 50%in the pore size range of 0.001 to 0.1 μm.The differential pore curves of clayey soils by the MIP method exhibited three distinct peaks in pore size range of 60 to 100,0.3 to 0.4 and 0.009 to 0.012 μm,respectively.In the three clayey soils,the ultramicropores(5-0.1μm) were determined to be the main pore class(on average 35.5%),followed by macropores(> 75 μm,31.4%),cryptopores(0.1-0.007μm,16.0%),micropores(30-5 μm,9.7%) and mesopores(75-30 μm,7.3%).The SOM greatly affected the pore structure and PSD of aggregates in clayey soils.In particular,SOM removal reduced the volume and porosity of 5-100 μm pores while increased those of <5 μm pores in the 5-2 and 2-0.25 mm aggregates of clayey soils.The increase in the volume and porosity of < 5 μm pores may be attributed to the disaggregation and partial emptying of small pores caused by the destruction of SOM.Soil pore size distribution（PSD） directly influences soil physical,chemical,and biological properties,and further knowledge of soil PSD is very helpful for understanding soil functions and processes.In this study,PSD of three clayey soils collected from the topsoil（0-20 cm） of Vertisols in Northern China was analyzed using the N2 adsorption（NA） and mercury intrusion porosimetry（MIP） methods.The effect of soil organic matter（SOM） on the PSD of clayey soils was also evaluated.The differential curves of pore volume of clayey soils by the NA method exhibited that the pores with diameter 0.01 μm accounted for more than 50%in the pore size range of 〈0.001 to 〈0.1 μm.The differential pore curves of clayey soils by the MIP method exhibited three distinct peaks in pore size range of 60 to 100,0.3 to 0.4 and 0.009 to 0.012 μm,respectively.In the three clayey soils,the ultramicropores（5-0.1μm） were determined to be the main pore class（on average 35.5%）,followed by macropores（ 75 μm,31.4%）,cryptopores（0.1-0.007μm,16.0%）,micropores（30-5 μm,9.7%） and mesopores（75-30 μm,7.3%）.The SOM greatly affected the pore structure and PSD of aggregates in clayey soils.In particular,SOM removal reduced the volume and porosity of 5-100 μm pores while increased those of 5 μm pores in the 5-2 and 2-0.25 mm aggregates of clayey soils.The increase in the volume and porosity of 〈5 μm pores may be attributed to the disaggregation and partial emptying of small pores caused by the destruction of SOM.

关 键 词：mercury intrusion porosimetry N2 adsorption pore volume POROSITY soil aggregate VERTISOL 

分 类 号：S153.6[农业科学—土壤学] S152[农业科学—农业基础科学]