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Three-dimensional fractal characteristics of soil pore structure and their relationships with hydraulic parameters in biochar-amended saline soil

生物炭 修正案 土壤科学 土壤结构 土壤质量 环境科学 土壤水分 化学 法学 政治学 热解 有机化学
作者
Xiaoqin Sun,Dongli She,Yuanhang Fei,Hongde Wang,Lei Gao
出处
期刊:Soil & Tillage Research [Elsevier BV]
卷期号:205: 104809-104809 被引量:72
标识
DOI:10.1016/j.still.2020.104809
摘要

Due to poor soil quality, coastal saline soil limits soil productivity. Therefore, it is of great importance to find appropriate and efficient methods to improve the quality of coastal saline soil. Biochar has been widely used as a soil amendment to improve soil properties, but the effects of biochar amendment on soil pore structure and soil hydraulic properties are unclear. In recent years, with the development of fractal theory and computer technology, fractal geometry based on image analysis has been employed for quantitatively characterizing the structure and heterogeneity of soil pores. In this study, field experiments were established with three proportions of straw biochar (0, 2 and 5 %, w/w) to study the biochar amendment effects on soil structure and soil hydraulic properties. Three replicates were set for each treatment. The results showed that the addition of biochar to saline soil improved soil pore structures and soil hydraulic characteristics. The biochar amendment led to the strong pore spatial variation, complex pore structure and irregular pore shape. The biochar-amended saline soil had a high considerable water retention capacity (θS, AWC). Biochar had a long-term effect on saline soil improvement. For multifractal analysis, it is better to use the ΔD and Δα values to analyze the multifractal characteristics of soil. The heterogeneity of the soil pore distribution became stronger after biochar amendment. Multifractal parameters had significant changes with the time of biochar amendment. The changes of soil pore structure resulted in the improvement of soil hydraulic characteristics. The Ks value improved as the pore connectivity increased. The strong pore spatial variation, complex pore structure and irregular pore shape aided in increasing the θs value. The available water content value was improved as the number of soil pores, especially the micropores, increased. In response, this study proposes a new approach to analyzing soil pore structure to explain the association between the soil pore structure and soil hydraulic characteristics in biochar-amended saline soil.
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