Biochar enhances soil hydrological function by improving the pore structure of saline soil

作者：Angyuan Jia, Xiaojun Song, Shengping Li, Zhipeng Liu, Xiaotong Liu, Zixuan Han, Huizhou Gao, Qiqi Gao, Yan Zha, Ying Liu, Xueping Wu, Gang Wang · 发表于：Agricultural Water Management · 年份：2024 · DOI：10.1016/j.agwat.2024.109170 · 被引用次数：79 · 研究领域：Soil and Unsaturated Flow、Soil Geostatistics and Mapping、Soil Carbon and Nitrogen Dynamics

The poor soil structure caused by salinization is a major factor affecting crop growth and soil structure will further affect hydrological function. Biochar is widely used to improve soil physical structure because of its special porous material. However, the mechanism of soil pore structure on hydrological function (e.g., soil saturated hydraulic conductivity, plant available water, least limiting water range) after biochar incorporation in saline soil remains unclear. Therefore, the present study examined the response of soil structural properties of different biochar addition in saline clay loam, and subsequently assessed how the pore structure influence soil hydrological function. The study involved four treatments: CK (Control)、C 1 (7.5 t ha −1 biochar)、C 2 (15 t ha −1 biochar)、C 3 (30 t ha −1 biochar). Soil aggregate stability increased from 15 % to 30 % when the amount of biochar addition increased from 7.5 t ha −1 to 30 t ha −1 . The highest connectivity index (2.36) and the highest fractal dimension (2.56) were found at the biochar addition of 30 t ha −1 . Biochar addition reduced the proportion of small pores (<50 µm pore size) at both soil depths of 0–10 cm and 10–20 cm, whereas increased the proportion of large pores (>300 µm pore size). Biochar amendment reduced the soil penetration resistance, with the soil saturated hydraulic conductivity, plant available water and the least limiting water range were measured 46 %, 27 % and 40 % greater in rate of 30 t ha −1 bi...