Effects of Treatments With Biochar From Crop Residues on Soil Detachment Capacity in Rills After Deforestation

生物炭 森林砍伐(计算机科学) 环境科学 农学 农林复合经营 作物 作物残渣 农业 化学 生物 热解 生态学 计算机科学 有机化学 程序设计语言
作者
Misagh Parhizkar,Manuel Esteban Lucas‐Borja,Pasquale Filianoti,Nikolaos Tziolas,Vesna Zupanc,Demetrio Antonio Zema
出处
期刊:Soil Use and Management [Wiley]
卷期号:41 (2)
标识
DOI:10.1111/sum.70070
摘要

ABSTRACT Rill erosion is the most common form in steep and long hillslopes, but studies about the biochar effects on soil detachment capacity in rills are scarce. This study has simulated soil detachment in rills ( D c ) by a laboratory flume on samples collected from forest soils in Northern Iran. The samples were treated with biochars (from rotten fruits of peach and almond, sugarcane bagasse, and straw of wheat, corn, and cotton) or untreated. D c has been measured under three soil slopes and four water flow rates. The erodibility factor (K r ) and critical shear stress (τ c ), important parameters for erosion models, have been estimated from interpolations between D c and the shear stress. Regression equations have also been proposed to predict D c from stream power or its unit value. The experiments have shown that wheat biochar is the most effective in reducing D c (−35% compared to the untreated soils). This reduction has been associated with higher organic matter (+65%) and stability of aggregates (> 80%) as well as with lower bulk density (−10%) of soils treated with this biochar. These effects may be due to the highest content of organic carbon, specific surface area, and cation exchange capacity of the substrate. No significant differences in D c have been measured for the soils treated with the other biochars. K r was 15%–35% lower compared to the untreated soils, while τ c noticeably increased after the treatment with all biochars. The stream power was a more accurate D c estimator than its unit value (Nash and Sutcliffe's coefficient > 0.90). This study helps land managers and hydrologists select the most effective substrate for soil conservation and estimate rill erosion in forests under similar environmental conditions.
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