Effects of Vegetation Restoration on Rill Erosion on the Chinese Loess Plateau

IF 3.6 2区 农林科学 Q2 ENVIRONMENTAL SCIENCES
JianFang Wang, YanFen Yang, Bing Wang, GuoBin Liu
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引用次数: 0

Abstract

Accurately describing rill erosion is important for building physical process models of soil erosion. Vegetation restoration may lead to differences in soil properties and root characteristics, and thus likely affects the rill erosion process to flowing water erosion, reflected by rill erodibility (Kr) and critical shear stress (τc). However, few studies have been conducted to evaluate this effect of vegetation restoration on the Loess Plateau of China. The present work chose eight typical herbaceous plants, commonly appearing at diverse vegetation succession periods on the Chinese Loess Plateau, for discovering how soil properties and root characteristics affect rill erosion. In total, we collected 240 undisturbed soil samples for overland flow scouring within the hydraulic flume in the presence of six shear stresses (range, 5.94–18.58 Pa). According to our findings, Kr and τc were 0.015–0.411 s m−1 and 0.050–6.059 Pa among eight typical grasslands. Cultivated grasslands have high Kr and low τc; the Kr was 5–25 times greater than that of other grasslands, and τc was 89%–98% less than that of other grasslands. Plants with tap root systems exhibited a 5‐fold increase in Kr value and a 50% reduction in τc compared to those with fibrous root systems. The Kr and τc were affected by the root‐soil complex, with interaction effects of root and soil being 54% and 50%, respectively. The Kr decreased with increasing bulk density (BD), soil cohesion, soil organic matter, and soil aggregate as power functions and decreased with increasing root surface area density (RSAD) and root length density as exponential functions. The τc increased with specific root length (SRL) and BD as power functions. Those above‐mentioned soil properties and root characteristics indicated that Kr was dominantly affected by cohesion and RSAD, and τc was affected by BD and SRL. Kr was simulated through soil cohesion (Coh) and RSAD, and τc was simulated by soil BD and SRL as power functions. Our constructed model achieved satisfactory performance.
黄土高原植被恢复对细沟侵蚀的影响
准确描述细沟侵蚀对建立土壤侵蚀物理过程模型具有重要意义。植被恢复可能导致土壤性质和根系特征的差异,从而可能将细沟侵蚀过程转化为流水侵蚀,反映在细沟可蚀性(Kr)和临界剪应力(τc)上。然而,对黄土高原植被恢复效果的评价研究较少。本文选取黄土高原不同植被演替时期常见的8种典型草本植物,研究土壤性质和根系特征对细沟侵蚀的影响。总的来说,我们收集了240个未受干扰的土壤样本,用于在6个剪切应力(范围,5.94-18.58 Pa)存在的情况下,在水力水槽内进行地面水流冲刷。结果表明,8个典型草地的Kr值为0.015 ~ 0.411 s m−1,τc值为0.050 ~ 6.059 Pa。人工草地的Kr高,τc低;Kr比其他草原大5 ~ 25倍,τc比其他草原小89% ~ 98%。与纤维根相比,丝状根系植物的Kr值增加了5倍,τc降低了50%。Kr和τc受根土复合体的影响,根土交互作用分别为54%和50%。Kr随容重、土壤黏聚力、土壤有机质和土壤团聚体的幂函数增加而减小,随根表面积密度和根长密度的指数函数增加而减小。τc随比根长度(SRL)和比根长度(BD)的幂函数而增大。上述土壤性质和根系特征表明,Kr主要受黏聚力和RSAD的影响,τc主要受BD和SRL的影响。Kr通过土壤黏聚力(Coh)和RSAD模拟,τc通过土壤BD和SRL作为幂函数模拟。我们构建的模型取得了令人满意的性能。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
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来源期刊
Land Degradation & Development
Land Degradation & Development 农林科学-环境科学
CiteScore
7.70
自引率
8.50%
发文量
379
审稿时长
5.5 months
期刊介绍: Land Degradation & Development is an international journal which seeks to promote rational study of the recognition, monitoring, control and rehabilitation of degradation in terrestrial environments. The journal focuses on: - what land degradation is; - what causes land degradation; - the impacts of land degradation - the scale of land degradation; - the history, current status or future trends of land degradation; - avoidance, mitigation and control of land degradation; - remedial actions to rehabilitate or restore degraded land; - sustainable land management.
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