Effects of water erosion on wind erosion studied in rain simulator and wind tunnel on silty material taken from the Chernozem

IF 5.4 1区 农林科学 Q1 GEOSCIENCES, MULTIDISCIPLINARY
Haiyu Li , Wei Hu , Mingming Guo , Xingyi Zhang , Meiyue Wang , Meng Li
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Abstract

Composite erosion resulting from both water and wind poses a significant challenge to croplands in the Songnen Plain, located in northeast China, resulting in substantial soil degradation and loss of fertility. Nonetheless, the factors driving the effect of water erosion on wind erosion remain unclear. To address this, the study conducted controlled laboratory experiments that simulated conditions of rainfall and wind. Moreover, soil samples were exposed to rainfall intensities of 0, 50, and 100 mm h−1, followed by wind tunnel tests with wind velocities of 9 m s−1, 12 m s−1, and 15 m s−1. We subsequently assessed wind erosion characteristics and measured the soil properties of the residual surface soil in the trough. Our findings indicated that higher rainfall intensity significantly decreased the intensity of wind erosion by 42.3 %-85.5 % at 50 and 100 mm h−1. Additionally, sediment transport height decreased by 4–10 cm across distinct rainfall intensities. Water erosion increased soil shear strength and compactness by 1.9 to 2.4 times and 2.8 to 4.8 times, respectively. Except for that, the clay content decreased by 14.2 %-39.2 % with different rainfall intensities and wind velocities. Moreover, the proportion of aggregates smaller than 0.25 mm decreased with increasing wind velocities. The contents of C, N, and CaCO3 also diminished with higher wind velocity and rainfall intensity. Structural equation modeling analysis demonstrated that rainfall intensity indirectly influenced wind erosion intensity by altering soil properties. Meanwhile, rainfall intensity exhibited the strongest direct and indirect negative effects on sediment transport height. A nonlinear empirical equation for soil wind erodibility parameters (K) based on clay content was established, incorporating soil shear strength, CaCO3 content, and rainfall intensity. This study offers a theoretical foundation for developing effective soil conservation strategies in the Songnen Plain.
在降雨模拟器和风洞中对黑钙土粉质材料进行了水蚀对风蚀的影响研究
水风复合侵蚀对中国东北松嫩平原的农田构成了重大挑战,导致土壤严重退化和肥力丧失。尽管如此,导致水蚀对风蚀影响的因素仍不清楚。为了解决这个问题,该研究进行了受控的实验室实验,模拟了降雨和风的条件。此外,将土壤样品暴露于0、50和100 mm h−1的降雨强度下,然后进行风速为9 m s−1、12 m s−1和15 m s−1的风洞试验。我们随后评估了风蚀特征,并测量了槽内残留表层土壤的土壤特性。研究结果表明,在50和100 mm h−1条件下,较高的降雨强度显著降低了风蚀强度42.3% ~ 85.5%。输沙高度在不同降雨强度下降低了4 ~ 10 cm。水侵蚀使土壤抗剪强度和密实度分别提高1.9 ~ 2.4倍和2.8 ~ 4.8倍。此外,在不同降雨强度和风速下,粘土含量降低14.2% ~ 39.2%。粒径小于0.25 mm的团聚体所占比例随风速的增大而减小。C、N和CaCO3含量也随风速和降雨强度的增大而降低。结构方程模型分析表明,降雨强度通过改变土壤性质间接影响风蚀强度。同时,降雨强度对输沙高度的直接和间接负作用最强。结合土壤抗剪强度、CaCO3含量和降雨强度,建立了基于粘土含量的土壤风蚀性参数(K)非线性经验方程。该研究为松嫩平原制定有效的土壤保持策略提供了理论基础。
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
Catena
Catena 环境科学-地球科学综合
CiteScore
10.50
自引率
9.70%
发文量
816
审稿时长
54 days
期刊介绍: Catena publishes papers describing original field and laboratory investigations and reviews on geoecology and landscape evolution with emphasis on interdisciplinary aspects of soil science, hydrology and geomorphology. It aims to disseminate new knowledge and foster better understanding of the physical environment, of evolutionary sequences that have resulted in past and current landscapes, and of the natural processes that are likely to determine the fate of our terrestrial environment. Papers within any one of the above topics are welcome provided they are of sufficiently wide interest and relevance.
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