在模拟降雨实验中,灌木丛提高了坡耕地侵蚀沉积物的大小选择性

IF 2.8 3区 地球科学 Q2 GEOGRAPHY, PHYSICAL Earth Surface Processes and Landforms Pub Date : 2024-08-28 DOI:10.1002/esp.5979
Hai Xiao, Junkui Guo, Zhenyao Xia, Ping Guo, Feng Gao, Rui Xiang, Deyu Liu, Yu Ding, Di Wang, Lun Zhang
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引用次数: 0

摘要

侵蚀沉积物的粒径分布(PSD)可有效反映侵蚀过程的变化。绿篱具有显著的水土保持效益,并能影响侵蚀过程。然而,绿篱对侵蚀沉积物粒径分布的影响仍不清楚。因此,建立了三种坡度条件(对照检查,CK;仅灌木树篱根部,R;整个灌木树篱,P),涉及两种坡度(15 和 25°)的配置,并在三种降雨强度(60、90 和 120 mm/h)下进行了模拟降雨实验。比较了不同坡度条件下的 PSD、沉积物分选过程和沉积物颗粒团聚程度,以评价水流侵蚀过程中绿篱对侵蚀沉积物粒径选择性的影响。此外,还通过相关分析和偏最小二乘路径模型(PLS-PM)揭示了绿篱对分选过程和泥沙颗粒团聚程度的直接和间接影响。与 CK 坡条件相比,R 坡条件下粘土、细粉砂和粗粉砂的平均含量分别减少了 1.37%、0.06% 和 1.71%,而含沙量则增加了 0.46%。在 P 坡条件下,粘土、细粉砂和粗粉砂的平均含量分别增加了 32.61%、38.71% 和 36.14%,而砂的平均含量则减少了 47.30%。在 CK 坡条件下,沉积物分选主要发生在降雨初期。在 R 坡条件下,早期阶段的沉积物分选持续时间延长,但分选程度降低;而在 P 坡条件下,整个降雨过程中沙子都在相互分选。在 R 坡条件下,由于雨滴的冲击,更多的聚集体分散成单个颗粒,而在 P 坡条件下,更多的细颗粒在降雨初期聚集,但松散的聚集体在降雨后期分散成单个颗粒。细粉砂和粗粉砂的富集率与坡度条件呈正相关,而与砂的富集率呈负相关。然而,坡度条件与各种大小颗粒的聚集率之间没有明显关系。PLS-PM表明,绿篱通过调节径流和泥沙侵蚀直接和间接地影响分选过程和泥沙颗粒聚集度,且直接影响大于间接影响。这些发现使人们对绿篱控制水土流失的影响机制有了全面的了解。
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Hedgerows enhance the size selectivity of eroded sediment from sloping farmland under simulated rainfall experiment

The particle size distribution (PSD) of eroded sediment can effectively reflect changes in erosion processes. Hedgerows provide significant soil and water conservation benefits and influence erosion processes. However, the impact of hedgerows on the PSD of eroded sediment remains unclear. Therefore, three slope conditions (control check, CK; only hedgerow root, R; and whole hedgerow, P) involving the configuration of two slope gradients (15 and 25°) were established, and simulated rainfall experiments were conducted under three rainfall intensities (60, 90, and 120 mm/h). The PSD, sediment sorting process, and sediment particle agglomeration degree under the different slope conditions were compared to evaluate the influence of hedgerows on the size selectivity of eroded sediment during water erosion. Moreover, the direct and indirect effects of hedgerows on the sorting process and sediment particle agglomeration degree were revealed via correlation analysis and partial least squares path modelling (PLS–PM). Compared with those under CK slope conditions, the average clay, fine silt, and coarse silt contents under R slope conditions decreased by 1.37%, 0.06%, and 1.71%, respectively, whereas the sand content increased by 0.46%. Under P slope conditions, the average clay, fine silt, and coarse silt contents increased by 32.61%, 38.71%, and 36.14%, respectively, whereas the average sand content decreased by 47.30%. Under CK slope conditions, sediment sorting occurred primarily during the early stages of rainfall. R slope conditions caused an increase in the duration of early-stage sediment sorting but caused a reduction in the degree of sorting, whereas P slope conditions exhibited interceptive sorting of sand throughout the rainfall event. Under R slope conditions, more aggregates were dispersed into individual particles due to raindrop impact, whereas under P slope conditions, more fine particles aggregated initially, but loose aggregates were dispersed into individual particles during the later rainfall stages. The enrichment rates of fine silt and coarse silt were positively correlated with slope conditions, whereas they were negatively correlated with the enrichment rate of sand. However, there was no significant relationship between the slope conditions and the aggregation rates of particles of various sizes. PLS–PM indicated that hedgerows directly and indirectly affect sorting processes and sediment particle agglomeration degree by regulating runoff and sediment erosion, and the direct effects exceed the indirect effects. These findings provide a comprehensive understanding of the influential mechanisms of hedgerows on controlling soil erosion.

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来源期刊
Earth Surface Processes and Landforms
Earth Surface Processes and Landforms 地学-地球科学综合
CiteScore
6.40
自引率
12.10%
发文量
215
审稿时长
4 months
期刊介绍: Earth Surface Processes and Landforms is an interdisciplinary international journal concerned with: the interactions between surface processes and landforms and landscapes; that lead to physical, chemical and biological changes; and which in turn create; current landscapes and the geological record of past landscapes. Its focus is core to both physical geographical and geological communities, and also the wider geosciences
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