土壤水文条件对沿海盐碱地斜坡降雨侵蚀的影响

IF 2.8 3区 地球科学 Q2 GEOGRAPHY, PHYSICAL
Shengqiang Tang, Dongli She, Haishen Lv, Hongde Wang, Xiaoqin Sun
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引用次数: 0

摘要

沿海填海区裸露斜坡上的土壤侵蚀降低了水利工程的效率,并对盐碱滩涂的水环境构成威胁。坡形和土壤水文条件受降雨时严重的土壤剥离和快速沉积过程的影响,进而影响土壤侵蚀过程。本研究通过模拟降雨实验研究了坡度、坡长、土壤初始含水量和地下水深度对盐碱地坡面侵蚀过程的影响。我们发现,坡度对土壤流失的影响随坡长而变化。对于初始风干土壤(AD)总长度相同的长坡处理,单位宽度沉积物产率(Rs)随着坡度从 30° 到 60° 的增加而显著增加(p = 0.05)。对于总长度不同的短坡处理,径流量和 Rs 随坡度增加的变化趋势相反。地表土壤初始饱和(SS)和地下水深度为 0.8 米(GW)的斜坡的 Rs 值明显(p = 0.05)大于 AD 处理下的 Rs 值。在 60° SS 处理斜坡以及 45° 和 60° GW 处理斜坡上,土壤侵蚀引起了明显的崩塌破坏,并改变了原有的斜坡形状,使斜坡坡度降低、长度增加,这反过来又显著增加了 Rs(p = 0.05)。典型相关分析(CCA)显示,因变量(泥沙产量和径流量)中 71.6% 的方差可由第一对典型变量(主要代表坡面地形因素)解释,12.1% 的方差可由第二对典型变量(主要代表土壤水文条件)解释。本研究的结论可为沿海填海地区的边坡防护提供理论依据。
本文章由计算机程序翻译,如有差异,请以英文原文为准。

Effect of soil hydrological conditions on rainfall erosion on coastal saline soil slopes

Effect of soil hydrological conditions on rainfall erosion on coastal saline soil slopes

Soil erosion on bare slopes in coastal reclamation areas reduces the efficiency of water conservation projects and poses a threat to the water environment in saline tidal flats. Slope shape and soil hydrological conditions are affected by severe soil detachment and rapid sedimentation processes during rainfall, which in turn influence soil erosion processes. In this study, the influences of slope gradient, slope length, initial soil water content and groundwater depth on slope erosion processes of saline sodic soils were investigated through simulated rainfall experiments. We found that the effect of slope gradient on soil loss varied with slope length. For the long-slope treatments with the same total length of initially air-dried soil (AD), the unit width sediment yield rate (Rs) significantly (p = 0.05) increased with increasing slope gradient from 30° to 60°. For the short-slope treatments with different total lengths, opposite trends were observed for the runoff rate and Rs variation with increasing gradient. The Rs values of the slopes with initially saturated surface soil (SS) and a groundwater depth of 0.8 m (GW) were significantly (p = 0.05) greater than that under the AD treatment. On the 60° SS treatment slopes and 45° and 60° GW treatment slopes, soil erosion induced distinct collapse failure and altered the original slope shape, yielding lower gradients and larger lengths, which significantly (p = 0.05) increased Rs in turn. Canonical correlation analysis (CCA) revealed that 71.6% of the variance in the set of dependent variables (sediment yield and runoff) could be explained by the first pair of canonical variables, which mainly represented slope topography factors, and 12.1% of the variance could be explained by the second pair, which mainly represented soil hydrological conditions. The conclusions of this study could provide a theoretical foundation for slope protection in coastal reclamation areas.

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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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