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首页> 外文期刊>Catena: An Interdisciplinary Journal of Soil Science Hydrology-Geomorphology Focusing on Geoecology and Landscape Evolution >Soil aggregate stability response to hydraulic conditions in water level fluctuation zone of the Three Gorges Reservoir, China
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Soil aggregate stability response to hydraulic conditions in water level fluctuation zone of the Three Gorges Reservoir, China

机译:中国三峡水库水位波动区水平稳定性稳定性响应

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Soil aggregate stability is a key indicator of soil quality and susceptibility to water erosion. The water level fluctuation zone (WLFZ) of Three Gorges Reservoir (TGR) experiences hydraulic disturbances induced by rainfall, reservoir wave, and water-level fluctuation. Soil aggregate in this region has a unique mechanism of disintegration different from other terrestrial soils. The traditional methods of soil aggregate stability measurement cannot reveal the complex external factors of the soil in the WLFZ. In the present study, an attempt has been made to establish an approach mimicking the real situation in the WLFZ to deeply understand the effects of water movement and periodical wetting on soil aggregate stability in the WLFZ. The soil samples from different elevations were allowed to stay under wetting and wet-shaking conditions for 3 and 81 min, followed by a quantitative separation of disintegrated aggregates by wet-sieving. The mean differences between wetting and wet-shaking for the mean weight diameter (Delta MWD) were highly significant at all elevations for 81 min. Contrary, both treatments applied within a short time period disintegrated aggregates at the same magnitude. Additional to slaking, the kinetic energy applied to soil has induced a mechanical breakdown as a result of water movement. The difference of aggregate stability index (ASI) was highly significant among the elevations p < 0.001 and strongly significant between lower and upper elevations. The Cation Exchange Capacity (CEC) was the most predominant factor determining the stability of soil aggregates with r(2) = 0.61, 0.65, 0.69 (p < 0.05) and r(2) = 0.71, 0.7, 0.77 (p < 0.05) for ASI, GMD and MWD recorded after wetting and wet-shaking, respectively. Crucially, understanding different effects between arising impacts of water level fluctuations and periodical inundations on soil aggregate stability is a promise for future studies in areas experiencing similar conditions.
机译:土壤团聚体稳定性是土壤质量和对水蚀敏感性的关键指标。三峡水库(TGR)水位波动带(WLFZ)经历了降雨、水库波浪和水位波动引起的水力扰动。与其他陆地土壤不同,该地区的土壤团聚体具有独特的崩解机制。传统的土壤团聚体稳定性测量方法无法揭示WLFZ区土壤的复杂外部因素。本研究试图建立一种模拟WLFZ实际情况的方法,以深入了解水运动和周期性湿润对WLFZ土壤团聚体稳定性的影响。不同海拔高度的土壤样品在湿润和湿振条件下停留3和81分钟,然后通过湿筛定量分离崩解骨料。在所有海拔81分钟内,平均重量直径(Delta MWD)的湿润和湿振之间的平均差异非常显著。相反,两种处理在短时间内以相同的幅度分解骨料。除了崩解之外,由于水的运动,施加在土壤上的动能还导致了机械破坏。骨料稳定性指数(ASI)在海拔高度之间的差异极显著(p<0.001),在低海拔和高海拔高度之间的差异极显著。阳离子交换容量(CEC)是决定土壤团聚体稳定性的最主要因素,湿润和湿振后分别记录的ASI、GMD和MWD的r(2)=0.61、0.65、0.69(p<0.05)和r(2)=0.71、0.7、0.77(p<0.05)。至关重要的是,了解水位波动和周期性洪水对土壤团聚体稳定性产生的影响之间的不同影响,有助于在经历类似条件的地区进行未来的研究。

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