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Erosion probability model of base-soil particle migration into a granular filter under local flow

International Journal of Sediment Research 2019年第5期34卷 455-460页

作者： Yuan Wei Mei-li Zhan Qing-fu Huang Jin-chang Sheng Yulong Luo Qing Zhou College of Water Conservancy and Hydropower Engineering Hohai University

To avoid soil erosion, filters often are installed in the downstream cross section of dams. However, the probability of piping failure and the filter effect both are related to the soil pore network. Previous erosion probability models for a base soil-filter system do not consider the effect of local flow. Therefore, in this study, an improved erosion probability model is established, in which the deviation between the main flow direction of the soil and the local flow direction in the filter was considered based on a previous model. The improved model was validated by numerical simulation. The erosion probability was found to affect the reasonable evaluation of filter effects and the optimal selection of filter thickness. The controlling constriction size in a granular filter was increased to D*c= Dc5 with a filter thickness of 59 Dm.

关键词： Granular filter Pore network Erosion probability local flow Deviation probability

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Quantification of the Mixture of Hydrothermal and Fresh Water in Tectonic Valleys

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Journal of Earth Science 2020年第5期31卷 1007-1015页

作者： Janete Moran-Ramirez Jose Ivan Morales-Arredondoc Maria Aurora Armienta-Hernandez Jose Alfredo Ramos-Leal National Council of Science and Technology National Autonomous University of MexicoInstitute of GeophysicsScientific Research CircuitUniversity CityCoyoacan 04150Mexico CityMexico National Autonomous University of Mexico Institute of GeophysicsUniversity CampusMexico CityMexico Potosino Institute for Scientific and Technological Research 78216 San Luis PotosiS.L.P.Mexico

This study was conducted to identify the origin, hydrogeochemical processes and evolution of groundwater in a tectonic valley. This study was carried out with the aim of quantifying the proportions of groundwater flows contributing to the water chemistry abstracted in a zone of convergence favored by the presence of active faults. The study area is located in the Trans-Mexican Volcanic Belt. End members methodology was applied to identify the mixing of hydrothermal with fresh groundwater, where changes in the aquifer geology result in distinct groundwater chemical signatures. Ternary mixing was quantified using conservative elements. Moreover, other evolutionary processes, such as ion exchange and silicate weathering occur due to changes in the geology of the area. In ternary mixing, each of the end members is associated with the lithology through which it circulates. The local flow contributes 70% of the water to the system, the intermediate flow contributes 14%, and the regional flow contributes 16%. Three types of water are produced: Na-HCO3, due to the interaction of water with volcanic rocks of rhyolitic composition, Na-Mg-HCO3, due to the interaction of water with volcanic rocks of basaltic-andesite composition, and Ca-HCO3, due to the interaction of water with sedimentary calcareous rocks.

关键词： hydrogeochemistry ternary mixing end members conservative elements local flow Mexico

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