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Titlebook: Water Circulation in Rocks; Laura Scesi,Paola Gattinoni Book 2010 Springer Science+Business Media B.V. 2010 Fractures.Hydrogeological risk

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發(fā)表于 2025-3-21 18:49:22 | 只看該作者 |倒序瀏覽 |閱讀模式
書目名稱Water Circulation in Rocks
編輯Laura Scesi,Paola Gattinoni
視頻videohttp://file.papertrans.cn/1021/1020928/1020928.mp4
概述Investigates water circulation in rocks which is of primary importance for civil, environmental and mining engineering.Studies aquifers in rocks that have not been studied much because the medium is c
圖書封面Titlebook: Water Circulation in Rocks;  Laura Scesi,Paola Gattinoni Book 2010 Springer Science+Business Media B.V. 2010 Fractures.Hydrogeological risk
描述.Understanding water circulation in rocks represents a very important element to solving many of the problems linked with civil, environmental and mining engineering. This book offers a synthesis of the actual knowledge about the fluid flow in rocks:..- from the medium characterization and the structural geological survey to the generation of stereonets;..- the evaluation of the hydrogeological parameters using either deterministic or probabilistic methodologies;..- the evaluation of the preferential flow direction considering the change of the hydrogeological structures;..- the methods and models used to simulate the flows...Three case studies are provided; water circulation and slope instability, hydrogeological risk linked with tunnelling, and hydrogeological risk linked with road construction..
出版日期Book 2010
關鍵詞Fractures; Hydrogeological risk; Permeability; Preferential Flow Direction; groundwater; hydrogeology
版次1
doihttps://doi.org/10.1007/978-90-481-2417-6
isbn_softcover978-94-024-0482-1
isbn_ebook978-90-481-2417-6
copyrightSpringer Science+Business Media B.V. 2010
The information of publication is updating

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Hydraulic Conductivity Assessment,ontinuities, the exact knowledge of their distribution and their characteristic parameters is fundamental to finding the features that describe the fluid flow, in particular, as far as the hydraulic conductivity assessment is concerned (that is the capability of a rock mass to be run through by wate
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Methods and Models to Simulate the Groundwater Flow in Rock Masses,xample, to correlate groundwater flow in the rock mass with the development of slope instability phenomena), requires the development of a model of the groundwater flow within the discontinuity network, according to specific boundary conditions. Quite often, the complexity of the problem sets limits
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Influence of Joint Features on Rock Mass Hydraulic Conductivity,icular, the water flow inside a single discontinuity is ruled by aperture and roughness, whereas the rock mass hydraulic conductivity also depends on the frequency and persistence of joints. Those features are extremely variable in space due to the heterogeneity of the rock mass system. The definiti
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