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

enamel

書目名稱Water Circulation in Rocks影響因子(影響力)




書目名稱Water Circulation in Rocks影響因子(影響力)學(xué)科排名




書目名稱Water Circulation in Rocks網(wǎng)絡(luò)公開度




書目名稱Water Circulation in Rocks網(wǎng)絡(luò)公開度學(xué)科排名




書目名稱Water Circulation in Rocks被引頻次




書目名稱Water Circulation in Rocks被引頻次學(xué)科排名




書目名稱Water Circulation in Rocks年度引用




書目名稱Water Circulation in Rocks年度引用學(xué)科排名




書目名稱Water Circulation in Rocks讀者反饋




書目名稱Water Circulation in Rocks讀者反饋學(xué)科排名

萬花筒

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

kyphoplasty

離開就切除

Bother

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

勤勞

Memorial

哀悼

暫時過來

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

Bernstein-test