Results 301 to 310 of about 702,691 (340)
Probabilistic failure assessment of bolt-stabilized pro-dip slopes considering shear effect. [PDF]
Wang DJ, Zhang YH, Cheng ZY, Wang YL.
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Instability mechanism of loess-mudstone landslides under rainfall infiltration conditions. [PDF]
Liu X+5 more
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Reductive degradation of carbon tetrachloride using tree leaf polyphenol-iron complexes for groundwater remediation. [PDF]
Lasagas RC+3 more
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Assessing the water quality hazard and challenges to achieving the freshwater goal in Sri Lanka. [PDF]
Shamsudduha M+8 more
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Proximity to Golf Courses and Risk of Parkinson Disease.
Krzyzanowski B+7 more
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Water Environment Research, 2008
Papers reviewed herein provide a general overview of groundwater quality around the world in 2010. These include groundwater quality survey and assessment in urban and rural areas, the impacts of land uses on groundwater quality, with a focus on groundwater contamination, pollution prevention, and remediation.
Bin Hua, John Yang, Baolin Deng
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Papers reviewed herein provide a general overview of groundwater quality around the world in 2010. These include groundwater quality survey and assessment in urban and rural areas, the impacts of land uses on groundwater quality, with a focus on groundwater contamination, pollution prevention, and remediation.
Bin Hua, John Yang, Baolin Deng
openaire +1 more source
Groundwater control by groundwater lowering
Geological Society, London, Engineering Geology Special Publications, 1986ABSTRACT When an excavation is to extend beneath the water table the ground conditions may be improved by lowering the level of the water table beneath the proposed base of the excavation. Groundwater lowering is accomplished by removing water from the ground at a faster rate than recharge can occur.
P.M. Cashman, F. G. Bell
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2012
Groundwater flows in the pores and fractures of soils and rocks, driven by changing mechanical and environmental boundary conditions, for example air temperature, humidity, and precipitation. Because the groundwater environment continuously changes, the steady--state condition is only a theoretical concept: the movement of water in soils and rocks is ...
PICARELLI, Luciano+5 more
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Groundwater flows in the pores and fractures of soils and rocks, driven by changing mechanical and environmental boundary conditions, for example air temperature, humidity, and precipitation. Because the groundwater environment continuously changes, the steady--state condition is only a theoretical concept: the movement of water in soils and rocks is ...
PICARELLI, Luciano+5 more
openaire +5 more sources