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Stability analysis of slope based on the coupling of well-point dewatering and chemical improvement slope stabilization. [PDF]
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The Leading Edge, 2010
We now understand the electrical double layer that exists between the minerals that form the rock matrix and the bulk electrolyte which saturates the pores of the rock, at least in the steady state. It is the presence of this double layer that allows the link between the electrical properties and the fluid-flow properties of the rock to exist.
Paul W.J. Glover, Matthew D. Jackson
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We now understand the electrical double layer that exists between the minerals that form the rock matrix and the bulk electrolyte which saturates the pores of the rock, at least in the steady state. It is the presence of this double layer that allows the link between the electrical properties and the fluid-flow properties of the rock to exist.
Paul W.J. Glover, Matthew D. Jackson
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2018
Borehole investigations allow practitioners to determine the nature and location of the different soil/rock layers, collect samples, carry out in situ tests and permeability tests, and, if necessary, install piezometers and other subsurface monitoring tools.
Kruse, Eduardo Emilio +3 more
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Borehole investigations allow practitioners to determine the nature and location of the different soil/rock layers, collect samples, carry out in situ tests and permeability tests, and, if necessary, install piezometers and other subsurface monitoring tools.
Kruse, Eduardo Emilio +3 more
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Resistivity Borehole Imaging in Challenging Borehole Environments
GEO 2010, 2010Until recently, the acquisition of resistivity borehole image data from well bores less than 6” in diameter has been impossible, due to the size of conventional borehole imaging tools currently available on the market. In addition, conventional deployment methods limit efficient rig time utilization and ultimately lead to higher risk and costs ...
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Borehole‐to‐borehole seam‐wave transmission
SEG Technical Program Expanded Abstracts 1983, 1983Charles C. Mosher, Iain M. Mason
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Symposium on the Application of Geophysics to Engineering and Environmental Problems 2016, 2016
Dave Walsh +14 more
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Dave Walsh +14 more
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Madras Agricultural Journal, 1919
Methods by which subterranean supplies of water may be made more available:- The water-bearing strata of the earth's crust may be broadly divided into three classes.- (1) Hard metamorphic rocks with fissures and cracks in them. (2) Stratified beds of rocks of varying degrees of porosity (3) massive or stratified deposits of sand or gravel.
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Methods by which subterranean supplies of water may be made more available:- The water-bearing strata of the earth's crust may be broadly divided into three classes.- (1) Hard metamorphic rocks with fissures and cracks in them. (2) Stratified beds of rocks of varying degrees of porosity (3) massive or stratified deposits of sand or gravel.
openaire +1 more source