Results 241 to 250 of about 35,940 (305)
Multiscale microscopic pore structure characterization and storage-flow coupling mechanisms in ultra-low permeability tight sandstone reservoirs. [PDF]
Sci RepLi CL +5 more
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A new method for determining the pore water pressure around twin shallow circular tunnels. [PDF]
Sci RepZhan T, Shan S, Wang C, He P, Zou J.
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Beyond Foundation Seepage : Hydrogeology, Seepage and GISTM
, 2023 The Global Industry Standard for Tailings Management (GISTM) and the associated Compendium (Oberle et al., 2020) contain numerous references to specific scientific streams that are required to inform the design, construction, operation, and management of tailings storage facilities (TSFs). These scientific streams include hydrogeology and geochemistry,
Keizer, Jonathan
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Impact of two-dimensional seepage flow on sediment incipient motion under waves
Applied Ocean Research, 2021 A small seepage could cause significant changes to the hydrodynamic gradient and further enhance the sediment incipient motion and scour. However, most previous studies either ignored the influence of seepage or only considered the upward seepage in the ...
Hualing Zhai +2 more
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Seepage Meters in Seepage and Recharge Studies
Journal of the Irrigation and Drainage Division, 1963A falling-head theory and field procedures are presented for measuring seepage and hydraulic conductivity of bottom materials in canals or ponds with seepage meters. Manometer techniques are used for measuring falling head. The method is applicable to uniform bottoms and to material that is underlain by much more, or much less, permeable soil.
Herman Bouwer, R. C. Rice
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1995
As a result of the hydrological cycle (rainfall, infiltration) it is inevitable that the voids between soil particles will fill with water until they become fully saturated. There then exists a zone of saturation below ground level the upper surface of which is called the water table.
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As a result of the hydrological cycle (rainfall, infiltration) it is inevitable that the voids between soil particles will fill with water until they become fully saturated. There then exists a zone of saturation below ground level the upper surface of which is called the water table.
openaire +1 more source
Models for predicting the seepage velocity and seepage force in a fiber reinforced silty soil
Computers and Geotechnics, 2016 Randomly reinforced soil is used in hydraulic projects such as temporary canals, earth dams, stream restoration and so on for controlling seepage. This paper presents an investigation into the effect of random reinforcement on the seepage velocity and ...
A R Estabragh +2 more
exaly +1 more source