Impact of soil compaction degree modulated by initial water content on maize root phenotype and hydraulic properties. [PDF]
Fu Y, Si Z, Ma S, Cheng Y, Liu Z, Gao Y.
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Airborne geophysical imaging of freshwater reservoir beneath the eastern margin of Great Salt Lake. [PDF]
Zhdanov MS +4 more
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Sodium Silicate Grouting: Mechanisms, Environmental Impacts, and Research Directions. [PDF]
Valibeknejad M +6 more
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Estimating seepage in heterogeneous earthfill dams on permeable foundations using explainable machine learning. [PDF]
Sayed Ahmed MM +4 more
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Rainfall and Temporal Influences on the Hydrodynamics of a Vertical Subsurface Flow Constructed Wetland Treating Domestic Sewage. [PDF]
Silva G, da Silva Júnior ÉD.
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Evaluation of Hydraulic Conductivity Functions of Saturated Soft Soils [PDF]
Hydraulic conductivities of soils rely significantly on three factors, the properties of their pore water, the relative quantity of their pore water, and changes in their pore structure. For saturated soft soils, that demonstrate a considerable degree of alteration in pore structure during densification, it is important to consider their volume ...
Mishra, Partha Narayan +2 more
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Soil saturated hydraulic conductivity plays a crucial role in the fields of hydrology, geotechnical and geological engineering. This study investigated the relationship between root characteristics and soil saturated hydraulic conductivity in a grassed ...
Qing Cheng +2 more
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SATURATED AND UNSATURATED HYDRAULIC CONDUCTIVITY OF SWELLING CLAYS
Soil Science, 1986The theory of water flow in swelling clays may be developed in a space coordinate system at rest, assuming that the flux of clay particles can be defined by the space gradients of potential responsible for the movement of clay particles, which is related to the gradients of water potential.
M. NAKANO, Y. AMEMIYA, K. FUJII
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VARIABILITY OF SATURATED HYDRAULIC CONDUCTIVITY IN A GLOSSAQUIC HAPLUDALF WITH MACROPORES
Soil Science, 1988The spatial variability of saturated hydraulic conductivity was measured in situ in a clayey soil with macropores. Ksat was determined at 37 equally spaced transect sampling locations using five different-sized, in situ soil columns.
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