Conservation tillage facilitates the accumulation of soil organic carbon fractions by affecting the microbial community in an eolian sandy soil. [PDF]
Li YM +6 more
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Effects of γ-polyglutamic acid on grassland sandy soil properties and plant functional traits exposed to drought stress. [PDF]
Skalski T +9 more
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Impact of some amendments on kinetics of leaching dissolved organic carbon and ammonium in calcareous sandy soil under vinasse addition. [PDF]
Amin AEAZ.
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Long-Term Benefits of Cenchrus fungigraminus Residual Roots Improved the Quality and Microbial Diversity of Rhizosphere Sandy Soil through Cellulose Degradation in the Ulan Buh Desert, Northwest China. [PDF]
Li J +12 more
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Abstract The vertical distribution of free and residual aviation gasoline, a light nonaqueous phase liquid (LNAPL), through the capillary fringe of a uniform, medium sand is measured and used to calibrate an existing model. The total saturation profile is governed by a classical moisture retention characteristic, with the matric ...
Ostendorf, DW, RICHARDS, RJ, BECK, FP
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Instability Behaviour for Sandy Soils
Geo-Frontiers 2011, 2011The concept of collapse line, CL, or instability line, IL have been reported in literature for analysing instability behaviour of sands under undrained shearing. The similarity, but different implications of these two concepts sometimes led to some confusion.
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Soil and environmental issues in sandy soils
Earth-Science Reviews, 2020Abstract Sandy soils are widely distributed across the world. Due to the growing global population and urbanization, these soils are increasingly used to provide food, feed, fiber, energy, and other services to our society. In this paper, we summarize some recent studies on sandy soils and review the main soil and environmental issues related to the ...
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Hydraulic Conductivity Prediction for Sandy Soils
Groundwater, 2004Abstract The potential for petroleum‐contaminated soils to impact ground water is evaluated using the soil leachability model in South Carolina and Georgia. In this model, the Green and Ampt (1911) equation is used to estimate unsat‐urated flow with saturated hydraulic conductivity (
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