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However, the effect of CWD on nitrogen (N) cycling in reclaimed oil sands soils has not been studied.
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While there is no dynamic effect of capillary pressure for fine-grained sands (soil samples).
Interior Flanders comprises most of East and West Flanders and has sand-silt or sand soils.
As a consequence, clay is relatively impervious, while sand soils can absorb plenty of water.
Extreme heat causes the water to evaporate, leaving behind clays and sand soils with a high concentration of minerals.
For loamy sand soils, application of zeolite effectively reduced soil hydraulic conductivity.
The mean percentages of Cd2+ reduction for clay loam and loamy sand soils were equal to 76.41% and 12.24%, respectively.
Data used in this study consisted of 109 CPT-SPT pairs for sand, sandy silt, and silty sand soils.
A two-dimensional unsaturated/saturated groundwater flow model was used to simulate a homogeneous soil layer for sand and loamy sand soils packed at various bulk densities, ρb.
A total of 126 CPT-PMT pairs of desert dune sand soils were used to develop those formulas.
OMW application influences the actinobacterial community structure only in loamy sand soils, indicating soil-dependent effects [ 18].
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