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Biophysical characteristics of the species vary based on peat depth, soil saturation, and fire history.
Experimental variables included subjects (people), soil depth, soil type, moisture content, and compaction level.
Variability of soil depth, soil effective friction angle, and soil cohesion were considered assuming a normal distribution.
The microtopographical differences in polygonal geomorphology produce heterogeneity in permafrost depth, soil temperature, soil moisture, soil geochemistry, and plant distribution.
At each sampling site near Tanana, the surface organic layer was excavated in July 2017 to create 30 cm depth soil pits.
For example, Blanco-Canqui et al. [5] reported that in the 7.5- to 45-cm soil depth, soil aggregate stability decreased with an increase in N application.
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Total soil C was influenced by soil depth, land use, soil type, soil drainage class, and geologic unit.
This study adopts the local and global sensitivity analyses to study the influence of the soil-tunnel-building system characters (e.g. soil properties, building's stiffness and position, tunnel volume-loss and embedment depth, soil-building interface properties) on the settlement and tilt of building.
Similar patterns were observed at subsurface 5 15-cm depth soils.
The objectives were met by collecting AS/SVE exhaust gas samples and vadose zone air from multi-depth soil vapor probes.
Then, the model was applied to simulate the vertical flow across a 3-m-depth soil during a 53-year period under variable climate conditions.
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