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Additionally, the effects of the slide width, the buried depth of pipelines, the internal friction angle of soils, the cohesion of soils and the bulk density of soils are investigated through parametric studies.
K, clay content and the earthworm density of soils.
Bulk density of soils at FC were measured by drying 100 cm3 of soil (four replicates) at 105 °C for 3 days, and were equal to 1.45 and 1.34 g of dry soil per cm3.
Similar to the particle density, the bulk density of soils of the study area showed significant variations due to land uses (P ≤ 0.01), soil depths (P ≤ 0.01) and interaction effects of land uses by soil depth (P ≤ 0.01) (Table 1).
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The density of soil macrofauna changed dramatically according to the chronosequence.
Namely, for density of soil organic carbon: forest > grassland > shrub grassland > shrub desert > desert; for density of soil inorganic carbon: forest, grassland < shrub grassland < shrub desert < desert (P < 0.05 in all cases).
Moreover, the effects of water content and dry density of soil on the model parameters are analyzed in detail.
In addition, it quantifies the uncertainty reduction that can be achieved with increased density of soil sampling.
The influences of pile embedment depth, relative density of soil, and arrangement of piles in a group on the uplift capacity of piles are investigated.
In the dry season, total density of soil macrofauna ranged from 1265 ± 308 individuals m−2 in F sites to 1924 ± 436 individuals m−2 in AF < 2 sites.
We manipulated the presence and bulk density of soil and added Galleria mellonella baits within capped and perforated 15 mL centrifuge tubes.
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