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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).
In addition, it quantifies the uncertainty reduction that can be achieved with increased density of soil sampling.
Moreover, the effects of water content and dry density of soil on the model parameters are analyzed in detail.
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.
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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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.
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).
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.
The results showed that: the soil bulk density of surface soil decreased and soil porosity and field capacity increased after afforestation with seabuckthorn.
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