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Coe et al. (2016) and Aaron & Hungr (2016a) both invoked low basal friction due to entrainment and overriding of saturated soil to explain the dynamics of the West Salt Creek rock avalanche and the Avalanche Lake rock avalanche, respectively.
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Further research is required to understand the cause of classical monodominance, which likely means investigations into mechanisms that do not invoke major differences in soils to explain the visibly obvious differences in overlying vegetation.
The contribution of rhizomorphs as a highly efficient medium for water and mineral compounds uptake from soils seems to explain the presence of Hg and Ag in fruiting bodies of Armillaria solidipes (Falandysz et al. 2012e; J.F., unpublished).
Soil hydrology can, in turn, be used to explain soil features (soil morphology), distributions (soil geography) and ecosystem functions (dynamics).
The specific objectives of this paper were (i) to draw the VID semi-detailed soil map; (ii) to explain the variability of soil properties; and (iii) to map the main soil characteristics related to irrigation management.
Figure 9 clearly shows that the features of the observed H/V cannot be described using only the shallow V S profile, indicating the shallow soil is insufficient to explain the H/V.
None of the household factors we built to measure common eating habits or common exposures to cat or soil was able to explain that heterogeneity among households.
Here we develop a soil-stratigraphic model to explain the observed occurrence of multisequal soils mantling dominantly glacial landforms of southern continental Chile.
For example, the higher amount of plant available P in Ter Yde soils might seem to explain why aphids performed better on plants grown on soils from this region.
We investigated the fate of root and litter derived carbon in soil organic matter and dissolved organic matter in soil profiles, in order to explain mechanisms of short-term soil carbon storage.
Consequently we expected softwood- and hardwood-related deadwood effects on soil to be explained by unequal enrichment of phenolic substances.
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