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In the absence of overlying materials on Mt. Arciano, the Avellino pumices provided a homogeneously developed soil with well-expressed andic soil properties.
As this vegetation developed, soil surface condition, as indicated by a nutrient cycling index, also progressed towards values found on nearby natural savannas.
The obtained results show that Turbic Cryosols from sorted patterned grounds featuring clear frost cracking, frost segregation, and cryoturbation are characterized by a lack of clearly developed soil horizons, loamy texture and low content of soil organic matter.
The lowest infiltration rate was measured for the Bw horizon of Haplic Cambisol, which had a poorly developed soil structure and a low fraction of large capillary pores and gravitational pores.
The developed soil model is divided into same sized mesh grids, and the strong ground motion at each grid point is calculated.
We compare the climate sensitivity of beech from a site with a shallow chalk soil with the sensitivity from a "typical" site in the same region, which has a deeper, more developed soil and a high water holding capacity.
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The desert regions have poorly developed soils of coarse texture containing many stones and unweathered rock fragments.
Glacial forefields host young, poorly developed soils with highly unstable environmental conditions.
In the semiarid areas bordering the desert, increased rainfall makes grass vegetation more plentiful, results in rocks becoming more weathered than in the desert, and produces better developed soils with a higher humus content.
Poorer developed soils were found at upper stratigraphic sequences (19th century) characterised by thick units of colluvium deposits, usually culminating sequences of short-lived continuous slackwater flood units.
Related to their greater age, they harbor higher plant diversity, more developed soils with greater soil organismal activity, as well as more diverse and dense assemblages of vertebrates and arthropods.
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