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Another function of the pavement is to prevent weakening of the subsoil by moisture intrusion, especially from rainfall and frost.
This leaves preparation of the seedbed as the best opportunity to create desirable structure, in which large and stable pores extend from the soil surface to the water table or drains, ensuring rapid infiltration and drainage of excess or free water and promoting aeration of the subsoil.
The settlement of the subsoil was determined by the vertical deformation of the water bags.
Water bags were distributed around pile caps to create a model of the subsoil.
Compaction of the subsoil is an almost irreversible damage to the soil resource.
In this equation, (N65) is the equivalent N-value, (N) is the N-value of the subsoil, and (( {sigma}_v^{hbox )) is the effective overburden pressure of the subsoil (kN/m2) calculated in the approach at different depths.
The frozen of the subsoil such as its thermal relaxation during the summer are analysed.
However, it remains unclear to what degree previous 2-D inversions yielded a reliable image of the subsoil.
Therefore, prevention of subsoil compaction is the best way to preserve the structure and quality of the subsoil.
Unsaturated hydraulic conductivities of the subsoil below the biomat (Kss) were estimated from capillary curves and water content measurements.
The proposed procedure was applied to the analysis of the subsoil of the City of Turin (Northern Italy).
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