Soil texture dominated the infiltration process in soils with a higher sand content (> 15%), whereas bulk density dominated the infiltration process in soils experiencing the effects of compaction due to agricultural activity.
These aliphatic complexes formed during coprecipitation may play an important, though often underestimated, role in C stabilization in soils experiencing frequent redox fluctuations and often characterized by elevated soluble Fe2+ and DOC concentrations.
The most important information acquired from these previous test sections was the fact that the foundation soils experienced significant gains in shear strength due to the more uniform consolidation of the soft foundation material during and immediately following embankment construction.
The minimal values for both the resilient modulus and the failure strength were frequently achieved after the specimen was exposed to about 3 7 freeze thaw cycles, therefore, the resilient modulus and the failure strength of soils experienced seven freeze thaw cycles could be applied to the process of cold region engineering design.
Soils experienced fluctuating redox conditions throughout the 30 week study (Fig. S2A).
However, in the field, colloidal suspensions flow through a small number of preferential flow paths, and the soil experiences succession of rainfalls, interrupted by dry periods.
The reddened soil experienced the highest burning temperatures resulting in the loss of organic carbon (OC), the conversion of goethite to maghemite or hematite, the destruction of kaolin, and dehydroxylation and permanent collapse of vermiculite and chlorite.
However, this approach ignores the fact that the remaining soil experiences different stress histories before and after scour, which can be expected to change the properties of the remaining soil.
On the other hand, following the geological idealisation that any soil experiencing the greatest stress in its history is normally consolidated, the second proposition suggests that the NCL also includes the initial portion of the compression curve before grain crushing becomes dominant.
