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As a result, they also show increases in clay content and in the extent of profile development from weathering of the loess particles.
Associated with the increments were mostly significant increases in clay dispersion rates at depths 0 10, 10 20 and 20 40 cm.
Clay content, including similar topsoil clay contents, similar subsoil clay contents and similar increases in clay content from topsoil to subsoil; Silt content, being high relative to the values for most South African soils, but common for Oakleaf soils.
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Additionally, at approximately 650 BP a marked increase in clay and silt deposition occurred.
This increase in C with depth in the soil can be attributed to an increase in clay content and C leaching resulting in stable carbon clay complexes.
However, with a systematic increase in clay loading, the dispersed clay structure of the nanocomposites changes from a highly delaminated to a flocculated and then to a stacked intercalated one.
It has been observed that the ionic conductivity of the nanocomposite gel polymer electrolytes increases with the increase in clay loading and attains a maximum value of 1.3 × 10−3 S/cm at room temperature as revealed by ac impedance spectroscopy.
Due to an increase in clay concentration, van der Waals interactions dominated polymer clay interactions resulting in a finite expansion of silicate interlayers and retention of clay structure.
It is obvious from the graph that increase in clay concentration has negative effects on sample H so that in the case of 0.45 wt% increasing clay concentration, solution viscosity decreased.
Dramatic rise in earthworm densities coupled with remarkable increase in clay contents and decrease in sand contents in T 3 plots compared to T 0 and other treatment plots are noticeable.
Increase in clay concentration from 16 to 20 wt% increases the basal spacing but the order is retained that appeared in the form of small peaks (Fig. 1) resulting in intercalated nanocomposites.
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