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Although the western part of the southern plains has a uniform volcanic origin, there are local differences in the colour, texture, and stone content of the region's soils.
The increase in stone content rapidly reduced the flow velocity.
Flow velocity increased with 0 15.23% of stone content but decreased at higher values.
Results indicated that stone content significantly affected flow velocity under increasing slope gradient.
We relate these findings to a larger stone content and a stronger macropore soil matrix interaction.
Maximum flow velocity of water was predicted at 15.23% of stone content.
Similar(37)
Soil C stocks were calculated by multiplying C concentration by bulk density, stone contents, and soil horizon thickness.
However, the available measures are more suitable to soils with low stone contents while there is currently no established method for stone-rich soils.
In this experiment, the large stone maximum particle size was reduced from 150 mm to 120 mm and the different large stone contents were 20%, 25 %, 30, and 35%.
The objective of this laboratory experiments was to measure water flow velocity over frozen slopes with different stone contents by using electrolyte trace method.
This study will help elucidate the hydrodynamics, soil erosion, and sediment transport behaviors of frozen or partially unfrozen hillslopes with different stone contents.
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