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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.
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.
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 experiments were performed under slope gradients of 5°, 10°, 15°, and 20°; flow discharge rates of 1, 2, 4, and 8 L/min; and stone contents of 0%, 10 %, 20, and 50% on mand basis.
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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.
Stone content was assessed based on field observations based on the menu of the Munsell Soil Color Chart.
Flow velocity increased with 0 15.23% of stone content but decreased at higher values.
We relate these findings to a larger stone content and a stronger macropore soil matrix interaction.
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