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- W2247925427 abstract "In order to investigate the effect of soil physical properties, runoff and infiltration water on soil erosion, soil samples were collected from 5 sites of dark brown soil(DBS), 6 sites of very dark brown volcanic ash soil(VDBAS), and 8 sites of black volcanic ash soil(BVAS) in Jeju. The relations between soil erosion and some physical characteristics of the soil were tested. The relationship between soil erosion and runoff was positively correlated, but infiltration water and saturated hydraulic conductivity were negatively correlated with soil erosion in all soils. In DBS, the soil erosion was negatively correlated with clay, clay/silt, clay+very fine sand, clay/(silt+very fine sand) and clay+fine sand(0.02-0.2 mm), but positively correlated with silt/clay. In BVAS, the soil erosion was negatively correlated with silt/clay and positively correlated with clay+fine sand (0.02-0.2 mm). The relationship between soil erosion and water stable aggregate was observed only in the DBS and VDBAS. Soil erosion in DBS was positively correlated with water stable aggregate (0.25-0.5 mm, 0.1-0.25 mm 0.25-0.5 mm, 0.1-0.25 mm 0.25-0.5 mm 0.5-1.0 mm), but the water stable aggregates (0.5-1.0 mm 1.0-2.0 mm >2.0 mm and 1.0-2.0 mm >2.0 mm) were prone to decrease soil erosion without statistical significancy. Soil erosion in VDBAS was positively correlated with water stable aggregate (0.1-0.25 mm, 0.25-0.5 mm and 0.1-0.25 mm 0.25-0.5 mm), but negatively correlated with water stable aggregate (0.5-1.0 mm 1.0-2.0 mm >2.0 mm and 1.0-2.0 mm >2.0 mm). In DBS and VDBAS, soil erosion decreased with increasing of soil organic matter content, but in BVAS, there was no relationship between soil erosion and organic matter content." @default.
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- W2247925427 date "2010-01-01" @default.
- W2247925427 modified "2023-09-24" @default.
- W2247925427 title "Soil erosion characteristics under rainfall simulator conditions of the Jeju soil in Korea." @default.
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