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KMID : 1098420090170030204
Korean Journal of Medicinal Crop Science
2009 Volume.17 No. 3 p.204 ~ p.209
Assessment on Water Movement in Paddy-Upland Rotation Soil Scheduled for Ginseng Cultivation
Hur Seung-Oh

Kim Jeong-Gyu
Lee Yun-Jeong
Yeon Byung-Ryul
Ha Sang-Geon
Jeon Sang-Ho
Abstract
This study was conducted to assess water movement in paddy-upland rotation soil scheduled for ginseng cultivation
through the measurement of infiltration and permeability of soil water. Soil sample was divided with four soil layers. The first soil layer (to 30cm from top soil) was loamy sand, the second and the third soil layers (30~70§¯) were sand, and the
fourth (< 120§¯) was sandy loam. The soil below 130§¯ of fourth soil layer was submerged under water. The shear strength, which represents the resisting power of soil against external force, was 3.1 §æ in the first soil layer. This corresponded to 1/8 of those of another soil layer and this value could result in soil erosion by small amount of rainfall. The rates of infiltration and permeability depending on soil layers were 39.86 §¯ hr-1 in top soil, 2.34 §¯ hr-1 in 30~70 §¯ soil layer, 5.23 §¯ hr-1 and 0.18 §¯ hr-1 in 70~120 §¯ soil layer, with drain tile, and without drain tile, respectively. We consider that ground water pooled in paddy soil and artificial formation of soil layer could interrupt water canal within soil and affect negatively on water movement. Therefore, we suggest that to drain at 5 m intervals be preferable when it makes soil dressing or soil accumulation to cultivate ginseng in paddy-upland rotation soil to reduce failure risk of ginseng cultivation.
KEYWORD
Paddy-Upland Rotation, Ginseng, Water Movement, Soil
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