소형 풍동을 이용한 토양의 풍식 가능 입경 분석
Experimental Investigation on Particle Size of Soils Erodible by Wind using Portable Wind Erosion Tunnel
1
조회
0
다운로드
1
인용
0
참고문헌
키워드
초록
The purpose of this study was to investigate maximum and minimum grain size which eroded by wind according to soil and windconditions, such as top soil water content, roughness, land slope, wind velocity and proportion of grain size under 0.84mm. Forperforming this study, portable wind erosion tunnel was designed and utilized during field test, which facilitated measuring actual winderosions under artificially controlled wind conditions. In the result, maximum, minimum grain size had strong negative correlation withroughness while weak positive correlation with wind velocity. Also, Slope which means the effect of gravity also influence grain sizeerodible by winds. Based on these results, regression equations were suggested for predicting maximum and minimum grain sizes byusing multiple linear regression analysis from SPSS 20.0. The equation for maximum grain size erodible by winds showed a goodagreement with the observed data with R2=0.896. Other equation for minimum grain size had R2=0.777.
Abstract
The purpose of this study was to investigate maximum and minimum grain size which eroded by wind according to soil and windconditions, such as top soil water content, roughness, land slope, wind velocity and proportion of grain size under 0.84mm. Forperforming this study, portable wind erosion tunnel was designed and utilized during field test, which facilitated measuring actual winderosions under artificially controlled wind conditions. In the result, maximum, minimum grain size had strong negative correlation withroughness while weak positive correlation with wind velocity. Also, Slope which means the effect of gravity also influence grain sizeerodible by winds. Based on these results, regression equations were suggested for predicting maximum and minimum grain sizes byusing multiple linear regression analysis from SPSS 20.0. The equation for maximum grain size erodible by winds showed a goodagreement with the observed data with R2=0.896. Other equation for minimum grain size had R2=0.777.
참고문헌 (12)
- Bitog, J. P., "Numerical simulation of an array of fences in Saemangeum reclaimed land", Atmospheric Environment, 43(2009), pp.4612~4621 (2009)
- Bouyoucos, G., "The alcohol method for determining moisture content of soils", Soil Science, 32(3), pp.173~180 (1931)
- Buschiazzo, D. E., "Validation of WEQ, RWEQ and WEPS wind erosion for different arable land management systems in the Argentinean Pampas", Earth Surface Processes and Landforms, 33(12), pp.1839~1850 (2008)
- Fister, W, "Wind erosion in the central Ebro Basin under changing land use management. Field experiments with a portable wind tunnel", Journal of Arid Environments, 73(2009), pp.996~1004 (2009)
- Hong, S. W, "Measurement and Prediction of Soil Erosion in Dry Field using Portable Wind Erosion Tunnel", Biosystems Engineering (2012)
- Park, H. K., "Environmental damages and control measures by highland agriculture – study on system improvement", 박사, pp.2006
- Saleh, A., "Soil roughness measurement : Chain method", Journal of Soil and Water Conservation, 48(6), pp.527~529 (1993)
- Webb, N. P., "Approaches to modeling land erodibility by wind", Progress in Physical Geography, 2009, pp.1~27 (2009)
- Zobeck. T. M., "Soil properties affecting wind erosion", Journal of Soil and Water Conservation, 46(2), pp.112~118 (1991)
- Lianyou, L., "Determination of erodible particles on cultivated soils by wind tunnel simulation", Chinese Science Bulletin, 43(19), pp.1646~1651 (1998)
- Bolte, K., "Determination of critical soil water content and matric potential for wind erosion", Journal of Soils Sediments, 11, pp.209~220 (2011)
- Lyles, L., "Basic wind erosion process", Agriculture, Ecosystems and Environment, 22-23, pp.91~101 (1988)
