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RUSLE 모델에 의한 군사격장 피탄지 토양유실량 평가: 토양 유실과 오염 화약물질 이동 상관성Assessment of Soil Loss at Military Shooting Range by RUSLE Model:Correlation Between Soil Loss and Migration of Explosive Compounds

Other Titles
Assessment of Soil Loss at Military Shooting Range by RUSLE Model:Correlation Between Soil Loss and Migration of Explosive Compounds
Authors
공효영이광표이종열김범준이아름배범한김지연
Issue Date
2012
Publisher
한국지하수토양환경학회
Keywords
Soil loss; GPS-TS; RUSLE; RDX; TNT
Citation
지하수토양환경, v.17, no.6, pp.119 - 128
Journal Title
지하수토양환경
Volume
17
Number
6
Start Page
119
End Page
128
URI
https://scholarworks.bwise.kr/gachon/handle/2020.sw.gachon/16995
ISSN
1598-6438
Abstract
The applicability and accuracy of Revised Universal Soil Loss Equation (RUSLE) model on the estimation of soil loss at impacted area of shooting range was tested to further the understanding of soil erosion at shooting ranges by using RUSLE. At a shooting range located in northern Kyunggi, the amount of soil loss was estimated by RUSLE model and compared with that estimated by Global Positioning System-Total Station survey. As results, the annual soil loss at a study site (202 m long by 79 m wide) was estimated to be 2,915 ton/ha/year by RUSLE and 3,058 ton/ha/year by GPS-TS survey, respectively. The error between two different estimations was less than 5%, however, information on site conditions should be collected more to adjust model coefficients accurately. At the study shooting range, sediments generated by rainfall was transported from the top to near the bottom of the sloping face through sheet erosion as well as rill erosion, forming a gully along the direction of the storm water flow. Coarser fractions of the sediments were redeposited in the limited area along the channel. Distribution characteristics of explosive compounds in soil before and after summer monsoon rainfall in the study area were compared with the erosion patterns. Soil sampling and analyses results showed that the dispersion of explosive compounds in surface soil was consistent with the characteristics of soil erosion and redeposition pattern of sediment movements after rainfalls.
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