한국산림과학회지 (Journal of Korean Society of Forest Science)

  • 제108권3호
  • /
  • Pages.311-321
  • /
  • 2019
  • /
  • 2586-6613(pISSN)
  • /
  • 2586-6621(eISSN)
한국산림과학회 (Korean Society of Forest Science)
권호 표지
DOI QR코드

DOI QR Code

GIS를 이용한 땅밀림지 특성 분석: 산지경사 및 산사태위험등급을 중심으로

Analysis of GIS for Characteristics on the Slow-Moving Landslide: With a Special Reference on Slope and Grade of Landslide

  • 박재현 (경남과학기술대학교 산림자원학과) ;
  • 서정일 (공주대학교 산림자원학과) ;
  • 이창우 (국립산림과학원 산림방재과)
  • Park, Jae-Hyeon (Department of Forest Resources, Gyeongnam National University of Science and Technology) ;
  • Seo, Jung Il (Depertment of Forest Resources, Kongju National University) ;
  • Lee, Changwoo (Division of Forest Disaster Management, National Institute of Forest Science)
  • 투고 : 2018.11.19
  • 심사 : 2019.01.28
  • 발행 : 2019.09.30
PDF 다운로드
⟨ 이전 논문 다음 논문 ⟩

초록

이 연구는 땅밀림위험등급을 구축하기 위하여 수행되었다. 땅밀림지의 평균산지경사는 $23.8^{\circ}$($11.8^{\circ}{\sim}37.0^{\circ}$), 땅밀림지 내에서 미세지형지의 평균사면경사는 $23.5^{\circ}$ ($10.7^{\circ}{\sim}41.5^{\circ}$)로 미소한 차이가 있는 것으로 분석되었다. 땅밀림지 및 땅밀림 재발생지에서 땅밀림지 내 등고선 간격과 땅밀림지 내 미세지형지의 등고선 간격은 5% 수준에서 유의한 결과를 나타내었다. 산사태위험등급에 포함되지 않는 땅밀림지는 전체 땅밀림지 중 1등급이 14개소(약 38.0%), 2등급이 6개소(약 16.0%), 3등급과 4등급이 각각 5개소(약 14.0%), 5등급이 16개소(약 43.0%), 산사태위험지등급 외 지역이 9개소(약 24.0%)이었다. 땅밀림지 중 산사태위험 1~5등급으로 지정되지 않은 면적 비율이 50.0% 이상인 지역은 8개소(약 22.0%), 20.0%~50.0% 이상인 지역은 18개소(약 49.0%), 20.0% 이상인 지역은 26개소(약 70.0%)이었다.

This study was carried out to establish basic data for the development of slow-moving landslide hazard classes. Mountain slopes in slow-moving landslide areas ranged from $11.8^{\circ}$ to $37.0^{\circ}$ with a mean slope of $23.8^{\circ}$. However, the slope inclination of microtopography in slow-moving landslide areas was slightly different, with a mean slope of $23.5^{\circ}$ ($10.7^{\circ}{\sim}41.5^{\circ}$) compared with the mountain slope. There was a significant difference (p < 0.05) between the contour intervals of microtopography and the contour intervals of the slow-moving landslide areas. Among all the slow-moving landslide areas examined, 14 plots (approximately 38.0%) were classified into landslide hazard class I, 6 plots (approximately 16.0%) into landslide hazard class II, 5 plots (approximately 14.0%) into landslide hazard class III and IV, and 16 plots (approximately 43.0%) into landslide hazard class V, whereas 9 plots (approximately 24.0%) fit the no landslide hazard class.

키워드

참고문헌

  1. Anderson, M.G. and Richards, K.S. 1987. Slope stability. Wildly and Sons. pp. 210.
  2. Auzet, A.V. and Ambroise, B. 1996. Soil creep dynamics, soil moisture and temperature conditions on a forested slope in the granitic Vosges Mountains, France. Earth Surface Processes and Landforms 21(6): 531-542. https://doi.org/10.1002/(SICI)1096-9837(199606)21:6<531::AID-ESP606>3.0.CO;2-B
  3. Biswajeet, P. and Lee, S.R. 2010. Landslide susceptibility assessment and factor effect analysis: backpropagation artificial neural networks and their comparison with frequency ratio and bivariate logistic regression modelling. Environmental Modelling & Software 25: 747-759. https://doi.org/10.1016/j.envsoft.2009.10.016
  4. Choi, K. 2018. Geological characteristics of land creep in korea. Korean Society of Forest Environment Research 21: 108-117.
  5. Culling, W.E.H. 1963. Soil creep and the development of hillside slopes. The Journal of Geology 71(2): 127-161. https://doi.org/10.1086/626891
  6. Jau, J.G., Park, S.J., Son, D.S. and Joo, S.H. 2000. The effects of geological and topographical features on landslide and land-creep. Journal of Korean Forest Society 89(3): 323-334.
  7. Jeong, J.H., Koo, K.S., Lee, C.H. and Kim, C.S. 2002. Physico-chemical properties of korean forest soils by reasons. Journal of Korean Forest Society 91(6): 694-700.
  8. Keijourou, N. 1964. Disaster conference, Land Creep. 1(1): 5-7.
  9. Kim, H.G. 2004. Slope stability and characteristics of shallow landslide occurred in granite hillslopes. Master. Thesis, KyungHee University, Seoul, Korea. pp. 150.
  10. Korea Forest Service. 2018. http://www.forest.go.kr/newkfsweb/html/HtmlPage.do?
  11. Lee, C.W., Woo, C.S. and Youn, H.J. 2009. Development and verifying of calculation method of standard rainfall on warning and evacuation for forest soil sediment disaster in mountainous area by using tank model. Journal of Korean Forest Society 98(3): 272-278.
  12. Lee, C.W., Woo, C.S. and Youn, H.J. 2011. Analysis of debris flow hazard zone by the optimal parameters extraction of random walk model. Journal of Korean Forest Society 100(4): 664-671.
  13. Lee, C.W., Kim, D.Y., Woo, C.S., Kim, Y.S., Seo, J.P. and Kwon, H.J. 2015. Construction and operation of the national landslide forecast system using soil water index in republic of korea. Journal of Korean Society Hazard Mitig 15(6): 213-221. https://doi.org/10.9798/KOSHAM.2015.15.6.213
  14. Matsukura, Y. and Tanaka, Y. 1983. Stability analysis for soil slips of two gruss slope in southern abukuma mountains, Japan. Transactions, Japanese Geomorphological Union 4: 229-239.
  15. Montgomery, D.R., Sullivan, K. and Greenberg, H.M. 1998. Regional test of a model for shallow landslide. Hydrological Processes 12: 943-955. https://doi.org/10.1002/(SICI)1099-1085(199805)12:6<943::AID-HYP664>3.0.CO;2-Z
  16. National Institute of Forest Science. 2017. A Precedent Investigation of the Foreign and in the country status of landslide by land creeping, rehabilitation and management. National Institute of Forest Science Report. pp. 153.
  17. National Geographic Infomation Institute. 2018. http://map.ngii.go.kr/
  18. Park, J.H. 2015. Analysis on the characteristics of the landslide - with a special reference on geo-topographical characteristics -. Journal of Korean Forest Society 104(4): 588-597. https://doi.org/10.14578/jkfs.2015.104.4.588
  19. Park, J.H. 2016. The actual conditions and management of land creep in korea. Korean Society of Forestry Environment Research 19: 40-50.
  20. Park, J.H., Choi, K., Lee, S.G., Ma, H.S., Lee, J.H. and Woo, B.M. 2003. Analysis on the characteristics of the landslide in nasamri(I) - with a special reference on geo-topographical characteristics -. Journal of Korean Forest Society 92(3): 246-253.
  21. Park, J.H., Choi, K., Bae, J.S., Ma, H.S. and Lee, J.H. 2005. Analysis on the characteristics of the landslide in maeri(I) - with a special reference on geo-topographical characteristics -. Journal of Korean Forest Society 94(3): 129-134.
  22. Park, J.H. 2018. What's land creep. Korean Society of Forest Environment Research 21: 96-107.
  23. Ranjan, K.D., Shuichi, H., Atsuko, N., Minoru, Y., Takuro, M. and Katsuhiro, N. 2008. GIS-based weights-of-evidence modeling of rainfall-induced landslides in small catchments for landslide susceptibility mapping. Environ Geology 54: 311-324. https://doi.org/10.1007/s00254-007-0818-3
  24. Shunji, I. 1978. Soil creep measurements in khumbu. Journal of the Japanese Society of Snow and Ice 40: 60-63. https://doi.org/10.5331/seppyo.40.Special_60
  25. Takaya, S. 2017. Facts of landcreep. Nokdo Publication. pp. 255.
  26. Tomio, H.Z., Sohei, A., Takeshi, N. and Tosihiko, S.T. 1990. Landslide disaster in temanggung, Indonesia. Journal of the Japan Society of Erosion Control Engineering 42(6): 57-59.
  27. Woo, B.M. 1992. Erosion control and conservation. Hayngmunsa. pp. 310.
  28. Woo, B.M., Park, J.H., Choi, H.T., Jeon, G.S. and Kim, K.H. 1996. A study on the characteristics of the landslide in hyuseok-dong(I) - topographical characteristics and surface displacement -. Journal of Korean Forest Society 85(4): 565-570.
  29. Woo, C.S., Kwon, H.J., Lee, C.W. and Kim, K.H. 2014. Landslide hazard prediction map based on logitic regression model for applying in the whole country of south korea. Journal of Korean Society Hazard Mitig 14(6): 117-123. https://doi.org/10.9798/KOSHAM.2014.14.6.117