• Proceedings of the KSEEG Conference
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• 2007.04a
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• pp.200-200
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• 2007

• Proceedings of the Korea Water Resources Association Conference
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• 2011.05a
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• pp.295-299
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• 2011

자연계에서 토양의 침식 및 퇴적 반복적 과정은 매우 복잡한 형태로 발생하며, 호우로 인한 토사유출은 유역의 지형 및 지질학적 특성과 수문기상학적 특성 등에 의해 매우 민감하게 반응한다. 즉, 토양 침식 및 퇴적은 유역의 형상, 토양종류, 토지 이용 및 피복상태, 강우사상 등에 따라 시 공간적 분포가 다양하게 변화한다. 따라서 유역내 침식 및 퇴적의 시·공간적 변동성을 분석하기 위해서는 지형학적 특성인자와 수문기상학적 특성인자에 따른 유역내 수문학적 응답을 이해해야 한다. 본 연구에서는 분포형 강우-유사-유출 모형을 이용하여 용담댐 상류 천천유역을 대상으로 Strahler 하천차수구분법에 의해 유역을 차수별 소유역으로 구분하고, 지형학적 특성인자(유역면적, 지표흐름 이동거리, 국부경사)와 수문학적 특성인자(총 강우량)에 따른 침식 및 퇴적의 공간분포 변화에 대하여 분석하였다.

• Journal of The Geomorphological Association of Korea
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• v.17 no.3
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• pp.49-57
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• 2010

The topographical rolling distribution characteristics of 10 geological areas in Gyeongsangbuk-do are analyzed using GIS. PEs, PEgrgn, Pp₂, Kav·Kiv, and Khgr regions occupy the more than 60% that are a steep slope-a high elevation and a steep slope-a middle elevation region, and form high moutains in Gyeongsangbuk-do. Meanwhile, Ke_1-9 and Te_1-2 regions take possession of the more than 70% that are a low elevation region. Ke_1-9 region form landward flatlands and hills around Nakdong river and tributaries of Nakdong river in Gyeongsangbuk-do. Then, Te_1-2 region form coastal lowlands adjacent the East sea in Gyeongsangbuk-do. Also, Jgr region take possession of the more than 70% that are a middle elevation region, and form low moutains or flatlands in Gyeongsangbuk-do. Finally, Ols₁ region take possession of the more than 50% that are a steep slope region, and form landward moutains in Gyeongsangbuk-do.

• Proceedings of the KSEEG Conference
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• 2002.04a
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• pp.463-465
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• 2002

연구지역은 좁은 면적에 비하여 800m 이상의 지형기복을 보이며, 계곡과 하천 충적층을 따라 마을이 발달된 전형적인 수계 상류의 농촌지역이다. 주요 상수원은 천부지하수이며, 농업용으로는 하천수를 이용한다. 지표수는 연구지역의 소유역(A, B)간 계절별 수질차이를 보이나, 지하수의 경우 유역간 및 계절별 변동이 상대적으로 작게 나타난다. B 소유역의 하류부에서는 지질매체의 영향으로 보이는 Fe, Mn, Zn 농도의 부화현상이 나타났으며, 이는 방이리층과 길왕리층을 기반암으로 하는 지역에 대한 전체적인 지하수질 조사가 필요함을 지시한다. 국지적인 수질오염원으로 과거에 개발되었던 폐금광이 존재하며, 이로 인한 산성수의 발생도 인지되었다.

• Proceedings of the Korea Water Resources Association Conference
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• 2022.05a
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• pp.280-280
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• 2022

급경사지의 붕괴원인은 강수량과 지형적, 지질적 원인 등이 있지만 최근 집중호우 및 홍수사상에서 많은 피해가 발생한 것에서 강수량과 급경사지 붕괴는 밀접한 상관관계를 가지고 있다. 급경사지 붕괴에 대한 많은 선행연구가 진행되었지만 특히, 강우량과의 상관성을 해석하고 기준을 지질과 지형적 특성에 대한 규명을 하고자 노력하였다. 2015년 행정안전부에서는 급경사지 지역의 주민피해를 최소화하기 위하여 주민대피 관리기준을 제시하였다. 주민대피 관리기준에는 계측기준과 강우량 기준으로 나누어 급경사지 하류지역의 주민대피를 위험단계별로 제시하였다. 그러나 최근의 강우가 급격하게 변화하고 급경사지 지역의 많은 피해가 발생하면서 주민대피 관리기준 중 강우기준의 조정에 대한 필요성이 제기되었다. 본 연구에서는 1999년부터 2020년 까지 발생한 급경사지 피해사례를 조사하여 산사태 피해지역의 강우량 자료를 수집하여 지속시간별 강우량과 1,2,3 시간에 대한 연속강우자료를 수집하여 위험단계별 주민대피 강우량을 제시하였다. 기존 2015년도 주민대피 강우기준을 산정시 분석에 적용된 지질별 강우를 고려하여 재산정하여 위험단계별 주민대피 강우기준을 산정하였다.

• Journal of the Korean Geotechnical Society
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• v.24 no.2
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• pp.37-44
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• 2008

The collapse of the cut slope occurs owing to mixed effect of many variable factors such as geological, geographic, and hydraulic factors. Nevertheless, it is very difficult to evaluate the influence of the complicated geological factors on the stability of the cut slope during various management stages. This study proposes a management plan for domestic cut slope for a series of the rock masses, based on the collapse charateristics of various rock masses and management case studies.

• Journal of the Korean Association of Geographic Information Studies
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• v.3 no.1
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• pp.35-43
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• 2000

The slope gradient of the Korean Peninsula was analyzed by using DEM(DTED level 1). The Peninsula has high percentages of gentle slopes. But low plains and very steep slope regions are scarcely distributed in the Peninsula. Altitude lower than 150m areas are composed of plains and undulated plains. The steepest and most rugged topographies are observed in the range of altitude from 500m to 1,000m areas. The areas of altitude greater than 1,000m show plateau landscapes. By overlapping digital geology maps and the gradient grade maps, We revealed the characteristics of slope regions by geological districts. High latitude with steep slope are well developed in the geological districts of granitic gneiss(ARgr) and gneiss($PR_1$) of the Pre-Cambrian, sandstone of the Paleozoic era(P-T), and sedimentary rocks of the Mesozoic era($J_2$). Low altitude with gentle slope areas are representative in the districts of granite of the Mesozoic era($Jgr_1$), the Cretaceous sedimentary rocks of the Mesozoic era($K_1$, $K_2$) and the Cenozoic strata(N). Basalt extruded the Quaternary($Q_1$) are observed in the areas of very gentle slope but greater than 1,000m altitude.

• Journal of Korean Society for Geospatial Information Science
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• v.19 no.1
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• pp.63-70
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• 2011

The national spatial information systems project which is promoted by our country has been extended from existing 2-D geographic information to 3-D spatial information as the basic geo-spatial Information. Most of the construction of the ground geo-spatial information are completed or underway, on the other hand, the construction of the subsurface geo-spatial information has difficulty caused by the lack of the drilling data characterizing the subsurface. In terms of the construction of the geo-spatial information of the subsurface, the subsurface information is constructed and managed by the domestic institutions, but the subsurface information which is possessed by the institutions was not shared mutually so it is managed inefficiently. This study presented the 3-D national underground information DB design by dividing with the ground DB item which configures the state of the ground and the soil DB item which configures the state of the soil in order to increase the efficiency of the construction of the subsurface spatial information. The implementation & utilization of the national underground information application technology was reviewed by applying the constructed DB to the actual model area, and the national underground information knowledge-based community establishment plan was presented.

• The Journal of Engineering Geology
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• v.19 no.3
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• pp.373-387
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• 2009

Many cultural heritages with various periods including the 'Three Kingdoms Period' were discovered in Chulmamyeon, Busan. Detailed geomorphological and geological investigation was performed due to archaeological importance of the study area. Aerial photographic analysis for geomorphology and analysis of vertical sedimentary sections to interpret the sedimentary characteristics were carried out. Many pebbles with specific features were discovered during the investigation. The characteristics and origin of the pebbles are analysed based on their size, rock type and shape. The study area is located in a relatively low and gentle slope compared with neighboring regions. The strong N-S trending lineaments may influence the topographic features and the distribution of wells discovered in this area. The exposed sections during excavation are divided into several layers depending on colors and materials included. Some of the layers may be developed not by nature but by human activities. The similarity of the pebbles indicates that these pebbles may artificially be collected or produced for a specific purpose. This study shows that geomorphology and geology can be important in location and development of archaeological sites. The analysis and interpretation for the origin of the pebbles indicates that geological studies can be helpful to interpretation of archaeological studies.

• Journal of The Geomorphological Association of Korea
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• v.21 no.4
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• pp.121-131
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• 2014

This study analyzed the spectral reflectance characteristics of kaolinite and ASTER(Advanced Spaceborne Thermal Emission and Reflectance Radiometer) image to extract the distribution of kaolin mines in Hadong area, Gyeongsangnam-do. The band ratio model was applied to extract kaolinite using difference of wavelength absorption band distinct feature of minerals from ASTER image which is the major mineral of kaolin mines. According to the spectral reflectance curve of kaolinite, it showed the absorption features around 0.96 and $2.18{\mu}m$ by Al-OH. Also, it affected 1.24 and $1.38{\sim}1.41{\mu}m$ by OH. Applying for new band ratio model from the spectral features of kaolinite to ASTER image, it is possible to make the distribution map of mining traces including present- developing kaolin mines.