• 한국지리정보학회지
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• 제20권1호
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• pp.71-84
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• 2017

토양, 암석, 지하수로부터 실내에 유입되는 라돈은 인간에게 큰 위해를 끼치는 방사능 가스이다. 라돈 가스의 위해성을 확인하기 위해 실내 라돈 농도를 측정해 오고 있는데, 추가적인 분석 수행을 위해서는 신뢰성 높은 분포도 작성이 매우 중요하다. 본 연구에서는 비대칭 분포를 나타내는 라돈 농도의 공간 분포도 작성을 위해 단변량 크리깅 기법들의 비교를 목적으로 정규 크리깅, 비선형 자료 변환 기반의 로그 정규 크리깅, 다중 가우시안 크리깅과 지시자 크리깅의 예측 능력을 비교하였다. 예측 능력을 비교 분석하기 위해 잭나이프 방법을 이용하여 검증을 수행하였으며, 자료 구간별 오차와 샘플링 밀도의 차이에 따른 오차도 추가적으로 분석하였다. 남한 지역을 대상으로 한 사례 연구 결과에서 전반적으로 정규 크리깅에 비해 비선형 자료 변환 기반 크리깅 기법들이 좋은 예측 능력을 보였으며, 비선형 자료 변환 기반 크리깅은 로그 정규 크리깅, 다중 가우시안 크리깅 순으로 좋게 나타났다. 그러나 공간 패턴과 높은 값의 재생산을 고려할 때, 높은 값의 예측 능력은 정규 크리깅이 가장 우수하였다. 본 연구의 결과는 비대칭 분포 자료의 공간 예측을 위한 크리깅 기법의 선정에 유용하게 사용될 것으로 기대된다.

• 한국토양환경학회지
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• 제4권2호
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• pp.77-86
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• 1999

난분해성 유기물로 오염된 토양/지하수의 복원을 위하여 계면활성제를 이용 시 토양에 흡착된 계면활성제가 미치는 영향을 평가하기 위하여 소수성 유기물의 흡수현상을 시험하였다. 흡착된 계면활성제에 대한 유기오염물의 흡수계수($K_ss$)는 평형상태에서의 계면활성제 흡착곡선과 밀접한 관계를 이루었다. 즉, 낮은 농도의 흡착에 대한 $K_ss$는 가장 큰 값을 보였고 흡착량이 증가할수록 감소하는 경향을 보였다. SDS에 대한 $K_ss$값은 미셀분배계수($K_mic$) 보다 컸으며 Tween 80에 대해서는 가장 낮은 흡착농도에서의 $K_ss$값을 제외하고 모든 농도 범위에서 $K_{mic}$ 보다 큰 값을 보였다. 유기오염물의 분배계수 또한 계면활성제의 주입량에 따라 변하며 주입되는 계면활성제 농도가 증가할수록 증가하며 일정 농도 이상의 계면활성제 농도에서 감소하기 시작하였다. 이러한 결과는 미셀과 흡착된 상태의 계면활성제 사이에서 오염물 흡수를 위한 상호경쟁에 기인되는 것으로 판단된다. 결론적으로 토양에의 계면활성제 흡착은 유기오염물의 지체현상을 증가시키는 역할을 하여 계면활성제를 이용한 유기오염물 제거 시 저해영향을 미치므로 각 오염부지의 특성별로 유기오염물의 분포를 계면활성제 주입량의 함수로써 평가하는 단계가 선행되어야 한다.다.

• 자원환경지질
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• 제32권2호
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• pp.177-187
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• 1999

Gravity, magnetic and VLF surveys were conducted to investigat the structural stability and hazards associated with the Ubong landfill in Pohang City, which has been built to dump industrial wastes. In 1994, the collapse of a bank happened in the 6th landfill site due to sudden heavy rain, and a large quantity of waste materials flowed out to the nearby landfill sites, factories and roads. We used $10{\times}10m$ resolution DEM data for gravity reductions. The maximum variation of the terrain effect in the survey area is about 0.5 mgal and the terrain effect is large in the vicinity of bank boundary. The Bouguer gravity anomaly map shows the effect due to the variatino of thickness and type of waste materials. The small negative gravity anomaly increases from the 9th site to the 6th site. The small negative gravity anomaly of the 9th site reflects the relatively shallow dumping depth of average 14.5 m in this site and increased density of waste materials by the repeated stabilization process of soil overlaying. The 6th site is located at the center of the former valley and rainfall and groundwater are expected to flow from south-east to north-west. Therefore, considering the previous accident of mixing waste and bank materials at the north-west boundary of the landfill, there may be some environmental problems of leakage of contaminated water and bank stability. The complex inversion technique using Simulated annealing and Marquardt-Levenberg methods was applied to calculate three-dimensional density distribution from gravity data. In the case of 6th site, it is apparent that the landfill had been dumped in four sectors. However, most part of the 9th site and showed that high magnetic industrial wastes were concentrated in the 6th site. The result of magnetic survey showing low magnetic anomalies along the boundaries of two sites is similar to that of gravity data. The VLF data also reveals four divided sectors in the 6th site, and overall anomaly trend indicates the directio of former valley.

• 한국지반공학회:학술대회논문집
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• 한국지반공학회 2005년도 춘계 학술발표회 논문집
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• pp.376-383
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• 2005

In this study, we conducted geophysical investigations for the organization of integrated geophysical methods to detect underground cavities of ground subsidence area at the field test site, located at Yongweol-ri, Muan-gun. We examined the applicability of geophysical methods such as electrical resistivity, electromagnetic, and microgravity to cavity detection with the aid of borehole survey results. Underground cavities are widely present within the limestone bedrock overlain by the alluvial deposits in the area of the test site where the ground subsidences have occurred in the past. The limestone cavities are mostly filled with groundwater and clays in the test site. Thus, cavities have low electrical resistivity and density compared to the surrounding host bedrock. The results of the study have shown that the zones of low resistivity and density correspond to the zones of the cavities identified in the boreholes at the site, and that the geophysical methods used are very effective to detect underground cavities. Furthermore, we could map the distribution of cavities more precisely with the test results incorporated from the various geophysical methods. It is also important to notice that the microgravity method is a very promising tool since it has rarely used for the cavity detection in korea. Beyond the investigation of underground cavities, the geophysical methods are required to provide useful information for the reinforcement design for the ground subsidence areas. It is, therefore, necessary to develop integrated geophysical technique incorporating different geophysical methods to precisely map underground cavities and image the subsurface of the ground subsidence areas.

• 지구물리와물리탐사
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• 제7권1호
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• pp.80-87
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• 2004

During excavation work for the construction of a highway bridge in a limestone area in Korea, several cavities were found, and construction work was stopped temporarily. Cavities under the bridge piers might seriously threaten the safety of the planned bridge, because they could lead to excessive subsidence and differential settlement of the pier foundations. In order to establish a method for reinforcement of the pier foundations, borehole radar reflection and tomography surveys were carried out, to locate cavities under the planned pier locations and to determine their sizes where they exist. Since travel time data from the crosshole radar survey showed anisotropy, we applied an anisotropic tomography inversion algorithm assuming heterogeneous elliptic anisotropy, in order to reconstruct three kinds of tomograms: tomograms of maximum and minimum velocities, and of the direction of the symmetry axis. The distribution of maximum velocity matched core logging results better than that of the minimum velocity. The degree of anisotropy, defined by the normalized difference between maximum and minimum velocities, was helpful in deciding whether an anomalous zone in a tomogram was a cavity or not. By careful examination of borehole radar reflection and tomography images, the spatial distributions of cavities were delineated, and most of them were interpreted as being filled with clay and/or water. All the interpretation results implied that two faults imaged clearly by a DC resistivity survey were among the most important factors controlling the groundwater movement in the survey area, and therefore were closely related to the development of cavities. The method of reinforcement of the pier foundations was based on the interpretation results, and the results were confirmed when construction work was resumed.

• 지질공학
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• 제17권1호
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• pp.135-142
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• 2007

토목구조물의 기초가 되는 암반은 암석자체로서는 강도가 높고 투수성이 작지만 공학적 성질은 암반내의 존재하는 크랙, 절리 등 불연속면의 영향을 크게 받는다. 천부 암반내에 지배적으로 분포하는 것은 절리이지만 그 수가 적은 지하심부에 있어서 지하수 투수성의 가능성을 고려하면 암석자체의 미소크랙의 연결성이 투수성 크랙으로서 충분히 고려되어져야 한다. 이 연구에서는 절리성 암반의 절리분포 및 투수성 해석 모델화 방법을 화강암 공시체의 미소크랙에 응용하여 손상진행에 따른 화강암의 투수 특성을 추정하는 것을 목적으로 하였다. 미소크랙 데이터로부터 투수모델을 작성하여 해석한 결과 평균투수계수에 있어서 실제의 투수시험 값과 잘 일치하는 것으로 나타났다. 또한 3차원 모델의 가시화를 가지고 모델표면에서의 미소크랙과의 비교로부터 손상발달에 의한 미소크랙 발생수와 유출면으로부터 계산한 평균투수계수는 비례관계로 실험결과와 잘 일치하는 것으로 해석되었다.

• 한국방재학회 논문집
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• 제3권4호
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• pp.145-151
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• 2003

생활폐기물 및 산업폐기물은 인간의 활동으로부터 배출되며 소각법 혹은 매립법 또는 2가지 방법을 동시에 이용하여 처리되고 있다. 특히 매립법은 침출수로 인하여 매립지가 있는 지역의 지하수계를 심각하게 오염시켜 환경재해를 발생시키고 있다. 따라서 오염지역의 침출수 오염특성을 3차원적으로 조사하여 환경재해를 최소화하는 것이 중요하다. 본 연구는 비위생 매립지인 충주시 노은 매립장의 3차원적 침출수 오염특성을 조사하였다. 조사를 위한 1개 측선의 방향은 주된 매립지 경계와 평행하도록 설치하였다. 노은 매립장을 탐사한 결과 가장 상부층은 안정화가 완전하게 진행되었으나 가장 하부층은 부분적으로 침출수가 일부 존재하는 것으로 분석되었다.

• 자원환경지질
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• 제16권1호
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• pp.11-18
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• 1983

Gyeongsang Basin in the southeastern part of the Korean peninsular is characterized by many fault systems. To decipher the geotectonical evolution of the Korean peninsular and marginal basins in her adjacent areas it is prerequisite to understand the spatial distribution pattern and mutual relationships of these fault systems. Because of difficulties in finding any criterion to recognize the faults in field, their extension and mutual relationships in ages are not very clear yet. As an attempt to find geophysical criteria to recognize the fault, geoelectrical resistivity survey was carried out in this study. With the Wenner configuration four resistivity soundings and twenty seven resistivity profilings were done. The electrode distance used was up to 50m. From the results of the resistivity soundings and boring data of earlier groundwater investigations the depth of alluvial and weathered zone was established to be at most 20m in the study area. In the resistivity profiling low resistivity anomaly zones are detected on every traverse, which are interpreted as caused by fractures, fault clays and mylonites in the fault zone. The width of the fault zone amounts to 0.3-1km. By correlating and connecting the negative anomaly zones from traverse to traverse one can determine the trend of th of the faultzone and therefore that of fault itself. The recognized fault trend in this way was $N15^{\circ}-20^{\circ}E$ and this coincides with the direction of the inferred fault line from earlier geological surface mapping. With the help of this characteristical negative anomaly the existance of another $N80^{\circ}W$ trending fault was estabished. This study has shown that geoelectrical resistivity survey can be applied successfully to the problem of tracing fault line insofar as a fault zone has been developed along fault line.

• 한국환경과학회지
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• 제23권4호
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• pp.561-569
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• 2014

The water resources system of Jeju-do Island entirely depends on groundwater. This study is making a precision observation of baseflow, surface water, water shortage that might be vulnerable to climate change and drought in future. The field observation of baseflow discharges in Akgeuncheon stream has regularly been made with ADCP and ADC and Flowmate every two weeks for twenty-two (22) months (July 8, 2011 to April 27, 2013). This paper represent the results of calculating discharge of a number of hydraulic structures (broad-crested weirs) with comparing and has been calculated more accurate discharges with suitability of different observation methods. The average discharge has been observed 0.851 $m^3/s$, whereas the average ADC and Flowmate is 0.709 $m^3/s$. Meanwhile, stream discharge has been calculated 0.709 $m^3/s$ through the broad-crested weir equation. The discharge has calculated with the weir equation greatly changed according to even a small change in the water level. However, it showed a similar trend to one of the observed discharge. Although, in past there were generating errors caused by observers' strides, vertical and horizontal flow velocity distribution when the average flow velocity had been measured, non-prismatic flow, turbulent flow and others in ADC. This study comes up with the weir equation is more suitable for the characteristics of Jeju-do could be presented through an observations of baseflow discharge.

• 한국토양비료학회지
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• 제48권4호
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• pp.246-254
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• 2015

This study explored the effect of rainfall pattern and soil characteristics on water management in rice paddy fields, using a soil water balance model, BUDGET. In two sites with different soil textural group, coarse loamy soil (Gangseo series) and fine soil (Hwadong series), respectively, we have monitored daily decrease of water depth, percolation rate, and groundwater table. The observed evapotranspiration (ET) was obtained from differences between water depth decrease and percolation rate. The root mean square difference values between observed and BUDGET-estimated ET ranged between 10% and 20% of the average observed ET. This is comparable to the measurement uncertainty, suggesting that the BUDGET model can provide reliable ET estimation for rice fields. In BUDGET model of this study, irrigation requirement was determined as minimum water need for maintaining water-saturated soil surface, assuming 100 mm of bund height and no lateral loss of water. The model results showed different water balance and irrigation requirement with the different soil profile and indicated that minimum percolation rate by plow pan could determine the irrigation requirement of rice paddy field. For the condition of different rainfall distribution, the results presented different irrigation period and amounts, representing the importance of securing water for irrigation against different rainfall pattern.