• 자원환경지질
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• 제40권5호
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• pp.705-711
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• 2007

우리가 생활하면서 부딪히는 수많은 판단들 속에서 특히 인간의 권리에 대한 사안은 민감하게 다루어진다. 특히 사실로 입증된 것만 인정하는 증거재환주의에 의해 물리적 증거의 확보 여부는 범죄수사과정에서 필수적임에 따라 과학수사의 중요성 및 수요는 증가하고 있다. 과학수사지질학은 지질학과 과학수사와의 융합 분야로, 과학수사를 위하여 지질학적 지식 및 기법을 바탕으로 물리적 증거를 비교 분석하여 범죄용의자와 범죄사건의 연관성을 파악함으로써 법정에서 유용한 자료로 활용된다. 1970년대 후반 과학수사지질학의 학문적 체계를 구축한 이래로 과학수사지질학의 연구대상은 암석, 광물, 토양, 퇴적물 등의 토양학적 증거에서 역사적 유물, 지뢰, 사체 등의 사회 문화적, 정치적, 군사적, 의학적 대상으로 확대되고 있다. 과학수사지질학의 역할이 단순 위치추적에서 고고학적 학설 증명, 역사적 사실 입증, 환경오염 원인 규명, 연대기적 식생 분포 및 인류학적 발생 규명 등으로 폭넓게 작용할 수 있음을 의미하고, 이는 발전된 지질학적 방법론을 적용할 수 있으며 다양한 과학수사지질학적 수요를 만족시킬 수 있다. 과학수사지질학의 연구 활동은 과학수사 전문기관을 중심으로 이루어지고 있으나, 우리나라 국립과학수사연구소의 과학수사 활동 분포에서 과학수사지질학적 비중은 극히 일부분으로 나타나고 있다. 따라서 전문 지질자원 연구기관을 중심으로 우리나라 지질학적 특성에 기반을 둔 연구방법 확보, 연구결과 활용사례 발굴 등 과학수사지질학의 역할 정립을 위한 체계적인 논의를 이끌어 낼 필요가 있다고 사료된다.

• 자원환경지질
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• 제35권6호
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• pp.589-595
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• 2002

• 자원환경지질
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• 제43권4호
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• pp.393-400
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• 2010

• 대한자원환경지질학회:학술대회논문집
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• 대한자원환경지질학회 2001년도 춘계 공동학술발표회
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• pp.259-262
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• 2001

• 지질공학
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• 제18권1호
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• pp.69-81
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• 2008

산사태연구는 산사태를 발생시키는 여러 인자들의 상호관계를 규명하는 방법, 확률론적으로 산사태 발생가능성을 예측하는 방법 사태물질의 이동경로와 확산범위를 산정함으로써 산사태 위험성을 평가하는 방법 등으로 구분할 수 있다. 우리나라에서 발생된 대부분의 산사태는 여름철의 집중호우에 기인되는 것으로 기반암 상부의 토층에서 발생되며, 강우조건, 지형조건과 지질 및 토질특성 등에 영향을 받는 것으로 알려져 있다. 산사태 조사부터 위험성평가에 이르기까지의 산사태연구는 다양한 산사태를 체계적으로 조사하고 해석함으로써 공학적 관점에서 여러 특징들을 관찰하고 그 특성들을 총괄적으로 해석하여야만 한다. 이 연구에서는 경상남도 마천지역을 대상으로 산사태 현장조사를 수행하였다. 조사결과를 토대로 자연사면 산사태에 대한 최적의 표준모델로 활용할 수 있는 산사태 조사 및 해석 기법을 제안하고자 한다.

• 자원환경지질
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• 제33권2호
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• pp.129-138
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• 2000

The various types of geohazards like landslides resulted from civil construction (i.e. highway construction) must of analysed considering all the possible influential factor systematically. Thus, by using GIS, slope stability can be evaluated, and it can be used as a data for further detailed investigation. So the aim of this study is to present a data for decision making in selecting suitable point for remediation. For analysing slope instability, through appropriate definition and classification, landslide mechanism must be understood. In building GIS model, the selection of appropriate factors and their rating system should be made. For this, the characteristics and the mechanism of landslide have to be understood. And suitable coverage should be chosen for the model considering the slope conditions. In this study, field investigation in lst and 2nd Section, Chung-ang highway was carried out. From the field data, GIS model on slope instability was created. 5 coverages were used for it. From the result of this study, 12 unstable sections were found out and more detailed investigation is needed there.

• 자원환경지질
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• 제37권1호
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• pp.49-59
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• 2004

The concectration and distribution of contaminants obtained from a contaminated land investigation or an environmental geochemistry survey constitutes the basis of a decision-making process on environmental policies or of scientific researches. As the quality of data determines the reliability of the result, the investigation plan should be adjusted according to the purpose of the investigation. In general, the effort to improve the data quality had been focused mainly on the QA/QC procedures in laboratories. The rapid progress of analytical instrument has also contributed toward improving the analytical precision to a sacrificable degree. Nevertheless, in many cases, it is not the analytical precision that needs improvement for the better precision of overall measurement process: it is rather during the sampling process in the field that is responsible for the poor precision. To assess the data quality on a measured value, ISO recommends to provide information on "measurement uncertainty" along with the measured value. The measurement uncertainty in an environmental measurement context can be explained as the statistical number that expresses the degree of the uncertainty stemming from the sampling and analytical procedures. There is a cost involved in order to improve the precision of sampling and analytical methods so as to decrease the degree of measurement uncertainty. The economical point of compromise in an investigation planning can be achieved when the allowable degree of uncertainty has been set before-hand. The investigation can then be planned accordingly not to exceed the uncertainty limit. Furthermore, if the measurement uncertainty estimated from the preliminary investigation can be separated into sampling and analytical uncertainties, it can be used as a criterion where the resources for the investigation should be allotted cost-effectively to reinforce the weakest link of the whole investigation process. This paper aims to present a method of estimating the level of measurement uncertainty of a measured contamination concentration at a site used as an example and to show how the estimated uncertainty can be applied to serve the particular purpose of an investigation.

• 자원환경지질
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• 제53권5호
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• pp.631-643
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• 2020

The central-western Korean Peninsula contains records of an Early Mesozoic collisional event related to the final amalgamation of the East Asian continent. Here, we present a renewed geologic map of the Deokjeok and Soya islands in the central-western Korean Peninsula and its explanatory note. Our geologic map was based on a detailed investigation of the northeastern area of both islands, which is characterized by a complex fault and shear zone system that accommodated the crustal deformation related to the Mesozoic post-collisional orogenic collapse and the subsequent structural inversion. We suggest future directions of study aiming at addressing issues regarding the deformational responses of crust to the Mesozoic tectonic transition and orogenic cycles.

• 한국석유지질학회:학술대회논문집
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• 대한자원환경지질학회/한국석유지질학회/한국암석학회 2000년도 추계공동학술발표회 초록집
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• pp.35-35
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• 2000

• 자원환경지질
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• 제23권2호
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• pp.215-219
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• 1990

Geological and electrical resistivity surveys along the survey line of about 3 km between Kyungsangbukdo Youngilgun Hodong and Gwangmyungdong using by dipole-dipole electrode array method were carried out to examine the boundary and structural relationship between Tertiary Pohang and Janggi basins. Electrical resistivity data were interpreted qualitatively and quantitatively by means of pseudosection of apparent electrical resitivity distribution and finite difference method for two dimensional geologic structure model. The nearly vertical fault zone with low electrical resistivity value of 1-5 Ohm-m and widths of about 200m at the surface and 400 m at depth exists around 1.2 km west of national road between Ocheoneup and Yangbukmyun. Mudrocks, sandstones and tuffaceous rocks are widely distributed with electrical resistivity values of 6-77 Ohm-m. Especially, tuffaceous rocks with relatively high electrical resistivity value are predominant at eastern side of fault zone. Consequently, it is known that Pohang and Janggi basins are in fault contact.