• 지구물리와물리탐사
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• 제4권4호
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• pp.110-114
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• 2001

2차 광상 성인에 의해서 형성된 미고결 역질층내에 배태되고 있는 금 광상이 분포하는 인도네시아 중부 칼리만탄의 타카오이 지역의 천부 지질정보 획득 및 탐사자료 특성 파악을 목적으로 물리탐사를 수행하였다. 사용된 물리 탐사법은 전기비저항탐사로서, 1999년 10월 15일부터 10월 27일 까지 수행하였다. 쌍극자 탐사는 전극간격 a=3m, 5m, 전극 전개수 n=10으로 5개 측선에 대하여, 수직탐사는 6개 지점에서 수행하였다. 취득된 자료들은 DIPRO와 SOUNDPRO 프로그램을 이용하여 처리$\cdot$해석하였다 자료해석 결과, 조사지역의 층서는 비교적 수평 층으로 분류할 수 있으며, 수직비저항 탐사자료 형태는 중간지층의 비저항 간이 높은 KH형을 보여주고 있다.

• 한국해양학회지
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• 제21권4호
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• pp.236-244
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• 1986

본 연구는 한국 동해 대륙붕에 출현하는 주요 저서 다모류의 서식지 환경에 대한 정보를 얻기 위해 1985년 4월에 수행되었다. 총 95출현종 중 조사 지역에서의 출현빈도, 출현량 또는 개체군 밀도에 있어서 중요한 우점종들로는 Terebellides stroemi, Chaetozone setosa, Magelona japonica, Ampharete arctica, Aglaophamus sinensis, Nothria holobranchiata, Lumbrineris japonica, Myriochele gracilis, Notoproctus pacificus 등 9개 종이다. 이들 우점동의 주된 먹이는 규조류와 기타 유기파편들로 구성되었으며 식이형에 있어서는 표층하 퇴적물 식자(subsurface deposit feeder)와 표층퇴적물 식자(surface deposit feeder)에 속하는 종들이 대부분 이다. 육식자로 간주되는 M. holobranchiata 와 L. japonica 의 경우에도 그들의 내 장 내용물이 세립질 퇴적물로 구성된 경우가 많다. 사질 또는 역질의 조립질 퇴적 물이 우세한 환경에 서식하는 관서 다모류는 내장이 매우 세립질의 퇴적물로 채워 져 있고 , 또한 그들의 서관도서식지 퇴적물에 비해 세립질의 입자들로 구성되어 있다. 이러한 사실들은 이들 다모류가 식이와 서관 형성에 서관의 구조와 지역적인 분포 양상은 동해 대륙붕에서의 서식지 환경 특징인 해저지형 구조 또는 수심, 먹 이의 공급원, 퇴적환경의 에너지 분포에 의한 퇴적물 입도 조성등과 잘 일치됨을 보여준다.

• 자원환경지질
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• 제43권4호
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• pp.349-358
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• 2010

탄성파 심도영역 중합전 역시간 구조보정은 음원영역 파동외삽과 수진기영역 파동외삽의 상호상관으로 지층구조를 영상화하는 방법으로 암염돔 하부, 단층, 습곡, 심한 경사층 등 복잡한 층서구조를 영상화하는데 주로 이용된다. 여기에서는 한국지질자원연구원에서 개발된 중합전 심도영역 역시간 구조보정 기술을 국내 대륙붕 제주분지 제 5광구 탄성파 현장자료에 적용하여 음원번호 1280번 하부에 존재하는 향사 층서구조 영상을 향상시키고자 하였다. 음원모음 신호음을 향상시키기 위해 기본 자료처리를 실시하였고, 반복적으로 속도스펙트럼을 계산하는 방법으로 중합속도를 결정하여 속도모델을 구축하였다. 중합단면도상에 나타나는 향사구조는 산란파 영향으로 지층경계면의 연속성이 떨어져 보이지만 구조보정 적용 결과 탄성파 반사 에너지가 집중된 곳에서 향사구조 영상이 향상된 심도영역 지층단면도를 구할 수 있었다.

• 한국자기학회지
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• 제14권3호
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• pp.94-98
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• 2004

MgCCo$_3$에서 Mg와 Co로 이루어진 (001)표면(MgCo-Term) 또는 C와 Co로 이루어진 (001표면(CCo-term)의 전자구조와 자성을 FLAPW 에너지띠 방법을 이용하여 이론적으로 계산하였다. MgCo-Term의 경우 표면에서 Co원자의 자기모멘트는 1.00$\mu$$_{B}$로서 가운데층에 비하여 많이 증가하였고 표면 바로 밑층에서는 가운데층과 비슷한 값을 보였다. CCo-Term의 경우 Co원자의 자기모멘트는 표면에서 뿐만 아니라 표면 바로 밑층에서도 증가하여 각각 0.75와 0.80$\mu$$_{B}$의 값을 나타내고 있다. C와 Mg원자는 두 경우 모두 Co원자와 반대방향으로 스핀분극되었다. 계산된 상태밀도로부터 이러한 표면에서의 자기모멘트의 증가는 Co-3d 띠의 국소화에 의함을 알 수 있었고 여기서 Co-3d와 C-2p 사이의 띠 혼성이 중요한 역할을 하였다.

• 지구물리와물리탐사
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• 제19권2호
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• pp.59-66
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• 2016

환경오염부지의 오염원은 대부분 전기비저항이란 고유물성과 상관관계를 보이기 때문에 전기비저항 탐사는 지중 환경오염조사에 매우 효과적인 방법이다. 이 연구에서는 폐기물 매립장 주변에서 전기비저항 탐사를 수행하여 매립장 주변 지역의 하부 지질구조를 규명하는 한편 침출수 존재 여부 및 영향 범위를 파악하였다. 또한, 주변 관측정의 수질분석 결과와 전기비저항 탐사의 연관성에 대해 분석하였다. 그 결과, 전기비저항 탐사는 수질분석 자료와 매우 높은 연관성을 보였으며, 시추조사 결과와도 상당히 일치하는 것을 확인하였다.

• Journal of Magnetics
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• 제12권3호
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• pp.97-102
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• 2007

We have investigated the electronic structures and magnetism of a full Heusler alloy $Co_2CrGa(001)$ surface by using the all-electron full-potential linearized augmented plane wave (FLAPW) method within the generalized gradient approximation (GGA). We considered two types of different terminations: the Co-terminated (Co-Term) and the CrGa-terminated (CrGa-Term) surfaces. From the calculated layer-projected density of states (LDOS), we found that the surface of the CrGa-Term shows nearly half-metallic character while that of the Co-Term is far from the half-metallic. For the Co-Term, the surface Co atom moves down to the bulk region by $0.05{\AA}A$, while the subsurface Cr and Ga atoms move up to the surface layer by 0.05 and $0.01{\AA}$, respectively. For the CrGa-Term, there is a large inward relaxation of the surface Ga atom $(0.07{\AA})$, but the relaxation of the surface Cr atom is very small $(0.01{\AA})$. The relaxations affect not much to the overall shapes of DOS for both terminations, but make the surface states of the surface Cr and Ga atoms for the CrGa-Term shift to higher energy that enhances the nearly half-metallic character of the CrGa-Term. The magnetic moments of the surface $Cr(2.98{\mu}_B)$ in the CrGa-Term and the surface $Co(1.17{\mu}_B)$ in the Co-Term were much increased compared to those of the inner-layers $(1.79\;and\;0.77{\mu}_B)$, respectively, while that of the subsurface Cr atom in the Co-Term was decreased to $1.19{\mu}_B$.

• 자원환경지질
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• 제25권2호
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• pp.167-177
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• 1992

The gravity measurement has been conducted at 53 and 34 stations with an interval of 1~1.5 km along the national roads of about 47 km and 34 km running from Duksungri to Yangpori and from Angangri to Byungpori, Kyungsangbookdo, respectively. The subsurface geology and geologic structure of Tertiary Pohang and Janggi basins along two survey lines are interpreted quantitatively by applying Fourier series and Talwani methods for Bouguer gravity anomaly. The depths of Conrad discontinuity vary from 11.8 to 12.5 km and 11.5 to 13.2 km along the survey lines between Duksungri and Yangpori, and Angangri and Byungpori, respectively. The depths of pre-Cambrian Gneiss complex underneath Kyungsang Supergroup vary from 3.8 to 4.2 km and 3.8 to 4.6 km along the survey lines between Duksungri and Yangpori, and Angangri and Byungpori, respectively. Massive granite bodies which are not exposed along the survey line between Duksungri and Yangpori are distributed on a large scale at the subsurface between Duksungri and Ochun, and Daegokri and Yangpori. Along the survey line between Angangri and Byungpori, it is exposed at Angangri, and extends underneath Chungrimdong, Pohang city. Andesite is distributed on a small scale underneath Pohang city and Ochun. The thicknesses of Tertiary Yonil and Janggi Groups are 0.2~0.9 km and 0.1~0.5 km, respectively. The Tuffaceous rocks which are the lowest formation of Tertiary sedimentary rocks are distributed with the thickness of 0.2 km at the surface and between Kyungsang Supergroup and Yonil or Janggi Groups. The Yonil and Janggi Groups are in fault contact by a fault running through Ochun and Chungrimdong, Pohang city. Two other faults are newly found near Heunghae-eup and Hyungsan river.

• 한국지하수토양환경학회지:지하수토양환경
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• 제19권1호
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• pp.54-62
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• 2014

To better understand dissimilatory iron and sulfate reduction (DIR and DSR) by subsurface microorganisms, we investigated the effects of sulfate and electron donors on the microbial goethite (${\alpha}$-FeOOH) reduction. Batch systems were created 1) with acetate or glucose (donor), 2) with goethite and sulfate (acceptor), and 3) with aquifer sediment (microbial source). With 0.2 mM sulfate, goethite reduction coupled with acetate oxidation was limited. However, with 10 mM sulfate, 8 mM goethite reduction occurred with complete sulfate reduction and x-ray absorption fine-structure analysis indicated the formation of iron sulfide. This suggests that goethite reduction was due to the sulfide species produced by DSR bacteria rather than direct microbial reaction by DIR bacteria. Both acetate and glucose promoted goethite reduction. The rate of goethite reduction was faster with glucose, while the extent of goethite reduction was higher with acetate. Sulfate reduction (10 mM) occurred only with acetate. The results suggest that glucose-fermenting bacteria rapidly stimulated goethite reduction, but acetate-oxidizing DSR bacteria reduced goethite indirectly by producing sulfides. This study suggests that the availability of specific electron donor and sulfate significantly influence microbial community activities as well as goethite transformation, which should be considered for the bioremediation of contaminated environments.

• 한국지하수토양환경학회지:지하수토양환경
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• 제19권4호
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• pp.31-44
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• 2014

In the present study, a few of recently developed geostatistical models are comparatively studied. The models are two-point statistics based sequential indicator simulation (SISIM) and generalized coupled Markov chain (GCMC), multi-point statistics single normal equation simulation (SNESIM), and object based model of FLUVSIM (fluvial simulation) that predicts structures of target object from the provided geometric information. Out of the models, SNESIM and FLUVSIM require additional information other than conditioning data such as training map and geometry, respectively, which generally claim demanding additional resources. For the comparative studies, three-dimensional fluvial reservoir model is developed considering the genetic information and the samples, as input data for the models, are acquired by mimicking realistic sampling (i.e. random sampling). For SNESIM and FLUVSIM, additional training map and the geometry data are synthesized based on the same information used for the objective model. For the comparisons of the predictabilities of the models, two different measures are employed. In the first measure, the ensemble probability maps of the models are developed from multiple realizations, which are compared in depth to the objective model. In the second measure, the developed realizations are converted to hydrogeologic properties and the groundwater flow simulation results are compared to that of the objective model. From the comparisons, it is found that the predictability of GCMC outperforms the other models in terms of the first measure. On the other hand, in terms of the second measure, the both predictabilities of GCMC and SNESIM are outstanding out of the considered models. The excellences of GCMC model in the comparisons may attribute to the incorporations of directional non-stationarity and the non-linear prediction structure. From the results, it is concluded that the various geostatistical models need to be comprehensively considered and comparatively analyzed for appropriate characterizations.

• 지질공학
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• 제31권3호
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• pp.269-281
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• 2021

Land creeping is the imperceptibly slow, steady, downward movement o f slope-forming soil or rock. Because creep-related failures occur frequently on a large scale without notice, they can be hazardous to both property and human life. Korea Forest Service has operated the prevention and response system from land creeping which has been on the rise since 2018. We categorized and proposed three survey steps (e.g., preliminary, regional, detailed) for investigation of creeping susceptibility site with a focus on geophysical mapping of a selected test site, Yongheung-dong, Pohang, Korea. The combination of geophysical (dipole-dipole electrical resistivity tomography and reciprocal seismic refraction technique, well-logging), geotechnical studies (standard penetrating test, laboratory tests), field mapping (tension cracks, uplift, fault), and comprehensive interpretation of their results provided the reliable information of the subsurface structures including the failure surface. To further investigate the subsurface structure including the sliding zone, we performed high-resolution geophysical mapping in addition to the regional survey. High-resolution seismic velocity structures are employed for stability analysis because they provided more simplified layers of weathering rock, soft rock, and hard rock. Curved slip plane of the land creeping is effectively delineated with a shape of downslope sliding and upward pushing at the apex of high resistive bedrock in high-resolution electrical resistivity model with clay-mineral contents taken into account. Proposed survey steps and comprehensive interpretation schemes of the results from geological, geophysical, and geotechnical data should be effective for data sets collected in a similar environment to land-creeping susceptibility area.