• 한국신재생에너지학회:학술대회논문집
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• 2007.11a
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• pp.560-563
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• 2007

속도와 밀도의 함수로 이루어진 음향 임피던스는 탄성파자로부터 물성변화를 확인하는 방법 중의 하나로 이용된다. 본 연구에서는 한국지질자원연구원에서 개발된 탄성파 탐사자료처리 무른모 지오빗올 이용하여 기본 자료처리를 실시하고, 음향 임피던스 변환 모듈올 적용하여 동해 가스 하이드레이트 현장자료에 대한 광역 임피던스변화를 구하고 이로부터 음향 임피던스 단면도를 구하고자였다. 음향 임피던스 단면도는 중합단면도상에서 음향 임피던스 변화를 보여주고 있으며 특히 왕복주시 2.9초 전후에서 해저면 반사파와 위상이 반대이며 고진폭을 나타내는 해저면 기인 고진폭 반사층으로 여길만한 지점에서 그 변화가 크게 나타남을 알 수 있었다. 탄생파자료는 10 Hz 이하 저주파 정보가 들어있지 않아 완전한 음향 임피던스를 구할 수 없으므로 층서해석이 이루어진 중합 단면도부터 광역 임피던스를 구하였다. 향후 시추자료를 활용할 경우 좀더 정확한 음향 임피던스 단면도를 생산할 수 있을 것으로 여겨진다.

• The Journal of Engineering Geology
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• v.7 no.2
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• pp.101-112
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• 1997

Gravity and electrical resistivity surveys were carried out across the Kwangju fault in the downstream area of the Jangsung Lake, to investigate the location and geometrical feature of the fault. In the resistivity survey, dipole - dipole array method was adopted for 3 survey lines of which length and electrode spacing are 500m and 25m, respectively. Resistivity data are interpreted with aid of computer program "RESIS" which is widely used in resistivity data analysis and two dimensional resistivity profiles are obtained for 3 survey lines. Two large fracture zones relevant to the Kwangju fault are identified in the resistivity profiles. The total of 80 gravity data are observed with the mean spacing of 40 m and the exact leveling is accompanied to obtain more precise gravity anomalies. The subterranean density discontinuities calculated from the inverse method are appeared at the depths of 650rn and 120m. It is considered that the deep discontinuity indicates boundary between Jurassic granites and oveflying Cretaceous tuff formation. while, the shallow discontinuity is interpreted to be a boundary between alluvial deposits and basements. The subsurface geological structure to satisfy the observed Bouguer anomaly is determined from the iterative forward method in which results from existing surface geological informations, the inverse method, and from the resistivity interpretations are employed as an iuitial model. In conclusion, Kwangju fault is appeared to be a high angle normal fault mainly formed in tension stress filed.

• The Journal of Engineering Geology
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• v.6 no.1
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• pp.15-22
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• 1996

Frequency content of seismic waves observed in field seismic survey in Korea has almost not exceeded 4kHz(wave length 1m). The limited frequency content not only restricts the minimum size of objects which can be surveyed in seismic tomogrpahic application, but also makes a fundamental limit in the resolution of tomogram. This paper shows the resonable result obtained by confirmimg and resolving the problems which can be occured m measuring procedure for the small - sized section through field application. Seismic tomographic field survey was performed for a concrete construction for railroad bridge in Korea, and to this the tomographic measurements for the stone-build foundation construction for a bell house of church in Germany were compared.

• Proceedings of the Korean Society for Rock Mechanics Conference
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• 1995.03a
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• pp.27-40
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• 1995

한강하저의 지질은 수많은 대ㆍ소 단층들로 인해 심하게 교란되어 있어 지질상황의 변화가 매우 심하며, 터널을 굴착함에 있어 지하수의 유입을 차단하는 것이 안전시공을 위한 필수 과제로 직면한다. 본 고에서는 기 시공실적을 바탕으로 암반상태에 따른 차수그라우딩의 패턴을 비교ㆍ검토하였다. 본 구간에서는 암반상태에 따라 5가지 패턴이 적용되었으며, 경암 암반일 경우는 상부반단면만을 주입범위(주입범위 : 3.5m, 28공)로 하고 암반의 전단강도증진을 위해 강관보강을 시행하였다. 연암 암반 내지 파쇄대가 부분적으로 협재된 경우는 상부반단면만을 주입하되 주입범위 및 그라우팅 공수를 늘리는 방식(주입범위 : 5∼7, 42∼56공)으로 보강하였다. 풍화암 암반의 경우는 전단면을 주입범위로 하여 그라우팅 공수를 늘림(주입범위 : 7m, 81공)으로서 차수효과를 증진시켰다. 또한 본 공사구간 중 가장 난제였던 연약지반대(잔류토 내지 풍화토) 85m 구간은 자문회의 등을 거쳐 주입범위, 주입길이 및 주입공수, bulk head 구간을 늘려 시공하고, 굴착하면서 차수효과를 확인하는 방식을 취하였다.

• The Journal of Engineering Geology
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• v.8 no.1
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• pp.1-12
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• 1998

The fracture size among geometric parameters of the fracture system is treated as one of the most important factors in the geotechnical and hydrogeological analysis. However, several uncertainties in data acquisition and analysis pmcess about the fracture size are not clear yet. This study presents the current status on the estimation of the fracture size and verifies the estimating method using forward modeling approach. The factors considered are the variation of fracture intersection probabilities with different assumptions on the orientation of sampling planes and fracture size by using a simulated tleee dimensional fracture network model. If it is possible to analyze precisely the fracture intersection probabilities and the characteristics of probabilistic distnbution fiom cavern walls, outcrops or boreholes,the actual fracture size developed in rock rnass can be estimated confidently.

• Journal of Wetlands Research
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• v.12 no.2
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• pp.1-12
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• 2010

This study examined geological characteristics of a wetland in Mountain Geumjeong in Busan Metropolitan City. Field survey and laboratory tests were performed to identify topographic features, geological and structural geological characteristics, rock strength along the distance from the wetland, soil profile in the wetland, and chemical property of the wetland soil. The bedrock of the wetland consists of hornblende granite. Hornblende granite and rhyolitic rock around the wetland have the joints with strikes of N-S, E-W, and NE-SW directions and with higher dips greater than $60^{\circ}$. Lower rock strength and higher weathering grades take place towards the wetlands. According to X-ray diffraction analysis of wetland soil samples, kaolinite, montmorillonite, and gibbsite appear which demonstrate weathered products of feldspars in the hornblende granite. The soil profile in the wetland comprises O, A, B, and C horizons from the land surface. The contents of the organic matters decrease from shallow parts to deeper parts of the soil profile. In addition, $K^+$ and $Na^+$ originating from the weathering of feldspars are dominant components among inorganic ions in the wetland soil.

• Proceedings of the Korean Society for Rock Mechanics Conference
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• 1996.03a
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• pp.25-34
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• 1996

터널은 긴 선상구조물로서 사전지질조사에 의해 설계에 필요한 정보를 정밀도 높게 구하는 것이 매우 어렵다. 따라서 터널시공 중 암반 및 지질상황을 관찰하고, 터널주변 지반의 거동을 계측하여 지반에 적합한 지보공을 설계ㆍ시공하는 것이 필수적이다. 이를 위해서 터널시공 중 정량적인 암반분류와 계측(일상관리계측과 대표단면계측)이 주기적으로 실시되고 있지만, 이러한 결과를 어떻게 시공에 반영하느냐는 터널의 합리적인 시공에 있어 매우 어려우면서도 중요한 문제라 할 수 있다. (중략)

• Proceedings of the KSEEG Conference
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• 2003.04a
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• pp.161-164
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• 2003

하천 주변은 이미 선사시대부터 거주지나 농경지 등으로서 인간활동의 중요한 무대가 되었다. 그러나 하천은 끊임없이 변화하고 있으며, 그 변화는 특히 홍수의 형태로 인간에게 큰피해를 주어왔다. 인간은 이러한 하천의 변화에에 적응하거나 조절하고자 노력하면서 하천이 어떻게 변화하는가에 관심을 갖게 되었다. 자연적 또는 인위적인 변화가 하천과 홍수에 어떻게 영향을 미치는지에 대한 과학적 연구는 이미 수백년 전에 시작되었다. (중략)

• The Journal of Engineering Geology
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• v.22 no.3
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• pp.331-341
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• 2012

Granitoid rocks are generally high-quality rock from a geotechnical perspective, because they rarely contain systematic joints or fragmented fault zones. Although the rock type at the Sanhak site is granite, a collapsed slope has a deep soil layer and shows no residual structures such as discontinuities or faults; surface avalanches from this slope can be observed in several places. To study the stability of this slope, we investigated rainfall duration, variation in pore-water pressure, and the factor of safety considering three cases (current cross-section, initial planning cross-section, revised planning cross-section). With increasing duration of rainfall, the groundwater level rises, up to 20 m in height from ground surface. In the initial planning cross-section, safety was secure for rainfall of 2 days duration, but inadequate for rainfall of 4 days duration. In the revised planning cross-section, however, safety factors were secure for rainfall of 4 days duration. Therefore, to ensure permanent stability at the Sanhak site, a slope degree of 1:1.8 should be maintained during cutting.

• Geophysics and Geophysical Exploration
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• v.27 no.2
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• pp.91-107
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• 2024

Single-channel seismic exploration has proven effective in delineating subsurface geological structures using small-scale survey systems. The seismic data acquired through zero- or near-offset methods directly capture subsurface features along the vertical axis, facilitating the construction of corresponding seismic sections. However, substantial noise in single-channel seismic data hampers precise interpretation because of the low signal-to-noise ratio. This study introduces a novel approach that integrate noise reduction and signal enhancement via matrix rank optimization to address this issue. Unlike conventional rank-reduction methods, which retain selected singular values to mitigate random noise, our method optimizes the entire singular value spectrum, thus effectively tackling both random and erratic noises commonly found in environments with low signal-to-noise ratio. Additionally, to enhance the horizontal continuity of seismic events and mitigate signal loss during noise reduction, we introduced an adaptive weighting factor computed from the eigenimage of the seismic section. To access the robustness of the proposed method, we conducted numerical experiments using single-channel Sparker seismic data from the Chukchi Plateau in the Arctic Ocean. The results demonstrated that the seismic sections had significantly improved signal-to-noise ratios and minimal signal loss. These advancements hold promise for enhancing single-channel and high-resolution seismic surveys and aiding in the identification of marine development and submarine geological hazards in domestic coastal areas.