• 제목/요약/키워드: fault area

검색결과 802건 처리시간 0.023초

중력탐사에 의한 삼척-태백간의 지하지질 및 지질구조 연구 (Gravity Survey of the Subsurface Geology and Geologic Structure between Samcheog and Taebaek Area)

  • 민경덕;조광은
    • 자원환경지질
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    • 제28권1호
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    • pp.79-88
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    • 1995
  • The gravity measurment has been carried out at 48 gravity stations with intervals of 1.0~1.5 km along the survey line between Samcheog, Gosari and Taebaek to study subsurface geology and geologic structure in the northeastern part of the Ockchon zone. The Bouguer gravity anomaly values were obtained from the measured gravity values through the gravity corrections. The subsurface geology and geologic structure were interpreted quantitatively by means of the Fourier series method and Talwani method for 2.5 dimensional body. In the study area, the depth of Conrad discontinuity is about 10 km at Samcheog, northeastern end of the survey line, and it is increased rapidly to about 12.5 km at Miro, 15 km at Gosari and 15.5 km at Dongjeom, southwestern end of the survey line, respectively. The depth of the basement of the Ockchon zone exposed at Samcheog is increased smoothly to about 2 km at 5 km from Samcheog along the survey line, and is exposed again in the area between Singiry and Gosari. Beyond Gosari its depth is increased to about 1.7 km, and displaced 2.3 km downward by Osipcheon fault near Dogyeri and 0.5 km by Baeksan thrust near Cheolam, respectively. Many V-shaped low Bouguer gravity anomalies resulted from the fracture zone associated with faults imply the existence of Osipcheon fault and several inferred faults. The low Bouguer gravity anomaly zone between Tongdong and Dongjeom is caused by Jurassic gneissose granite. A local high Bouguer gravity anomaly at 35 km along the survey line from Samcheog is interpreted by the effect of iron deposit of high density existed at subsurface. The thickness of Great Limestone Group varies from 0.5 km to 1.4 km, that of Pyeongan Supergroup from 0.4 km to 0.9 km, and that of Yangdeog Group is about 0.3 km. The thickness of Jurassic gneissose granite varies from 1.5 to 3.0 km.

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스팀터빈 발전기 비동기 투입 사례연구를 통한 비동기 방지 알고리즘 개발 (Development of Asynchronous Blocking Algorithm through Asynchronous Case Study of Steam Turbine Generator)

  • 이종훤
    • 전기학회논문지
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    • 제61권10호
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    • pp.1542-1547
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    • 2012
  • Asynchronous phenomenon occurs on the synchronous generators under power system when a generator's amplitude of electromagnetic force, phase angle, frequency and waveform etc become different from those of other synchronous generators which can follow instantly varying speed of turbine. Because the amplitude of electromagnetic force, phase frequency and waveform differ from those of other generators with which are to be put into parallel operation due to the change of excitation condition for load sharing and the sharing load change, if reactive current in the internal circuit circulates among generators, the efficiency varies and the stator winding of generators are overheated by resistance loss. When calculation method of protection settings and logic for protection of generator asynchronization will be recommended, a distance relay scheme is commonly used for backup protection. This scheme, called a step distance protection, is comprised of 3 steps for graded zones having different operating time. As for the conventional step distance protection scheme, zone 2 can exceed the ordinary coverage excessively in case of a transformer protection relay especially. In this case, there can be overlapped protection area from a backup protection relay and, therefore, malfunctions can occur when any fault occurs in the overlapped protection area. Distance relays and overcurrent relays are used for backup protection generally, and both relays have normally this problem, the maloperation, caused by a fault in the overlapped protection area. Corresponding to an IEEE standard, this problem can be solved with the modification of the operating time. On the other hand, in Korea, zones are modified to cope with this problem in some specific conditions. These two methods may not be obvious to handle this problem correctly because these methods, modifying the common rules, can cause another coordination problem. To overcome asynchronizing protection, this paper describes an improved backup protection coordination scheme using a new logic that will be suggested.

Consideration for the Highest Temperature Point Movement of the Dongrae Thermal Water in the Pusan Area. (Poster)

  • Kim Tong-Kwon;Lee Jin-Soo;Lee Seung-Gu;Song Yoon-Ho;Kim Tack-Hyun
    • 한국지하수토양환경학회:학술대회논문집
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    • 한국지하수토양환경학회 2005년도 INTERNATIONAL SYMPOSIUM ON SOIL & GROUNDWATER ENVIRONMENT
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    • pp.158-159
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    • 2005
  • This study showed that the highest temperature point of the Dongrae thermal spring in Pusan was moved to the north direction of the Dongrae fault as times goes by. The Br concentration(1.5mg/L) in Dongrae thermal waters indicated the influence of 2% seawater mixing. If the simple mixing without hydrochemical reaction occurs between seawater and thermal water, the concentration of Mg will be about 20mg/L. But the low concentration(0.1 mg/L) of Mg, contrary to high concentration(10 mg/L) of surrounding groundwater not affected by thermal water, suggested the thermal water, seawater and rock interactions. The calculation of saturation index(SI) by using the geochemical code of EQ3NR showed that the Mg in thermal groundwater, which was introduced by seawater, was removed by the precipitation of Antigorite (SI: log Q/K =71.753, $Mg_{48}Si_{24}O_{85}(OH)_{62}$) and Tremolite (SI: 8.463, $Ca_2Mg_5Si_8O_{22}(OH)_2$), Talc (SI: 6.409, $Mg_3Si_4O_{10}(OH)_2$), Dolomite (SI: 2.014, $CaMg(CO_3)_2$), Chrysotile (SI: 3.698, $Mg_3Si_2O_5(OH)_4$) in the crack of fault zone. The highest temperature point in the study area will move to north direction and stop in the Jangjun area without the input of seawater.

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석영의 파동소광을 이용한 포천-기산리 일대의 화강암 변형의 정량화 (Quantification of Granite Deformation of Pocheon-Gisanri Area Using Wavy Extinction of Quartz Grain)

  • 정원석;윤현수;나기창
    • 암석학회지
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    • 제12권3호
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    • pp.101-109
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    • 2003
  • 석영의 파동소광은 암석의 변형도를 나타낼 수 있는 좋은 지표로서 사용할 수 있다. 암석의 변형도를 결정하기 위해 석영의 파동소광강도(IWE)를 편광현미경, 디지털 카메라, NIH Image 프로그램으로 측정하였다. 이러한 방법을 이용하여 흑운모화강암(Gb), 석류석흑운모화강암(Ggb) 그리고 복운모화강암(Gtm)으로 구성되어 있는 포천-기산리 일대의 쥬라기의 화강암류의 변형정도를 측정하였다. 본 연구에서는 크게 포천읍을 기준으로 서부에 분포하는 Gb와 동부에 분포하는 Ggb에서 파동소광의 강도 측정이 이루어 졌다. 측정 결과 Gb는 D2 이하의 낮은 변형도가 나타났고, Ggb는 D3이상의 고변형이 나타나, 전반적으로 조사지역의 북서부에서 남동부로 갈수록 변형도가 증가하는 양상을 보여주었다. 이는 1:250,000지질도에 기재된 Ggb상을 관통하는 단층에 의한 영향으로 사료된다.

옥천대(沃川帶)에서의 화성활동(火成活動) -특(特)히 옥천대동북부(沃川帶東北部)에서의 화성활동(火成活動)- (Igneous Activity in Ogcheon Geosynclinal Zone, Korea -with Special Reference to the Igneous Activity in its Northeastern Part-)

  • 이대성;김용준
    • 자원환경지질
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    • 제18권1호
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    • pp.23-39
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    • 1985
  • The northeastern part of Ogcheon zone which consisted mainly of Cambro-Ordovician arenaceous, argillaceous and calcareous formations and Carboni-Triassic arenaceous and argillaceous formations is delineated as the eastern mass of a thrust fault along Choongju-Moongyong-Cheongsan in the middle of the zone. The present study proposes a geotectonic line, Imgye-Samchog fault(see, figure 1) which divides the northeastern part into two blocks, Hambacksan block in the west and East coast block in the east. The igneous rocks in the Hambacksan block ranging from granite to gabbro are distributed in a symmetrical zones parallel to general direction of Ogcheon zone as follows (Fig. 2 and Table 2). Southeast igneous rock zone: it aligns Jurassic granites in its south and Precambrian leucocratic granites in its north. Central igneous rock zone: it aligns Cretaceous granites in its south and Jurassic granites, and some of diorite and gabbro in its north. Northwest igneous rock zone: aligns Jurassic granites in its south and huge batholithic granodiorite in its north. The distribution of the igneous rocks in the East coast block shows an entirely different features from those of Hanbacksan block. In the southern part of the block they assemble in a narrow area ranging in age from Early Proterozoic, through Middle to Late Proterozoic, Devonian, Jurassic, Cretaceous to Tertiary, whereas, the igneous rocks in the northern part of the block gathered to a restricted area, in ages of Middle Proterozoic and Cretaceous. The assemblage of the igneous rocks in the studied area shows a compositionally restricted, mixed S-type and I-type granites, $^{87}Sr/^{86}Sr$ > 0.706, rare volcanics and shortening with upright folding. These lithologic and structural features suggest that the igneous activity in this part related intimately to Hercynotype Orogeny of Pitcher(1979). Chronological episodes of igneous activity from Early Proterozoic to Early Tertiary in the northeastern part are figured.

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임피던스 계전기를 이용한 발전기 비동기 투입 보호 연구 (A Study on Protection of Generator Asynchronization by Impedance Relaying)

  • 이종훤
    • 전기학회논문지
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    • 제60권11호
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    • pp.2000-2006
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    • 2011
  • Asynchronous phenomenon occurs on the synchronous generators under power system when a generator's amplitude of electromagnetic force, phase angle, frequency and waveform etc become different from those of other synchronous generators which can follow instantly varying speed of turbine. Because the amplitude of electromagnetic force, phase frequency and waveform differ from those of other generators with which are to be put into parallel operation due to the change of excitation condition for load sharing and the sharing load change, if reactive current in the internal circuit circulates among generators, the efficiency varies and the stator winding of generators are overheated by resistance loss. Where calculation method of protection settings and Logic for Protection of Generator Asynchronization will be recommended, A distance relay scheme is commonly used for backup protection. This scheme, called a step distance protection, is comprised of 3 steps for graded zones having different operating time. As for the conventional step distance protection scheme, Zone 2 can exceed the ordinary coverage excessively in case of a transformer protection relay especially. In this case, there can be overlapped protection area from a backup protection relay and, therefore, malfunctions can occur when any fault occurs in the overlapped protection area. Distance relays and overcurrent relays are used for backup protection generally, and both relays have normally this problem, the maloperation, caused by a fault in the overlapped protection area. Corresponding to an IEEE standard, this problem can be solved with the modification of the operating time. On the other hand, in Korea, zones are modified to cope with this problem in some specific conditions. These two methods may not be obvious to handle this problem correctly because these methods, modifying the common rules, can cause another coordination problem. To overcome asynchronizing protection this paper describes an improved backup protection coordination scheme using a new Logic that will be suggested.

단양탄전, 영춘지역의 지질구조 (Geological Structures of the Yeongchun Area, Danyang Coalfield, Korea)

  • 김정환;이제용;남길현
    • 자원환경지질
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    • 제25권2호
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    • pp.179-190
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    • 1992
  • 연구지역은 충청북도 단양군 영춘면을 중심으로 하는 단양탄전 중부지역으로 단양읍의 북동부에 위치하고 있다. 연구지역내에는 선캠브라아기의 화강암질암을 기저로 하여 캠브로 오도비스기의 조선누층군, 석탄기 - 트라이아스기의 평안누층군, 트라이아스기 - 쥬라기의 반송층군이 각각 부정합을 이루며 분포하고, 대부분의 지층들은 북동 - 남서방향의 주향과 북서 방향의 경사를 가지고 대상으로 분포한다. 전반적인 지질구조의 특성으로 미루어 보아 연구지역내의 지층들은 4번에 걸쳐서 변형작용을 받았다. 첫번째 변형시기$(D_1)$에 옥동단층이 형성되었으며 이를 따라 압쇄암이 분포하고 있다. 이후에 평안누층군이 퇴적되었다. 두번째의 변형시기$(D_2)$에는 북서 - 남동 방향의 축을 갖는 습곡구조와 이와 관련된 신장선구조가 발달하였다. 이후에 화산분출작용으로 인하여 응회암이 퇴적되었으며, 이 상위로 반송층군이 퇴적되었다. 반송층군의 퇴적 이후에 두번째의 화산작용이 있었다. 대보조산운동$(D_3)$ 에 의해 발달된 각동드러스트단층에 의해 북북동 - 남남서 방향의 축을 갖는 gentle to open type의 습곡구조와 파랑선구조가 형성되었으며 flexural slip 변형작용이 드러스트 운동과 함께 우세하게 작용하였다. 마지막의 변형작원$(D_4)$에 의해 동서방향의 축을 갖는 gentle type의 습곡구조와 주향이동성 단층이 발달하였다. 변형량 분석결과, 전반적으로 암석내의 변형정도가 낮으며, 드러스트를 기준으로 상반은 prolate type, 하반은 plane strain - weak oblate type, 그리고 하반에서 비교적 먼 지역에서는 oblate type을 보여준다.

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물리탐사기법에 의한 울산광역시 약수지역 천부지하구조 조사 (Shallow Subsurface Structure of the Yaksoo Area, Ulsan, Korea by Geophysical Surveys)

  • 이정모;공영세;장태우;박동희;김태경
    • 지구물리
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    • 제3권1호
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    • pp.57-66
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    • 2000
  • 울산단층의 구조와 위치는 한반도 동남부의 지각 진화 해석에 중요한 역할을 한다. 울산단층을 피복하고 있는 충적층의 두께와 충적층 하부의 단층 수반 파쇄대를 조사하고 가능하다면 주단층의 정확한 위치를 파악하기 위하여 굴절법 탄성파탐사와 쌍극자 전기비저항탐사를 수행하고 분석하였으며, 이들 결과와 함께 이 지역에서 독립적으로 수행된 타연구의 반사법 탄성파탐사 결과를 도입하여 종합적인 해석을 하였다. 전기비저항탐사에서 동천 동쪽에서의 탐사선에서는 단층으로 사료되는 비저항 이상대가 발견되지 않았으나, 동천 서족 탐사선에는 잘 발달된 연속적인 낮은 비저항이상대를 발견하였다. 이는 울산단층의 주단층은 동천이나 동천 서쪽에 위치하는 것을 시사한다. 동천 동쪽 탐사선에서 실시한 굴절법 탄성파탐사에서는 기반암과 충적층의 경계 및 지하수면으로 사료되는 두 굴절면을 발견하였으며, 충적층의 두께는 약 30 m정도로 해석되었다. 결과해석의 신뢰도를 높이기 위하여 본 조사와 별도로 실시된 반사법 탄성파 자료를 참고한 결과 반사법 탄성파 탐사에서 발견된 많은 단층대가 굴절법탐사나 비저항탐사에서는 나타나지 않았다. 낮은 비저항 이상은 파쇄대를 따른 함수량의 영향보다는 점토의 영향에 밀접한 관련이 있는 것으로 가정할 때 고원인은 설명되나, 굴절법탐사나 비저항탐사의 해상도와 관련이 있을 수 있다. 정확한 원인구명을 위해서는 정밀한 연구가 필요하다. 일반적으로 전기비저항 탐사는 단층위치 파악에 유용한 지구물리학적 탐사법으로 알려져 있으나 본 조사에서는 반사법 탄성파 탐사에 비해 그 효과가 뚜렷하지 못하였다. 쌍극자 전기비저항탐사에서 해상도를 유지하면서 가탐심도를 증가시키기 위해서는 전개수를 늘려야 한다. 그러나 배경잡음 때문에 한계점을 가지는데, 본 조사에서 측정치의 통계학적 성질을 볼 때 조사지역에서의 측정치가 전개수 16까지는 충분한 의미를 가짐을 알 수 있었다.

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과테말라 Estancia de la Virgen 지역 금-은-동-비스무스 광화대의 산상과 광물특성 (Occurrence and Mineral Characteristics of Au-Ag-Cu-Bi Bearing Quartz Veins in the Estancia de la Virgen area, Guatemala)

  • 신의철;김수영;홍세선;김인준
    • 자원환경지질
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    • 제31권6호
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    • pp.463-472
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    • 1998
  • 이 연구는 과테말라 에스탄시아 데 라 비르겐 (Estancia de la Virgen) 지역에 분포하는 광화대의 산상과 광물특성을 밝혀내기 위해 수행되었다. 이 연구를 위해 1:2,000 축척의 정밀광상 지질조사가 이루어졌다. 금-은 광화작용은 산 아구스틴 (San Agustin) 단층과 카바나스 (Cabanas) 단층사이의 단층 블럭내에 발달하며 단층구조에 의한 규제를 받았다. 금은 미량에서 부터 최고 72 g/t, 은은 미량에서 초고 180 g/t까지의 품위를 보인다. 정밀광상 지질조사에 의하면 석영맥은 북동방향으로 연장 500 m 이상 추적되며 연속성은 불량하지만 1,000 m 이상 연장되는 양상을 보인다. 석영맥에서의 광물생성순서는 3개 단계를 나눌 수 있다. 1단계에는 황철석, 방연석, 섬아연석, 황동석이 일차 금-은 광물과 수반되며 2단계에는 휘동석, 코벨라이트, 리나라이트와 같은 Cu-Bi-Au-Ag 황화광물이 형성되었으며 이들은 대체로 방연석이나 황동석의 미세구조에 침착-부화되었다. 3단계에는 방연석, 섬아연석의 탄산염화작용, 방연석의 표성부화작용이 지표환경에서 일어났다. 이 과정에서 용탈된 일부 은이 지하수면 근처에서 산화작용이 일어나는 동안 동광석이나 방연석에 침착되었다. 섬아연석과 황동석에서 각기 Fe와 Zn의 함량이 적은 것은 이들 광물이 비교적 저온에서 형성되었음을 의미하며 이는 이전에 연구된 유체포유물의 균일화온도와도 일치한다.

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Automatic Detection of Malfunctioning Photovoltaic Modules Using Unmanned Aerial Vehicle Thermal Infrared Images

  • Kim, Dusik;Youn, Junhee;Kim, Changyoon
    • 한국측량학회지
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    • 제34권6호
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    • pp.619-627
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    • 2016
  • Cells of a PV (photovoltaic) module can suffer defects due to various causes resulting in a loss of power output. As a malfunctioning cell has a higher temperature than adjacent normal cells, it can be easily detected with a thermal infrared sensor. A conventional method of PV cell inspection is to use a hand-held infrared sensor for visual inspection. The main disadvantages of this method, when applied to a large-scale PV power plant, are that it is time-consuming and costly. This paper presents an algorithm for automatically detecting defective PV panels using images captured with a thermal imaging camera from an UAV (unmanned aerial vehicle). The proposed algorithm uses statistical analysis of thermal intensity (surface temperature) characteristics of each PV module to verify the mean intensity and standard deviation of each panel as parameters for fault diagnosis. One of the characteristics of thermal infrared imaging is that the larger the distance between sensor and target, the lower the measured temperature of the object. Consequently, a global detection rule using the mean intensity of all panels in the fault detection algorithm is not applicable. Therefore, a local detection rule was applied to automatically detect defective panels using the mean intensity and standard deviation range of each panel by array. The performance of the proposed algorithm was tested on three sample images; this verified a detection accuracy of defective panels of 97% or higher. In addition, as the proposed algorithm can adjust the range of threshold values for judging malfunction at the array level, the local detection rule is considered better suited for highly sensitive fault detection compared to a global detection rule. In this study, we used a panel area extraction method that we previously developed; fault detection accuracy would be improved if panel area extraction from images was more precise. Furthermore, the proposed algorithm contributes to the development of a maintenance and repair system for large-scale PV power plants, in combination with a geo-referencing algorithm for accurate determination of panel locations using sensor-based orientation parameters and photogrammetry from ground control points.