• 한국전자파학회논문지
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• 제9권5호
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• pp.687-697
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• 1998

최근 국내 전력설비에서 발생하는 전자계에 대한 관심이 증가하고 있지만 이에 대한 정확한 자료 파악은 극히 미미한 실정이다. 본고에서는 송전선로에서 발생하는 전계와 자계의 수준을 알아보기 위하여 전국 1537H의 송전 선로를 대상으로 전계와 자계를 측정하였다. 측정 지점의 전계와 자계 최대치들의 중간값은 각각 0.47 kV /m, 11.6 mG 최고 값은 각각 3.16 kV /m, 125 mG로 나타났으며, 전세계의 전자계 관련 권고치나 기준치에 비해 낮은 값임을 알 수 있었다. 아울러 몇 가지 경우에 대하여 가전제품에서 발생하는 자계와 일일 자계 노출량올 측정 하였고 이를 송전선로의 자계 크기와 비교하였다.

• 대한원격탐사학회:학술대회논문집
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• 대한원격탐사학회 2006년도 Proceedings of ISRS 2006 PORSEC Volume I
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• pp.157-157
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• 2006

• 한국마린엔지니어링학회:학술대회논문집
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• 한국마린엔지니어링학회 2011년도 전기공동학술대회 논문집
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• pp.244-244
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• 2011

• 지질공학
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• 제28권4호
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• pp.619-630
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• 2018

울릉도 화산암체 내 단층 및 관입암체의 존재 여부 등을 파악하기 위한 목적으로 자력탐사를 실시하고 이의 정성적인 해석을 통해 자기이상 변화를 분석하였다. 울릉도 전역에 대한 자력탐사 자료 분석결과, 염기성암인 현무암질암류는 높은 자기이상을 나타내고 산성암인 조면암질암류는 낮은 자기이상을 나타내었다. 이들 자기이상은 모두 울릉도 화산암체의 암상과 대체로 잘 일치하며 화산암의 종류에 따라 대비를 이루고 있어 자기이상 분포의 상호 분석을 통한 전석, 충적층, 퇴적층 등으로 피복되어 있는 지역의 암상 구분에 활용 가능이 가능하다. 또한, 나리칼데라에서 현무암질암류가 관찰되지는 않으나 $1,000{\gamma}$ 이상의 높은 자기이상이 분포하는 것은 조면암질암류의 분출 이전에 형성된 현무암질암류로 이루어진 화구 및 화도에 의한 것으로 추정된다. 나리칼데라 이외 지역에서 나타나는 높은 자기이상의 분포지역 중 일부는 화구 및 화도로 추정이 가능하며 울릉도 남서쪽의 남양리 부근에 분포하는 큰 규모의 $1,000{\gamma}$ 이상의 높은 자기이상은 현무암질암류의 화구 및 화도 가능성이 클 것으로 사료된다.

• 자원환경지질
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• 제14권2호
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• pp.77-91
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• 1981

An airborne magnetometer survey was carried out over an offshore area of about $200,000km^2$ from the southeastern, southern and western part of Korea. Detailed magnetic studies on the geological structure of the southern part of above area ($100,000km^2$) was accomplished. Residual aeromagnetic map was made in order to delineate magnetic provinces, magnetic lineaments and sedimentary basins by application of least square method using computer system. To determine the depth of the sedimentary basins pseudo-gravimetric method was applied. 1. The area studied is divided into four magnetic provinces for the purpose of interpretation on the basis of the magnetic maps. 2. Near shore area and its attached islands of southern part (fiirst and second magnetic province) can be regarded as being the extension from the land geology due to presentation of strong magnetic anomalies and shallow magnetic basements. 3. Magnetic lineament 1-1 is strong magnetic anomalous region which is presumably relevant to volcanic activities in Cretaceous. The depth of magnetic basement of the lineament was determined to 1,500 m. Negative magnetic anomalous zones B1-1 and B1-2 which represent Tertiary basins showed depth of magnetic basement 3 km and 4 km each. The latter can be interpreted as extension of the Taiwan basin which is consisted of Tertiary sediments. 4. Magnetic lineament 2-1 coincide with Rainan-Fukien massif running NE-SW direction. A lineament located in central part of magnetic lineament 2-1 is well connected with extension of Sobacksan anticlinal axis on land. Volcanic rocks in Gyongsang system concentrated along this lineament. 5. The characteristics of magnetic pattern in the southern Yellow sea basin of western part of Jeju island show weaker magnetic anomalies and deeper magnetic basements than first and second magnetic provinces indicating geological structure of this basin seems to be quite different from that of Jeju strait. 6. In southern part of Jeju island, smoother magnetic pattern develope southward. Maximum depth of magnetic basement in sedimentary basins BIV-1 and BIV-2 were determined down to 6,000 m increasing its thickness toward Taiwan up to 11,000 m in the shelf area off Taichung, Taiwan. Judging from the fact that hydrocarbon was founded in the Tertiary sediments of western coastal area of Taiwan, it can be expected that hydrocarbon will be existed in these sedimentary basins of southern part of Jeju island.

• 자원환경지질
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• 제30권5호
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• pp.451-458
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• 1997

The horizontal magnetic dipole as well as electrical dipole was adopted as a source to compute one-dimensional electromagnetic field behavior in controlled source magnetotellurics. he Cagniard impedances due to horizontal magnetic dipole source, especially phases, showed better frequency characteristics than those due to electric one. The magnetic dipole is inferior to the electric dipole in the point of relatively weak transmitting power at low frequency. But considering high resistivity charateristics of Korean geology, the magnetic dipole source is recommended for the survey up to depth of 500 m. A vector CSMT was introduced to get more reliable data in the area of two- or three-dimensional structures. A software and interpretation technique using polarization ellipses were developed. The technique was tested by synthetic data, which provided theoretical basis of the methodology. Although CSMT has inevitable limitation of investigation depth due to practically possible source-receiver separation, we proposed to use the technique developed in this paper where MT is not available, for example, in extremely noisy area or for shallow target.

• 대한한방부인과학회지
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• 제19권2호
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• pp.261-270
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• 2006

Purpose : The purpose of this study is to show the effect of acupuncture, moxibustion and magnetic innervation therapy for urinary incontinence symptoms. Methods : Ten female patients suffering from urinary incontinence had been given the treatments of acupuncture, moxibustion and magnetic innervation therapy for more than 8 times. Before and after treatment, they accomplished questionnaire for quality life survey and checked vaginal pressure measurement with perionometer. Results : The results were as follows 1) The mean${\pm}SD$ of Questionnaire score was significantly decreased from $35.40{\pm}11.88$ to $21.20{\pm}7.66$ after treatment(P<&0.047). 2) The mean${\pm}SD$ of maximum vaginal presssure was significantly increased from $48.80{\pm}25.35mmHg$ to $62.20{\pm}25.09mmHg$(p<&0.040). 3) The mean${\pm}SD$ of average vaginal presssure was significantly increased from $33.50{\pm}19.62mmHg$ to$43.10{\pm}16.49mmHg$(p<&0.015). Conclusion : Our results suggested that acupuncture, moxibustion and magnetic innervation therapy is effective for urinary incontinence symptoms.

• 천문학회보
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• 제45권1호
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• pp.59.3-60
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• 2020

We present the results of polarization observations at submillimeter wavelengths towards Monoceros R2 (Mon R2). The polarized thermal dust emission was obtained from SCUBA-2/POL-2 at 450 ㎛ and 850 ㎛, simultaneously. This observation is a part of the JCMT BISTRO survey project. The polarization angle distributions at 450 ㎛ and 850 ㎛ are similar and the mean value of angle differences at two wavelengths is 5.5 degrees. The Mon R2 is one of massive star-forming regions containing a clear hub-filamentary structure. The hub region shows star formation activities, and surrounding filaments provide channels for matters to move into the hub region. It is not well known the role of magnetic fields in a hub-filamentary structure. Some studies have shown well-ordered polarization segments along a filamentary structure and magnetic field morphology traced by polarization segments is interpreted as to help gas flow along the filamentary structrue. Our observations shows that filaments in Mon R2 have spiral structure and the magnetic field lines are parallel to the filaments. We interpret that the spiral structure can be formed by a rotation hub-filament system with gas flowing along the filaments to the hub. We found several dust clumps at the central part of the hub region of the Mon R2. They seems to be formed at locations where spiral field lines meet each other. These results show one observational example that a magnetic field play a role in gas flow.

• 한국지구물리탐사학회:학술대회논문집
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• 한국지구물리탐사학회 2003년도 Proceedings of the international symposium on the fusion technology
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• pp.410-415
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• 2003

Ground subsidence has occurred in the downtown of Muan-eup in Korea. Integrated geophysical survey, including two-dimensional resistivity, CSMT(Controlled source magnetotelluric), magnetic, borehole logging, GPR and resistivity tomography, has been conducted to investigate the cause of subsidence and ground conditions. Since the target area is in the city downtown, there were no spaces for surface geophysical methods. To get regional geology and to facilitate the detailed geophysical interpretation in the survey area, two-dimensional resistivity, CSMT and magnetic surveys have been applied in the outer region of the downtown. From these results, we could accurately define the Gwangju fault system and estimate the geologic conditions in the downtown. For the detailed survey of the downtown area, resistivity tomography and borehole logging data have been acquired using a few tens of densely located boreholes. Among these survey results, borehole logging data provided the guide to classification of the rock type and we could define the geologic boundary of granite and limestone formations. From the resistivity tomograms of 42 sections, which are densely located enough to be interpreted in a three-dimensional manner, we could delineate the possible weak zones or cavities in the limestone formations. In particular, resistivity tomograms in the subsided area showed the real image of ground subsidence. The map of hazardous zone has been derived from the joint interpretation of these survey results and we could provide the possible reinforcement strategy in this area.

• 한국재난관리표준학회지
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• 제1권4호
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• pp.73-81
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• 2008

전자유도 탐사는 매설관로에서 발생되는 자기장을 측정하는 탐사방법으로 하나의 관로만 매설되어 있는 경우에는 20 cm 이내의 높은 정확도를 보이지만, 탐지대상 관로 인근에 다른 관로가 매설되어 있으면 자기장의 교란으로 정확도가 감소한다. 본 연구에서는 지하매설물 탐지 정확도 향상을 위하여 대칭성을 이용하여 매설관로의 수평위치를 검증하는 방법과 에너지 크기 비교법과 삼각법을 이용하여 매설심도를 검증하는 방법에 대해 고찰하였다. 다음으로 현재 판매되는 전자유도 탐사장비가 별도의 저장장치를 가지고 있지 않아 측정자료의 분석이 불가능한 문제를 개선하기 위하여, Bluetooth 무선통신장치를 이용하여 측정자료를 저장하는 방법을 개발하였다. 마지막으로 두 개의 인접관로를 하나로 오인하는 문제점을 개선하기 위하여 현장모형실험을 통해 인접관로의 거리에 따른 분해능을 고찰하였다.