• 한국지반공학회논문집
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• 제19권5호
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• pp.327-333
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• 2003

터널 및 지하공동 설계에 이용된 23개 지역의 578개의 시추공발파 진동 data와 시공 중인 일반터널의 4개 지역으로부터 221개 진동 data를 이용, 시추공발파의 진동전달 특성을 분석하였다. 시추공발파와 일반터널발파의 진동속도 감쇠 경향을 비교 분석한 결과 시추공발파의 입지상수들이 크게 나타났다. 환산거리가 클 때 최대 허용장약량은 시추공발파의 식으로 계산한 것이 더 적었다. 주진동수에 대한 주파수 분석결과 시추공발파는 30∼60Hz, 일반터널발파는 60∼90Hz로 나타났다. 이러한 결과로부터 시추공발파 자료를 터널발파 설계에 직접 사용하는데 다소의 문제가 있는 것으로 판단되며 보다 정확한 설계를 위하여 통계적 처리가 불가피할 것으로 보인다.

• 설비공학논문집
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• 제18권10호
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• pp.783-790
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• 2006

A one-dimensional numerical model coupled with parameter estimation is used to predict the effective thermal conductivities of soil formations and borehole resistances from in situ field test data. In this application a new method of using initial ignoring time (IIT) obtained from error estimation is tried and turned out to be successful in determining soil thermal conductivities. This method is used for single-U and double-U borehole system. The results of this method are compared and agreed well with those of existing software (GPM) in the analysis of single-U borehole data. In the analysis of double-U borehole data this method seems to be better in predicting soil and borehole properties.

• 한국지반공학회:학술대회논문집
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• 한국지반공학회 2002년도 가을 학술발표회 논문집
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• pp.231-236
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• 2002

The understanding of underground geologic structures is of great importance for the surface and subsurface constructions, prevention of natural hazards such as land-slides and subsidence, and many other areas. To get the information on the geologic conditions, many of investigations such as geologic survey, geophysical explorations, testings on the physical properties of rocks, drilling tests and logging, and groundwater surveys are usually conducted, and tremendous data are collected accordingly. In general, however, these huge amount of data are interpreted in the individual areas only. If these data are analyzed collectively, much more information on the geologic conditions can be obtained. In this study, 3D visualization of borehole logging data is attempted. Borehole logging data are obtained at the urban subsidence area. To compare the 3D logging data with other geologic and geophysical data such as resistivity tomography data, interface module was developed. The 3D visualization of logging data and the comparison with other data can be helpful for the understanding of underground geologic structures.

• 한국태양에너지학회 논문집
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• 제29권5호
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• pp.20-27
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• 2009

The effect of borehole thermal resistance on the borehole length is studied. In performing this work a new concept BLRR(borehole length reduction rate) is developed based on the line source model. The solution of line source model is shown to be valid through the comparison with the data of thermal response test. It is shown that BLRR is a function of soil thermal conductivity(k) and borehole thermal resistance($R_b$). The value of BLRR increases with increasing k, which means reducing $R_b$ is more effective when k is high. The reduction of borehole length with change of $R_b$ is easily estimated with BLRR. The validity of BLRR is also examined with EED analysis.

• 대한기계학회논문집B
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• 제30권8호
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• pp.764-771
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• 2006

Knowledge of ground thermal properties is most important for the proper design of large BHE(borehole heat exchanger) systems. Thermal response tests with mobile measurement devices were first introduced in Sweden and USA in 1995. Thermal response tests have so far been used primarily for in insitu determination of design data for BHE systems, but also for evaluation of grout material, heat exchanger types and ground water effects. The main purpose has been to determine insitu values of effective ground thermal conductivity, including the effect of ground-water flow and natural convection in the boreholes. Test rig is set up on a small trailer, and contains a circulation pump, a heater, temperature sensors and a data logger for recording the temperature data. A constant heat power is injected into the borehole through the pipe system of test rig and the resulting temperature change in the borehole is recorded. The recorded temperature data are analysed with a line-source model, which gives the effective insitu values of rock thermal conductivity and borehole thermal resistance.

• 한국지반공학회:학술대회논문집
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• 한국지반공학회 2004년도 춘계학술발표회
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• pp.815-822
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• 2004

A knowledge of in situ stress state is important to design various engineering structures such as dams, tunnels and so on. There are about three wellknown indicators that is, borehole will breakouts, hydraulic fracturing, ellipsoidal cross section of borehole that have been attributed to the state of stress in the vicinity of borehole. Fortunately, Televiewer traveltime image can be used as a caliper log with 144 or 288 arms, which allows to determine the borehole shape. Televiewer amplitude image will give detailed information about the distribution and character of breakouts and hydraulic fracturing as well. For investigation purposes, a series of boreholes(total 195 boreholes: 12.239m) that have been logged all over the country during past 10 years are analyzed. The primary objective of this paper are to examnine the ability of a Televiewer to determine the shape of borehole, to present data inferred by stress indicators, to indicate their possible relationship with the anisotropic horizontal stresses. It is shown that in most cases the fracture orientation statistically estimated from observed fractures denotes an excellent correlation with the orientations inferred by stress indicators. Many intervals of breakouts are terminated at the intersection of oblique fracture with the borehole. The results from Televiewer data are further compared with those of hydraulic fracturing techniques.

• Journal of electromagnetic engineering and science
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• 제14권2호
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• pp.79-81
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• 2014

In B-scan data measured by a pulse-type monostatic borehole radar, target signatures are seriously obscured by two clutters that differ in orientation and intensity. The primary clutter appears as a nearly constant time delay, which is caused by internal ringing between antenna and transceiver in the radar system. The secondary clutter occurs as an oblique time delay due to the guided borehole wave along the logging cable of the radar antenna. This issue led us to perform adaptive filtering processing for orientation-based clutter removal. This letter describes adaptive filtering processing consisting of a combination of edge detection, data rotation, and eigenimage filtering. We show that the hyperbolic signatures of a dormant air-filled tunnel target can be more distinctly enhanced by applying the proposed approach to the B-scan data, which are measured in a well-suited test site for underground tunnel detection.

• 한국신재생에너지학회:학술대회논문집
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• 한국신재생에너지학회 2009년도 추계학술대회 논문집
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• pp.581-586
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• 2009

Knowledge of ground thermal properties is most important for the proper design of large scale BHE(borehole heat exchanger) systems. The type, pipe size and thermal performance of the BHE is highly dependent on the ground source heatpump system-efficiency and instruction cost. Thermal response tests with mobile measurement devices were developed primarily for insitu determination of design data for large diameter BHE for triple-U spacer apply. The main purpose has been to determine insitu values of effective ground thermal conductivity and thermal resistance, including the effect of ground-water flow and natural convection in the boreholes. The test rig is set up on a some trailer, and contains a circulation pump, a inline heater, temperature sensors, flow meter, power analysis meter and a data logger for recording the temperature, fluid flow data. A constant heat power is injected into the borehole through the tripl-U pipes system of test rig and the resulting temperature change in the borehole is recorded. The recorded temperature data are analysed with a line-source model, which gives the effective insitu values of rock thermal conductivity and borehole thermal resistance of large diameter BHE for spacer apply.

• 지구물리와물리탐사
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• 제16권4호
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• pp.203-210
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• 2013

화천 시추공 지진관측소의 부지특성을 살펴보기 위해 지표와 시추공 자료에 기록된 배경잡음과 지진신호의 특성을 분석하였다. 배경잡음을 분석한 결과, 비교적 잡음유입이 적은 밤 시간대에 비하여 낮 시간대에서 지표/시추공 잡음에너지 비가 약 15배 높게 나타났으며, 저주파에서 고주파로 갈수록 지표/시추공 스펙트럼 비가 크게 나타났다. 지진신호에 대해서는 P파와 SH파의 우세주파수 양상을 비교하였는데, 진앙거리가 가깝고, 규모가 작은 국내지진은 지표자료에서 8 Hz와 46 Hz에서 우세주파수를 보이며 시추공 자료와 다른 값을 나타내었다. 이는 수평/수직 스펙트럼 비 분석으로 구한 퇴적층의 공명주파수(7.4 Hz, 46 Hz)와 일치하며 상부 퇴적층에 영향을 받아 증폭현상이 나타나고 있음을 시사한다. 이번 연구를 통해 지표 관측소에 비하여 시추공 관측소에서는 배경잡음이 최대 20,000배 이상 감소되고, 상부퇴적층에 의한 증폭현상이 나타나지 않아 양질의 자료를 획득하여 지진관측능력이 향상될 수 있음을 알 수 있었다.

• 한국지하수토양환경학회:학술대회논문집
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• 한국지하수토양환경학회 2004년도 임시총회 및 추계학술발표회
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• pp.431-434
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• 2004

To understand the stratigraphy for a hydrogeological setting, borehole logging data are used. The test site is located in Mangyeong-river bank area in Dodeok-dong Jeonju. 11 boreholes are developed to monitor groundwater level and quality. Based on the borehole data, SOLID model is used to get the distribution of each layer.