• 한국지하수토양환경학회:학술대회논문집
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• 한국지하수토양환경학회 2005년도 INTERNATIONAL SYMPOSIUM ON SOIL & GROUNDWATER ENVIRONMENT
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• pp.259-260
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• 2005

• 자원환경지질
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• 제32권2호
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• pp.169-175
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• 1999

The water leakage of reservoir embankment usually occurs through water vein, which gives little influence on the embankment in a normal state. However, the embankment can be destroyed when the water level of reservoir increases with heavy rain in summer. Investigating the water vein and its path is therefore very important from the viewpoint of disater prevention and embankment protection. This paper presents survey results of one-meter-depth ground temperature and multi-point temperature logging in an embankment in Japan to delineate water veins and permeable formations. Four water veins have been predicted in the embankment by comparing measured one-meter-depth ground temperatures with the background ones which have no effect of water vein. The multi-point temperature logging was carried out in the borehole drilled at one of the predicted water veins. Depth and thickness of the permeable formation in the borehole can be determined from temperature restoration ratios with elapsed time. From these results we can find that the water leakage of reservoir embankment mainly occurs in sandy soil formation in the embankment.

• 정보교육학회논문지
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• 제18권1호
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• pp.25-33
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• 2014

최근 교육용 로봇 하드웨어 발달로 연산 처리 속도 및 확장성이 매우 좋아졌다. 이에 따라 로봇 하드웨어에 MBL용 온도 센서나 자이로 센서도 호환되어 데이터 로깅이 가능해졌다. 데이터 로깅이 가능한 교육용 로봇으로 학생들은 과학적인 탐구 예측, 수집, 데이터 분석이 가능한 실험을 할 수 있게 된 것이다. 이에 본 연구에서는 학급 SNS와 스마트폰을 활용한 'Smart r-Learning'에 데이터로깅이 가능한 교육용 로봇을 도입하여 과학 프로젝트 수업을 개발하고 적용했다. 데이터 로깅 활용 Smart r-Learning 프로젝트 수업을 초등학교 5학년 학생들에게 적용한 결과 논리적 사고력 6개 영역 중 4개 영역이 유의미하게 향상된 것으로 나타났다.

• 자원환경지질
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• 제32권5호
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• pp.503-517
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• 1999

The purpose of this study is to verfify a more effecive techique for calculating geothermal gradient. this study examines 370 data of temperature-logging having been collected since 1985. The daya are divided into three different grades grades according to the type of temperature-depth plots: 204 data show typical linear gradient (Grade A); 126 data do not explicitily show the gradient becase of various external effects such as water flow (Grade B); and the rest 40 data do not show the gradient at all (Grade D). The new technique for calculating geothermal gradient is to be required to use Greade-B data more effctiviely. This new technique includes (1) calculating the independer depth of atmospheric temperature in the earth; (2) drawing a distribution map of subsurface tempurature by using the distribution map of subsurface temperature by using Grade-A data at the independent depth; and (3) recalculating geothermal gradient of Grade-B data by using the distrbution map of subsurface temperature, borehole depth, and bottom temperature of Grade-B data by using the distribution map of subsurface temperature, borehole depth, and bottom temperature of Grade-B data. As a result, 330 data-both Grade-A and Grade-B data--can be used to draw a distribution map of hot spradient. The map clearly distinguishes anomaly areas, and helps interpret their relations to the distribution of hot springs, geology, geological structures, and geophysical anomaly areas. These new results reveal that the average of geothermal in south Korea is 25.6$^{\circ}C$/km, when calculated to the Kriging method.

• 한국지구물리탐사학회:학술대회논문집
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• 한국지구물리탐사학회 2003년도 Proceedings of the international symposium on the fusion technology
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• pp.432-436
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• 2003

Geophysical well logging techniques which are useful for delineating permeability of geological formation have been reviewed. A new technique for obtaining permeability using conductivity log technique has been discussed. This conductivity logging technique has been tested by monitoring the conductivity change within the model hole using borehole environment water and incoming-outgoing water of different salinity with constant flow rate by maintaining balance between inflow and outflow. Conductivity variation features depended mainly on flow rate, density contrasts due to salinity and temperature contrasts between fluid within the hole and incoming-outgoing fluid. The results of the experiment show uniform change of fluid conductivity within bore hole with time, and a fairly good correlation between the flow rate and the conductivity change rate. This conductivity logging technique is expected to be an efficient tool for determining permeability.

• 센서학회지
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• 제16권3호
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• pp.187-191
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• 2007

This paper presents a development of the multi-channel data acquisition/logging system for a sensor signal processing and a method of the evaluation and a temperature compensation for the A/D converters with the specific analog and digital circuit including the software. Also, we have designed a hardware and a software filters with smart algorithm for better signal processing of the proposed system. Software approach was adopted to obtain the stable data from A/D converter.

• 전자공학회논문지CI
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• 제48권2호
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• pp.96-105
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• 2011

유비쿼터스 센서 네트워크(USN: Ubiquitos Sensor Network)는 우리 생활 전반적으로 다양하게 적용되고 있는 기술이다. 본 논문은 온도와 습도를 일정하게 유지해야 할 필요가 있는 공간을 효율적으로 관리할 수 있는 USN 기술 기반의 시스템에 대한 설계 및 이의 구현 사례를 소개한다. 본 시스템은 온 습도 센서가 내장된 다수의 센서 모듈을 이용하여 대상 공간에 무선 센서 네트워크를 구성하고, 각 모듈의 센서로부터 감지된 온 습도 정보를 실시간으로 수집하여 Database에 기록함과 동시에 사용자가 그래픽 인터페이스를 통해 대상 공간의 온 습도 현황을 Monitoring 할 수 있는 시스템이다. 또한, 각 온 습도 센서 모듈의 관리 대상 공간에 대하여 특정 온 습도 값을 지정하고 이 값과 일정 수준 이상의 오차가 발생하면 경고를 발생토록 한다. 본 논문에서 소개하는 시스템은 수동적이었던 기존의 데이터 수집 및 관리 방식을 자동화함으로서 보다 편리하고 효율적으로 대상 공간의 온 습도를 관리할 수 있으며, 저장된 데이터를 이용하여 온 습도로 인해 발생된 문제점에 대한 사후 분석 및 환경의 개선에 필요한 정보를 얻을 수 있다.

• 한국지하수토양환경학회:학술대회논문집
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• 한국지하수토양환경학회 2002년도 추계학술발표회
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• pp.9-12
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• 2002

The purpose of this study is to understand the high saline water phenomenon of Handong-ri area in the eastern coast of Jeju Island, were investigate the tidal effect of groundwater level, variation of electric conductivity and temperature, geological logging on the monitoring wells, chemical water quality, and ratios of oxygen istope of groundwater and seawater Results in investigating variation of interface zone of freshwater and saline water represented that the hyaloclastites formed at below groundwater table is developing toward the coast; this area consisted of stratum of good permeability. Hyaloclastites is presumed the main path of the high salinity water There are a lot of movement by the tide at upper layer. Salinity of lower layer spreads to upper up step in proportion to tidal energy. Because of hydrogeological characteristics, Interface zone of freshwater and saline water is made, High salinity of groundwater occur in east coastal area of Jeju Island. Therefore, I think that high saline groundwater phenomenon is natural condition by simple mixing.

• 한국신재생에너지학회:학술대회논문집
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• 한국신재생에너지학회 2005년도 춘계학술대회
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• pp.693-696
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• 2005

KIGAM (Korea Institute of Geoscience and Mineral Resources) launched a new project to develop the low-temperature geothermal water in the area showing high geothermal anomaly, north of Pohang city, for large-scale space heating. Surface geologic and geophysical surveys including Landsat 1M image analysis, gravity, magnetic, Magnetotelluric (MT) and controlled-source audio-frequency MT (CSAMT), and self-potential (SP) methods have been conducted and the possible fracture zone was found that would serve as deeply connected geothermal water conduit. In 2004, two test wells of 1.1km and 1.5km depths have been drilled and various kinds of borehole survey including geophysical logging, pumping test, SP monitoring, core logging and sample analysis have followed. Temperature of geothermal water at the bottom of 1.5km borehole reached over $70^{\circ}C$ and the pumping test showed that the reservoir contained huge amount of geothermal water. Drilling for the production well of 2 km depth is on going. After test utilization and the feasibility study, geothermal water developed from the production well is going to be provided to nearby apartments.

• 지질공학
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• 제21권1호
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• pp.45-55
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• 2011

본 연구에서는 소하천변 충적층을 대상으로 9개 지하수 관측공내 유속 실험과 온도 계측을 통한 시간별, 심도별 온도 변화 추이 평가 및 지화학 분석 등을 통하여 지표수와 지하수간의 상호 작용에 대하여 분석하였다. 하천변에 근접한 2개 지하수 관측공은 타 관측공과 달려 지하수 유향이 하천에서 주변 충적층으로 향하고 있으며, 계절에 따른 온도 변화가 대기 및 하천과 유사하게 나타난다. 또한 이들 지점은 하천수의 영향을 받은 지화학 특성을 보일 뿐 아니라 계절에 따라 지화학 특성이 변화하는 등 지표수의 유입 유출이 활발한 지점에 해당한다. 본 연구에서 사용된 온도 측정 장치인 Thermochron I-button은 저비용의 소규모 장치로서 지표수와 지하수의 상호 작용 평가에 활용도가 높다.