• Journal of Biosystems Engineering
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• 제27권6호
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• pp.537-546
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• 2002

In this study an automatic soil hardness measuring system mountable on agricultural tractors was developed to improve the accuracy of manual soil hardness testers by a constant penetrating rate, right direction of the cone-penetrometer and the isolation of vibration from the operator. This was necessary to supply similar experimental condition for performance test of new model and comparative experiment. The results of the study are summaried as follows; 1. The system consisted of a sensing part of soil hardness, a driving part of the measuring system and an attaching part between the tractor and the measuring system. 2. The allowable limit value of the system developed was set to 392N to protect from breaking the serve motor and the coupling used in this system. 3. The driving shaft penetrated into soil by 0.3m to measure soil hardness. The soil hardness was measured at the depth of 0.3m from the soil surface but the penetrating work was stopped and the driving shaft was pulled out to protect the system when the value of the soil hardness was too big on foreign substances like stones or straws. 4. Two values measured by automatic measuring system developed in this research and manual penetrometer were compared by statistics hypothesis testing method. When two people measured the soil hardness at the depth of 0.1 and 0.15m by manual cone penetrometer, there was no relationship between two values by two people but the values at the same depths by automatic measuring system developed showed similarity. The automatic system, therefore, developed in this research was proper for measuring soil hardness.

• 지질공학
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• 제17권4호
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• pp.517-523
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• 2007

이 연구에서는 초정지역의 충적층 지하수와 관련된 풍화대분포를 파악하고 단층파쇄대 조사를 위해 복합물리탐사(탄성파굴절법, 전기비저항, 지하투과레이더탐사)를 수행하였다. 탄성파속도 정보로부터 풍화대는 대상지역의 남서부로 갈수록 깊어지는 것으로 나타나는데 기반암까지의 심도 즉 풍화대의 두께는 또한 기존의 시추자료 및 지하수위 자료와 거의 일치한다. 소규모 단층과 관련된 파쇄대 조사에서는 탄성파굴절법, 전기비저항, 레이더탐사 자료를 속도와 비저항 구조를 복합적으로 천부까지 해석하여 단층파쇄대의 지표 경계등을 파악하였다. 복합 지구물리탐사로 정확히 제시된 풍화대와 파쇄대 등에 대한 정보는 충적층 지하수의 분포를 알아내는데 충분히 활용될 수 있을 것으로 보인다.

• Computers and Concrete
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• 제6권1호
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• pp.79-93
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• 2009

In the present paper, a methodology has been presented for the reliability assessment of concrete barriers that lie at a certain depth in the soil, and a missile (a rigid projectile) impacts the top of the soil cover normally, and subsequently after penetrating the soil cover completely it hits the barrier with certain striking velocity. For this purpose, using expressions available in the literature, striking velocity of missile at any depth of soil has been derived and then expressions for the depths of penetration in crater and tunnel region of concrete barrier have been deduced. These depths of penetration have been employed for the derivation of limit state functions. Using the derived limit state functions reliability assessment of underground concrete barrier has then been carried out through First Order Reliability Method (FORM). To study the influence of various random variables on barrier reliability, sensitivity analysis has also been carried out. In addition, a number of parametric studies is conducted to obtain the results of practical interest.

• 한국구조물진단유지관리공학회 논문집
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• 제20권2호
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• pp.86-93
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• 2016

본 연구에서는 토조에 설치한 관의 종류 및 매립 깊이, 공동 깊이 및 포장 조건 등에 대한 GPR(Ground Penetrating Radar) 탐사를 진행하여 매립관의 종류 및 공동 탐사 능력을 실험적으로 규명하였다. 아스팔트 포장 및 비포장의 경우, 콘크리트 포장 및 철근 콘크리트 포장 대비 매립관의 탐사가 용이한 것으로 평가되었다. 또한 공기 공동의 경우, 매립 깊이 1 m에서는 탐지가 가능한 것으로 평가되었다.

• 한국지구물리탐사학회:학술대회논문집
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• 한국지구물리탐사학회 2005년도 공동학술대회 논문집
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• pp.151-154
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• 2005

전 지구적 환경 모니터링을 위한 빙하 시추의 예비 탐사로서 남극 리빙스톤섬에서 GPR (Ground Penetrating Radar) 탐사를 실시하였다. 탐사지역은 세종기지가 위치한 킹죠지섬으로부터 남서쪽으로 80 km 위치한 곳으로 해발 340 m의 Mt. Charra 부근에 위치한다. 총 5개의 측선을 탐사했으며 3개의 반사법과 2개의 CMP (Common Midpoint) 방법을 실시하였다. 탐사결과 연구지역에서 빙하층은 전자기파의 속도와 반사단면의 특징으로 3개로 나누었다. 빙하의 두께는 $80{\~}110\;m$에 이르는 것으로 추정되고 층에 따라 빙하 내부에 다량의 물과 화산재를 포함하고 있는 것으로 해석된다.

• 지구물리
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• 제8권2호
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• pp.63-66
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• 2005

전 지구적 환경 모니터링을 위한 빙하 시추의 예비 탐사로서 남극 리빙스톤섬에서 GPR (Ground Penetrating Radar) 탐사를 실시하였다. 탐사지역은 세종기지가 위치한 킹죠지섬으로부터 남서쪽으로 80 km 위치한 곳으로 해발 340 m의 Mt. Charra 부근에 위치한다. 총 5개의 측선을 탐사했으며 3개의 반사법과 2개의 CMP(Common Midpoint) 방법을 실시하였다. 탐사결과 연구지역에서 빙하층은 전자기파의 속도와 반사단면의 특징으로 3개로 나누었다. 빙하의 두께는 80∼110 m에 이르는 것으로 추정되고 층에 따라 빙하 내부에 다량의 물과 화산재를 포함하고 있는 것으로 해석된다.

• 한국산업보건학회지
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• 제25권1호
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• pp.82-88
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• 2015

Objectives: This study is designed to analyze the penetration performance into ceiling materials containing asbestos of scattering prevention agents and investigate the change in penetration depth and viscosity according to the dilution rate of anti-scattering agents diluted with distilled water. Methods: Five different types of scattering prevention agents were spread on plate-type asbestos ceiling materials. The penetration depth of each coated ceiling material was measured by energy dispersive spectroscopy (EDS) analysis, based on X-ray fluorescence (XRF) results of the non-coated ceiling materials. Test equipment installed the ceiling materials and 60 minutes were collected at a flow rate of $10{\ell}/min$ at a filter of 25 mm. Results: An EDS analysis of the cross-section of ceiling materials constructed with a scattering prevention agent revealed that potassium is detected in the process of penetrating hardener solidification and this element could be an indicator for infiltration. When anti-scattering agents with different viscosities were constructed and the penetration depth was analyzed by potassium detection assessment using EDS, the depth results with viscosities of 5.0, 2.5, and 1.9 cP were 98.5, 103, and $147{\mu}m$, respectively. Penetration performance improved with decrease in viscosity. Conclusions: For asbestos ceiling materials, it is concluded that a higher dilution rate of the scattering prevention agent leads to lower viscosity, and hence a deeper penetration depth from $156{\mu}m$ to 3 mm. The asbestos anti-scattering properties according to the penetration depth will be confirmed through further study.

• 터널과지하공간
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• 제5권2호
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• pp.114-122
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• 1995

The principle and applications of GPR(Ground Penetrating Radear) are familiar to engineering geologists and geophsicists as very attractive technique for continuous high resolution images of the subsurface. However, the main limitation of GPR is obviously related to presence of clayey or silty conductive soils, resulting in complete attenuation of radar signals. This difficulty gives hesitation for the exploration of the deeper targets for example detecting bedrock, particularly in Korean situation that most regions have conductive overburden. In order to prove usefulness of geological survey with GPR in that situation, the technique was tried to investigate depth of bedrock under thick conductive overburden and the other geolocgical informations for the constructionof foundation in the Dongbu apartment site, Kimhae. The reflection patterns on the processed GPR sections are well correlated with the geotechnical units-bedrock, alluvium, landfill unit and their internal layer-boundaries of boring data before GPR survey, except upper contact of bedrock. The isopach maps of the geotechnical units for the 3-D interpretations are made from GPR sections. The maps provided useful geological information that bedrock was distributed as plain and valley with 22~27m depth under alluvium unit (this depth is 5~8 m deeper than drill log) and sedimentary layers subsided and bended along growth fault with NNE strike/15$^{\circ}$SE dip in alluvium unit.

• 전자공학회논문지
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• 제54권5호
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• pp.74-84
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• 2017

휴대용 지뢰 탐지기의 특성상 병사가 직접 손에 들고 운용하기 때문에 빠르고 정확하게 표적 탐지를 수행하는 시스템을 개발해야한다. 그러나 우리나라의 군에서 사용하고 있는 휴대용 지뢰 탐지기는 금속 성분의 지뢰만 탐지가 가능하다는 문제점이 있다. 이러한 문제를 해결하고, 우리나라 환경에 알맞은 휴대용 지뢰 탐지 시스템을 개발하는 것이 중요하다. 본 논문에서는 지면 투과 레이더를 이용하여 지뢰를 탐지 하고, 우리나라 환경에 알맞은 휴대용 지뢰 탐지 시스템을 제안한다. 제안하는 시스템은 전처리 단계로 깊이 보상, 정합 필터링, 주파수 이동 필터링을 이용하고, 탐지 단계에서 에지 비율을 통해 최종적으로 표적을 탐지한다. 제안하는 시스템의 성능을 검증하기 위하여 우리나라 토양의 대부분을 차지하는 사양토를 이용하였고, 탐지해야하는 지뢰를 매설한 후 휴대용 지뢰 탐지기를 이용하여 데이터를 획득하였다. 획득한 데이터를 기반으로 패치의 크기 및 위치와 이동 주파수에 대한 실험을 진행하여 최적의 성능을 나타내는 값을 찾아내고, 해당 값을 이용하여 탐지 성능을 확인하였다. 실험 결과, 제안하는 전처리 알고리즘이 낮은 오경보율에서 모든 지뢰를 탐지하는 우수한 성능을 나타내는 것을 확인하였고, 기존 연구와의 비교를 통해 제안하는 시스템의 성능이 우수함을 확인하였다.

• Journal of Biosystems Engineering
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• 제12권3호
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• pp.1-6
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• 1987

The objective of this study is to develop a soil hardness tester which can estimate tillage resistance with tae travelling cone-penetrometer. For the study, a series of tests was performed using the cone penetrating in the horizontal direction. Based on the tests above, soil hardness was represented by travelling cone-index vs depth of cone penetration, travelling speed and moisture contents of the soil Resistance characteristics obtained from the experiments were compared with those by a vertical cone-penetrometer and the Yamanaka's soil hardness tester. Following conclusions were made from the study. 1. 8 to 9 peaks per one meter were detected in the resistance curve of cone penetration regardless of the travelling speed of cone-penetrometer when it penetrated the soil in the horizontal direction. This phenomenon seemed to be a similar one noticed in shearing pitch of plowing. 2. Cone index increased as travelling speed increased from 0.08m/sec to 0.5m/sec. 3. Linear relationship was found between the cone indices measured by the travelling coe-penetrometer and Yamanaka's hardness tester. 4. Increasing rate of the cone indices measured by vertical cone-penetrometer decreased as the depth of soil increased while the cone indices by the travelling cone-pentrometer increased linearly.