• Title/Summary/Keyword: Ground Penetration Radar Exploration

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Delineation of internal heterogeneities of Geum River point bar deposits in Buyeo area using GPR Data (지하 투과 레이다 조사를 통한 부여 지역 금강변의 충적 대수층 내부 불균질성 파악)

  • Rhee, Chul-Woo;Kim, Hyoung-Soo;Lee, Kyung-Joo
    • Journal of the Korean Geophysical Society
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    • v.5 no.4
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    • pp.337-344
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    • 2002
  • The alluvial deposits along meandering rivers can be used as an artificial aquifer for infiltration of river waters. Internal heterogeneity of the alluvial deposits is a prerequisite information for the development of alluvial groundwater because vortical and lateral movement of alluvial ground water depends on the internal heterogeneity The internal heterogeneity due to variations in channel behavior can be delineated using GPR survey, GPR profiles for the point bar deposits near Buyeo county reveals two different stratigraphic units: the lower inclined heterogeneous strata and the upper horizontally stratified strata. The upper unit is largely indicative of vertical accumulation by overbank floods within a floodplain, whereas the lower one represents typical point bar deposits formed by lateral accretion. The stratigraphic variation in the heterogeneity shows that GPR survey is a useful and necessary investigation method for the development of alluvial ground water.

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A geophysical survey result over a hydrocarbon contaminated site (물리탐사를 이용한 국내 유류오염지역 조사 사례)

  • Song Yoonho;Park Sam Gyu;Seol Soon Jn;Choi Seong-Jun;Chung Seung-Hwan
    • 한국지구물리탐사학회:학술대회논문집
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    • 2001.09a
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    • pp.122-140
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    • 2001
  • We have applied the geophysical survey, mainly electric and electromagnetic (EM) methods, to a test site contaminated by hydrocarbon waste disposal and local spill. The multi-frequency, moving source & receiver EM survey along with ground penetrating radar (GPR) showed a fairly good performance in detection of buried metal pipes and objects. Magnetic survey measuring vertical and horizontal gradients were so sensitive to the small metallic objects spread over the surface that it's hard to discriminate the buried pipe. We chose electrical resistivity, EM and GPR survey to examine the soil contamination. Depth slices of resistivity distribution as the results of the inversion of resistivity and EM data coincided each other and closely matched the contaminated area determined by chemical analysis of the soil samples. GPR images did not show the reflection events related with contamination plume since there are no distinct spill in this site. We inferred the contamination using the penetration depth of the GPR energy, which could be used as auxiliary information to the resistivity and EM results. We summarized the applicability of each survey methods based on this results and proposed a desirable survey scheme for the determination of hydrocarbon contaminated site.

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