傾斜計を用いた地下水流動評価法の開発とモデル解析 Development of a Method for Estimating Groundwater Flow by Titltmeters and Model Analysis

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Revising the method proposed by Vasco et al., we developed a new method for more accurately estimating groundwater flow by an inverse analysis of tilt data on the surface. The features of this method are that 1) a region (V) where groundwater flow occurs is divided into elements in which the volume change in groundwater per unit volume of rock (Δ<I>ν</I>) and the Skempton coefficient <I>B</I> are assumed to vary in a linear or quadratic manner with the coordinates, that 2) the values of Δ<I>ν</I> are set to zero at the boundaries of the region V and that 3) as constraining conditions which are weighed and added to a squared error in tilt, the sum of squared second derivatives of Δ<I>ν</I> are used. We call the method using linear interpolation Inversion-1 and that using quadratic interpolation Inversion-2.<BR>First, analyses by these methods were conducted for two flow models of water injection to know the applicability of the methods. It was shown that both Inversion-1 and Inversion-2 can evaluate the volume change in groundwater much more accurately than the method by Vasco et al. when Δ<I>ν</I> varies relatively gently with the distance from the injection point (Model 1). However, when Δ<I>ν</I> varies steeply with the distance from the injection point (Model 2), either Inversion-1 or Inversion-2 cannot produce good results. This was considered to be caused by the fact that the measured data are much fewer than Δ<I>ν</I> to be determined. Furthermore, the effect of the size of the region V on the estimation of Δ<I>ν</I> was analyzed since it is usually difficult to accurately estimate the size of a region where water flow occurs. The results showed that the effect of the size of the region V is relatively small for both Inversion-1 and Inversion-2 unless the size is much smaller than the real one and that Inversion-2 produces a smaller error than Inversion-1. Thus, it can be said that it is better to perform an analysis by Inversion-2 with a large size of the region V in the beginning.

収録刊行物

  • Journal of MMIJ : journal of the Mining and Materials Processing Institute of Japan

    Journal of MMIJ : journal of the Mining and Materials Processing Institute of Japan 123(1), 17-25, 2007-01-25

    The Mining and Materials Processing Institute of Japan

参考文献:  10件中 1-10件 を表示

  • <no title>

    OHMURA K.

    Geothermal Energy 28, 65-76, 2003

    被引用文献1件

  • <no title>

    NAKAGOME O.

    Proceedings of World Geothermal Congress 2000, 2000

    被引用文献1件

  • <no title>

    ZIENKIEWICZ O. C.

    The Finite Element Method, 1977

    被引用文献1件

  • <no title>

    MATSUOKA T.

    Journal of Society of Materials Science, Japan 51, 152-156, 2002

    被引用文献1件

  • <no title>

    GUEGUEN Y.

    Mechanics of Fluid-Saturated Rocks, 2004

    被引用文献1件

  • <no title>

    COUSSY O.

    Poromechanics, 2004

    被引用文献1件

  • <no title>

    KONDO J.

    Differential Equation and Fourier Analysis, 1969

    被引用文献1件

  • <no title>

    VASCO D. W.

    J. Geotech. Geoenviron. Eng. 124, 29-37, 1998

    被引用文献7件

  • <no title>

    VASCO D. W.

    J. Geophys. Res. 93, 3232-3242, 1988

    DOI 被引用文献5件

  • <no title>

    SEGALL P.

    J. Geophys. Res. 90, 6801-6816, 1985

    被引用文献5件

被引用文献:  1件中 1-1件 を表示

各種コード

  • NII論文ID(NAID)
    10018749135
  • NII書誌ID(NCID)
    AA12188381
  • 本文言語コード
    JPN
  • 資料種別
    ART
  • ISSN
    18816118
  • NDL 記事登録ID
    8729076
  • NDL 雑誌分類
    ZP41(科学技術--金属工学・鉱山工学)
  • NDL 請求記号
    Z17-315
  • データ提供元
    CJP書誌  CJP引用  NDL  J-STAGE 
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