groundwater recharge" /> Sang-Ki Moon" /> Sang-Ki Moon and Nam-chil Woo

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. Econ. Environ. Geol. 2002;35:479-90. https://doi.org/">

Econ. Environ. Geol. 2002; 35(5): 479-490

Published online October 31, 2002

© THE KOREAN SOCIETY OF ECONOMIC AND ENVIRONMENTAL GEOLOGY

Contribution of Hydrogeological Factors to Groundwater Recharge Ratio

Sang-Ki Moon and Nam-chil Woo

Dept. of Earth System Sciences, Yonsei Univ., Seoul, 120-749, Korea

Correspondence to :

Sang-Ki Moon

skmun@ysgeo.yonsei.ac.kr

Received: September 26, 2002; Accepted: October 24, 2002

Abstract

The aim of this study is to evaluate the contributions of each hydrogeological factors to groundwater recharge ratios in order to determine areal estimates of recharges in entire inland area of South Korea. For this purpose, various statistical analyses and overlay techniques of GIS were conducted for entire area and 4 river basins of South Korea. As a result, the spatial distribution of recharge, South Korea were visualized.

Keywords

groundwater recharge, GIS, river basins, hydrogeological factors

Article

Econ. Environ. Geol. 2002; 35(5): 479-490

Published online October 31, 2002

Copyright © THE KOREAN SOCIETY OF ECONOMIC AND ENVIRONMENTAL GEOLOGY.

Contribution of Hydrogeological Factors to Groundwater Recharge Ratio

Sang-Ki Moon and Nam-chil Woo

Dept. of Earth System Sciences, Yonsei Univ., Seoul, 120-749, Korea

Correspondence to:

Sang-Ki Moon

skmun@ysgeo.yonsei.ac.kr

Received: September 26, 2002; Accepted: October 24, 2002

Abstract

The aim of this study is to evaluate the contributions of each hydrogeological factors to groundwater recharge ratios in order to determine areal estimates of recharges in entire inland area of South Korea. For this purpose, various statistical analyses and overlay techniques of GIS were conducted for entire area and 4 river basins of South Korea. As a result, the spatial distribution of recharge, South Korea were visualized.

Keywords

groundwater recharge, GIS, river basins, hydrogeological factors

    KSEEG
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