Prediction of Regolith Depth Using Topographic and Environmental Variables in the Central Mountain Division, Taiwan

Article Preview

Abstract:

Due to several reasons, there is a shortage of water resources in Taiwan, despite abundant rainfall. These reasons include high population density, uneven spatial and temporal distribution of rainfall, and rivers with steep gradients. According to the data collected by Central Geological Survey in the project: Pumping of Groundwater Resources in the Central Division of Mountain Areas of Taiwan, the abundant underground water in mountain areas exists in areas with thick regolith, broken rock or sandstone. Therefore, the investigation of regolith depth distribution would help us to further understand the amount of underground water, and the areas that can be exploited. This study is based on 441 drilling data over the Da-Chia and Choshui river basins, and aims to construct a relation model of topographic and environmental variables and to estimate the regolith depth in the study area. The amount of drilling data will be increased each year so that the model can be improved, developed and converged. Moreover, it can help in developing a model that is most suitable for estimating regolith depth in Taiwan.

You might also be interested in these eBooks

Info:

Periodical:

Pages:

1489-1493

Citation:

Online since:

January 2013

Export:

Price:

Permissions CCC:

Permissions PLS:

Сopyright:

© 2013 Trans Tech Publications Ltd. All Rights Reserved

Share:

Citation:

[1] R. A. Eggleton: The Regolith Glossary : Surficial Geology, Soils, and Landscapes ( CRC for Landscape Evolution & Mineral Exploration, 2001).

Google Scholar

[2] S. H. Chiang, M. L. Hsu: Journal of Geographical Science Vol. 44 (2006), p.23.

Google Scholar

[3] International Society for Rock Mechanics: International Journal of Rock Mechanics and Mining Sciences Vol. 18 (1981), p.85.

Google Scholar

[4] I.C. Roach: Explanatory Notes for the Canbelego 1: 100, 000 Regolith-Landforms Map New South Wales ( CRC for Landscape Evolution & Mineral Exploration, 2008).

Google Scholar

[5] R. R. Lin: Ti-Chih Vol. 30 (2011), p.78.

Google Scholar

[6] B. Minasny, and A. B. McBratney: Geoderma, Vol. 90 (1999), p.3.

Google Scholar

[7] T. K. Tesfa, D. G. Tarboton, D. G. Chandler, and J. P. McNamara: Water Resources Research Vol. 45 (2009), p.1.

Google Scholar

[8] M. Heimsath, W. E. Dietrich, K. Nishiizumi, and R. C. Finkel: Geomorphology Vol. 27 (1999), p.151.

Google Scholar

[9] Ozdemir: Journal of Hydrology Vol. 405 (2011), p.123.

Google Scholar

[10] M. A. Carson, and M. J. Kirkby: Hillslope Form and Process (London Cambridge University Press, 1972).

Google Scholar

[11] E. Small, R. S. Anderson, and G. S. Hancock: Geomorphology Vol. 27 (1999), p.131.

Google Scholar

[12] M. Heimsath, J. Chappell, W. E. Dirtrich, K. Nishiizumi, and R. C. Finkel: Quaternary International Vol. 83-85 (2001), p.169.

DOI: 10.1016/s1040-6182(01)00038-6

Google Scholar

[13] H. Chung: Terrain Stability Analysis Using Hydrologic Model for Predicting Shallow Landslides-A Study on Piya Creek Watershed (National Central University, Taiwan 2008).

Google Scholar

[14] T. K. Tesfa, D. G. Tarboton, D. G. Chandler, and J. P. McNamara: Water Resources Research Vol. 45 (2009), p.1.

Google Scholar

[15] K. J. Beven, and M. J. Kirkby: Hydrological Science Bulletin Vol. 24 (1979), p.43.

Google Scholar

[16] Central Geological Survey: Investigation and Assessment of Groundwater Resources in Central Division of Mountain Area, Taiwan (2/4) (Central Geological Survey, Taiwan 2011).

Google Scholar