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ESTIMATION OF SOIL EROSION IN A RESERVOIR WATERSHED USING ^137CS FALLOUT RADIONUCLIDE

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Y. J. CHIU[1] A. M. BORGHUIS[2] H. Y. LEE[3] K. T. CHANG[4] J. H. CHAO[5]

[1]Dept. of Civil Engineering, National Taiwan Univ., Taipei, Taiwan, China [2]Utrecht Univ., Department of Physical Geography, Heidelberglaan 2, 3584 CS Utrecht, The Netherlands [3]Dept. of Civil Engineering, and Hydraulic Research Laboratory, National Taiwan Univ., Taipei, Taiwan, China [4]Dept. of Geography, National Taiwan Univ., Taipei, Taiwan, China [5]Research scientist,Nuclear Science and Technology Development Center, National Tsing Hua Univ., Hsinchu, Taiwan, China

国际泥沙研究:英文版
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国际标准刊号:ISSN 1001-6279
1 INTRoDUCTIoN As the main source of reservoir sedimentation,soil erosion is a critical watershed management issue.M ost rivers in Taiwan are short and steep.Intense rainfal1 events often generate substantial sed iment erosion within the watershed,which ultimately reduces the reservoir capacity and shortens the reservoir’s lifespan.M any methods have been developed to estimate soil erosion rate.
International Journal of Sediment Research

栏目信息:

Technical Papers

分 类 号:

X53

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ESTIMATION OF SOIL EROSION IN A RESERVOIR WATERSHED USING ^137CS FALLOUT RADIONUCLIDE

Abstract:

Sedimentation from soil erosion is a critical reservoir watershed management issue. Due to the difficulty of field investigations, empirical formulas are commonly used to estimate the soil erosion rate. However, these estimations are often far from accurate. An effective alternative to estimating soil erosion is to analyze the spatial variation of ^137Cs inventory in the soil. ^137Cs can be adsorbed by the soil and is widely, assumed to change its distribution only when disturbed by rainfall and human activities. Thus, ^137Cs distributed in soils can be a useful environmental tracer to estimate soil erosion. In this study, the net soil loss estimate is 108,346 t/yr and the gross erosion and net erosion rates are 10.1 and 9 t/ha yr respectively. The sediment delivery ratio is therefore estimated to be 0.9 baled on the two erosion rates. Because of the steep hillsides in the watershed, only 10% of the sediment yield stayed in the deposition sites and 90% was transported to the river as the sediment output. Soil erosion estimates from spatial variations of the ^137Cs activity in the Baishi fiver watershed showed satisfactory accuracy when compared to sediment yield data. Using soil ^137Cs concentrations is therefore a feasible method for estimating soil loss or deposition in Taiwan. Data sampling, analysis and result of this approach are given in this paper.[著者文摘]

Key words:

Soil erosion, Radionuclide ^137Cs, Baishi watershed, Spatial distribution, Sediment yield

收稿日期: 2007-02
修订日期: 2007-10

基金资助:

This study was financially supported by the Northem Bureau of the Water Resources Agency, Ministry of Economic Affair, Taiwan, China. The authors would like to thank the staff of the bureau for their assistance.

作者简介:

corresponding author, E-mail: yujiachiu@ntu.edu.tw

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