Grain-Size Fractal Characteristics of Fluvial Sediment in Xianyang Section of Weihe River
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Grain-Size Fractal Characteristics of Fluvial Sediment in Xianyang Section of Weihe River
Bulletin of Soiland Water ConservationVol. 30, Issue 2, Pages: 22-26(2011)
作者机构:
1. 陕西师范大学旅游与环境学院
2. 成都理工大学地球科学学院
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Published:2011
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SHI Xing-min, HAN Yan. Grain-Size Fractal Characteristics of Fluvial Sediment in Xianyang Section of Weihe River[J]. Bulletin of Soiland Water Conservation, 2011, 30(2): 22-26.
DOI:
SHI Xing-min, HAN Yan. Grain-Size Fractal Characteristics of Fluvial Sediment in Xianyang Section of Weihe River[J]. Bulletin of Soiland Water Conservation, 2011, 30(2): 22-26.DOI:
Grain-Size Fractal Characteristics of Fluvial Sediment in Xianyang Section of Weihe River
Fractal theory was applied to analyze grain size distribution of the sediment of Weihe River in Xianyang City.The fractal scaleless range and the fractal dimension of grain size distribution were determined.In the non-scaled range
the correlation coefficients(R2) of 53 samples were all higher than 0.95 and the average fractal dimension was 2.12
which shows that the distribution of sediment particle size exhibited good fractal characteristics.The fractal dimension as a new parameter of sediment grain size analysis was compared with traditional granularity index such as mean-diameter(Φ)
standard deviation(σ)
skewness and kurtosis.The correlation coefficients of fractal dimension of sediment grain size with mean diameter
standard deviation
kurtosis and skewness are 0.807
0.707
0.675
and 0.112
respectively
implying fractal dimension correlated significantly positively with mean diameter