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Spatio-temporal variability of groundwater level in China's Hebei plain
Liu, Zhi-Guo (1); Wang, En-De (1); Fu, Jian-Fei (1); Shao, An-Lin (1)
2007, 28 (5):
717-720.
DOI: -
Based on the spatially analytic function of GIS, the spatio-temporal variability of groundwater level in China's Hebei plain was studied by using the semivariogram and ordinary Kriging method of geostatistics, from which the spherical model fitted both the data sets in the periods 1986-1990 and 1996-2000. The spatial heterogeneity of groundwater level caused by its authigenic factors was big and, as an anisotropic result of groundwater level, it was found that there was a significant level difference in the period 1986-1990. The spatial distribution mapping of groundwater level by Kriging interpolation with the data of groundwater level in 1986-1990 and 1996-2000 showed that the trend of spatial distribution as a whole is that the groundwater level becomes high gradually from east to west and from the littoral plain to the piedmont plain, and the groundwater in the west middle plain is deeper than in the littoral plain. In conclusion, on the whole, there was a drawdown in the period from 1986 to 2000 because of such influencing factors as population, irrigation area, rainfall and run-off, which affects seriously the sustainable economic development of Hebei Province.
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