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Analysis of phreatic evaporation law and influence factors of typical lithology in Hebei Plain

Peng CHEN1,2, Kang CHEN1, Ye-xin GAO2( )
Hebei University of geology, Shijiazhuang, 050000, China
Institute of hydrogeology and environmental geology, CAGS, Shijiazhuang, 050000, China
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Abstract

Based on three typical mediums (sandy loam, loam and sandy clay loam) in Hebei Plain, this paper designs phreatic evaporation experiments under different lithology and phreatic depth. Based on the analysis of experimental data, the phreatic evaporation law and influencing factors of three mediums were studied. The results showed that: (1) The shallower the phreatic depth, the larger the phreatic evaporation. (2) Sandy clay loam has the biggest response to the increase of the phreatic depth, sandy loam is the second and loam is the smallest. (3) The limit depth of phreatic evaporation of sandy clay loam is about 3 m and that of loam and sandy loam is about 2 m and 3 m, seperately. (4) By fitting the daily evaporation of phreatic water and phreatic depth, the results showed that sandy loam and sandy clay loam are exponential functions and loam is power functions.

Keywords

Influencing factorsHebei PlainTypical lithologyPhreatic water evaporationEmpirical formula

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Journal of Groundwater Science and Engineering
Volume 6 Issue 4,
December 2018
Pages 270-279
DOI: 10.19637/j.cnki.2305-7068.2018.04.003
Cite this article:
CHEN P, CHEN K, GAO Y-x. Analysis of phreatic evaporation law and influence factors of typical lithology in Hebei Plain. Journal of Groundwater Science and Engineering, 2018, 6(4): 270-279. https://doi.org/10.19637/j.cnki.2305-7068.2018.04.003

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Received: 01 September 2018
Accepted: 11 October 2018
Published: 28 December 2018
© 2018 Journal of Groundwater Science and Engineering Editorial Office
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