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

CHEN Peng; CHEN Kang; GAO Ye-xin

doi:10.19637/j.cnki.2305-7068.2018.04.003

Volume 6 Issue 4

Dec. 2018

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CHEN Peng, CHEN Kang, GAO Ye-xin. 2018: Analysis of phreatic evaporation law and influence factors of typical lithology in Hebei Plain. Journal of Groundwater Science and Engineering, 6(4): 270-279. doi: 10.19637/j.cnki.2305-7068.2018.04.003

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

doi: 10.19637/j.cnki.2305-7068.2018.04.003

1Hebei University of geology, Shijiazhuang, 050000, China. 2 Institute of hydrogeology and environmental geology, GAGS, Shijiazhuang, 050000, China.

Publish Date: 2018-12-28

Abstract

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.
- Hebei Plain,
- Typical lithology,
- Phreatic water evaporation,
- Influencing factors,
- Empirical formula

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References(16)

References

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This work is licensed under a Creative Commons Attribution-NonCommercial-NoDerivatives 4.0 International License.

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