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Geological Journal of China Universities ›› 2023, Vol. 29 ›› Issue (6): 934-944.DOI: 10.16108/j.issn1006-7493.2022048

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Characteristics of Water Saturation During Drainage and Imbibition Processes in Unsaturated Zones

ZHANG Shengshan1,WEI Yunbo2*,GU Xi3   

  1. 1. Huzhou Zhongjiao Investment Development Co., Ltd., Huzhou 31300, China;
    2. School of Earth Sciences and Engineering, Hohai University, Nanjing 210013, China;
    3. School of Earth Sciences and Engineering, Nanjing Univerisity, Nanjing 210023, China
  • Online:2023-12-20 Published:2023-12-18

Abstract: The unsaturated zone, which is the link between the s urface water and groundwater, plays a key role in controlling water exchange and solute transport in the soils. Infiltration in the unsaturated zone is in essence a problem of twophase
(air and water) immiscible displacement. A deep understanding of the airwater displacement process in the unsaturated zone is of great significance for the management and sustainable use of groundwater. A s eries of drainageimbibition
experiments are carried out to study the watercontent distribution in the unsaturated zone. The light transmission method is used to monitor water content in the 2-dimensional sandbox during the drainageimbibition cycles. It is found that the lateral fluctuation of water content in the drainage process (0.145-0.175) is greater than that in the imbibition process (0.150-0.165) due to the existence of unstable drainage processes at the pore-scale. The difference of water content between drainage and imbibition means that the mechanism happened at pore-scales should also be affected by water movement at darcy-scales.

Key words: unsaturated zone, water content distribution, drainage and imbi bition process, light transmission method

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