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Hysteresis of saturation-capillary pressure relations under consecutive drainage-imbibition cycles in fine sandy medium

Hysteresis of saturation-capillary pressure relations under consecutive drainage-imbibition cycles in fine sandy medium
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摘要 The hysteresis of saturation-capillary pressure (S-p) relations was investigated in a fine sandy medium under consecutive drainage-imbibition cycles, which resulted from scheduled water level fluctuations. A drainage-imbibition cycle starts with a drainage process and ends with an imbibition process in sequence. The saturation and capillary pressure were measured online with time domain reflectometry (TDR) probes and T5 tensiometers, respectively. Results show that the relation between the degree of hysteresis and the number of the drainage-imbibition cycles is not obvious. However, the degree decreases with the increase of the initial water saturation of the imbibition processes in these drainage-imbibition cycles. The air-entry pressure of a sandy medium is also found to be constant, which is independent of the drainage-imbibition cycles and the initial water saturation of the drainage process. In all the imbibition processes, parameter a of the van Genuchten (VG) model decreases with the increase of the initial water saturation, which corresponds positively to the magnitude of the hysteresis. The hysteresis of saturation-capillary pressure(S-p) relations was investigated in a fine sandy medium under consecutive drainage-imbibition cycles,which resulted from scheduled water level fluctuations.A drainage-imbibition cycle starts with a drainage process and ends with an imbibition process in sequence.The saturation and capillary pressure were measured online with time domain reflectometry(TDR) probes and T5 tensiometers,respectively.Results show that the relation between the degree of hysteresis and the number of the drainage-imbibition cycles is not obvious.However,the degree decreases with the increase of the initial water saturation of the imbibition processes in these drainage-imbibition cycles.The air-entry pressure of a sandy medium is also found to be constant,which is independent of the drainage-imbibition cycles and the initial water saturation of the drainage process.In all the imbibition processes,parameter α of the van Genuchten(VG) model decreases with the increase of the initial water saturation,which corresponds positively to the magnitude of the hysteresis.
作者 XIE Xiao-xi LI Yan XIA Bei-cheng XU Li-min SU Yu GU Qing-bao 谢小茜;李雁;夏北成;许丽敏;苏钰;谷庆宝(School of Environmental Science and Engineering,Sun Yat-sen University,Guangzhou 510275,China;School of Marine Sciences,Sun Yat-sen University,Guangzhou 510275,China;Guangdong Huizhou Environmental Protection Agency,Huizhou 516001,China;Guangdong Environmental Protection Engineering Research and Institute,Guangzhou 510635,China;Chinese Research Academy of Environmental Sciences,Beijing 100012,China)
出处 《Journal of Central South University》 SCIE EI CAS 2012年第1期222-230,共9页 中南大学学报(英文版)
基金 Project(41072182) supported by the National Natural Science Foundation of China Project(2010Z1-E101) supported by the Science and Technology Program of Guangzhou City,China Project(200809095) supported by the Special Funds for Environmental Nonprofit Research,China Project(8151027501000008) supported by the Natural Science Foundation of Guangdong Province,China
关键词 S-p relation HYSTERESIS drainage IMBIBITION van Genuchten model 水饱和度 毛细压力 排水 周期 细沙 毛细管压力 迟滞 时域反射计
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