Water Migration Law of Loess Deep Filled Ground

YU Yong-tang, SUN Mo, CAO Jing-yuan, ZHU Jian-min, ZHANG Long

Journal of Changjiang River Scientific Research Institute ›› 2024, Vol. 41 ›› Issue (7) : 103-109.

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Journal of Changjiang River Scientific Research Institute ›› 2024, Vol. 41 ›› Issue (7) : 103-109. DOI: 10.11988/ckyyb.20230315
Rock-Soil Engineering

Water Migration Law of Loess Deep Filled Ground

  • YU Yong-tang1,2, SUN Mo3, CAO Jing-yuan2, ZHU Jian-min2, ZHANG Long4
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Abstract

To unveil the rainfall infiltration patterns at a loess deep filled site, a monitoring station was established in Yan’an to continuously monitor the soil moisture content within a 28 m depth over 31 months under natural rainfall conditions. The water migration within compacted loess was scrutinized based on rainfall, evaporation, and temperature data. Results indicate that atmospheric influence extends to a depth of 3.5 m. With the change of rainfall and evaporation, soil water content exhibits obvious peaks and troughs and annual trend. At 1.0 m depth, atmospheric influence is more pronounced. Soil moisture content shows slight fluctuations below 29 mm/d daily rainfall, followed by sharp increases beyond this threshold. Greater rainfall intensity and duration lead to deeper water migration and infiltration, with a maximum depth observed between 6.0-7.0 m during the monitoring period.

Key words

loess / deep filled ground / moisture content / rainfall / water migration

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YU Yong-tang, SUN Mo, CAO Jing-yuan, ZHU Jian-min, ZHANG Long. Water Migration Law of Loess Deep Filled Ground[J]. Journal of Changjiang River Scientific Research Institute. 2024, 41(7): 103-109 https://doi.org/10.11988/ckyyb.20230315

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