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Temporal and spatial evolution of soil water potential of high-filled slope in Loess Plateau, China
ID：1521 View Protection：ATTENDEE Updated Time：2021-12-14 17:42:48 Hits：216 Poster Presentation

Start Time：Pending（Asia/Shanghai）

Duration：Pending

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Abstract
The Loess Plateau arid region has a complex disaster development pattern and variable soil and water hydrological characteristics, and many high-filled slopes have been formed in this environmentally fragile area due to trenching and land reclamation projects. Soil moisture controls the surface evapotranspiration, water transport and stability of loess slopes, and there are few studies on soil moisture in loess areas. Therefore, in this study, long-term in-situ monitoring was conducted on the high-filled slopes in loess areas during the concentrated rainfall period of the year (July to October).
Keywords
Loess plateau;high-filled slope;soil water potential;zero flux plane
Speaker
Han Bao
Chang'an University

Guanmiao Guo
Chang'an University

Submission Author
Han BAO Chang'an University
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Important Date

  • Conference Date

    Dec 17

    2021

    to

    Dec 20

    2021

  • Dec 16 2021

    Contribution Submission Deadline

  • Dec 24 2021

    Registration deadline

Sponsored By
Chinese Overseas Transportation Association
Chang'an University
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