干旱区科学2024,Vol.16Issue(7) :895-909.DOI:10.1007/s40333-024-0079-y

Effects of gravel on the water absorption characteristics and hydraulic parameters of stony soil

MA Yan WANG Youqi MA Chengfeng YUAN Cheng BAI Yiru
干旱区科学2024,Vol.16Issue(7) :895-909.DOI:10.1007/s40333-024-0079-y

Effects of gravel on the water absorption characteristics and hydraulic parameters of stony soil

MA Yan 1WANG Youqi 2MA Chengfeng 2YUAN Cheng 2BAI Yiru1
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作者信息

  • 1. Breeding Base for State Key Laboratory of Land Degradation and Ecological Restoration in Northwest China,Ningxia University,Yinchuan 750021,China;School of Geography and Planning,Ningxia University,Yinchuan 750021,China
  • 2. Breeding Base for State Key Laboratory of Land Degradation and Ecological Restoration in Northwest China,Ningxia University,Yinchuan 750021,China;School of Ecology and Environment,Ningxia University,Yinchuan 750021,China
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Abstract

The eastern foothills of the Helan Mountains in China are a typical mountainous region of soil and gravel,where gravel could affect the water movement process in the soil.This study focused on the effects of different gravel contents on the water absorption characteristics and hydraulic parameters of stony soil.The stony soil samples were collected from the eastern foothills of the Helan Mountains in April 2023 and used as the experimental materials to conduct a one-dimensional horizontal soil column absorption experiment.Six experimental groups with gravel contents of 0%,10%,20%,30%,40%,and 50%were established to determine the saturated hydraulic conductivity(Ks),saturated water content(θs),initial water content(θi),and retention water content(θr),and explore the changes in the wetting front depth and cumulative absorption volume during the absorption experiment.The Philip model was used to fit the soil absorption process and determine the soil water absorption rate.Then the length of the characteristic wetting front depth,shape coefficient,empirical parameter,inverse intake suction and soil water suction were derived from the van Genuchten model.Finally,the hydraulic parameters mentioned above were used to fit the soil water characteristic curves,unsaturated hydraulic conductivity(Kθ)and specific water capacity(C(h)).The results showed that the wetting front depth and cumulative absorption volume of each treatment gradually decreased with increasing gravel content.Compared with control check treatment with gravel content of 0%,soil water absorption rates in the treatments with gravel contents of 10%,20%,30%,40%,and 50%decreased by 11.47%,17.97%,25.24%,29.83%,and 42.45%,respectively.As the gravel content increased,inverse intake suction gradually increased,and shape coefficient,Ks,θs,and θr gradually decreased.For the same soil water content,soil water suction and Kθ gradually decreased with increasing gravel content.At the same soil water suction,C(h)decreased with increasing gravel content,and the water use efficiency worsened.Overall,the water holding capacity,hydraulic conductivity,and water use efficiency of stony soil in the eastern foothills of the Helan Mountains decreased with increasing gravel content.This study could provide data support for improving soil water use efficiency in the eastern foothills of the Helan Mountains and other similar rocky mountainous areas.

Key words

stony soil/gravel content/water absorption characteristics/hydraulic parameters/one-dimensional horizontal soil column absorption experiment/van Genuchten model/eastern foothills of Helan Mountains

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基金项目

National Natural Science Foundation of China(32360321)

Natural Science Foundation of Ningxia Hui Autonomous Region,China(2023AAC03046)

Natural Science Foundation of Ningxia Hui Autonomous Region,China(2023AAC02018)

Ningxia Key Research and Development Project(2021BEG02011)

出版年

2024
干旱区科学
中国科学院新疆生态与地理研究所,科学出版社

干旱区科学

CSTPCD
影响因子:1.743
ISSN:1674-6767
参考文献量2
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