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Quanhou Dai

Biographic Data

ID7993978
NAMEQuanhou Dai
GIVEN NAMESQuanhou
FAMILY NAMEDai
SIGNATUREDAI Q
AFFILIATIONSKey Laboratory of Karst Georesources and Environment Ministry of Education, Guizhou University Guiyang PR China
ORCID0000-0002-7273-5140
VERIFIEDYes
TOTAL WORKS5
TOTAL CITATIONS0
AUTHOR COUNT5
EDITOR COUNT0
FIRST PUBLICATION YEAR2020
LATEST PUBLICATION YEAR2026
H-INDEX0
  • Control of Fissure Development on Soil Erosion in Karst Forestland Revealed by Simulated Rainfall Experiments

    Open Access•Guangqin Wu, Pengwei Ding et al.•ARTICLE•Land Degradation and Development•2026

    Monitoring soil erosion in karst regions poses significant challenges because of the complex geological structures, particularly in forestland characterised by frequent root activity where rainfall‐runoff processes remain poorly understood. In this study, the mechanisms underlying the control of underground fissure development on runoff generation and sediment transport in karst forests were investigated. Indoor simulated rainfall experiments wer…

  • Effects of rainfall intensity and underground pore density on the soil erosion mechanism of sloping maize farmland in a typical karst area of SW China

    Open Access•Yong Wang, Quanhou Dai et al.•ARTICLE•Land Degradation and Development•2023

    The rainfall intensity, slope, and underground pore density are major factors affecting the soil erosion of maize‐covered karst slopes. We studied the erosion process of maize‐covered karst slopes and the influencing mechanism of soil erosion on these slopes under different rainfall intensities, slopes, and underground pore density via simulated rainfall tests. The results are as follows: (1) No runoff was observed on the slope surface under ligh…

  • Effects of vegetation restoration types on soil erosion reduction of a shallow karst fissure soil system in the degraded karst areas of Southwestern China

    Open Access•Youjin Yan, Quanhou Dai et al.•ARTICLE•Land Degradation and Development•2023

    Shallow karst fissures are the main hydrological paths, underground loss channels, and one of the most critical root habitats in fragile karst rocky desertification areas. Revegetation may alter the type of vegetation cover in fissures, resulting in changes to soil properties and erosion reduction. In this study, we evaluate the influence of revegetation on the soil erosion reduction of fissure‐soil–plant systems (FSPS) for three vegetation types…

  • Effects of preferential flow on soil nutrient transport in karst slopes after recultivation

    Open Access•Youjin Yan, Yuqiong Yang et al.•ARTICLE•Environmental Research Letters•2023

    In response to the global food shortage, a large amount of abandoned land in karst areas has been reclaimed as cultivated land, causing severe nonpoint source pollution. Preferential flow-driven soil nutrient transport on karst slopes remains poorly studied, though it is a major factor in nonpoint source pollution, as it responds to changes caused by reclamation. We explored the characteristics of soil preferential flow differences in recultivate…

  • The mechanisms of nutrient output through water flow from sloping farmland with slight rocky desertification in a karst region

    Open Access•Ruxue Gao, Quanhou Dai et al.•ARTICLE•Environmental Research Letters•2020

    Nutrient loss from sloping farmland with rocky desertification in karst regions leads to low farmland productivity and non-point source pollution. The mechanisms of nutrient outputs through water flow in such contexts under different rainfall intensities and slope angles were studied by using artificial rainfall simulation. Research showed that surface water flow occurred when the rainfall intensity was between 30 mm · h ^−1 and 50 mm · h ^−1 , a…

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  • The mechanisms of nutrient output through water flow from sloping farmland with slight rocky desertification in a karst region

    Open Access•Ruxue Gao, Quanhou Dai et al.•ARTICLE•Environmental Research Letters•2020

    Nutrient loss from sloping farmland with rocky desertification in karst regions leads to low farmland productivity and non-point source pollution. The mechanisms of nutrient outputs through water flow in such contexts under different rainfall intensities and slope angles were studied by using artificial rainfall simulation. Research showed that surface water flow occurred when the rainfall intensity was between 30 mm · h ^−1 and 50 mm · h ^−1 , a…

  • Effects of rainfall intensity and underground pore density on the soil erosion mechanism of sloping maize farmland in a typical karst area of SW China

    Open Access•Yong Wang, Quanhou Dai et al.•ARTICLE•Land Degradation and Development•2023

    The rainfall intensity, slope, and underground pore density are major factors affecting the soil erosion of maize‐covered karst slopes. We studied the erosion process of maize‐covered karst slopes and the influencing mechanism of soil erosion on these slopes under different rainfall intensities, slopes, and underground pore density via simulated rainfall tests. The results are as follows: (1) No runoff was observed on the slope surface under ligh…

  • Effects of vegetation restoration types on soil erosion reduction of a shallow karst fissure soil system in the degraded karst areas of Southwestern China

    Open Access•Youjin Yan, Quanhou Dai et al.•ARTICLE•Land Degradation and Development•2023

    Shallow karst fissures are the main hydrological paths, underground loss channels, and one of the most critical root habitats in fragile karst rocky desertification areas. Revegetation may alter the type of vegetation cover in fissures, resulting in changes to soil properties and erosion reduction. In this study, we evaluate the influence of revegetation on the soil erosion reduction of fissure‐soil–plant systems (FSPS) for three vegetation types…

  • Effects of preferential flow on soil nutrient transport in karst slopes after recultivation

    Open Access•Youjin Yan, Yuqiong Yang et al.•ARTICLE•Environmental Research Letters•2023

    In response to the global food shortage, a large amount of abandoned land in karst areas has been reclaimed as cultivated land, causing severe nonpoint source pollution. Preferential flow-driven soil nutrient transport on karst slopes remains poorly studied, though it is a major factor in nonpoint source pollution, as it responds to changes caused by reclamation. We explored the characteristics of soil preferential flow differences in recultivate…

  • Control of Fissure Development on Soil Erosion in Karst Forestland Revealed by Simulated Rainfall Experiments

    Open Access•Guangqin Wu, Pengwei Ding et al.•ARTICLE•Land Degradation and Development•2026

    Monitoring soil erosion in karst regions poses significant challenges because of the complex geological structures, particularly in forestland characterised by frequent root activity where rainfall‐runoff processes remain poorly understood. In this study, the mechanisms underlying the control of underground fissure development on runoff generation and sediment transport in karst forests were investigated. Indoor simulated rainfall experiments wer…

Soil erosion and sediment transport (5 works) · Environmental Science (4 works) · Erosion (4 works) · Geology (4 works) · Karst (4 works) · Karst Systems and Hydrogeology (4 works) · Soil Science (4 works) · Surface runoff (4 works) · Ecology (3 works) · Geomorphology (3 works)

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