FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W3150250042> ?p ?o ?g. }

• W3150250042 endingPage "432" @default.
• W3150250042 startingPage "419" @default.
• W3150250042 abstract "A permanent collapsing gully, locally called Benggang, formed on slopes with deep granite red soil and is a type of unique gully erosion widely prevalent in southern China. Three different soil configurations (SC), ie, red-transition-sandy (SC Ⅰ, the transition is the soil layer between the red soil and the sandy soil layer), transition-sandy (SC Ⅱ) or sandy (SC Ⅲ) are usually present in the soil profile of the Benggang slope. However, little attention has been paid to impacts of SCs on the triggering of Benggang erosion. In this study, we aimed to explore the relationships between soil water content (SWC) and triggering of Benggang erosion under different SC conditions. The soil properties of different soil layers were measured and the SWC at depths of 20, 40, 60, and 80 cm were monitored at 5-min intervals along a typical Benggang (SC Ⅰ) during 2016–2018. The SWC of Benggang slopes with different SCs were simulated by VADOSE/W model. Results showed that the red soil layer had a higher water retention capacity and shear strength than the sandy soil layer. Even if the SWC is higher (e.g., 0.42 cm 3 /cm 3 ) at red soil layer or transition layer, the corresponding shear strength is greater than that of sandy soil layer with a lower SWC (e.g., 0.32 cm 3 /cm 3 ). Relationships between shear strength and SWC of different soil layers indicate that Benggang erosion is triggered by an increase in the SWC in the deep sandy layer. Results also showed that differences exist in the SWC distribution among the different SCs. The SWC is higher in topsoil than in deeper soil in SC Ⅰ and SC Ⅱ, while in SC Ⅲ, the opposite trend is observed. These results revealed that the presence of the red soil or transition layer can reduce the infiltration of rainwater into the deep sandy layer, thus can reduce the possibility of collapse. Our results show that the SC affects the stability of the headwall, and results provide great significances to guide the mitigation of Benggang erosion." @default.
• W3150250042 created "2021-04-13" @default.
• W3150250042 creator A5017964554 @default.
• W3150250042 creator A5018087945 @default.
• W3150250042 creator A5029878173 @default.
• W3150250042 creator A5045139626 @default.
• W3150250042 creator A5076909690 @default.
• W3150250042 creator A5079530450 @default.
• W3150250042 date "2021-09-01" @default.
• W3150250042 modified "2023-10-08" @default.
• W3150250042 title "The soil configuration on granite residuals affects Benggang erosion by altering the soil water regime on the slope" @default.
• W3150250042 cites W1645947060 @default.
• W3150250042 cites W1655569767 @default.
• W3150250042 cites W1742448746 @default.
• W3150250042 cites W1840365138 @default.
• W3150250042 cites W1963900566 @default.
• W3150250042 cites W1964977988 @default.
• W3150250042 cites W1974593219 @default.
• W3150250042 cites W1982068729 @default.
• W3150250042 cites W1982235412 @default.
• W3150250042 cites W1983104972 @default.
• W3150250042 cites W1985707702 @default.
• W3150250042 cites W1988039264 @default.
• W3150250042 cites W1991842752 @default.
• W3150250042 cites W1993310267 @default.
• W3150250042 cites W2006005027 @default.
• W3150250042 cites W2009054435 @default.
• W3150250042 cites W2010185694 @default.
• W3150250042 cites W2013341751 @default.
• W3150250042 cites W2013352515 @default.
• W3150250042 cites W2015726067 @default.
• W3150250042 cites W2016702755 @default.
• W3150250042 cites W2019341254 @default.
• W3150250042 cites W2027686574 @default.
• W3150250042 cites W2029608510 @default.
• W3150250042 cites W2036589170 @default.
• W3150250042 cites W2040047744 @default.
• W3150250042 cites W2040792651 @default.
• W3150250042 cites W2045659879 @default.
• W3150250042 cites W2059738852 @default.
• W3150250042 cites W2062716071 @default.
• W3150250042 cites W2063940073 @default.
• W3150250042 cites W2064596878 @default.
• W3150250042 cites W2065343409 @default.
• W3150250042 cites W2068810943 @default.
• W3150250042 cites W2069726299 @default.
• W3150250042 cites W2070547953 @default.
• W3150250042 cites W2071209355 @default.
• W3150250042 cites W2071246728 @default.
• W3150250042 cites W2076263928 @default.
• W3150250042 cites W2090000070 @default.
• W3150250042 cites W2090270418 @default.
• W3150250042 cites W2092211157 @default.
• W3150250042 cites W2106823745 @default.
• W3150250042 cites W2146112928 @default.
• W3150250042 cites W2147367215 @default.
• W3150250042 cites W2149265959 @default.
• W3150250042 cites W2170450462 @default.
• W3150250042 cites W2170482933 @default.
• W3150250042 cites W2236594864 @default.
• W3150250042 cites W2314774750 @default.
• W3150250042 cites W2320106964 @default.
• W3150250042 cites W2326920397 @default.
• W3150250042 cites W2463432670 @default.
• W3150250042 cites W2560130654 @default.
• W3150250042 cites W2601183962 @default.
• W3150250042 cites W2609325811 @default.
• W3150250042 cites W2746634979 @default.
• W3150250042 cites W2754643323 @default.
• W3150250042 cites W2774783505 @default.
• W3150250042 cites W2777247168 @default.
• W3150250042 cites W2780412280 @default.
• W3150250042 cites W2780794412 @default.
• W3150250042 cites W2791843258 @default.
• W3150250042 cites W2802433047 @default.
• W3150250042 cites W2805825477 @default.
• W3150250042 cites W2886539148 @default.
• W3150250042 cites W2902893073 @default.
• W3150250042 cites W2947478025 @default.
• W3150250042 cites W2965099054 @default.
• W3150250042 cites W2974224379 @default.
• W3150250042 cites W625873563 @default.
• W3150250042 doi "https://doi.org/10.1016/j.iswcr.2021.03.003" @default.
• W3150250042 hasPublicationYear "2021" @default.
• W3150250042 type Work @default.
• W3150250042 sameAs 3150250042 @default.
• W3150250042 citedByCount "12" @default.
• W3150250042 countsByYear W31502500422021 @default.
• W3150250042 countsByYear W31502500422022 @default.
• W3150250042 countsByYear W31502500422023 @default.
• W3150250042 crossrefType "journal-article" @default.
• W3150250042 hasAuthorship W3150250042A5017964554 @default.
• W3150250042 hasAuthorship W3150250042A5018087945 @default.
• W3150250042 hasAuthorship W3150250042A5029878173 @default.
• W3150250042 hasAuthorship W3150250042A5045139626 @default.
• W3150250042 hasAuthorship W3150250042A5076909690 @default.
• W3150250042 hasAuthorship W3150250042A5079530450 @default.
• W3150250042 hasBestOaLocation W31502500421 @default.

• next