FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W2897187859> ?p ?o ?g. }

• W2897187859 endingPage "11" @default.
• W2897187859 startingPage "1" @default.
• W2897187859 abstract "The SEEP/W module of finite element software GEO-slope is used to analyze the effects of fracture depth, permeability coefficient ratio, fracture angle, and fracture number on the rainwater infiltration process. Moreover, the effect of fracture seepage anisotropy on slope stability is discussed combining with unsaturated seepage theory. The results show that the pore water pressure in the fracture increases rapidly with the rainfall until it changes from negative pressure to positive pressure. The greater the fracture depth is, the greater the pore water pressure in the fracture is, and the greater the infiltration depth at the time of rainfall stopping is. When the permeability coefficient is greater than the rainfall intensity, the permeability coefficient ratio has a great influence on the infiltration process of rainwater. The smaller the fracture angle is, the greater the maximum pore water pressure is in the fracture depth range, and the greater the depth of the positive pore water pressure is. However, with the increase of fracture angle, the infiltration depth decreases, and the range of the surface saturation area of slope increases obviously. With the increase of fracture density, the saturated positive pressure region is connected to each other in the slope. The influence range and the degree of the rainwater on the seepage field are larger and larger. There is a power relation between the saturation area and the fracture number, and also the concentration distribution of long fractures directly forms the large-connected saturated zone and raises groundwater. The range of the saturated zone and variation law of the pore water pressure under fracture seepage are obtained, which provide a reference for the parameter partition assignment of slope stability analysis under fracture seepage." @default.
• W2897187859 created "2018-10-26" @default.
• W2897187859 creator A5028134415 @default.
• W2897187859 creator A5036929951 @default.
• W2897187859 creator A5041949027 @default.
• W2897187859 creator A5077788674 @default.
• W2897187859 creator A5082692640 @default.
• W2897187859 date "2018-10-17" @default.
• W2897187859 modified "2023-10-16" @default.
• W2897187859 title "Effect of Colluvial Soil Slope Fracture’s Anisotropy Characteristics on Rainwater Infiltration Process" @default.
• W2897187859 cites W2000196309 @default.
• W2897187859 cites W2030158375 @default.
• W2897187859 cites W2039019444 @default.
• W2897187859 cites W2087009022 @default.
• W2897187859 cites W2093498878 @default.
• W2897187859 cites W2124955104 @default.
• W2897187859 cites W2152929226 @default.
• W2897187859 cites W2158549841 @default.
• W2897187859 cites W2170008375 @default.
• W2897187859 cites W2256953958 @default.
• W2897187859 cites W2271961188 @default.
• W2897187859 cites W2528622710 @default.
• W2897187859 cites W2613138308 @default.
• W2897187859 cites W2755359840 @default.
• W2897187859 cites W2757496364 @default.
• W2897187859 cites W2765094096 @default.
• W2897187859 cites W2770454802 @default.
• W2897187859 cites W2791714531 @default.
• W2897187859 cites W2806456938 @default.
• W2897187859 cites W2807122461 @default.
• W2897187859 cites W2835277138 @default.
• W2897187859 doi "https://doi.org/10.1155/2018/7351628" @default.
• W2897187859 hasPublicationYear "2018" @default.
• W2897187859 type Work @default.
• W2897187859 sameAs 2897187859 @default.
• W2897187859 citedByCount "11" @default.
• W2897187859 countsByYear W28971878592019 @default.
• W2897187859 countsByYear W28971878592020 @default.
• W2897187859 countsByYear W28971878592021 @default.
• W2897187859 countsByYear W28971878592022 @default.
• W2897187859 countsByYear W28971878592023 @default.
• W2897187859 crossrefType "journal-article" @default.
• W2897187859 hasAuthorship W2897187859A5028134415 @default.
• W2897187859 hasAuthorship W2897187859A5036929951 @default.
• W2897187859 hasAuthorship W2897187859A5041949027 @default.
• W2897187859 hasAuthorship W2897187859A5077788674 @default.
• W2897187859 hasAuthorship W2897187859A5082692640 @default.
• W2897187859 hasBestOaLocation W28971878591 @default.
• W2897187859 hasConcept C102579867 @default.
• W2897187859 hasConcept C114614502 @default.
• W2897187859 hasConcept C120882062 @default.
• W2897187859 hasConcept C121332964 @default.
• W2897187859 hasConcept C127313418 @default.
• W2897187859 hasConcept C153400128 @default.
• W2897187859 hasConcept C159390177 @default.
• W2897187859 hasConcept C159985019 @default.
• W2897187859 hasConcept C185592680 @default.
• W2897187859 hasConcept C187320778 @default.
• W2897187859 hasConcept C18903297 @default.
• W2897187859 hasConcept C192562407 @default.
• W2897187859 hasConcept C33923547 @default.
• W2897187859 hasConcept C41625074 @default.
• W2897187859 hasConcept C43369102 @default.
• W2897187859 hasConcept C55493867 @default.
• W2897187859 hasConcept C62520636 @default.
• W2897187859 hasConcept C76177295 @default.
• W2897187859 hasConcept C83419821 @default.
• W2897187859 hasConcept C85725439 @default.
• W2897187859 hasConcept C86803240 @default.
• W2897187859 hasConcept C9930424 @default.
• W2897187859 hasConceptScore W2897187859C102579867 @default.
• W2897187859 hasConceptScore W2897187859C114614502 @default.
• W2897187859 hasConceptScore W2897187859C120882062 @default.
• W2897187859 hasConceptScore W2897187859C121332964 @default.
• W2897187859 hasConceptScore W2897187859C127313418 @default.
• W2897187859 hasConceptScore W2897187859C153400128 @default.
• W2897187859 hasConceptScore W2897187859C159390177 @default.
• W2897187859 hasConceptScore W2897187859C159985019 @default.
• W2897187859 hasConceptScore W2897187859C185592680 @default.
• W2897187859 hasConceptScore W2897187859C187320778 @default.
• W2897187859 hasConceptScore W2897187859C18903297 @default.
• W2897187859 hasConceptScore W2897187859C192562407 @default.
• W2897187859 hasConceptScore W2897187859C33923547 @default.
• W2897187859 hasConceptScore W2897187859C41625074 @default.
• W2897187859 hasConceptScore W2897187859C43369102 @default.
• W2897187859 hasConceptScore W2897187859C55493867 @default.
• W2897187859 hasConceptScore W2897187859C62520636 @default.
• W2897187859 hasConceptScore W2897187859C76177295 @default.
• W2897187859 hasConceptScore W2897187859C83419821 @default.
• W2897187859 hasConceptScore W2897187859C85725439 @default.
• W2897187859 hasConceptScore W2897187859C86803240 @default.
• W2897187859 hasConceptScore W2897187859C9930424 @default.
• W2897187859 hasFunder F4320335777 @default.
• W2897187859 hasLocation W28971878591 @default.
• W2897187859 hasLocation W28971878592 @default.
• W2897187859 hasOpenAccess W2897187859 @default.
• W2897187859 hasPrimaryLocation W28971878591 @default.
• W2897187859 hasRelatedWork W2002161059 @default.

• next