FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W2898840253> ?p ?o ?g. }

• W2898840253 endingPage "93" @default.
• W2898840253 startingPage "84" @default.
• W2898840253 abstract "Abstract This study proposed an apparatus for measuring the sediment transport capacity, which is an important parameter for rill erosion prediction and modeling. Laboratory experiments were conducted to measure the sediment transport capacity of partially thawed black soil slope under different hydraulic conditions and thawed depths (five slope gradients of 5°, 10°, 15°, 20°, and 25°; three flow discharges of 1, 2, and 4 dm 3 min −1 ; and four thawed depths of 1, 2, 5, and 10 cm). The effect of thawed depth on sediment transport capacity was quantified with experimental data under different slope gradients and flow discharges. A quadratic model was used to relate sediment transport capacity to thawed depth, slope gradient, and flow discharge, and its key factors that influenced sediment transport capacity were determined by using stepwise regression. Results showed that sediment transport capacity decreased with the increase of thawed depth from 1 to 5 cm, but it tended to be steady when the thawed depth was greater than 5 cm. Model‐fitting results showed that sediment transport capacity was positively correlated with slope gradient and flow discharge but negatively correlated with thawed depth. The proposed method and experimental device solved the difficulties of insufficient sediment supply on the measurement of sediment transport capability, and it can be used to measure the sediment transport capacity of concentrated water flow under different conditions of slope gradient, thawed depth, and flow discharge. The method is helpful to the research of erosion process of partially thawed soil under concentrated water." @default.
• W2898840253 created "2018-11-09" @default.
• W2898840253 creator A5007165718 @default.
• W2898840253 creator A5010230464 @default.
• W2898840253 creator A5037427972 @default.
• W2898840253 creator A5089049740 @default.
• W2898840253 creator A5090716417 @default.
• W2898840253 date "2018-11-14" @default.
• W2898840253 modified "2023-10-06" @default.
• W2898840253 title "Effects of thawed depth on the sediment transport capacity by melt water on partially thawed black soil slope" @default.
• W2898840253 cites W1508872785 @default.
• W2898840253 cites W1965817975 @default.
• W2898840253 cites W1982680817 @default.
• W2898840253 cites W1989556826 @default.
• W2898840253 cites W1991269377 @default.
• W2898840253 cites W1996381847 @default.
• W2898840253 cites W2006654056 @default.
• W2898840253 cites W2007270603 @default.
• W2898840253 cites W2021845518 @default.
• W2898840253 cites W2026972949 @default.
• W2898840253 cites W2027437840 @default.
• W2898840253 cites W2029297029 @default.
• W2898840253 cites W2029707476 @default.
• W2898840253 cites W2035040212 @default.
• W2898840253 cites W2039356720 @default.
• W2898840253 cites W2039523243 @default.
• W2898840253 cites W2051231047 @default.
• W2898840253 cites W2054577799 @default.
• W2898840253 cites W2072369927 @default.
• W2898840253 cites W2073971686 @default.
• W2898840253 cites W2108389745 @default.
• W2898840253 cites W2114415341 @default.
• W2898840253 cites W2134412768 @default.
• W2898840253 cites W2135181820 @default.
• W2898840253 cites W2140107731 @default.
• W2898840253 cites W2147320839 @default.
• W2898840253 cites W2163383536 @default.
• W2898840253 cites W2167601678 @default.
• W2898840253 cites W2279384332 @default.
• W2898840253 cites W2333508126 @default.
• W2898840253 cites W2611599369 @default.
• W2898840253 cites W2639210142 @default.
• W2898840253 doi "https://doi.org/10.1002/ldr.3213" @default.
• W2898840253 hasPublicationYear "2018" @default.
• W2898840253 type Work @default.
• W2898840253 sameAs 2898840253 @default.
• W2898840253 citedByCount "18" @default.
• W2898840253 countsByYear W28988402532019 @default.
• W2898840253 countsByYear W28988402532020 @default.
• W2898840253 countsByYear W28988402532021 @default.
• W2898840253 countsByYear W28988402532022 @default.
• W2898840253 countsByYear W28988402532023 @default.
• W2898840253 crossrefType "journal-article" @default.
• W2898840253 hasAuthorship W2898840253A5007165718 @default.
• W2898840253 hasAuthorship W2898840253A5010230464 @default.
• W2898840253 hasAuthorship W2898840253A5037427972 @default.
• W2898840253 hasAuthorship W2898840253A5089049740 @default.
• W2898840253 hasAuthorship W2898840253A5090716417 @default.
• W2898840253 hasBestOaLocation W28988402531 @default.
• W2898840253 hasConcept C114793014 @default.
• W2898840253 hasConcept C123157820 @default.
• W2898840253 hasConcept C127313418 @default.
• W2898840253 hasConcept C159390177 @default.
• W2898840253 hasConcept C187320778 @default.
• W2898840253 hasConcept C2524010 @default.
• W2898840253 hasConcept C2779135002 @default.
• W2898840253 hasConcept C2816523 @default.
• W2898840253 hasConcept C33923547 @default.
• W2898840253 hasConcept C38349280 @default.
• W2898840253 hasConcept C39432304 @default.
• W2898840253 hasConcept C65589250 @default.
• W2898840253 hasConcept C76886044 @default.
• W2898840253 hasConceptScore W2898840253C114793014 @default.
• W2898840253 hasConceptScore W2898840253C123157820 @default.
• W2898840253 hasConceptScore W2898840253C127313418 @default.
• W2898840253 hasConceptScore W2898840253C159390177 @default.
• W2898840253 hasConceptScore W2898840253C187320778 @default.
• W2898840253 hasConceptScore W2898840253C2524010 @default.
• W2898840253 hasConceptScore W2898840253C2779135002 @default.
• W2898840253 hasConceptScore W2898840253C2816523 @default.
• W2898840253 hasConceptScore W2898840253C33923547 @default.
• W2898840253 hasConceptScore W2898840253C38349280 @default.
• W2898840253 hasConceptScore W2898840253C39432304 @default.
• W2898840253 hasConceptScore W2898840253C65589250 @default.
• W2898840253 hasConceptScore W2898840253C76886044 @default.
• W2898840253 hasFunder F4320321001 @default.
• W2898840253 hasIssue "1" @default.
• W2898840253 hasLocation W28988402531 @default.
• W2898840253 hasOpenAccess W2898840253 @default.
• W2898840253 hasPrimaryLocation W28988402531 @default.
• W2898840253 hasRelatedWork W1744977351 @default.
• W2898840253 hasRelatedWork W185418307 @default.
• W2898840253 hasRelatedWork W1990458937 @default.
• W2898840253 hasRelatedWork W2043720786 @default.
• W2898840253 hasRelatedWork W2061765463 @default.
• W2898840253 hasRelatedWork W2122638437 @default.
• W2898840253 hasRelatedWork W2171810161 @default.
• W2898840253 hasRelatedWork W2347660463 @default.

• next