FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W3128532142> ?p ?o ?g. }

• W3128532142 endingPage "103236" @default.
• W3128532142 startingPage "103236" @default.
• W3128532142 abstract "It hasn't yet fully understood the influence of freeze-thaw action on hydrological processes in the active layer of permafrost regions. So this article investigated one permafrost cross-section at the northern slope of Bayan Har Mountains in the Source Area of the Yellow River in Qinghai-Tibet Plateau. According to the data of field monitoring, seasonal variability of soil hydrological processes in the active layer of permafrost regions was studied and simulated by the freeze–thaw module of HYDRUS-1D software. The results show that: 1) The soil moisture and the suprapermafrost water-level are divided into four stages based on the freeze-thaw process. Rainfall infiltration is the main driving force of soil hydrological processes, and the freeze-thaw front are the main limiting factors. 2) The active layer thickness (ALT) is greater on the upslope than that on the downslope due to the influence of terrain slope. It leads to that the change variation of the soil moisture and the suprapermafrost water-level on the upslope is also more gently than that on the downslope. 3) Temperature is the key factor that affects soil hydrologic process of the active layer in permafrost regions. Soil temperature and soil moisture showed a significant exponential linear correlation at different depths. The relationship between soil temperature and suprapermafrost water level shows Boltzmann function relations. 4) Soil moisture has a downward migration trend after a freeze-thaw cycle. It will result in the formation of underground ice near the permafrost table. Driven by the temperature gradient, the unfrozen water in the active layer moves from bottom to top during the freezing stage." @default.
• W3128532142 created "2021-02-15" @default.
• W3128532142 creator A5000585322 @default.
• W3128532142 creator A5035840776 @default.
• W3128532142 creator A5036442264 @default.
• W3128532142 creator A5052407661 @default.
• W3128532142 creator A5056737897 @default.
• W3128532142 creator A5088823863 @default.
• W3128532142 date "2021-04-01" @default.
• W3128532142 modified "2023-10-02" @default.
• W3128532142 title "Soil hydrological process and migration mode influenced by the freeze-thaw process in the activity layer of permafrost regions in Qinghai-Tibet Plateau" @default.
• W3128532142 cites W1536862309 @default.
• W3128532142 cites W1948181119 @default.
• W3128532142 cites W1964297347 @default.
• W3128532142 cites W1968289388 @default.
• W3128532142 cites W1969344177 @default.
• W3128532142 cites W2042680364 @default.
• W3128532142 cites W2049458272 @default.
• W3128532142 cites W2069943188 @default.
• W3128532142 cites W2091602088 @default.
• W3128532142 cites W2093972211 @default.
• W3128532142 cites W2111157073 @default.
• W3128532142 cites W2126667681 @default.
• W3128532142 cites W2138861510 @default.
• W3128532142 cites W2145748202 @default.
• W3128532142 cites W2160628588 @default.
• W3128532142 cites W2462096431 @default.
• W3128532142 cites W2524345951 @default.
• W3128532142 cites W2586775077 @default.
• W3128532142 cites W2611030641 @default.
• W3128532142 cites W2767734416 @default.
• W3128532142 cites W2783117129 @default.
• W3128532142 cites W2970980872 @default.
• W3128532142 doi "https://doi.org/10.1016/j.coldregions.2021.103236" @default.
• W3128532142 hasPublicationYear "2021" @default.
• W3128532142 type Work @default.
• W3128532142 sameAs 3128532142 @default.
• W3128532142 citedByCount "9" @default.
• W3128532142 countsByYear W31285321422021 @default.
• W3128532142 countsByYear W31285321422022 @default.
• W3128532142 countsByYear W31285321422023 @default.
• W3128532142 crossrefType "journal-article" @default.
• W3128532142 hasAuthorship W3128532142A5000585322 @default.
• W3128532142 hasAuthorship W3128532142A5035840776 @default.
• W3128532142 hasAuthorship W3128532142A5036442264 @default.
• W3128532142 hasAuthorship W3128532142A5052407661 @default.
• W3128532142 hasAuthorship W3128532142A5056737897 @default.
• W3128532142 hasAuthorship W3128532142A5088823863 @default.
• W3128532142 hasConcept C111368507 @default.
• W3128532142 hasConcept C114793014 @default.
• W3128532142 hasConcept C121332964 @default.
• W3128532142 hasConcept C127313418 @default.
• W3128532142 hasConcept C133830359 @default.
• W3128532142 hasConcept C134306372 @default.
• W3128532142 hasConcept C15098985 @default.
• W3128532142 hasConcept C153400128 @default.
• W3128532142 hasConcept C159390177 @default.
• W3128532142 hasConcept C159985019 @default.
• W3128532142 hasConcept C176864760 @default.
• W3128532142 hasConcept C178790620 @default.
• W3128532142 hasConcept C185592680 @default.
• W3128532142 hasConcept C187320778 @default.
• W3128532142 hasConcept C18903297 @default.
• W3128532142 hasConcept C192562407 @default.
• W3128532142 hasConcept C24939127 @default.
• W3128532142 hasConcept C2776026197 @default.
• W3128532142 hasConcept C2779227376 @default.
• W3128532142 hasConcept C2780030769 @default.
• W3128532142 hasConcept C33923547 @default.
• W3128532142 hasConcept C39432304 @default.
• W3128532142 hasConcept C76886044 @default.
• W3128532142 hasConcept C86803240 @default.
• W3128532142 hasConcept C87359718 @default.
• W3128532142 hasConcept C97355855 @default.
• W3128532142 hasConceptScore W3128532142C111368507 @default.
• W3128532142 hasConceptScore W3128532142C114793014 @default.
• W3128532142 hasConceptScore W3128532142C121332964 @default.
• W3128532142 hasConceptScore W3128532142C127313418 @default.
• W3128532142 hasConceptScore W3128532142C133830359 @default.
• W3128532142 hasConceptScore W3128532142C134306372 @default.
• W3128532142 hasConceptScore W3128532142C15098985 @default.
• W3128532142 hasConceptScore W3128532142C153400128 @default.
• W3128532142 hasConceptScore W3128532142C159390177 @default.
• W3128532142 hasConceptScore W3128532142C159985019 @default.
• W3128532142 hasConceptScore W3128532142C176864760 @default.
• W3128532142 hasConceptScore W3128532142C178790620 @default.
• W3128532142 hasConceptScore W3128532142C185592680 @default.
• W3128532142 hasConceptScore W3128532142C187320778 @default.
• W3128532142 hasConceptScore W3128532142C18903297 @default.
• W3128532142 hasConceptScore W3128532142C192562407 @default.
• W3128532142 hasConceptScore W3128532142C24939127 @default.
• W3128532142 hasConceptScore W3128532142C2776026197 @default.
• W3128532142 hasConceptScore W3128532142C2779227376 @default.
• W3128532142 hasConceptScore W3128532142C2780030769 @default.
• W3128532142 hasConceptScore W3128532142C33923547 @default.
• W3128532142 hasConceptScore W3128532142C39432304 @default.
• W3128532142 hasConceptScore W3128532142C76886044 @default.
• W3128532142 hasConceptScore W3128532142C86803240 @default.

• next