FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W4381893062> ?p ?o ?g. }

• W4381893062 endingPage "129861" @default.
• W4381893062 startingPage "129861" @default.
• W4381893062 abstract "Studying the dynamic mechanism of water-level variations during the freeze–thaw period in seasonally frozen soil regions is an important premise and foundation for winter agricultural irrigation and groundwater resource assessment. Freezing and thawing-induced groundwater-level variations have been observed in regions with a shallow water table depth. However, whether the groundwater level is affected by the freeze–thaw process and the extent of this effect should be verified and discussed on a wider spatiotemporal scale. To this end, this study selected the plain area of Jilin Province, China as an example, and based on a comprehensive analysis of dynamic groundwater-level monitoring data from 114 monitoring wells, the distribution of the meteorological data and soil types and two typical experimental monitoring sites in the area, the dynamic characteristics and influencing factors of groundwater-level variations during the freeze–thaw period were identified. Combined with a multi-factor statistical analysis of the monitoring data at the regional scale of the plain area of Jilin Province, China, the response mechanism of the groundwater level to the freeze–thaw process in the seasonally frozen plain area was summarized. The results showed that: (1) The dynamic phenomenon where the groundwater level falls in the freezing period and rises in the thawing period due to the freeze–thaw process was widespread in seasonally frozen soil regions; (2) The depth threshold of the groundwater level affected by the freeze–thaw process was the sum of the maximum frozen soil depth and the maximum capillary rise height; (3) The main factors controlling the groundwater-level variation during the freeze–thaw period were the initial water-level depth and the maximum snow cover thickness; based on a random forest model, the groundwater-level variation during the freeze–thaw process could be accurately calculated with these main controlling factors; (4) The groundwater-level dynamics during the freeze–thaw process was mainly controlled by the exchange of water between the groundwater and the vadose zone system, and the rise in the water level was only partially replenished by the snowmelt water. The research results have an important guiding significance for winter agricultural irrigation and groundwater recharge resource evaluation." @default.
• W4381893062 created "2023-06-25" @default.
• W4381893062 creator A5030570455 @default.
• W4381893062 creator A5031677706 @default.
• W4381893062 creator A5038156281 @default.
• W4381893062 creator A5055329626 @default.
• W4381893062 creator A5055582538 @default.
• W4381893062 creator A5067046839 @default.
• W4381893062 creator A5070149461 @default.
• W4381893062 creator A5092254418 @default.
• W4381893062 date "2023-10-01" @default.
• W4381893062 modified "2023-10-17" @default.
• W4381893062 title "Response mechanism of groundwater dynamics to Freeze–thaw process in seasonally frozen soil areas: A comprehensive analysis from site to regional scale" @default.
• W4381893062 cites W1506954298 @default.
• W4381893062 cites W1824063337 @default.
• W4381893062 cites W1921648414 @default.
• W4381893062 cites W1980488427 @default.
• W4381893062 cites W1982546148 @default.
• W4381893062 cites W2000628210 @default.
• W4381893062 cites W2029926590 @default.
• W4381893062 cites W2033780566 @default.
• W4381893062 cites W2067632765 @default.
• W4381893062 cites W2067804742 @default.
• W4381893062 cites W2074418666 @default.
• W4381893062 cites W2091683557 @default.
• W4381893062 cites W2094141941 @default.
• W4381893062 cites W2149725474 @default.
• W4381893062 cites W2156242321 @default.
• W4381893062 cites W2164509249 @default.
• W4381893062 cites W2208293910 @default.
• W4381893062 cites W2329731234 @default.
• W4381893062 cites W2566631835 @default.
• W4381893062 cites W2621367204 @default.
• W4381893062 cites W2789245453 @default.
• W4381893062 cites W2811291286 @default.
• W4381893062 cites W2902899832 @default.
• W4381893062 cites W2909354181 @default.
• W4381893062 cites W2911288853 @default.
• W4381893062 cites W2911964244 @default.
• W4381893062 cites W2921434269 @default.
• W4381893062 cites W2922051790 @default.
• W4381893062 cites W2943844017 @default.
• W4381893062 cites W3010833015 @default.
• W4381893062 cites W3034711722 @default.
• W4381893062 cites W3127225892 @default.
• W4381893062 cites W3141995413 @default.
• W4381893062 cites W3151874731 @default.
• W4381893062 cites W4205891915 @default.
• W4381893062 cites W4290667669 @default.
• W4381893062 cites W4311770299 @default.
• W4381893062 cites W4312077130 @default.
• W4381893062 cites W4322588487 @default.
• W4381893062 cites W4323353634 @default.
• W4381893062 cites W68263387 @default.
• W4381893062 cites W807788440 @default.
• W4381893062 doi "https://doi.org/10.1016/j.jhydrol.2023.129861" @default.
• W4381893062 hasPublicationYear "2023" @default.
• W4381893062 type Work @default.
• W4381893062 citedByCount "0" @default.
• W4381893062 crossrefType "journal-article" @default.
• W4381893062 hasAuthorship W4381893062A5030570455 @default.
• W4381893062 hasAuthorship W4381893062A5031677706 @default.
• W4381893062 hasAuthorship W4381893062A5038156281 @default.
• W4381893062 hasAuthorship W4381893062A5055329626 @default.
• W4381893062 hasAuthorship W4381893062A5055582538 @default.
• W4381893062 hasAuthorship W4381893062A5067046839 @default.
• W4381893062 hasAuthorship W4381893062A5070149461 @default.
• W4381893062 hasAuthorship W4381893062A5092254418 @default.
• W4381893062 hasConcept C127313418 @default.
• W4381893062 hasConcept C131227075 @default.
• W4381893062 hasConcept C187320778 @default.
• W4381893062 hasConcept C18903297 @default.
• W4381893062 hasConcept C2993807900 @default.
• W4381893062 hasConcept C39432304 @default.
• W4381893062 hasConcept C39769621 @default.
• W4381893062 hasConcept C75622301 @default.
• W4381893062 hasConcept C76177295 @default.
• W4381893062 hasConcept C76886044 @default.
• W4381893062 hasConcept C86803240 @default.
• W4381893062 hasConcept C88862950 @default.
• W4381893062 hasConceptScore W4381893062C127313418 @default.
• W4381893062 hasConceptScore W4381893062C131227075 @default.
• W4381893062 hasConceptScore W4381893062C187320778 @default.
• W4381893062 hasConceptScore W4381893062C18903297 @default.
• W4381893062 hasConceptScore W4381893062C2993807900 @default.
• W4381893062 hasConceptScore W4381893062C39432304 @default.
• W4381893062 hasConceptScore W4381893062C39769621 @default.
• W4381893062 hasConceptScore W4381893062C75622301 @default.
• W4381893062 hasConceptScore W4381893062C76177295 @default.
• W4381893062 hasConceptScore W4381893062C76886044 @default.
• W4381893062 hasConceptScore W4381893062C86803240 @default.
• W4381893062 hasConceptScore W4381893062C88862950 @default.
• W4381893062 hasLocation W43818930621 @default.
• W4381893062 hasOpenAccess W4381893062 @default.
• W4381893062 hasPrimaryLocation W43818930621 @default.
• W4381893062 hasRelatedWork W1996185918 @default.
• W4381893062 hasRelatedWork W2021901612 @default.
• W4381893062 hasRelatedWork W2146049854 @default.

• next