FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W4320175900> ?p ?o ?g. }

• W4320175900 abstract "Quantitative estimates on the magnitude and dynamics of vadose and groundwater zones in subarctic conditions are rare. Furthermore, knowledge on the constraints of different data on numerical groundwater recharge estimates (i.e., data worth analyses) is limited. We built a process-based three-dimensional hydrological model to describe and analyze the dynamics and magnitude of groundwater recharge, vadose zone, and related key hydrological components in subarctic conditions. Three-year time series of daily groundwater level and soil moisture (five different depths) data were used to identify plausible model realizations. Thereafter, long-term simulations over 6 years were conducted. The model adequately corresponded with the magnitude and dynamics of the observations, even though the simulations and observations occasionally differed. Simulations with several different plausible parameterizations showed how soil moisture and groundwater level fluctuations, as well as recharge estimates, are sensitive to water retention parameter variations, whereas precipitation and evapotranspiration controlled the recharge magnitude. Recharge showed clear interannual variability (annual mean 0.28–0.60 m). The fraction of annual mean recharge over precipitation was 39%–66% during our simulation period. We showed how groundwater level data can set more constraints on the recharge estimates than soil moisture data, and how both of the data types together constrained the recharge estimates the most. We showed how the vadose zone had modest dynamics and storage properties (typically 2%–8% of the total soil water) in terms of the bulk soil water storage. However, the average amount of the air-filled pore space (0.70 m) and water (0.38 m) in the vadose zone were proportional to annual precipitation and evapotranspiration, respectively. Thus, the vadose zone can form an important boundary between the soil surface and groundwater zone, and its role is not highly sensitive to hydrometeorological fluctuations. Data worth analyses provide a potential opportunity to move toward increasingly reliable model-based groundwater recharge estimates and system understanding." @default.
• W4320175900 created "2023-02-13" @default.
• W4320175900 creator A5012232805 @default.
• W4320175900 creator A5041512676 @default.
• W4320175900 date "2023-04-01" @default.
• W4320175900 modified "2023-09-30" @default.
• W4320175900 title "Analyzing Groundwater Recharge and Vadose Zone Dynamics by Combining Soil Moisture and Groundwater Level Data with a Numerical Model in Subarctic Conditions" @default.
• W4320175900 cites W1503360627 @default.
• W4320175900 cites W1539136003 @default.
• W4320175900 cites W1597050087 @default.
• W4320175900 cites W1972445152 @default.
• W4320175900 cites W1980965960 @default.
• W4320175900 cites W1982937037 @default.
• W4320175900 cites W1982952270 @default.
• W4320175900 cites W1983872304 @default.
• W4320175900 cites W1984061088 @default.
• W4320175900 cites W1996294474 @default.
• W4320175900 cites W2003696872 @default.
• W4320175900 cites W2005348293 @default.
• W4320175900 cites W2020622595 @default.
• W4320175900 cites W2034926839 @default.
• W4320175900 cites W2043003992 @default.
• W4320175900 cites W2046654411 @default.
• W4320175900 cites W2048409756 @default.
• W4320175900 cites W2049059559 @default.
• W4320175900 cites W2051889289 @default.
• W4320175900 cites W2055668893 @default.
• W4320175900 cites W2064184119 @default.
• W4320175900 cites W2076800104 @default.
• W4320175900 cites W2078794786 @default.
• W4320175900 cites W2106414049 @default.
• W4320175900 cites W2111375255 @default.
• W4320175900 cites W2116821716 @default.
• W4320175900 cites W2119403063 @default.
• W4320175900 cites W2122854726 @default.
• W4320175900 cites W2124593651 @default.
• W4320175900 cites W2133364621 @default.
• W4320175900 cites W2136328522 @default.
• W4320175900 cites W2145500754 @default.
• W4320175900 cites W2160948275 @default.
• W4320175900 cites W2162604832 @default.
• W4320175900 cites W2212518052 @default.
• W4320175900 cites W2266601256 @default.
• W4320175900 cites W2406318355 @default.
• W4320175900 cites W2726032495 @default.
• W4320175900 cites W2735318952 @default.
• W4320175900 cites W2738192059 @default.
• W4320175900 cites W2747607226 @default.
• W4320175900 cites W2766295919 @default.
• W4320175900 cites W2783715341 @default.
• W4320175900 cites W2788419196 @default.
• W4320175900 cites W2809779735 @default.
• W4320175900 cites W2912517250 @default.
• W4320175900 cites W2970619772 @default.
• W4320175900 cites W2994088469 @default.
• W4320175900 cites W3016611325 @default.
• W4320175900 cites W3021633053 @default.
• W4320175900 cites W3082230505 @default.
• W4320175900 cites W3112617402 @default.
• W4320175900 cites W3132781201 @default.
• W4320175900 cites W746291689 @default.
• W4320175900 doi "https://doi.org/10.1061/jhyeff.heeng-5842" @default.
• W4320175900 hasPublicationYear "2023" @default.
• W4320175900 type Work @default.
• W4320175900 citedByCount "0" @default.
• W4320175900 crossrefType "journal-article" @default.
• W4320175900 hasAuthorship W4320175900A5012232805 @default.
• W4320175900 hasAuthorship W4320175900A5041512676 @default.
• W4320175900 hasConcept C107054158 @default.
• W4320175900 hasConcept C127313418 @default.
• W4320175900 hasConcept C153294291 @default.
• W4320175900 hasConcept C159390177 @default.
• W4320175900 hasConcept C159750122 @default.
• W4320175900 hasConcept C174091901 @default.
• W4320175900 hasConcept C176650113 @default.
• W4320175900 hasConcept C176783924 @default.
• W4320175900 hasConcept C176864760 @default.
• W4320175900 hasConcept C187320778 @default.
• W4320175900 hasConcept C187606762 @default.
• W4320175900 hasConcept C18903297 @default.
• W4320175900 hasConcept C205649164 @default.
• W4320175900 hasConcept C24939127 @default.
• W4320175900 hasConcept C35588792 @default.
• W4320175900 hasConcept C39432304 @default.
• W4320175900 hasConcept C75622301 @default.
• W4320175900 hasConcept C76177295 @default.
• W4320175900 hasConcept C76886044 @default.
• W4320175900 hasConcept C86803240 @default.
• W4320175900 hasConceptScore W4320175900C107054158 @default.
• W4320175900 hasConceptScore W4320175900C127313418 @default.
• W4320175900 hasConceptScore W4320175900C153294291 @default.
• W4320175900 hasConceptScore W4320175900C159390177 @default.
• W4320175900 hasConceptScore W4320175900C159750122 @default.
• W4320175900 hasConceptScore W4320175900C174091901 @default.
• W4320175900 hasConceptScore W4320175900C176650113 @default.
• W4320175900 hasConceptScore W4320175900C176783924 @default.
• W4320175900 hasConceptScore W4320175900C176864760 @default.
• W4320175900 hasConceptScore W4320175900C187320778 @default.
• W4320175900 hasConceptScore W4320175900C187606762 @default.
• W4320175900 hasConceptScore W4320175900C18903297 @default.

• next