FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W2804199042> ?p ?o ?g. }

• W2804199042 endingPage "13" @default.
• W2804199042 startingPage "1" @default.
• W2804199042 abstract "Core Ideas Soil water stable isotope profiles can be used to quantify groundwater recharge. Climate conditions are recorded in water stable isotope profiles of the unsaturated zone. Soil water isotope profiles provide insight into the seasonality of recharge events. A reliable estimate of recharge is needed for the sustainable management of groundwater resources. Water stable isotope (δ 18 O and δ 2 H) profiles in the unsaturated zone are frequently used to quantify groundwater recharge based on the seasonality of water isotopic compositions in precipitation. A very simple approach consists of integrating the soil water content between peak values of soil water isotopic composition, typically corresponding to precipitation signatures from warm and cold seasons. When precipitation isotopic compositions are available, a conceptual surface water isotopes budget and lumped parameter dispersion model can be computed. These models were applied on two field sites with similar permeable soils with grass cover but contrasting recharge regimes and seasonality, one in the Paris Basin (France) with continuous recharge from autumn to spring and the other in the St. Lawrence Lowlands (Quebec, Canada) with episodic recharge in fall and after snowmelt. For the two sites, the peak‐to‐peak method and isotope surface budget led to comparable recharge intensities. At least at the Paris Basin site, evaporation was shown to slightly modify the average unsaturated zone and hence groundwater isotope composition. The proposed parameterization of isotope fractionation due to evaporation allows qualitative estimation of the fraction of evaporation, at least during the recharge seasons. In spite of its simplifications and limitations, the proposed parsimonious model can give estimates of recharge in a variety of sites even if they are not well characterized, as it benefits from the large availability of monthly isotopic compositions in precipitation." @default.
• W2804199042 created "2018-06-01" @default.
• W2804199042 creator A5018636879 @default.
• W2804199042 creator A5018711103 @default.
• W2804199042 creator A5024923884 @default.
• W2804199042 creator A5027840313 @default.
• W2804199042 creator A5028183448 @default.
• W2804199042 creator A5031709707 @default.
• W2804199042 creator A5070060465 @default.
• W2804199042 creator A5075021056 @default.
• W2804199042 creator A5088284382 @default.
• W2804199042 creator A5090487274 @default.
• W2804199042 creator A5091638744 @default.
• W2804199042 date "2018-01-01" @default.
• W2804199042 modified "2023-10-07" @default.
• W2804199042 title "Using Water Stable Isotopes in the Unsaturated Zone to Quantify Recharge in Two Contrasted Infiltration Regimes" @default.
• W2804199042 cites W1511829535 @default.
• W2804199042 cites W1517854276 @default.
• W2804199042 cites W1559839988 @default.
• W2804199042 cites W1961477324 @default.
• W2804199042 cites W1965247133 @default.
• W2804199042 cites W1993388356 @default.
• W2804199042 cites W2002115844 @default.
• W2804199042 cites W2017320921 @default.
• W2804199042 cites W2018769657 @default.
• W2804199042 cites W2028615479 @default.
• W2804199042 cites W2030368947 @default.
• W2804199042 cites W2035840698 @default.
• W2804199042 cites W2044810350 @default.
• W2804199042 cites W2045958826 @default.
• W2804199042 cites W2046638784 @default.
• W2804199042 cites W2051827283 @default.
• W2804199042 cites W2057040463 @default.
• W2804199042 cites W2057296492 @default.
• W2804199042 cites W2063267042 @default.
• W2804199042 cites W2065201713 @default.
• W2804199042 cites W2065344889 @default.
• W2804199042 cites W2070666875 @default.
• W2804199042 cites W2081807741 @default.
• W2804199042 cites W2085712758 @default.
• W2804199042 cites W2086084157 @default.
• W2804199042 cites W2093622567 @default.
• W2804199042 cites W2096092308 @default.
• W2804199042 cites W2122941804 @default.
• W2804199042 cites W2128677326 @default.
• W2804199042 cites W2152608230 @default.
• W2804199042 cites W2155039315 @default.
• W2804199042 cites W2276246310 @default.
• W2804199042 cites W2291169292 @default.
• W2804199042 cites W2336308352 @default.
• W2804199042 cites W2484804024 @default.
• W2804199042 cites W2516236611 @default.
• W2804199042 cites W2600777534 @default.
• W2804199042 cites W2774557542 @default.
• W2804199042 cites W4230271547 @default.
• W2804199042 cites W97725961 @default.
• W2804199042 doi "https://doi.org/10.2136/vzj2017.09.0170" @default.
• W2804199042 hasPublicationYear "2018" @default.
• W2804199042 type Work @default.
• W2804199042 sameAs 2804199042 @default.
• W2804199042 citedByCount "19" @default.
• W2804199042 countsByYear W28041990422018 @default.
• W2804199042 countsByYear W28041990422019 @default.
• W2804199042 countsByYear W28041990422020 @default.
• W2804199042 countsByYear W28041990422021 @default.
• W2804199042 countsByYear W28041990422022 @default.
• W2804199042 countsByYear W28041990422023 @default.
• W2804199042 crossrefType "journal-article" @default.
• W2804199042 hasAuthorship W2804199042A5018636879 @default.
• W2804199042 hasAuthorship W2804199042A5018711103 @default.
• W2804199042 hasAuthorship W2804199042A5024923884 @default.
• W2804199042 hasAuthorship W2804199042A5027840313 @default.
• W2804199042 hasAuthorship W2804199042A5028183448 @default.
• W2804199042 hasAuthorship W2804199042A5031709707 @default.
• W2804199042 hasAuthorship W2804199042A5070060465 @default.
• W2804199042 hasAuthorship W2804199042A5075021056 @default.
• W2804199042 hasAuthorship W2804199042A5088284382 @default.
• W2804199042 hasAuthorship W2804199042A5090487274 @default.
• W2804199042 hasAuthorship W2804199042A5091638744 @default.
• W2804199042 hasBestOaLocation W28041990421 @default.
• W2804199042 hasConcept C107054158 @default.
• W2804199042 hasConcept C121332964 @default.
• W2804199042 hasConcept C127313418 @default.
• W2804199042 hasConcept C153294291 @default.
• W2804199042 hasConcept C153400128 @default.
• W2804199042 hasConcept C159390177 @default.
• W2804199042 hasConcept C159750122 @default.
• W2804199042 hasConcept C174091901 @default.
• W2804199042 hasConcept C187320778 @default.
• W2804199042 hasConcept C187606762 @default.
• W2804199042 hasConcept C205649164 @default.
• W2804199042 hasConcept C22117777 @default.
• W2804199042 hasConcept C2779334269 @default.
• W2804199042 hasConcept C35588792 @default.
• W2804199042 hasConcept C39432304 @default.
• W2804199042 hasConcept C62520636 @default.
• W2804199042 hasConcept C75622301 @default.
• W2804199042 hasConcept C76177295 @default.

• next