FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W2815641145> ?p ?o ?g. }

• W2815641145 endingPage "084011" @default.
• W2815641145 startingPage "084011" @default.
• W2815641145 abstract "Seawater intrusion has often resulted in scarce fresh groundwater resources in coastal lowlands. Careful management is essential to avoid the overexploitation of these vulnerable fresh groundwater resources, requiring detailed information on their spatial occurrence. Airborne electromagnetics (EM) has proved a valuable tool for efficient mapping of ground conductivity, as a proxy for fresh groundwater resources. Stakeholders are, however, interested in groundwater salinity, necessitating a translation of ground conductivity to groundwater salinity. This paper presents a methodology to construct a high-resolution (50 × 50 × 0.5 m3) 3D voxel model of groundwater chloride concentration probability, based on a large-scale (1800 km2, 9640 flight line kilometres) airborne EM survey in the province of Zeeland, the Netherlands. Groundwater chloride concentration was obtained by combining pedotransfer functions with detailed lithological information. The methodology includes a Monte Carlo based forward uncertainty propagation approach to quantify the inherent uncertainty in the different steps. Validation showed good correspondence both with available groundwater chloride analyses, and with ground-based hydrogeophysical measurements. Our results show the limited occurrence of fresh groundwater in Zeeland, as 75% of the area lacks fresh groundwater within 15 m below ground surface. Fresh groundwater is mainly limited to the dune area and sandy creek ridges. In addition, significant fresh groundwater resources were shown to exist below saline groundwater, where infiltration of seawater during marine transgressions was hindered by the presence of clayey aquitards. The considerable uncertainty in our results highlights the importance of applying uncertainty analysis in airborne EM surveys. Uncertainty in our results mainly originated from the inversion and the 3D interpolation, and was largest at transition zones between fresh and saline groundwater. Reporting groundwater salinity instead of ground conductivity facilitated the rapid uptake of our results by relevant stakeholders, thereby supporting the necessary management of fresh groundwater resources in the region." @default.
• W2815641145 created "2018-07-19" @default.
• W2815641145 creator A5000010870 @default.
• W2815641145 creator A5000744880 @default.
• W2815641145 creator A5012032240 @default.
• W2815641145 creator A5019653867 @default.
• W2815641145 creator A5023750816 @default.
• W2815641145 creator A5025503903 @default.
• W2815641145 creator A5027499778 @default.
• W2815641145 creator A5029636398 @default.
• W2815641145 creator A5053116229 @default.
• W2815641145 creator A5057814189 @default.
• W2815641145 creator A5059256495 @default.
• W2815641145 creator A5067095186 @default.
• W2815641145 creator A5070199879 @default.
• W2815641145 creator A5070577636 @default.
• W2815641145 creator A5071483444 @default.
• W2815641145 creator A5090359137 @default.
• W2815641145 date "2018-07-27" @default.
• W2815641145 modified "2023-10-06" @default.
• W2815641145 title "Large-scale, probabilistic salinity mapping using airborne electromagnetics for groundwater management in Zeeland, the Netherlands" @default.
• W2815641145 cites W1872845361 @default.
• W2815641145 cites W1964932790 @default.
• W2815641145 cites W1966182904 @default.
• W2815641145 cites W1975661364 @default.
• W2815641145 cites W1981436876 @default.
• W2815641145 cites W2004659909 @default.
• W2815641145 cites W2011119786 @default.
• W2815641145 cites W2013569938 @default.
• W2815641145 cites W2031401646 @default.
• W2815641145 cites W2035927985 @default.
• W2815641145 cites W2050402478 @default.
• W2815641145 cites W2052687175 @default.
• W2815641145 cites W2067444340 @default.
• W2815641145 cites W2068906281 @default.
• W2815641145 cites W2071829124 @default.
• W2815641145 cites W2079141634 @default.
• W2815641145 cites W2083527554 @default.
• W2815641145 cites W2087452412 @default.
• W2815641145 cites W2096910235 @default.
• W2815641145 cites W2100319368 @default.
• W2815641145 cites W2108310690 @default.
• W2815641145 cites W2120591714 @default.
• W2815641145 cites W2123307153 @default.
• W2815641145 cites W2125095996 @default.
• W2815641145 cites W2126546037 @default.
• W2815641145 cites W2139241101 @default.
• W2815641145 cites W2140167071 @default.
• W2815641145 cites W2152368231 @default.
• W2815641145 cites W2153261214 @default.
• W2815641145 cites W2159050085 @default.
• W2815641145 cites W2166928582 @default.
• W2815641145 cites W2168155226 @default.
• W2815641145 cites W2442059877 @default.
• W2815641145 cites W2569983659 @default.
• W2815641145 cites W2606666270 @default.
• W2815641145 cites W268878312 @default.
• W2815641145 cites W2741000561 @default.
• W2815641145 cites W3123305572 @default.
• W2815641145 cites W4211124384 @default.
• W2815641145 cites W784795887 @default.
• W2815641145 doi "https://doi.org/10.1088/1748-9326/aad19e" @default.
• W2815641145 hasPublicationYear "2018" @default.
• W2815641145 type Work @default.
• W2815641145 sameAs 2815641145 @default.
• W2815641145 citedByCount "40" @default.
• W2815641145 countsByYear W28156411452018 @default.
• W2815641145 countsByYear W28156411452019 @default.
• W2815641145 countsByYear W28156411452020 @default.
• W2815641145 countsByYear W28156411452021 @default.
• W2815641145 countsByYear W28156411452022 @default.
• W2815641145 countsByYear W28156411452023 @default.
• W2815641145 crossrefType "journal-article" @default.
• W2815641145 hasAuthorship W2815641145A5000010870 @default.
• W2815641145 hasAuthorship W2815641145A5000744880 @default.
• W2815641145 hasAuthorship W2815641145A5012032240 @default.
• W2815641145 hasAuthorship W2815641145A5019653867 @default.
• W2815641145 hasAuthorship W2815641145A5023750816 @default.
• W2815641145 hasAuthorship W2815641145A5025503903 @default.
• W2815641145 hasAuthorship W2815641145A5027499778 @default.
• W2815641145 hasAuthorship W2815641145A5029636398 @default.
• W2815641145 hasAuthorship W2815641145A5053116229 @default.
• W2815641145 hasAuthorship W2815641145A5057814189 @default.
• W2815641145 hasAuthorship W2815641145A5059256495 @default.
• W2815641145 hasAuthorship W2815641145A5067095186 @default.
• W2815641145 hasAuthorship W2815641145A5070199879 @default.
• W2815641145 hasAuthorship W2815641145A5070577636 @default.
• W2815641145 hasAuthorship W2815641145A5071483444 @default.
• W2815641145 hasAuthorship W2815641145A5090359137 @default.
• W2815641145 hasBestOaLocation W28156411451 @default.
• W2815641145 hasConcept C111368507 @default.
• W2815641145 hasConcept C127313418 @default.
• W2815641145 hasConcept C129513315 @default.
• W2815641145 hasConcept C131227075 @default.
• W2815641145 hasConcept C132594454 @default.
• W2815641145 hasConcept C159390177 @default.
• W2815641145 hasConcept C176650113 @default.
• W2815641145 hasConcept C187320778 @default.

• next