FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W259084889> ?p ?o ?g. }

• W259084889 endingPage "156" @default.
• W259084889 startingPage "145" @default.
• W259084889 abstract "The knowledge of soil salinity and the temporal changes of its distribution in the soil profiles can give warnings for the protection of saline habitats. This study described and compared the salinity profiles of the soils from four hypersaline wetlands at inland, ill-drained depressions in NE Spain, which were sampled throughout the year in 1979–1980 and 1999–2000, and differed in land use. The halophytic communities dictated the location of sampling sites. After the saturated pastes of 404 soil samples were prepared, the electrical conductivity of the extracts (ECe) and the concentrations of major ions were measured, and additional supplementary analyses were performed. A subset of the samples was titrated for calcium carbonate equivalent and gypsum content. ECe and ion concentrations calculated for synthetic soil layers facilitated the comparisons of the vertical distribution of soil salinity among dates, depths, and sites. The shape of the mean ECe profiles over all sampling dates indicated moderate differences between the two wetlands closest to each other, Plan de Callén (PC) and Paúl de Almuniente (AL), which had similar (< ~ 10 dS m− 1) ECe. In contrast, the ECe profile at Paúl de Anzano (AN) ranged from 40 dS m− 1 to 50 dS m− 1 in the upper meter of the soil, which decreased steadily to 20 dS m− 1 at a 2-m depth. At Saladar de Agustín (AG), ECe was much higher and the profile had the opposite shape, ECe ~ 55 dS m− 1 at the surface and > 80 dS m− 1 at an 80-cm depth. The shape of ECe profiles at AL, PC, and AG was rather stable over time, contrasting with the measured desalination of the soil at AL after its conversion into a rice paddy. The changes in the sodium adsorption ratio (SAR) in the soil profiles at AN, PC, and AL are indicators of the potential extremes in the hydric behavior of the soils. At AG, the mineralogical clays are a minor component of these gypseous soils; therefore, the SAR, only, was used as a measure of the relative concentrations of Na+ versus Ca2 + plus Mg2 +. The median SAR of all AG soil samples did not differ significantly among sampling sites or dates. The shorter sampling depth intervals used in 1979–80 were responsible for the greater spread in the distribution and the increase in extreme SAR values compared to the data collected in 1999–2000." @default.
• W259084889 created "2016-06-24" @default.
• W259084889 creator A5017000366 @default.
• W259084889 creator A5031318541 @default.
• W259084889 date "2015-10-01" @default.
• W259084889 modified "2023-10-16" @default.
• W259084889 title "Temporal changes in soil salinity at four saline wetlands in NE Spain" @default.
• W259084889 cites W1527276631 @default.
• W259084889 cites W1964223518 @default.
• W259084889 cites W1975135213 @default.
• W259084889 cites W1979204143 @default.
• W259084889 cites W1997854466 @default.
• W259084889 cites W2000776552 @default.
• W259084889 cites W2005380719 @default.
• W259084889 cites W2007944447 @default.
• W259084889 cites W2008626430 @default.
• W259084889 cites W2019730000 @default.
• W259084889 cites W2029703554 @default.
• W259084889 cites W2039816958 @default.
• W259084889 cites W2040970173 @default.
• W259084889 cites W2042033669 @default.
• W259084889 cites W2050164446 @default.
• W259084889 cites W2053048087 @default.
• W259084889 cites W2054038662 @default.
• W259084889 cites W2059791617 @default.
• W259084889 cites W2061076790 @default.
• W259084889 cites W2066607643 @default.
• W259084889 cites W2077439296 @default.
• W259084889 cites W2108828563 @default.
• W259084889 cites W2168369208 @default.
• W259084889 cites W790241851 @default.
• W259084889 doi "https://doi.org/10.1016/j.catena.2015.04.017" @default.
• W259084889 hasPublicationYear "2015" @default.
• W259084889 type Work @default.
• W259084889 sameAs 259084889 @default.
• W259084889 citedByCount "13" @default.
• W259084889 countsByYear W2590848892016 @default.
• W259084889 countsByYear W2590848892018 @default.
• W259084889 countsByYear W2590848892019 @default.
• W259084889 countsByYear W2590848892020 @default.
• W259084889 countsByYear W2590848892023 @default.
• W259084889 crossrefType "journal-article" @default.
• W259084889 hasAuthorship W259084889A5017000366 @default.
• W259084889 hasAuthorship W259084889A5031318541 @default.
• W259084889 hasBestOaLocation W2590848892 @default.
• W259084889 hasConcept C111368507 @default.
• W259084889 hasConcept C127313418 @default.
• W259084889 hasConcept C129513315 @default.
• W259084889 hasConcept C141650431 @default.
• W259084889 hasConcept C156634047 @default.
• W259084889 hasConcept C159390177 @default.
• W259084889 hasConcept C159750122 @default.
• W259084889 hasConcept C187320778 @default.
• W259084889 hasConcept C18903297 @default.
• W259084889 hasConcept C39432304 @default.
• W259084889 hasConcept C50516716 @default.
• W259084889 hasConcept C67715294 @default.
• W259084889 hasConcept C76886044 @default.
• W259084889 hasConcept C86803240 @default.
• W259084889 hasConceptScore W259084889C111368507 @default.
• W259084889 hasConceptScore W259084889C127313418 @default.
• W259084889 hasConceptScore W259084889C129513315 @default.
• W259084889 hasConceptScore W259084889C141650431 @default.
• W259084889 hasConceptScore W259084889C156634047 @default.
• W259084889 hasConceptScore W259084889C159390177 @default.
• W259084889 hasConceptScore W259084889C159750122 @default.
• W259084889 hasConceptScore W259084889C187320778 @default.
• W259084889 hasConceptScore W259084889C18903297 @default.
• W259084889 hasConceptScore W259084889C39432304 @default.
• W259084889 hasConceptScore W259084889C50516716 @default.
• W259084889 hasConceptScore W259084889C67715294 @default.
• W259084889 hasConceptScore W259084889C76886044 @default.
• W259084889 hasConceptScore W259084889C86803240 @default.
• W259084889 hasFunder F4320321837 @default.
• W259084889 hasLocation W2590848891 @default.
• W259084889 hasLocation W2590848892 @default.
• W259084889 hasOpenAccess W259084889 @default.
• W259084889 hasPrimaryLocation W2590848891 @default.
• W259084889 hasRelatedWork W1975206529 @default.
• W259084889 hasRelatedWork W2015915379 @default.
• W259084889 hasRelatedWork W2354704048 @default.
• W259084889 hasRelatedWork W2388863227 @default.
• W259084889 hasRelatedWork W2527710048 @default.
• W259084889 hasRelatedWork W2787253449 @default.
• W259084889 hasRelatedWork W3091808392 @default.
• W259084889 hasRelatedWork W39878644 @default.
• W259084889 hasRelatedWork W4252609644 @default.
• W259084889 hasRelatedWork W2491803073 @default.
• W259084889 hasVolume "133" @default.
• W259084889 isParatext "false" @default.
• W259084889 isRetracted "false" @default.
• W259084889 magId "259084889" @default.
• W259084889 workType "article" @default.