Matches in SemOpenAlex for { <https://semopenalex.org/work/W2597505989> ?p ?o ?g. }
- W2597505989 endingPage "45" @default.
- W2597505989 startingPage "35" @default.
- W2597505989 abstract "Serpentine soils have elevated concentrations of trace metals including nickel, cobalt, and chromium compared to non-serpentine soils. Identifying the nickel bearing minerals allows for prediction of potential mobility of nickel. Synchrotron-based techniques can identify the solid-phase chemical forms of nickel with minimal sample treatment. Element concentrations are known to vary among soil particle sizes in serpentine soils. Sonication is a useful method to physically disperse sand, silt and clay particles in soils. Synchrotron-based techniques and sonication were employed to identify nickel species in discrete particle size fractions in several serpentine (ultramafic) topsoils to better understand solid-phase nickel geochemistry. Nickel commonly resided in primary serpentine parent material such as layered-phyllosilicate and chain-inosilicate minerals and was associated with iron oxides. In the clay fractions, nickel was associated with iron oxides and primary serpentine minerals, such as lizardite. Linear combination fitting (LCF) was used to characterize nickel species. Total metal concentration did not correlate with nickel speciation and is not an indicator of the major nickel species in the soil. Differences in soil texture were related to different nickel speciation for several particle size fractionated samples. A discussion on LCF illustrates the importance of choosing standards based not only on statistical methods such as Target Transformation but also on sample mineralogy and particle size. Results from the F-test (Hamilton test), which is an underutilized tool in the literature for LCF in soils, highlight its usefulness to determine the appropriate number of standards to for LCF. EXAFS shell fitting illustrates that destructive interference commonly found for light and heavy elements in layered double hydroxides and in phyllosilicates also can occur in inosilicate minerals, causing similar structural features and leading to false positive results in LCF." @default.
- W2597505989 created "2017-04-07" @default.
- W2597505989 creator A5004701262 @default.
- W2597505989 creator A5037434079 @default.
- W2597505989 creator A5084857922 @default.
- W2597505989 date "2017-07-01" @default.
- W2597505989 modified "2023-09-26" @default.
- W2597505989 title "Nickel speciation in several serpentine (ultramafic) topsoils via bulk synchrotron-based techniques" @default.
- W2597505989 cites W1966366969 @default.
- W2597505989 cites W1972761036 @default.
- W2597505989 cites W1985234731 @default.
- W2597505989 cites W1985654479 @default.
- W2597505989 cites W1988977715 @default.
- W2597505989 cites W1993596116 @default.
- W2597505989 cites W1995136139 @default.
- W2597505989 cites W1999802494 @default.
- W2597505989 cites W2002207351 @default.
- W2597505989 cites W2002877849 @default.
- W2597505989 cites W2004272142 @default.
- W2597505989 cites W2004624603 @default.
- W2597505989 cites W2014552610 @default.
- W2597505989 cites W2017214802 @default.
- W2597505989 cites W2025532608 @default.
- W2597505989 cites W2028131066 @default.
- W2597505989 cites W2029855766 @default.
- W2597505989 cites W2031118270 @default.
- W2597505989 cites W2035828895 @default.
- W2597505989 cites W2046049141 @default.
- W2597505989 cites W2055188225 @default.
- W2597505989 cites W2066314695 @default.
- W2597505989 cites W2071278571 @default.
- W2597505989 cites W2073825873 @default.
- W2597505989 cites W2074017132 @default.
- W2597505989 cites W2075207600 @default.
- W2597505989 cites W2077412628 @default.
- W2597505989 cites W2078421810 @default.
- W2597505989 cites W2080955605 @default.
- W2597505989 cites W2083894805 @default.
- W2597505989 cites W2084093827 @default.
- W2597505989 cites W2085216938 @default.
- W2597505989 cites W2089098203 @default.
- W2597505989 cites W2089892742 @default.
- W2597505989 cites W2095361501 @default.
- W2597505989 cites W2095539356 @default.
- W2597505989 cites W2101565783 @default.
- W2597505989 cites W2108376374 @default.
- W2597505989 cites W2116535007 @default.
- W2597505989 cites W2139346975 @default.
- W2597505989 cites W2140777719 @default.
- W2597505989 cites W2141796847 @default.
- W2597505989 cites W2146728676 @default.
- W2597505989 cites W2156357930 @default.
- W2597505989 cites W2162059183 @default.
- W2597505989 cites W2163423183 @default.
- W2597505989 cites W2166742259 @default.
- W2597505989 cites W2243650506 @default.
- W2597505989 cites W2318367266 @default.
- W2597505989 doi "https://doi.org/10.1016/j.geoderma.2017.03.008" @default.
- W2597505989 hasPublicationYear "2017" @default.
- W2597505989 type Work @default.
- W2597505989 sameAs 2597505989 @default.
- W2597505989 citedByCount "23" @default.
- W2597505989 countsByYear W25975059892017 @default.
- W2597505989 countsByYear W25975059892018 @default.
- W2597505989 countsByYear W25975059892019 @default.
- W2597505989 countsByYear W25975059892020 @default.
- W2597505989 countsByYear W25975059892021 @default.
- W2597505989 countsByYear W25975059892022 @default.
- W2597505989 countsByYear W25975059892023 @default.
- W2597505989 crossrefType "journal-article" @default.
- W2597505989 hasAuthorship W2597505989A5004701262 @default.
- W2597505989 hasAuthorship W2597505989A5037434079 @default.
- W2597505989 hasAuthorship W2597505989A5084857922 @default.
- W2597505989 hasBestOaLocation W25975059891 @default.
- W2597505989 hasConcept C107872376 @default.
- W2597505989 hasConcept C127313418 @default.
- W2597505989 hasConcept C159390177 @default.
- W2597505989 hasConcept C159750122 @default.
- W2597505989 hasConcept C17409809 @default.
- W2597505989 hasConcept C185592680 @default.
- W2597505989 hasConcept C191897082 @default.
- W2597505989 hasConcept C192562407 @default.
- W2597505989 hasConcept C195081551 @default.
- W2597505989 hasConcept C199289684 @default.
- W2597505989 hasConcept C2777612664 @default.
- W2597505989 hasConcept C504270822 @default.
- W2597505989 hasConcept C544153396 @default.
- W2597505989 hasConceptScore W2597505989C107872376 @default.
- W2597505989 hasConceptScore W2597505989C127313418 @default.
- W2597505989 hasConceptScore W2597505989C159390177 @default.
- W2597505989 hasConceptScore W2597505989C159750122 @default.
- W2597505989 hasConceptScore W2597505989C17409809 @default.
- W2597505989 hasConceptScore W2597505989C185592680 @default.
- W2597505989 hasConceptScore W2597505989C191897082 @default.
- W2597505989 hasConceptScore W2597505989C192562407 @default.
- W2597505989 hasConceptScore W2597505989C195081551 @default.
- W2597505989 hasConceptScore W2597505989C199289684 @default.
- W2597505989 hasConceptScore W2597505989C2777612664 @default.