دورية أكاديمية

Neodymium isotope analyses after combined extraction of actinide and lanthanide elements from seawater and deep‐sea coral aragonite

التفاصيل البيبلوغرافية
العنوان: Neodymium isotope analyses after combined extraction of actinide and lanthanide elements from seawater and deep‐sea coral aragonite
المؤلفون: Struve, Torben, Van De Flierdt, Tina, Robinson, Laura F., Bradtmiller, Louisa I., K. Hines, Sophia, Adkins, Jess F., Lambelet, Myriam, Crocket, Kirsty, Kreissig, Katharina, Coles, Barry, Auro, Maureen
المصدر: Struve , T , Van De Flierdt , T , Robinson , L F , Bradtmiller , L I , K. Hines , S , Adkins , J F , Lambelet , M , Crocket , K , Kreissig , K , Coles , B & Auro , M 2016 , ' Neodymium isotope analyses after combined extraction of actinide and lanthanide elements from seawater and deep‐sea coral aragonite ' , Geochemistry Geophysics Geosystems , vol. 17 , no. 1 , 10.1002/2015GC006130 , pp. 232-240 . https://doi.org/10.1002/2015GC006130Test
سنة النشر: 2016
المجموعة: University of the Highlands and Islands: Research Database of UHI
مصطلحات موضوعية: deep-sea corals, seawater, extraction methods, neodymium isotopes, GEOTRACES
الوصف: Isotopes of the actinide elements protactinium (Pa), thorium (Th), and uranium (U), and the lanthanide element neodymium (Nd) are often used as complementary tracers of modern and past oceanic processes. The extraction of such elements from low abundance matrices, such as seawater and carbonate, is however labor-intensive and requires significant amounts of sample material. We here present a combined method for the extraction of Pa, Th, and Nd from 5 to 10 L seawater samples, and of U, Th, and Nd from <1 g carbonate samples. Neodymium is collected in the respective wash fractions of Pa-Th and U-Th anion exchange chromatographies. Regardless of the original sample matrix, Nd is extracted during a two-stage ion chromatography, followed by thermal ionization mass spectrometry (TIMS) analysis as NdO+. Using this combined procedure, we obtained results for Nd isotopic compositions on two GEOTRACES consensus samples from Bermuda Atlantic Time Series (BATS), which are within error identical to results for separately sampled and processed dedicated Nd samples (εNd = −9.20 ± 0.21 and −13.11 ± 0.21 for 15 and 2000 m water depths, respectively; intercalibration results from 14 laboratories: εNd = −9.19 ± 0.57 and −13.14 ± 0.57). Furthermore, Nd isotope results for an in-house coral reference material are identical within analytical uncertainty for dedicated Nd chemistry and after collection of Nd from U-Th anion exchange chromatography. Our procedure does not require major adaptations to independently used ion exchange chromatographies for U-Pa-Th and Nd, and can hence be readily implemented for a wide range of applications.
نوع الوثيقة: article in journal/newspaper
وصف الملف: application/pdf
اللغة: English
العلاقة: https://pure.uhi.ac.uk/en/publications/f812747c-c227-4cec-a7b5-a68112dc0b59Test
DOI: 10.1002/2015GC006130
DOI: 10.1002/2015GC006130/full
الإتاحة: https://doi.org/10.1002/2015GC006130Test
https://pure.uhi.ac.uk/en/publications/f812747c-c227-4cec-a7b5-a68112dc0b59Test
https://pureadmin.uhi.ac.uk/ws/files/1892898/Struve_et_al_G3_submitted_4_Oct_15_1.pdfTest
حقوق: info:eu-repo/semantics/closedAccess
رقم الانضمام: edsbas.8E2CD614
قاعدة البيانات: BASE