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Bibliographic Details
Main Authors: Fritz, Michael, Laux, Kristoffer, Juhls, Bennet
Format: Dataset Open Access
Language:en
Published: PANGAEA 2025
Subjects:
Absorption coefficient, colored dissolved organic matter at 254 nm; Arctic; AWI Arctic Land Expedition; biogeochemistry; CA-Land_2019_ICE-01; CA-Land_2019_ICE-02; CA-Land_2019_ICE-03; CA-Land_2019_ICE-04; CA-Land_2019_ICE-05; CA-Land_2019_ICE-06; CA-Land_2019_ICE-07; CA-Land_2019_ICE-08; CA-Land_2019_ICE-09; CA-Land_2019_ICE-10; CA-Land_2019_ICE-11; CA-Land_2019_ICE-12; CA-Land_2019_YukonCoast_spring; Carbon, organic, dissolved; coloured dissolved organic matter (CDOM); Conductivity, electrical; DATE/TIME; Depth, bathymetric; DEPTH, ice/snow; Deuterium excess; dissolved organic carbon (DOC); Event label; Hydrogen isotopes; IC; Ice corer; LATITUDE; LONGITUDE; Mass spectrometer, Finnigan, Delta-S; NUNATARYUK; NUNATARYUK, Permafrost thaw and the changing Arctic coast, science for socioeconomic adaptation; Oxygen isotopes; Permafrost; Sample ID; Sea ice; Sea ice salinity; Sea ice thickness; Specific ultraviolet absorbance normalized to DOC, 254 nm, per mass carbon; stable water isotopes; Suspended particulate matter; Suspended Particulate Matter (SPM); Yukon_Coast_2019_spring; δ18O, ice; δ Deuterium, ice
Online Access:https://doi.org/10.1594/PANGAEA.984650
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Table of Contents:
  • Isotope analyses at AWI Potsdam were performed using DELTA-S Finnigan MAT mass spectrometers (USA) employing the equilibration method, described in Meyer et al. (2000). The isotope ratios are reported in per mil (‰) relative to the Vienna Standard Mean Ocean Water (VSMOW) as the international reference standard. In addition to the δ¹⁸O and δD values, the second-order parameter deuterium excess (d) was calculated according to the equation (after Dansgaard, 1964): d = δD − 8 × δ¹⁸O

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