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author Lin, Tsai-Wen
Nehrke, Gernot
Grotheer, Hendrik
Koch, Boris P
Mollenhauer, Gesine
author_facet Lin, Tsai-Wen
Nehrke, Gernot
Grotheer, Hendrik
Koch, Boris P
Mollenhauer, Gesine
collection Datos científicos de ciencias marinas y ambientales
contents This datasheet includes radiocarbon and thermogravimetric analysis (TGA) results of permafrost leachate from samples collected in the Lena Delta. The leaching protocol followed Ksionzek et al. (2018). Around 200 mg of dried sediment was leached in 20 mL deionized water for 24 hours at 4 °C, with intermittent shaking every 6−8 hours. The leachates were filtered through 0.7 μm GF/F filters, acidified to pH 2 using 37% HCl, and analyzed by high-temperature catalytic combustion (Shimadzu, TOC-VCPN). Pretreatment and measurement of radiocarbon analysis followed protocols in Mollenhauer et al. (2021). Freeze-dried leachates were wrapped into silver boats and converted into graphite targets using Elementar vario Isotope coupled to Ionplus AG, AGE-3. Radiocarbon isotopic ratios were measured using MICADAS at AWI, Bremerhaven. For TGA analysis, leachate samples of ~10 mg were analyzed in 70 μL aluminum oxide crucibles using a Mettler Toledo TGA/DSC 1. The samples were heated from 25 to 1000 °C at a rate of 10 °C min-1 under a constant argon flow of 20 mL min-1, following similar settings from Smeaton & Austin (2022). Following Lopez-Capel et al. (2006), weight loss between 200–400 °C is attributed to the decomposition of labile organic matter (OML), while weight loss between 400–650°C corresponds to the decomposition of recalcitrant and refractory organic matter (OMR). The percentage of labile organic matter (OML/OM) is calculated as [OML/(OML+OMR)]*100%
format Dataset Open Access
id pangaea_https___doi_org_10_1594_PANGAEA_984752
institution PANGAEA
language en
publishDate 2025
publisher PANGAEA
record_format pangaea
spellingShingle Radiocarbon and thermogravimetric analysis (TGA) results of permafrost leachate from the Lena Delta, Arctic
Lin, Tsai-Wen
Nehrke, Gernot
Grotheer, Hendrik
Koch, Boris P
Mollenhauer, Gesine
Arctic; AWI Arctic Land Expedition; CAC19-Y; CAC19-Y1; Calculated; Carbon, organic, dissolved, water extractable, per unit mass total organic carbon; Comment; DEPTH, sediment/rock; DRILL; Drilling/drill rig; Event label; F14C; Fraction modern carbon; Fraction modern carbon, error; High-temperature catalytic combustion, Shimadzu, Shimadzu TOC-VCPH; labile OM; Lena 2018; Lena 2019; Lena Delta; Lena Delta, Siberia; Mini Carbon Dating System (MICADAS); OML; OMR; Organic matter, labile; Organic matter, labile, per unit sediment mass; Organic matter, recalcitrant and refractory, per unit sediment mass; permafrost; permafrost leachate; refractory and recalcitrant OM; RU-Land_2018_Lena; RU-Land_2019_Lena; SAM18-01; SOIL; Soil profile; TGA; thermogravimetric analysis; Thermogravimetric analyzer (TGA) and differential scanning calorimeter (DSC), Mettler Toledo, TGA/DSC 1
This datasheet includes radiocarbon and thermogravimetric analysis (TGA) results of permafrost leachate from samples collected in the Lena Delta. The leaching protocol followed Ksionzek et al. (2018). Around 200 mg of dried sediment was leached in 20 mL deionized water for 24 hours at 4 °C, with intermittent shaking every 6−8 hours. The leachates were filtered through 0.7 μm GF/F filters, acidified to pH 2 using 37% HCl, and analyzed by high-temperature catalytic combustion (Shimadzu, TOC-VCPN). Pretreatment and measurement of radiocarbon analysis followed protocols in Mollenhauer et al. (2021). Freeze-dried leachates were wrapped into silver boats and converted into graphite targets using Elementar vario Isotope coupled to Ionplus AG, AGE-3. Radiocarbon isotopic ratios were measured using MICADAS at AWI, Bremerhaven. For TGA analysis, leachate samples of ~10 mg were analyzed in 70 μL aluminum oxide crucibles using a Mettler Toledo TGA/DSC 1. The samples were heated from 25 to 1000 °C at a rate of 10 °C min-1 under a constant argon flow of 20 mL min-1, following similar settings from Smeaton & Austin (2022). Following Lopez-Capel et al. (2006), weight loss between 200–400 °C is attributed to the decomposition of labile organic matter (OML), while weight loss between 400–650°C corresponds to the decomposition of recalcitrant and refractory organic matter (OMR). The percentage of labile organic matter (OML/OM) is calculated as [OML/(OML+OMR)]*100%
title Radiocarbon and thermogravimetric analysis (TGA) results of permafrost leachate from the Lena Delta, Arctic
topic Arctic; AWI Arctic Land Expedition; CAC19-Y; CAC19-Y1; Calculated; Carbon, organic, dissolved, water extractable, per unit mass total organic carbon; Comment; DEPTH, sediment/rock; DRILL; Drilling/drill rig; Event label; F14C; Fraction modern carbon; Fraction modern carbon, error; High-temperature catalytic combustion, Shimadzu, Shimadzu TOC-VCPH; labile OM; Lena 2018; Lena 2019; Lena Delta; Lena Delta, Siberia; Mini Carbon Dating System (MICADAS); OML; OMR; Organic matter, labile; Organic matter, labile, per unit sediment mass; Organic matter, recalcitrant and refractory, per unit sediment mass; permafrost; permafrost leachate; refractory and recalcitrant OM; RU-Land_2018_Lena; RU-Land_2019_Lena; SAM18-01; SOIL; Soil profile; TGA; thermogravimetric analysis; Thermogravimetric analyzer (TGA) and differential scanning calorimeter (DSC), Mettler Toledo, TGA/DSC 1
url https://doi.org/10.1594/PANGAEA.984752