(Figure 3) Sedimentological and biogeochemical analyses of outcrop PG2038-1 ...
X-ray diffractometry - For information about the mineral contents, the samples were ground and analysed by X-ray diffractometry (XRD) using a Panalytic Empyrean X-ray diffractometer. The mineral peak area intensities were determined graphically and calculated using Macdiff (Petschick 2012). Followin...
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ftdatacite:10.1594/pangaea.833692 2024-09-09T19:26:53+00:00 (Figure 3) Sedimentological and biogeochemical analyses of outcrop PG2038-1 ... Schleusner, Philipp Biskaborn, Boris K Kienast, Frank Wolter, Juliane Subetto, Dmitry A Diekmann, Bernhard 2015 text/tab-separated-values https://dx.doi.org/10.1594/pangaea.833692 https://doi.pangaea.de/10.1594/PANGAEA.833692 en eng PANGAEA https://dx.doi.org/10.1594/pangaea.833695 https://dx.doi.org/10.1111/bor.12084 Creative Commons Attribution 3.0 Unported https://creativecommons.org/licenses/by/3.0/legalcode cc-by-3.0 SibLake DEPTH, sediment/rock Stratigraphy Carbon, total Nitrogen, total Sulfur, total Carbon, organic, total Carbon, inorganic, total Carbonates Carbon, organic, total/Nitrogen, total ratio δ13C Grain size, mean Size fraction < 0.002 mm, clay Silt Sand Sorting Skewness Quartz/total intensity ratio Anorthite/total intensity ratio Illite/total intensity ratio Quartz/Feldspar ratio Grab Carbon and nitrogen and sulfur CNS isotope element analyzer, Elementar, Vario EL III Carbon and nitrogen and sulfur CNS isotope element analyzer, Elementar, Elementar Vario MAX Cube Calculated Mass spectrometer Finnigan Delta-S Beckman Coulter Laser diffraction particle size analyzer LS 200 X-ray diffraction XRD RU-Land_2010_Lena AWI Arctic Land Expedition Permafrost Research Periglacial Dynamics @ AWI AWI_PerDyn dataset Dataset 2015 ftdatacite https://doi.org/10.1594/pangaea.83369210.1594/pangaea.83369510.1111/bor.12084 2024-06-17T09:47:39Z X-ray diffractometry - For information about the mineral contents, the samples were ground and analysed by X-ray diffractometry (XRD) using a Panalytic Empyrean X-ray diffractometer. The mineral peak area intensities were determined graphically and calculated using Macdiff (Petschick 2012). Following Vogt (2009), the semi-quantitative mineral contents were determined by the ratio of the individual peak intensities against each other. Here we used the ratio of the quartz- and feldspar peaks, and the ratio of the illite peak against the total peak area intensities of all minerals (TI).Grain-size distribution - The samples were pretreated with acetic acid to remove the inorganic carbon. In order to destroy the organic compounds, a hydrogen peroxide treatment was conducted on a platform shaker, where ammonia was used for neutralization of the pH. The sample material was dispersed and homogenized on an overhead shaker using tetrasodium pyrophosphate. The grain-size distribution was measured using a Beckmann ... Dataset Arctic permafrost DataCite Arctic Coulter ENVELOPE(-58.033,-58.033,-83.283,-83.283) |
institution |
Open Polar |
collection |
DataCite |
op_collection_id |
ftdatacite |
language |
English |
topic |
SibLake DEPTH, sediment/rock Stratigraphy Carbon, total Nitrogen, total Sulfur, total Carbon, organic, total Carbon, inorganic, total Carbonates Carbon, organic, total/Nitrogen, total ratio δ13C Grain size, mean Size fraction < 0.002 mm, clay Silt Sand Sorting Skewness Quartz/total intensity ratio Anorthite/total intensity ratio Illite/total intensity ratio Quartz/Feldspar ratio Grab Carbon and nitrogen and sulfur CNS isotope element analyzer, Elementar, Vario EL III Carbon and nitrogen and sulfur CNS isotope element analyzer, Elementar, Elementar Vario MAX Cube Calculated Mass spectrometer Finnigan Delta-S Beckman Coulter Laser diffraction particle size analyzer LS 200 X-ray diffraction XRD RU-Land_2010_Lena AWI Arctic Land Expedition Permafrost Research Periglacial Dynamics @ AWI AWI_PerDyn |
spellingShingle |
SibLake DEPTH, sediment/rock Stratigraphy Carbon, total Nitrogen, total Sulfur, total Carbon, organic, total Carbon, inorganic, total Carbonates Carbon, organic, total/Nitrogen, total ratio δ13C Grain size, mean Size fraction < 0.002 mm, clay Silt Sand Sorting Skewness Quartz/total intensity ratio Anorthite/total intensity ratio Illite/total intensity ratio Quartz/Feldspar ratio Grab Carbon and nitrogen and sulfur CNS isotope element analyzer, Elementar, Vario EL III Carbon and nitrogen and sulfur CNS isotope element analyzer, Elementar, Elementar Vario MAX Cube Calculated Mass spectrometer Finnigan Delta-S Beckman Coulter Laser diffraction particle size analyzer LS 200 X-ray diffraction XRD RU-Land_2010_Lena AWI Arctic Land Expedition Permafrost Research Periglacial Dynamics @ AWI AWI_PerDyn Schleusner, Philipp Biskaborn, Boris K Kienast, Frank Wolter, Juliane Subetto, Dmitry A Diekmann, Bernhard (Figure 3) Sedimentological and biogeochemical analyses of outcrop PG2038-1 ... |
topic_facet |
SibLake DEPTH, sediment/rock Stratigraphy Carbon, total Nitrogen, total Sulfur, total Carbon, organic, total Carbon, inorganic, total Carbonates Carbon, organic, total/Nitrogen, total ratio δ13C Grain size, mean Size fraction < 0.002 mm, clay Silt Sand Sorting Skewness Quartz/total intensity ratio Anorthite/total intensity ratio Illite/total intensity ratio Quartz/Feldspar ratio Grab Carbon and nitrogen and sulfur CNS isotope element analyzer, Elementar, Vario EL III Carbon and nitrogen and sulfur CNS isotope element analyzer, Elementar, Elementar Vario MAX Cube Calculated Mass spectrometer Finnigan Delta-S Beckman Coulter Laser diffraction particle size analyzer LS 200 X-ray diffraction XRD RU-Land_2010_Lena AWI Arctic Land Expedition Permafrost Research Periglacial Dynamics @ AWI AWI_PerDyn |
description |
X-ray diffractometry - For information about the mineral contents, the samples were ground and analysed by X-ray diffractometry (XRD) using a Panalytic Empyrean X-ray diffractometer. The mineral peak area intensities were determined graphically and calculated using Macdiff (Petschick 2012). Following Vogt (2009), the semi-quantitative mineral contents were determined by the ratio of the individual peak intensities against each other. Here we used the ratio of the quartz- and feldspar peaks, and the ratio of the illite peak against the total peak area intensities of all minerals (TI).Grain-size distribution - The samples were pretreated with acetic acid to remove the inorganic carbon. In order to destroy the organic compounds, a hydrogen peroxide treatment was conducted on a platform shaker, where ammonia was used for neutralization of the pH. The sample material was dispersed and homogenized on an overhead shaker using tetrasodium pyrophosphate. The grain-size distribution was measured using a Beckmann ... |
format |
Dataset |
author |
Schleusner, Philipp Biskaborn, Boris K Kienast, Frank Wolter, Juliane Subetto, Dmitry A Diekmann, Bernhard |
author_facet |
Schleusner, Philipp Biskaborn, Boris K Kienast, Frank Wolter, Juliane Subetto, Dmitry A Diekmann, Bernhard |
author_sort |
Schleusner, Philipp |
title |
(Figure 3) Sedimentological and biogeochemical analyses of outcrop PG2038-1 ... |
title_short |
(Figure 3) Sedimentological and biogeochemical analyses of outcrop PG2038-1 ... |
title_full |
(Figure 3) Sedimentological and biogeochemical analyses of outcrop PG2038-1 ... |
title_fullStr |
(Figure 3) Sedimentological and biogeochemical analyses of outcrop PG2038-1 ... |
title_full_unstemmed |
(Figure 3) Sedimentological and biogeochemical analyses of outcrop PG2038-1 ... |
title_sort |
(figure 3) sedimentological and biogeochemical analyses of outcrop pg2038-1 ... |
publisher |
PANGAEA |
publishDate |
2015 |
url |
https://dx.doi.org/10.1594/pangaea.833692 https://doi.pangaea.de/10.1594/PANGAEA.833692 |
long_lat |
ENVELOPE(-58.033,-58.033,-83.283,-83.283) |
geographic |
Arctic Coulter |
geographic_facet |
Arctic Coulter |
genre |
Arctic permafrost |
genre_facet |
Arctic permafrost |
op_relation |
https://dx.doi.org/10.1594/pangaea.833695 https://dx.doi.org/10.1111/bor.12084 |
op_rights |
Creative Commons Attribution 3.0 Unported https://creativecommons.org/licenses/by/3.0/legalcode cc-by-3.0 |
op_doi |
https://doi.org/10.1594/pangaea.83369210.1594/pangaea.83369510.1111/bor.12084 |
_version_ |
1809896426475356160 |