Granulometry of sediments collected by differently inclined sediment traps in Comau Fjord ...

The meltwater reaching Chile's Comau Fjord carries glacial sediment, resulting in a high sediment input in the fjord system. To record the sedimentary material, sediment traps (0.5 m long PVC pipes closed at the bottom end, diameter 0.05 m) were attached at different angles of inclination to la...

Full description

Bibliographic Details
Main Authors: Gottschlich, Svantje, Laudien, Jürgen, Häussermann, Verena, Försterra, Günter
Format: Dataset
Language:English
Published: PANGAEA 2023
Subjects:
Online Access:https://dx.doi.org/10.1594/pangaea.955324
https://doi.pangaea.de/10.1594/PANGAEA.955324
id ftdatacite:10.1594/pangaea.955324
record_format openpolar
institution Open Polar
collection DataCite Metadata Store (German National Library of Science and Technology)
op_collection_id ftdatacite
language English
topic granulometry
sediment analysis
Sediment trap ID
Angle range, degrees
Size fraction < 0.040 µm, >14.6 phi
Size fraction 0.043-0.040 µm, 14.5-14.6 phi
Size fraction 0.046-0.043 µm, 14.4-14.5 phi
Size fraction 0.050-0.046 µm, 14.3-14.4 phi
Size fraction 0.053-0.050 µm, 14.2-14.3 phi
Size fraction 0.057-0.053 µm, 14.1-14.2 phi
Size fraction 0.061-0.057 µm, 14.0-14.1 phi
Size fraction 0.065-0.061 µm, 13.9-14.0 phi
Size fraction 0.070-0.065 µm, 13.8-13.9 phi
Size fraction 0.075-0.070 µm, 13.7-13.8 phi
Size fraction 0.081-0.075 µm, 13.6-13.7 phi
Size fraction 0.086-0.081 µm, 13.5-13.6 phi
Size fraction 0.093-0.086 µm, 13.4-13.5 phi
Size fraction 0.099-0.093 µm, 13.3-13.4 phi
Size fraction 0.106-0.099 µm, 13.2-13.3 phi
Size fraction 0.114-0.106 µm, 13.1-13.2 phi
Size fraction 0.122-0.114 µm, 13.0-13.1 phi
Size fraction 0.131-0.122 µm, 12.9-13.0 phi
Size fraction 0.140-0.131 µm, 12.8-12.9 phi
Size fraction 0.150-0.140 µm, 12.7-12.8 phi
Size fraction 0.161-0.150 µm, 12.6-12.7 phi
Size fraction 0.173-0.161 µm, 12.5-12.6 phi
Size fraction 0.185-0.173 µm, 12.4-12.5 phi
Size fraction 0.198-0.185 µm, 12.3-12.4 phi
Size fraction 0.213-0.198 µm, 12.2-12.3 phi
Size fraction 0.228-0.213 µm, 12.1-12.2 phi
Size fraction 0.244-0.228 µm, 12.0-12.1 phi
Size fraction 0.262-0.244 µm, 11.9-12.0 phi
Size fraction 0.280-0.262 µm, 11.8-11.9 phi
Size fraction 0.301-0.280 µm, 11.7-11.8 phi
Size fraction 0.322-0.301 µm, 11.6-11.7 phi
Size fraction 0.345-0.322 µm, 11.5-11.6 phi
Size fraction 0.370-0.345 µm, 11.4-11.5 phi
Size fraction 0.397-0.370 µm, 11.3-11.4 phi
Size fraction 0.425-0.397 µm, 11.2-11.3 phi
Size fraction 0.456-0.425 µm, 11.1-11.2 phi
Size fraction 0.488-0.456 µm, 11.0-11.1 phi
Size fraction 0.523-0.488 µm, 10.9-11.0 phi
Size fraction 0.561-0.523 µm, 10.8-10.9 phi
Size fraction 0.601-0.561 µm, 10.7-10.8 phi
Size fraction 0.644-0.601 µm, 10.6-10.7 phi
Size fraction 0.691-0.644 µm, 10.5-10.6 phi
Size fraction 0.740-0.691 µm, 10.4-10.5 phi
Size fraction 0.793-0.740 µm, 10.3-10.4 phi
Size fraction 0.850-0.793 µm, 10.2-10.3 phi
Size fraction 0.911-0.850 µm, 10.1-10.2 phi
spellingShingle granulometry
sediment analysis
Sediment trap ID
Angle range, degrees
Size fraction < 0.040 µm, >14.6 phi
Size fraction 0.043-0.040 µm, 14.5-14.6 phi
Size fraction 0.046-0.043 µm, 14.4-14.5 phi
Size fraction 0.050-0.046 µm, 14.3-14.4 phi
Size fraction 0.053-0.050 µm, 14.2-14.3 phi
Size fraction 0.057-0.053 µm, 14.1-14.2 phi
Size fraction 0.061-0.057 µm, 14.0-14.1 phi
Size fraction 0.065-0.061 µm, 13.9-14.0 phi
Size fraction 0.070-0.065 µm, 13.8-13.9 phi
Size fraction 0.075-0.070 µm, 13.7-13.8 phi
Size fraction 0.081-0.075 µm, 13.6-13.7 phi
Size fraction 0.086-0.081 µm, 13.5-13.6 phi
Size fraction 0.093-0.086 µm, 13.4-13.5 phi
Size fraction 0.099-0.093 µm, 13.3-13.4 phi
Size fraction 0.106-0.099 µm, 13.2-13.3 phi
Size fraction 0.114-0.106 µm, 13.1-13.2 phi
Size fraction 0.122-0.114 µm, 13.0-13.1 phi
Size fraction 0.131-0.122 µm, 12.9-13.0 phi
Size fraction 0.140-0.131 µm, 12.8-12.9 phi
Size fraction 0.150-0.140 µm, 12.7-12.8 phi
Size fraction 0.161-0.150 µm, 12.6-12.7 phi
Size fraction 0.173-0.161 µm, 12.5-12.6 phi
Size fraction 0.185-0.173 µm, 12.4-12.5 phi
Size fraction 0.198-0.185 µm, 12.3-12.4 phi
Size fraction 0.213-0.198 µm, 12.2-12.3 phi
Size fraction 0.228-0.213 µm, 12.1-12.2 phi
Size fraction 0.244-0.228 µm, 12.0-12.1 phi
Size fraction 0.262-0.244 µm, 11.9-12.0 phi
Size fraction 0.280-0.262 µm, 11.8-11.9 phi
Size fraction 0.301-0.280 µm, 11.7-11.8 phi
Size fraction 0.322-0.301 µm, 11.6-11.7 phi
Size fraction 0.345-0.322 µm, 11.5-11.6 phi
Size fraction 0.370-0.345 µm, 11.4-11.5 phi
Size fraction 0.397-0.370 µm, 11.3-11.4 phi
Size fraction 0.425-0.397 µm, 11.2-11.3 phi
Size fraction 0.456-0.425 µm, 11.1-11.2 phi
Size fraction 0.488-0.456 µm, 11.0-11.1 phi
Size fraction 0.523-0.488 µm, 10.9-11.0 phi
Size fraction 0.561-0.523 µm, 10.8-10.9 phi
Size fraction 0.601-0.561 µm, 10.7-10.8 phi
Size fraction 0.644-0.601 µm, 10.6-10.7 phi
Size fraction 0.691-0.644 µm, 10.5-10.6 phi
Size fraction 0.740-0.691 µm, 10.4-10.5 phi
Size fraction 0.793-0.740 µm, 10.3-10.4 phi
Size fraction 0.850-0.793 µm, 10.2-10.3 phi
Size fraction 0.911-0.850 µm, 10.1-10.2 phi
Gottschlich, Svantje
Laudien, Jürgen
Häussermann, Verena
Försterra, Günter
Granulometry of sediments collected by differently inclined sediment traps in Comau Fjord ...
topic_facet granulometry
sediment analysis
Sediment trap ID
Angle range, degrees
Size fraction < 0.040 µm, >14.6 phi
Size fraction 0.043-0.040 µm, 14.5-14.6 phi
Size fraction 0.046-0.043 µm, 14.4-14.5 phi
Size fraction 0.050-0.046 µm, 14.3-14.4 phi
Size fraction 0.053-0.050 µm, 14.2-14.3 phi
Size fraction 0.057-0.053 µm, 14.1-14.2 phi
Size fraction 0.061-0.057 µm, 14.0-14.1 phi
Size fraction 0.065-0.061 µm, 13.9-14.0 phi
Size fraction 0.070-0.065 µm, 13.8-13.9 phi
Size fraction 0.075-0.070 µm, 13.7-13.8 phi
Size fraction 0.081-0.075 µm, 13.6-13.7 phi
Size fraction 0.086-0.081 µm, 13.5-13.6 phi
Size fraction 0.093-0.086 µm, 13.4-13.5 phi
Size fraction 0.099-0.093 µm, 13.3-13.4 phi
Size fraction 0.106-0.099 µm, 13.2-13.3 phi
Size fraction 0.114-0.106 µm, 13.1-13.2 phi
Size fraction 0.122-0.114 µm, 13.0-13.1 phi
Size fraction 0.131-0.122 µm, 12.9-13.0 phi
Size fraction 0.140-0.131 µm, 12.8-12.9 phi
Size fraction 0.150-0.140 µm, 12.7-12.8 phi
Size fraction 0.161-0.150 µm, 12.6-12.7 phi
Size fraction 0.173-0.161 µm, 12.5-12.6 phi
Size fraction 0.185-0.173 µm, 12.4-12.5 phi
Size fraction 0.198-0.185 µm, 12.3-12.4 phi
Size fraction 0.213-0.198 µm, 12.2-12.3 phi
Size fraction 0.228-0.213 µm, 12.1-12.2 phi
Size fraction 0.244-0.228 µm, 12.0-12.1 phi
Size fraction 0.262-0.244 µm, 11.9-12.0 phi
Size fraction 0.280-0.262 µm, 11.8-11.9 phi
Size fraction 0.301-0.280 µm, 11.7-11.8 phi
Size fraction 0.322-0.301 µm, 11.6-11.7 phi
Size fraction 0.345-0.322 µm, 11.5-11.6 phi
Size fraction 0.370-0.345 µm, 11.4-11.5 phi
Size fraction 0.397-0.370 µm, 11.3-11.4 phi
Size fraction 0.425-0.397 µm, 11.2-11.3 phi
Size fraction 0.456-0.425 µm, 11.1-11.2 phi
Size fraction 0.488-0.456 µm, 11.0-11.1 phi
Size fraction 0.523-0.488 µm, 10.9-11.0 phi
Size fraction 0.561-0.523 µm, 10.8-10.9 phi
Size fraction 0.601-0.561 µm, 10.7-10.8 phi
Size fraction 0.644-0.601 µm, 10.6-10.7 phi
Size fraction 0.691-0.644 µm, 10.5-10.6 phi
Size fraction 0.740-0.691 µm, 10.4-10.5 phi
Size fraction 0.793-0.740 µm, 10.3-10.4 phi
Size fraction 0.850-0.793 µm, 10.2-10.3 phi
Size fraction 0.911-0.850 µm, 10.1-10.2 phi
description The meltwater reaching Chile's Comau Fjord carries glacial sediment, resulting in a high sediment input in the fjord system. To record the sedimentary material, sediment traps (0.5 m long PVC pipes closed at the bottom end, diameter 0.05 m) were attached at different angles of inclination to large concrete pipes with screw clamps. After four weeks, these were sealed and recovered by research divers. The sediment was transferred to vessels for sedimentation and the clear supernatant was removed 48 hours later. The remaining sediment-seawater mixture was fixed with formol (final concentration 4%). Samples were treated with hydrogen peroxide and acetic acid to remove organic content. For particle size determination, samples were analysed using a Laser Particle Analyser (Cilias, Quantachrome Cilas 1180 Particle Analyser, Orleans, France). In this method, the grain size is measured based on the different diffraction of a laser beam on the particles. The evaluation of the laser granulometry took place using ... : Data are given in volume percentage; samples treated with hydrogen peroxide and acetic acid; error is < 1%. This dataset was generated in the frame of the co-operation between the Huinay Scientific Field Station (http://www.huinay.cl) and the Alfred Wegener Institute, Helmholtz Center for Polar and Marine Research (http://www.awi.de). ...
format Dataset
author Gottschlich, Svantje
Laudien, Jürgen
Häussermann, Verena
Försterra, Günter
author_facet Gottschlich, Svantje
Laudien, Jürgen
Häussermann, Verena
Försterra, Günter
author_sort Gottschlich, Svantje
title Granulometry of sediments collected by differently inclined sediment traps in Comau Fjord ...
title_short Granulometry of sediments collected by differently inclined sediment traps in Comau Fjord ...
title_full Granulometry of sediments collected by differently inclined sediment traps in Comau Fjord ...
title_fullStr Granulometry of sediments collected by differently inclined sediment traps in Comau Fjord ...
title_full_unstemmed Granulometry of sediments collected by differently inclined sediment traps in Comau Fjord ...
title_sort granulometry of sediments collected by differently inclined sediment traps in comau fjord ...
publisher PANGAEA
publishDate 2023
url https://dx.doi.org/10.1594/pangaea.955324
https://doi.pangaea.de/10.1594/PANGAEA.955324
genre Alfred Wegener Institute
genre_facet Alfred Wegener Institute
op_relation https://dx.doi.org/10.1594/pangaea.841459
op_rights Creative Commons Attribution 4.0 International
https://creativecommons.org/licenses/by/4.0/legalcode
cc-by-4.0
op_doi https://doi.org/10.1594/pangaea.95532410.1594/pangaea.841459
_version_ 1797574767595749376
spelling ftdatacite:10.1594/pangaea.955324 2024-04-28T07:54:04+00:00 Granulometry of sediments collected by differently inclined sediment traps in Comau Fjord ... Gottschlich, Svantje Laudien, Jürgen Häussermann, Verena Försterra, Günter 2023 text/tab-separated-values https://dx.doi.org/10.1594/pangaea.955324 https://doi.pangaea.de/10.1594/PANGAEA.955324 en eng PANGAEA https://dx.doi.org/10.1594/pangaea.841459 Creative Commons Attribution 4.0 International https://creativecommons.org/licenses/by/4.0/legalcode cc-by-4.0 granulometry sediment analysis Sediment trap ID Angle range, degrees Size fraction < 0.040 µm, >14.6 phi Size fraction 0.043-0.040 µm, 14.5-14.6 phi Size fraction 0.046-0.043 µm, 14.4-14.5 phi Size fraction 0.050-0.046 µm, 14.3-14.4 phi Size fraction 0.053-0.050 µm, 14.2-14.3 phi Size fraction 0.057-0.053 µm, 14.1-14.2 phi Size fraction 0.061-0.057 µm, 14.0-14.1 phi Size fraction 0.065-0.061 µm, 13.9-14.0 phi Size fraction 0.070-0.065 µm, 13.8-13.9 phi Size fraction 0.075-0.070 µm, 13.7-13.8 phi Size fraction 0.081-0.075 µm, 13.6-13.7 phi Size fraction 0.086-0.081 µm, 13.5-13.6 phi Size fraction 0.093-0.086 µm, 13.4-13.5 phi Size fraction 0.099-0.093 µm, 13.3-13.4 phi Size fraction 0.106-0.099 µm, 13.2-13.3 phi Size fraction 0.114-0.106 µm, 13.1-13.2 phi Size fraction 0.122-0.114 µm, 13.0-13.1 phi Size fraction 0.131-0.122 µm, 12.9-13.0 phi Size fraction 0.140-0.131 µm, 12.8-12.9 phi Size fraction 0.150-0.140 µm, 12.7-12.8 phi Size fraction 0.161-0.150 µm, 12.6-12.7 phi Size fraction 0.173-0.161 µm, 12.5-12.6 phi Size fraction 0.185-0.173 µm, 12.4-12.5 phi Size fraction 0.198-0.185 µm, 12.3-12.4 phi Size fraction 0.213-0.198 µm, 12.2-12.3 phi Size fraction 0.228-0.213 µm, 12.1-12.2 phi Size fraction 0.244-0.228 µm, 12.0-12.1 phi Size fraction 0.262-0.244 µm, 11.9-12.0 phi Size fraction 0.280-0.262 µm, 11.8-11.9 phi Size fraction 0.301-0.280 µm, 11.7-11.8 phi Size fraction 0.322-0.301 µm, 11.6-11.7 phi Size fraction 0.345-0.322 µm, 11.5-11.6 phi Size fraction 0.370-0.345 µm, 11.4-11.5 phi Size fraction 0.397-0.370 µm, 11.3-11.4 phi Size fraction 0.425-0.397 µm, 11.2-11.3 phi Size fraction 0.456-0.425 µm, 11.1-11.2 phi Size fraction 0.488-0.456 µm, 11.0-11.1 phi Size fraction 0.523-0.488 µm, 10.9-11.0 phi Size fraction 0.561-0.523 µm, 10.8-10.9 phi Size fraction 0.601-0.561 µm, 10.7-10.8 phi Size fraction 0.644-0.601 µm, 10.6-10.7 phi Size fraction 0.691-0.644 µm, 10.5-10.6 phi Size fraction 0.740-0.691 µm, 10.4-10.5 phi Size fraction 0.793-0.740 µm, 10.3-10.4 phi Size fraction 0.850-0.793 µm, 10.2-10.3 phi Size fraction 0.911-0.850 µm, 10.1-10.2 phi dataset Dataset 2023 ftdatacite https://doi.org/10.1594/pangaea.95532410.1594/pangaea.841459 2024-04-02T09:48:38Z The meltwater reaching Chile's Comau Fjord carries glacial sediment, resulting in a high sediment input in the fjord system. To record the sedimentary material, sediment traps (0.5 m long PVC pipes closed at the bottom end, diameter 0.05 m) were attached at different angles of inclination to large concrete pipes with screw clamps. After four weeks, these were sealed and recovered by research divers. The sediment was transferred to vessels for sedimentation and the clear supernatant was removed 48 hours later. The remaining sediment-seawater mixture was fixed with formol (final concentration 4%). Samples were treated with hydrogen peroxide and acetic acid to remove organic content. For particle size determination, samples were analysed using a Laser Particle Analyser (Cilias, Quantachrome Cilas 1180 Particle Analyser, Orleans, France). In this method, the grain size is measured based on the different diffraction of a laser beam on the particles. The evaluation of the laser granulometry took place using ... : Data are given in volume percentage; samples treated with hydrogen peroxide and acetic acid; error is < 1%. This dataset was generated in the frame of the co-operation between the Huinay Scientific Field Station (http://www.huinay.cl) and the Alfred Wegener Institute, Helmholtz Center for Polar and Marine Research (http://www.awi.de). ... Dataset Alfred Wegener Institute DataCite Metadata Store (German National Library of Science and Technology)