In-situ observation of bubble trapping in polar firn

The air trapped in polar ice cores is not a direct record of past atmospheric composition but is strongly influenced by the process of firnification as bubbles are only sealed at a certain point, when the respective horizontal layer reaches a so called “critical” porosity. In order to investigate th...

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Main Authors: Schaller, Christoph Florian, Freitag, Johannes, Sowers, Todd, Vinther, Bo, Weinhart, Alexander, Eisen, Olaf
Format: Conference Object
Language:unknown
Published: 2017
Subjects:
Online Access:https://epic.awi.de/id/eprint/49628/
https://epic.awi.de/id/eprint/49628/1/EGU2017-14721-1.pdf
https://hdl.handle.net/10013/epic.05b61388-a40d-4e9d-968e-b76257565c78
id ftawi:oai:epic.awi.de:49628
record_format openpolar
spelling ftawi:oai:epic.awi.de:49628 2024-09-15T17:42:12+00:00 In-situ observation of bubble trapping in polar firn Schaller, Christoph Florian Freitag, Johannes Sowers, Todd Vinther, Bo Weinhart, Alexander Eisen, Olaf 2017-04-24 application/pdf https://epic.awi.de/id/eprint/49628/ https://epic.awi.de/id/eprint/49628/1/EGU2017-14721-1.pdf https://hdl.handle.net/10013/epic.05b61388-a40d-4e9d-968e-b76257565c78 unknown https://epic.awi.de/id/eprint/49628/1/EGU2017-14721-1.pdf Schaller, C. F. , Freitag, J. orcid:0000-0003-2654-9440 , Sowers, T. , Vinther, B. , Weinhart, A. orcid:0000-0003-2856-2630 and Eisen, O. orcid:0000-0002-6380-962X (2017) In-situ observation of bubble trapping in polar firn , EGU General Assembly, Vienna, 23 April 2017 - 28 April 2017 . hdl:10013/epic.05b61388-a40d-4e9d-968e-b76257565c78 EPIC3EGU General Assembly, Vienna, 2017-04-23-2017-04-28 Conference notRev 2017 ftawi 2024-06-24T04:22:11Z The air trapped in polar ice cores is not a direct record of past atmospheric composition but is strongly influenced by the process of firnification as bubbles are only sealed at a certain point, when the respective horizontal layer reaches a so called “critical” porosity. In order to investigate this process, we performed high-resolution (approximately 25μm) 3D-XCT measurements of the complete lock-in zone for two polar ice cores representing opposite extremes of the temperature and accumulation rate range: B53, close to Dome Fuji, East Antarctica and RECAP_S2, Renland, Greenland. For every 1m core segment, we scanned a minimum number of five sections of approximately 3.5cm height of the full core diameter with a focus on homogenous layers. This allows us to non-destructively deduce detailed profiles of open and closed porosity on a solid statistical basis. For each of the cores individually, we find that the trapping of bubbles in a single layer is solely determined by its total porosity and thereby independent of depth. We can confirm the existence of a distinct Schwander-type relation of closed and total porosity. Even though the two cores deviate from each other significantly in critical porosity, 0.0907 for B53 compared to 0.1025 for RECAP_S2, we observe many similarities. We hypothesize, that the determining factors of bubbletrapping are the average size and variability of pore space structures. This could potentially allow the reconstruction of past close-off porosities from the remaining pore structures in deep ice, e.g. from bubble number densities. Conference Object Antarc* Antarctica East Antarctica Greenland Alfred Wegener Institute for Polar- and Marine Research (AWI): ePIC (electronic Publication Information Center)
institution Open Polar
collection Alfred Wegener Institute for Polar- and Marine Research (AWI): ePIC (electronic Publication Information Center)
op_collection_id ftawi
language unknown
description The air trapped in polar ice cores is not a direct record of past atmospheric composition but is strongly influenced by the process of firnification as bubbles are only sealed at a certain point, when the respective horizontal layer reaches a so called “critical” porosity. In order to investigate this process, we performed high-resolution (approximately 25μm) 3D-XCT measurements of the complete lock-in zone for two polar ice cores representing opposite extremes of the temperature and accumulation rate range: B53, close to Dome Fuji, East Antarctica and RECAP_S2, Renland, Greenland. For every 1m core segment, we scanned a minimum number of five sections of approximately 3.5cm height of the full core diameter with a focus on homogenous layers. This allows us to non-destructively deduce detailed profiles of open and closed porosity on a solid statistical basis. For each of the cores individually, we find that the trapping of bubbles in a single layer is solely determined by its total porosity and thereby independent of depth. We can confirm the existence of a distinct Schwander-type relation of closed and total porosity. Even though the two cores deviate from each other significantly in critical porosity, 0.0907 for B53 compared to 0.1025 for RECAP_S2, we observe many similarities. We hypothesize, that the determining factors of bubbletrapping are the average size and variability of pore space structures. This could potentially allow the reconstruction of past close-off porosities from the remaining pore structures in deep ice, e.g. from bubble number densities.
format Conference Object
author Schaller, Christoph Florian
Freitag, Johannes
Sowers, Todd
Vinther, Bo
Weinhart, Alexander
Eisen, Olaf
spellingShingle Schaller, Christoph Florian
Freitag, Johannes
Sowers, Todd
Vinther, Bo
Weinhart, Alexander
Eisen, Olaf
In-situ observation of bubble trapping in polar firn
author_facet Schaller, Christoph Florian
Freitag, Johannes
Sowers, Todd
Vinther, Bo
Weinhart, Alexander
Eisen, Olaf
author_sort Schaller, Christoph Florian
title In-situ observation of bubble trapping in polar firn
title_short In-situ observation of bubble trapping in polar firn
title_full In-situ observation of bubble trapping in polar firn
title_fullStr In-situ observation of bubble trapping in polar firn
title_full_unstemmed In-situ observation of bubble trapping in polar firn
title_sort in-situ observation of bubble trapping in polar firn
publishDate 2017
url https://epic.awi.de/id/eprint/49628/
https://epic.awi.de/id/eprint/49628/1/EGU2017-14721-1.pdf
https://hdl.handle.net/10013/epic.05b61388-a40d-4e9d-968e-b76257565c78
genre Antarc*
Antarctica
East Antarctica
Greenland
genre_facet Antarc*
Antarctica
East Antarctica
Greenland
op_source EPIC3EGU General Assembly, Vienna, 2017-04-23-2017-04-28
op_relation https://epic.awi.de/id/eprint/49628/1/EGU2017-14721-1.pdf
Schaller, C. F. , Freitag, J. orcid:0000-0003-2654-9440 , Sowers, T. , Vinther, B. , Weinhart, A. orcid:0000-0003-2856-2630 and Eisen, O. orcid:0000-0002-6380-962X (2017) In-situ observation of bubble trapping in polar firn , EGU General Assembly, Vienna, 23 April 2017 - 28 April 2017 . hdl:10013/epic.05b61388-a40d-4e9d-968e-b76257565c78
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