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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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) |
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Alfred Wegener Institute for Polar- and Marine Research (AWI): ePIC (electronic Publication Information Center) |
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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 |
_version_ |
1810488699095351296 |