In Situ X-Ray-micro-tomography of snow at the EPICA-Drill Site Dronning Maud Land (DML) Antarctica

The firnificaton of dry polar firn has been investigated with the means of X-ray micro-computer tomography (CT). The measurements were carried out on shallow firn cores and snow pit samples during the field campaign 2005/2006 at the EPICA (European Project of Ice Coring in Antarctica) DML-drill site...

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Main Authors: Freitag, Johannes, Kipfstuhl, Sepp, Faria, S.
Format: Conference Object
Language:unknown
Published: 2007
Subjects:
DML
Online Access:https://epic.awi.de/id/eprint/17546/
https://hdl.handle.net/10013/epic.27906
id ftawi:oai:epic.awi.de:17546
record_format openpolar
spelling ftawi:oai:epic.awi.de:17546 2024-09-15T17:46:35+00:00 In Situ X-Ray-micro-tomography of snow at the EPICA-Drill Site Dronning Maud Land (DML) Antarctica Freitag, Johannes Kipfstuhl, Sepp Faria, S. 2007 https://epic.awi.de/id/eprint/17546/ https://hdl.handle.net/10013/epic.27906 unknown Freitag, J. orcid:0000-0003-2654-9440 , Kipfstuhl, S. and Faria, S. (2007) In Situ X-Ray-micro-tomography of snow at the EPICA-Drill Site Dronning Maud Land (DML) Antarctica , EGU ViennaApril 2007. . hdl:10013/epic.27906 EPIC3EGU ViennaApril 2007., 15 Conference notRev 2007 ftawi 2024-06-24T04:00:13Z The firnificaton of dry polar firn has been investigated with the means of X-ray micro-computer tomography (CT). The measurements were carried out on shallow firn cores and snow pit samples during the field campaign 2005/2006 at the EPICA (European Project of Ice Coring in Antarctica) DML-drill site, Antarctica. The CT-devices have been successfully tested in the field and offered us a novel method to study the fragile three dimensional structures of deposited snow and firn. Several events of dune formation have been observed during the summer campaign. The dunes are well preserved in the deeper snow with the consequence of highly stratified firn. In this presentation we give a detailed description of stratigraphy with the focus on the evolution of pore/ice cluster sizes and intergranular bonding. We show that the number of bonds per cluster in samples near the surface is highly correlated to their respective density. Accordingly, the neck radii are anticorrelated to the density. Maxima of pore size and anisotropy are observed at 2 to 3 meter depth where the metamorphism is dominated by temperature gradients. To highlight the methodological aspect we present different size parametrisations and discuss the three dimensional CT- approach in relation to the standard two dimensional techniques. Conference Object Antarc* Antarctica DML Dronning Maud Land EPICA 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 firnificaton of dry polar firn has been investigated with the means of X-ray micro-computer tomography (CT). The measurements were carried out on shallow firn cores and snow pit samples during the field campaign 2005/2006 at the EPICA (European Project of Ice Coring in Antarctica) DML-drill site, Antarctica. The CT-devices have been successfully tested in the field and offered us a novel method to study the fragile three dimensional structures of deposited snow and firn. Several events of dune formation have been observed during the summer campaign. The dunes are well preserved in the deeper snow with the consequence of highly stratified firn. In this presentation we give a detailed description of stratigraphy with the focus on the evolution of pore/ice cluster sizes and intergranular bonding. We show that the number of bonds per cluster in samples near the surface is highly correlated to their respective density. Accordingly, the neck radii are anticorrelated to the density. Maxima of pore size and anisotropy are observed at 2 to 3 meter depth where the metamorphism is dominated by temperature gradients. To highlight the methodological aspect we present different size parametrisations and discuss the three dimensional CT- approach in relation to the standard two dimensional techniques.
format Conference Object
author Freitag, Johannes
Kipfstuhl, Sepp
Faria, S.
spellingShingle Freitag, Johannes
Kipfstuhl, Sepp
Faria, S.
In Situ X-Ray-micro-tomography of snow at the EPICA-Drill Site Dronning Maud Land (DML) Antarctica
author_facet Freitag, Johannes
Kipfstuhl, Sepp
Faria, S.
author_sort Freitag, Johannes
title In Situ X-Ray-micro-tomography of snow at the EPICA-Drill Site Dronning Maud Land (DML) Antarctica
title_short In Situ X-Ray-micro-tomography of snow at the EPICA-Drill Site Dronning Maud Land (DML) Antarctica
title_full In Situ X-Ray-micro-tomography of snow at the EPICA-Drill Site Dronning Maud Land (DML) Antarctica
title_fullStr In Situ X-Ray-micro-tomography of snow at the EPICA-Drill Site Dronning Maud Land (DML) Antarctica
title_full_unstemmed In Situ X-Ray-micro-tomography of snow at the EPICA-Drill Site Dronning Maud Land (DML) Antarctica
title_sort in situ x-ray-micro-tomography of snow at the epica-drill site dronning maud land (dml) antarctica
publishDate 2007
url https://epic.awi.de/id/eprint/17546/
https://hdl.handle.net/10013/epic.27906
genre Antarc*
Antarctica
DML
Dronning Maud Land
EPICA
genre_facet Antarc*
Antarctica
DML
Dronning Maud Land
EPICA
op_source EPIC3EGU ViennaApril 2007., 15
op_relation Freitag, J. orcid:0000-0003-2654-9440 , Kipfstuhl, S. and Faria, S. (2007) In Situ X-Ray-micro-tomography of snow at the EPICA-Drill Site Dronning Maud Land (DML) Antarctica , EGU ViennaApril 2007. . hdl:10013/epic.27906
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