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MICRODIFFRACTION AND RAMAN STUDY OF MICRO-INCLUSIONS IN THE EPICA-DML ICE CORE

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MICRODIFFRACTION AND RAMAN STUDY OF

MICRO-INCLUSIONS IN THE EPICA-DML ICE CORE

Christian Weikusat

1,2

, Sérgio H. Faria

1

, Gernot Nehrke

2

, Sepp Kipfstuhl

2

, Sebastian Schöder

3

, Werner F. Kuhs

1

1GZG, Sect. of Crystallography, Göttingen University, Göttingen, Germany 2Alfred Wegener Institute for Polar and Marine Research, Bremerhaven, Germany 3European Synchrotron Radiation Facility, Grenoble Cedex, France

Microdiffraction

Raman spectroscopy

Sample directly after mounting.

Diameter of the glass plate is ~15 mm. Diffraction pattern of an air hydrate crystal

Microdiffraction experiments were conducted at the beamline ID13 of the ESRF in Grenoble.

Various software bugs and technical difficulties

(especially deposition of copious amounts of frost) prevented the detection and identification of single microinclusions.

Diffraction patterns of larger air hydrate crystals could be acquired.

New methods for frost prevention and data treatment have to be developed.

Raman spectroscpy was performed at GZG, University of Göttingen, and at AWI Bremerhaven. Results obtained with the two

systems are in perfect agreement with each other. Several crystalline microinclusions could be identified (* denotes Raman bands of the ice matrix):

Sample after ~12 hours of measurements.

The excessive production of frost is evident.

*

*

*

*

*

*

*

*

CaSO4 · 2 H2O (Gypsum) some sodium sulfate

SiO2 (Quartz) alkali feldspar

References

A.J. Gow,  T. Williamson, Geol. Soc. Am. Bull., 87, 1665­1677 (1976)

S.H. Faria, J. Freitag, S. Kipfstuhl, Quaternary Science Reviews, 29, 338­351 (2010) T. Sakurai et al., Journal of Glaciology, 55, 777­783 (2009)

A. Nedelcu, ongoing PhD­thesis, University of Göttingen (2010)

2346.9 2383.9 2386 2396 2406.8 2416 2456

0%

10%

20%

30%

40%

50%

60%

70%

80%

90%

100%

misc. Silicates Quartz

misc. Sulfates Na sulfate Ca sulfate

no peaks/high bg unidentified

Depth / m

Frequency

Preliminary results for the MIS6-MIS5e transition.

The increased frequency of quartz and

silicates in the deeper parts could account for the observed changes in mechanical

properties (e.g. borehole closure).

Statistic of microinclusions

Referenzen

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