Why you Can’t Use Water to Make Cryoporometric Measurements of the Pore Size Distributions in Meteorites – or in High Iron Content Clays, Rocks or Concrete.

Why you Can’t Use Water to Make Cryoporometric Measurements of the Pore Size Distributions in Meteorites – or in High Iron Content Clays, Rocks or Concrete.

Many porous materials have high susceptibility magnetic gradients in the pores, due to the presence of iron or other magnetic materials. Thus if probe liquids are placed in the pores they exhibit fast decaying signals with a short T2*. Usually the actual T2 of the liquids is also reduced, due the pr...

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Bibliographic Details
Main Authors: Webber, J.B., Bland, Phil, Strange, J., Anderson, R., Tohidi, B.
Format: Journal Article
Published: Diffusion Fundamentals 2009
Subjects:
cryoporometry
plastic ice
meteorite
porosity
confined geometry
Online Access:http://www.uni-leipzig.de/diffusion/pdf/volume10/diff_fund_10(2009)3.pdf
http://hdl.handle.net/20.500.11937/40839

Internet

http://www.uni-leipzig.de/diffusion/pdf/volume10/diff_fund_10(2009)3.pdf
http://hdl.handle.net/20.500.11937/40839

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