Diffusion of water in thermally fractured granite rock cores studied by PFG NMR and MRI

Diffusion of water in thermally fractured granite rock cores studied by PFG NMR and MRI

Diffusion of water in thermally fractured granite was studied by using pulsed field gradient NMR (PFGNMR) and MRI methods. Two different approaches gave consistent results, indicating that these methods can be applied for materials of low porosity with fracture networks.

Bibliographic Details
Main Authors: Yamaguchi, Makoto, Suzuki, Kazunori, Altobelli, Stephen
Other Authors: Institute of Research and Innovation,
Format: Article
Language:English
Published: Universitätsbibliothek Leipzig 2016
Subjects:
Diffusion
Transport
diffusion
transport
ddc:530
Online Access:http://nbn-resolving.de/urn:nbn:de:bsz:15-qucosa-194883
http://nbn-resolving.de/urn:nbn:de:bsz:15-qucosa-194883
http://www.qucosa.de/fileadmin/data/qucosa/documents/19488/diff_fund_3%282005%2924.pdf
Description
Summary:Diffusion of water in thermally fractured granite was studied by using pulsed field gradient NMR (PFGNMR) and MRI methods. Two different approaches gave consistent results, indicating that these methods can be applied for materials of low porosity with fracture networks.

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