Core Flood Experiments on carbonate rocks
Grant: ACT ELEGANCY, Project No 271498. Medical CT scans for drainage multiphase flow through carbonate rock cores. The steady state drainage multiphase flow at elevated pressure using nitrogen and DI water, are carried out for three heterogeneous carbonate rocks to characterize the impact of heterogeneity on flow. Core Floods are performed on three carbonate rocks namely, Indiana limestone, Estaillades limestone and Edwards dolomites. Experiments are carried out using medical CT scanner and N2-water fluid system at high pressure. Drainage core floods are carried out by varying nitrogen fractional flow rates from 0 to 1. Residual trapping is obtained at the end of drainage cycle by water flooding of the core. These rocks are from three difference quarries. Indiana carbonate is from Salem Formation located in Indian, USA. Estaillades limestone is from Oppède quarry, France. Edwards dolomite is from Texas, USA. The data set contain medical CT Dry scans, nitrogen scans , water scans and scans at varying fractional flow of nitrogen; 1 readme file; 1 excel file; 27 zip files.
nonGeographicDataset
http://www.bgs.ac.uk/ukccs/accessions/index.html#item133485
function: download
https://www.bgs.ac.uk/services/ngdc/accessions/index.html#item133485
function: download
https://dx.doi.org/10.5285/26323d5b-c4a4-48ac-a8f7-9a83f52ddaa4
name: Digital Object Identifier (DOI)
function: information
http://data.bgs.ac.uk/id/dataHolding/13607600
eng
geoscientificInformation
publication
2008-06-01
Carbonate rocks
UKCCS
Carbon capture and storage
Limestone
Tomography
NGDC Deposited Data
Dolomite (rock)
revision
2022
NERC_DDC
2019-01-31
2019-03-19
publication
2020-03-11
notApplicable
Core Floods are performed on three carbonate rocks namely, Indiana limestone, Estaillades limestone and Edwards dolomites. Experiments are carried out using medical CT scanner and N2-water fluid system as high pressure and temperature. Drainage core floods are carried out by varying nitrogen fractional flow rates from 0 to 1. Residual trapping is obtained at the end of drainage cycle by water flooding of the core.
publication
2011
false
See the referenced specification
publication
2010-12-08
false
See http://eur-lex.europa.eu/LexUriServ/LexUriServ.do?uri=OJ:L:2010:323:0011:0102:EN:PDF
.dicom
The copyright of materials derived from the British Geological Survey's work is vested in the Natural Environment Research Council [NERC]. No part of this work may be reproduced or transmitted in any form or by any means, or stored in a retrieval system of any nature, without the prior permission of the copyright holder, via the BGS Intellectual Property Rights Manager. Use by customers of information provided by the BGS, is at the customer's own risk. In view of the disparate sources of information at BGS's disposal, including such material donated to BGS, that BGS accepts in good faith as being accurate, the Natural Environment Research Council (NERC) gives no warranty, expressed or implied, as to the quality or accuracy of the information supplied, or to the information's suitability for any use. NERC/BGS accepts no liability whatever in respect of loss, damage, injury or other occurence however caused.
Imperial College London
London
United Kingdom
author
Imperial College London
London
United Kingdom
pointOfContact
British Geological Survey
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United Kingdom
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pointOfContact
2024-04-11