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.
Nenalezeno https://resources.bgs.ac.uk/images/geonetworkThumbs/a0ab4b71-c63d-6bff-e054-002128a47908.png
non geographic dataset
: http://data.bgs.ac.uk/id/dataHolding/13607600
English
Geoscientific information
GEMET - INSPIRE themes, version 1.0: BGS Thesaurus of Geosciences:
Carbonate rocks
UKCCS
Carbon capture and storage
Limestone
Tomography
NGDC Deposited Data
Dolomite (rock)
Free:
NERC_DDC
publication: 2020-03-11
2019-01-31 - 2019-03-19
Imperial College London
Sojwal Manoorkar
London, United Kingdom
email: not available
Role: author
Imperial College London
Sojwal Manoorkar
London, United Kingdom
email: not available
Role: point of contact

Data Quality

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.
INSPIRE Implementing rules laying down technical arrangements for the interoperability and harmonisation of Geology
Commission Regulation (EU) No 1089/2010 of 23 November 2010 implementing Directive 2007/2/EC of the European Parliament and of the Council as regards interoperability of spatial data sets and services

Constraints

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.
Available under the Open Government Licence subject to the following acknowledgement accompanying the reproduced NERC materials "Contains NERC materials ©NERC [year]"

Metadata about metadata

a0ab4b71-c63d-6bff-e054-002128a47908
British Geological Survey
The Lyell Centre, Research Avenue South, EDINBURGH, EH14 4AP, United Kingdom
tel: +44 131 667 1000
email: enquiries@bgs.ac.uk
Role: point of contact
2024-04-24

Coupled Resource