84253d2d-ba4c-1d9f-e054-002128a47908
English
dataset
British Geological Survey
+44 131 667 1000
The Lyell Centre, Research Avenue South
EDINBURGH
LOTHIAN
EH14 4AP
United Kingdom
enquiries@bgs.ac.uk
pointOfContact
2024-03-18
UK GEMINI
2.3
http://data.bgs.ac.uk/id/dataHolding/13607431
WGS 84 / UTM zone 55S (EPSG::32755)
Field and analytical data from Tipperary CO2 seep, Daylesford, Australia (2017)
2019-03-15
publication
http://data.bgs.ac.uk/id/dataHolding/13607431
This dataset contains: 1. An excel spreadsheet of field data from Tipperary pool, including CO2 bubble locations, raw and derived flux data, and field description. March 2017 field campaign. 2. Python scripts for two point correlation function, a spatial statistical method used to describe the spatial distribution of points, and applied to Tipperary pool CO2 bubbling points to determine geological control on their distribution. As reported in: Roberts, J.J., Leplastrier, A., Feitz, A., Bell, A., Karolyte, R., Shipton, Z.K. Structural controls on the location and distribution of CO2 leakage at a natural CO2 spring in Daylesford, Australia. IJGHGC.
Jennifer Roberts
University of Strathclyde
United Kingdom
not available
author
Jennifer Roberts
University of Strathclyde
United Kingdom
not available
pointOfContact
notApplicable
https://resources.bgs.ac.uk/images/geonetworkThumbs/84253d2d-ba4c-1d9f-e054-002128a47908.png
Geology
GEMET - INSPIRE themes
2008-06-01
publication
Monitoring
Carbon capture and storage
Carbon dioxide
Geology
BGS Thesaurus of Geosciences
2011
revision
NERC_DDC
otherRestrictions
licenceOGL
Available under the Open Government Licence subject to the following acknowledgement accompanying the reproduced NERC materials "Contains NERC materials ©NERC [year]"
otherRestrictions
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]"
English
geoscientificInformation
144.1200
144.1200
-37.3300
-37.3300
2017-03-01
2018-03-01
The full method is described in Roberts, J.J., Leplastrier, A., Feitz, A., Bell, A., Karolyte, R., Shipton, Z.K. Structural controls on the location and distribution of CO2 leakage at a natural CO2 spring in Daylesford, Australia. IJGHGC. Bubble locations were determined using an Altus APS3G high precision GNSS survey system for Real Time Kinematic (RTK) position measurements. The UTM coordinates of the feature are relative to a base station at Tipperary. CO2 flux measurements were obtained using a West Systems portable flux system with attached accumulation chamber (type B) and LI-840A CO2/H2O gas analyser. A hollow 50mm PVC pipe frame was attached to the base of the accumulation chamber as a floatation device in order to facilitate flux sampling at the water surface. The base of the accumulation chamber was therefore slightly submerged in water and this change in volume was accounted for when applying the ACK (a conversion factor between ppm/sec (instrument unit) and g/m2/day). ACK temperature and pressure corrections (see Annex A) were made using meteorological measurements recorded at the nearby Ballarat Airport at 10 min intervals. The maximum bubble rate was determined using the West Systems Software (Flux Revision 3.99.4) and optimizing the flux integration for the maximum slope over 20 seconds (bubbles) and 60 seconds (background).
.xlsx
.py python code
http://www.bgs.ac.uk/ukccs/accessions/index.html#item126354
download
http://dx.doi.org/10.5285/fa71e160-8016-4fb8-adab-6087466aaea2
Digital Object Identifier (DOI)
information
dataset
dataset
INSPIRE Implementing rules laying down technical arrangements for the interoperability and harmonisation of Geology
2011
publication
See the referenced specification
false
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
2010-12-08
publication
See http://eur-lex.europa.eu/LexUriServ/LexUriServ.do?uri=OJ:L:2010:323:0011:0102:EN:PDF
false
The full method is described in Roberts, J.J., Leplastrier, A., Feitz, A., Bell, A., Karolyte, R., Shipton, Z.K. Structural controls on the location and distribution of CO2 leakage at a natural CO2 spring in Daylesford, Australia. IJGHGC. Bubble locations were determined using an Altus APS3G high precision GNSS survey system for Real Time Kinematic (RTK) position measurements. The UTM coordinates of the feature are relative to a base station at Tipperary. CO2 flux measurements were obtained using a West Systems portable flux system with attached accumulation chamber (type B) and LI-840A CO2/H2O gas analyser. A hollow 50mm PVC pipe frame was attached to the base of the accumulation chamber as a floatation device in order to facilitate flux sampling at the water surface. The base of the accumulation chamber was therefore slightly submerged in water and this change in volume was accounted for when applying the ACK (a conversion factor between ppm/sec (instrument unit) and g/m2/day). ACK temperature and pressure corrections (see Annex A) were made using meteorological measurements recorded at the nearby Ballarat Airport at 10 min intervals. The maximum bubble rate was determined using the West Systems Software (Flux Revision 3.99.4) and optimizing the flux integration for the maximum slope over 20 seconds (bubbles) and 60 seconds (background).