Lyell Collection

Geological Society, London, Special Publications

Lyell Centre  |   Lyell Collection  |   Subscriptions   |   Geological Society  |   Email alerts  |   Online bookshop  |   Help


Keywords:
Author:
Advanced search>>
This Article
Right arrow Full Text (PDF)
Right arrow References
Right arrow Alert me when this article is cited
Right arrow Alert me if a correction is posted
Services
Right arrow Email this article to a friend
Right arrow Similar articles in this journal
Right arrow Alert me to new issues of the journal
Right arrow Download to citation manager
Right arrow Request Permissions
Citing Articles
Right arrow Citing Articles via HighWire
Right arrow Citing Articles via Google Scholar
Google Scholar
Right arrow Articles by Nuttall, C. A.
Right arrow Articles by Younger, P. L.
Right arrow Search for Related Content
GeoRef
Right arrow GeoRef Citation
Geological Society, London, Special Publications; 2002; v. 198; p. 315-326;
DOI: 10.1144/GSL.SP.2002.198.01.21
© 2002 Geological Society of London

Integrated hydraulic-hydrogeochemical assessment of flooded deep mine voids by test pumping at the Deerplay (Lancashire) and Frances (Fife) Collieries

C. A. Nuttall, R. Adams & P. L. Younger

Hydrogeochemical Engineering Research Outreach (HERO) Department of Civil Engineering, University of Newcastle, Newcastle upon Tyne, NE1 7RU, UK c.a.nuttall{at}ncl.ac.uk

To provide the basis for the design of two Coal Authority mine water management schemes, IMC Consulting Engineers (IMC) carried out step-drawdown pumping tests at the Deerplay (Lancashire) and Frances (Fife) abandoned collieries in the summer of 2000. Supplementary hydrochemical investigations were funded by NERC and undertaken by the University of Newcastle and Queen’s University Belfast (QUB).

The results of the step-drawdown tests can only be interpreted by invoking a substantial component of turbulent flow in large open voids. Overall, the Deerplay system behaves in a manner analogous to natural aquifers, lending itself to modelling (using VSS-NET) to obtain effective hydraulic parameters that may be applicable in similar systems of flooded bord-and-pillar workings elsewhere.

The hydrochemical results for both sites showed some similarities, for example there was evidence of depth stratification of water quality in both cases, but also contrasts. For instance, although the total iron in the mine water pumped from the Deerplay Colliery rose gradually to a plateau at around 30 mg 1–1, the water remained net-alkaline throughout the test. By contrast, not only did the total iron in the Frances waters rise in abrupt steps to as much as 600 mg 1–1, but the water also switched from being net-alkaline at the beginning of the test to become strongly net-acidic by the end.





This article has been cited by other articles:


Home page
Geological Society, London, Special PublicationsHome page
P. L. Younger and N. S. Robins
Challenges in the characterization and prediction of the hydrogeology and geochemistry of mined ground
Geological Society, London, Special Publications, 2002; 198: 1 - 16.
[Abstract] [PDF]