Annual Report 1997–1998
Okehampton Exeter
DEVON
3 Torbay Plymouth 4 * Dartmouth
ENGLISH CHANNEL
British Geological Survey
Annual Report 1997–1998
Natural Environment Research Council Foreword
The British Geological Survey Review; a review which, as you will have seen, produced a very (BGS) is an important part of positive outcome in terms of funding for science. the Natural Environment I am pleased to see that the new management arrangements put in Research Council (NERC) place at the BGS are already having an impact. Recommendations and I take pleasure in con- from the reviews of 1997 have been taken on board throughout the tributing this Foreword to organisation and measures are being put in place to meet them. The their Annual Report for reviews did identify two programme areas which required strength- 1997/98. ening and in these areas Programme Development Groups have During the past four and a half been established by the BGS Board to do just that. On top of this, years I have made numerous the new Director has set in motion a wide-ranging strategic enjoyable visits to Keyworth planning exercise. Involving staff at all levels within the BGS and and Edinburgh to learn of the also customer consultation, this process is designed to position the work in progress there. This BGS to meet the challenges facing the geosciences at the start of the year I was especially privileged new millennium. to be invited to join the Despite this year of change, the BGS has continued to deliver against Director and BGS staff on a the agreed programme objectives in both its Core Strategic and field trip to the Lake District; this provided me with insight into the Commissioned Research programmes. The fact that progress was skill, enthusiasm and dedication of those working in the field on maintained against targets during this period is a testament to the pro- mapping programmes. fessionalism and dedication of every member of BGS staff. This report The period covered by the report has been one of great change for the clearly sets out that progress, illustrating the relevance of the science, BGS. It underwent a major, five-yearly review of its entire Core the benefits it brings to society, and the contribution it can make Programme of public-good science. This review culminated in a toward achieving the goal of sustainable development. And geoscience thorough Science and Management Audit and I am happy to say that clearly has a vital role to play in achieving that goal: in finding the the BGS came out of the review process with its stock riding high. At resources that society needs; in helping to dispose safely of the waste the same time there were changes at the management level with the society produces; and in understanding the risks and hazards associ- arrival of a new Director, Dr David Falvey, and the establishment of ated with both these activities. It is a role which puts the BGS at the the BGS Board, under its Chairman Dr Eric Hassall. These changes heart of the science that the NERC must deliver for the nation. occurred against a backdrop of change at the national level, with the new Labour Government taking a very active interest in science, and Professor John Krebs FRS its contribution to society, as part of their Comprehensive Spending Chief Executive of the Natural Environment Research Council.
Main cover photograph Small cover photographs This shows the effect of volcanic ash on the centre of Plymouth, the former capital town Thick Ordovician sandstone turbidites (pale) interbedded with mudstones (dark) north of of Montserrat in the Eastern Caribbean. In the picture, a phone box and the war Ceibwr Bay, west of Cardigan, SW Wales. A study in the architecture and dynamics of memorial on the seafront are partially covered these rocks, which were strongly folded during the Caledonian Orogeny, is being under- by ash and debris deposited by pyroclastic taken as part of the primary survey of the Cardigan area (page 5). (Photo by R A Waters). flows and subsequent mudflows since June Cenozoic amber from a Baltic tree containing a fungus gnat and a spider is one of the 1997. Volcanic activity since July 1995 has illustrations in the new BGS Popular Publication Fossils–– the story of life (page 18). rendered a large part of the south of (Photo: BGS/Sedgwick Museum). Montserrat uninhabitable. Numerous pyro- clastic flows have travelled down all flanks of The Permian trace fossil Umfolozzia longula, found during the Falkland Islands the Soufrière Hills volcano (background to mapping (page 23), is one detail in the evidence linking the islands' rock formations photo), destroying a large part of several with those of South Africa. (Photo by D T Aldiss). towns, including Plymouth, and inundated The macroseismic survey for the magnitude 2.8 ML Dartmouth earthquake, 16 October valuable agricultural land. 19 people were 1997, 00:19 UTC, see Geophysical Monitoring (page 10). Areas of EMS intensities 3 and killed by pyroclastic flows in the summer of 4 are depicted. The epicentre is shown as a yellow star. 1997. The BGS has been involved in the monitoring programme of the Montserrat Volcano Observatory since early in the crisis Bibliographical reference as part of a multidisciplinary and multi- BRITISH GEOLOGICAL SURVEY, 1998. organisation project funded by DFID Annual Report of the British Geological Survey 1997–1998. (page 27). (Photo by G E Norton). (Swindon, Wiltshire: Natural Environment Research Council). Editor: Martin Litherland Design & Production: Adrian Minks
The maps of Great Britain used in this report which are based on Ordnance Survey Mapping, are Print Production: John Stevenson reproduced with permission of the Controller of Her Majesty’s Stationery Office © Crown copyright. Ordnance Survey licence number GD 272191/1998. © NERC 1998. All rights reserved. 10/98 C30 ISBN 0 85272 322 9 Report of the British Geological Survey 1997–98
The Mission of the British Geological Survey is to:
Advance geoscientific knowledge of the United Kingdom landmass and its adjacent continental shelf by means of systematic surveying and data collection, long-term monitor- ing and high-quality research.
Provide comprehensive, objective, impartial and up-to-date geoscientific information, advice and services which meet the needs of customers in the industrial, engineering, governmental and scientific communitiues of the UK and overseas, thereby contributing to the economic competitiveness of the United Kingdom, the effectiveness of public services and policy, and quality of life.
Enhance the UK science base by providing knowledge, information, education and training in the geo- sciences, and promote the public under- standing of the relevance of geoscience to resource and environment issues.
Natural Environment Research Council Contents
Director’s Introduction ...... 1 CORE AND PARTNERSHIP PROGRAMMES Geological Mapping of Britain ...... 2 Minerals and Geochemistry ...... 8 Geophysics ...... 10 Hydrogeology ...... 12 Marine and Coastal Geology ...... 14 Records and Databases ...... 16 Science for All ...... 18 Northern Ireland ...... 20 Isotope Geosciences ...... 21 COMMISSIONED PROGRAMME International Development and Assistance: — Mapping and Minerals ...... 22 — Groundwater and Pollution ...... 24 — Hydrocarbons ...... 26 — Geohazards ...... 27 — Environmental Geoscience ...... 28 Resources: — Minerals ...... 30 — Oil and Gas ...... 31 Geology and Geohazards ...... 32 Environmental Geoscience ...... 34
C F Adkin APPENDICES 'Gene' Shoemaker died tragically only 1. Organisation ...... 38 months after delivering our Distinguished 2. Finance ...... 39 Lecture of 1997 and receiving his medal (above). He was probably the most influen- 3. Publishing ...... 40 tial planetary geologist of our age. His ashes 4. Staff List ...... 50 are on board Lunar Prospector, and will 5. Academic Collaboration ...... 56 eventually land on the Moon. 6. Business Collaboration ...... 58 7. Committees ...... 60 8. Acronyms ...... 61 9. Core Strategic Programme Achievements ...... 62 10.The BGS Board ...... 70
British Geological Survey
Dr John Carney demonstrates hand-augering as part of an orientation course for those BGS staff without formal geological training. P A Tod Director’s Introduction
It is far easier to build from a position of partnership approach will take various strength than from one of decline. For forms, from user panels for the BGS’s this reason I concluded that 1998, being public-good programme to more formal the first year without a major external consortia with industrial and commercial review for some considerable time, partners, where appropriate. The second presented the BGS with a golden oppor- element can be summarised as a change in tunity to plan for a successful future. I emphasis from data acquisition to data therefore initiated a major strategic exploitation. Of course, there will be a planning exercise, a process which has continuing need to acquire new and better now been running for eight months. It data, but in the future the emphasis will has involved contributions from all kinds be placed firmly on providing solutions to of people, from junior staff to the BGS problems and helping customers to realise Board, and will increasingly involve our opportunities. stakeholders in Government, industry These two key elements of the new and the universities, too. Its aim is to strategy are linked intimately, because it produce a new Strategic Plan for the is through closer relationships with BGS which will set the context for future customers that the BGS will develop a Business and Programme Planning and fuller understanding of the problems and guide the organisation into the new mil- I am delighted to have this opportunity opportunities facing society. In this lennium. to introduce the BGS Annual Report for respect, the new strategy will focus the 1997/98, the first during my term of The process is not yet complete, but it is BGS on the delivery of ‘outcomes’ which office as Director. It gives me a chance to possible to set out a few of the emerging match BGS data, knowledge and reflect on a busy first year in the job and elements of the new strategy. I will expertise to society’s needs. This to look forward to some of the things I confine myself to just two. Firstly, the promises an exciting future for the BGS hope to achieve during what I am sure BGS will become more and more closely — for the problems may be great but the will be a long and happy association with allied with the needs of its customers, opportunities are many. the BGS. working in partnership with David A Falvey When I became Director in January them to set the direction for BGS Director of the British Geological Survey 1998, I inherited a successful organisa- November 1998. tion which was emerging from a series of science. This demanding reviews with great credit. My predecessor, Peter Cook, working with a proactive Programme Board, laid the foundations for that success. Since the start of 1998 the Board has been re- constituted as the BGS Board, with responsibility across all BGS activities. I look forward to building on these foun- dations with the new Board. I must say that I have been impressed with the range of expertise and the quality of the science to be found in the BGS. The breadth and depth of the staff’s capabilities, when combined with the unique data and knowledge held by the BGS, present a significant opportunity to provide the nation with both scientific and economic benefits. The contents of this report show that the BGS has much to offer across a range of overlapping issues: energy, minerals, water and land resources; geological hazards and risks; waste and pollution; and the impacts of global change. Winter at the Keyworth site (photo: P A Tod).
1 CORE AND PARTNERSHIP PROGRAMMES
The BGS is dedicated to CORE STRATEGIC PROGRAMME provide, on maps and in This, the principal business task of the BGS, entails long- databases and written term mapping/surveying, monitoring, databasing, support- accounts, geological ing scientific research and the provision of scientific advice. The Core Strategic Programme contains the underpinning information for all parts scientific activity which provides geoscientific information in of Great Britain and her support of decision making by public and private bodies at territorial waters, com- national to local levels on broad issues relating to resources, mensurate with the land use, geohazards and the environment. A small, but key needs of the whole user element of the Core Strategic Programme is the promotion of community. the public understanding of science. The programme’s primary funding is from the Science Budget. Geological Mapping of Britain
The 15-year programme of geological ● Southern Highlands: mapping efforts mapping carried out within the have concentrated on the turbiditic Multidisciplinary Regional Surveys sub- Southern Highland Group (below left). programme was started in 1990/91. The The work has been particularly useful in cumulative output over the seven years is developing theories relating to 159 resurveyed or revised 1:50 000 geo- Dalradian structural development, both logical maps, 62 memoirs, three new in terms of proposing mechanisms for editions of regional guides and two sub- cleavage growth, and refining the larger surface memoirs. During the current year scale tectonic collisional models that 3303 square kilometres were resurveyed imply movement towards the north-east or revised; 299 1:10 000 maps were during the peak of the Grampian View looking north-north-west from Ben released to the public (including 24 orogeny. Collaboration with the univer- Venue over Loch Katrine. The hills in the digital maps) and 103 technical reports sities of Edinburgh and Leicester, and foreground are underlain by Southern written. Eight shallow boreholes, the East Kilbride Reactor Centre aims Highland Group rocks, giving way to pro- totalling 667 metres, were drilled. to characterise an important volcaniclas- gressively older rocks northwards. tic unit, termed the Green Beds. Preliminary Green Bed geochemical data suggests that they originate from a mixed plume- and N-MORB* basaltic source. Stream sediment geochemistry is helping to unravel the original basin architecture of the Southern Highland Group turbidite sediments. ● East Grampian: cathode luminescence work on thin sections from Dalradian metacarbonate rocks collected in the Tomintoul area has enabled mapping of detailed variations in their strontium content. Preliminary results from the Tayvallich Limestone in the south- western part of the Grampian Highlands suggest that Sr87/86 ratios may be compatible with Neoproterozoic sea water curves. This technique allows an assessment of the age of the meta-
C W Thomas limestone to be made independently of
*See list of Acronyms (Appendix 8).
2 GEOLOGICAL MAPPING OF BRITAIN GEOLOGICAL MAPPING OF BRITAIN
PARTNERSHIP PROGRAMME
This is an extension of the Core Strategic Programme, consisting of research activities co-funded by the BGS from Science Budget appropriations, and by partners in the private and public sectors (including the EU). Co-funded projects address surveying and generic research issues relevant to the BGS Core Strategic Programme and to the strategic interests of the co-funding partners. Co-funding helps demonstrate specific customer support for elements of our core strategic programme and is expected to expand in the future.
other isotopic and stratigraphical con- Fell Sandstone groups. The occurrence straints. of large calcite petrifications of Cordaites trees from the Middle Coal Measures, ● Monadhliath: with more than 65% of found in an opencast coal mine near the Central Highlands now covered at Chester-le-Street (Sheet 20 Newcastle the 1:50 000 scale, regional syntheses upon Tyne) was investigated in collabo- and a multi-disciplinary approach have ration with staff of Durham and been successfully combined to identify a London universities (right). Proposals to series of marine rift basins of investigate the nature and distribution Proterozoic age. Ongoing detailed of mine gas emissions, mainly the Quaternary mapping and microstruc- mixture of nitrogen and carbon dioxide tural studies of glaciolacustrine known as ‘stythe’, in the sediments (bottom right) have provided Northumberland Coalfield has new data and ideas on the patterns of attracted media attention. ice movement and deglaciation in the Spey valley and across the Central ● Lake District: the Borrowdale Highlands. Volcanic Group has been traced to the Appleby district (Sheet 30). Many ● Midland Valley: work continued on andesite sheets have been recorded in the revision of the Lanark district (Sheet the dominantly volcaniclastic upper 23), where new opencast mining explo- part of the group. Farther south, in the ration data has enabled the compilation Kendal district, detailed work on the B Young of a complete Carboniferous sequence upper part of the sedimentary Large petrified Cordaites trunk in in the Coalburn-Douglas area. In the Windermere Supergroup has estab- sandstone above High Main Coal, Prior’s Kilmarnock district (Sheet 22), comple- lished systematic lithological variation Close North Opencast site, Great Lumley, tion of the survey has enabled a revision which will necessitate a partial revision near Chester-le-Street, County Durham. of the lithostratigraphy and the clarifica- of the local lithostratigraphy. tion of the volcanic processes that produced the Clyde Plateau Volcanic ● East Midlands: research into the sub- Formation. A regional Midland Valley surface geology of the Loughborough project was initiated to produce a 3-D district (Sheet 141) continued with the computer model of geological surfaces drilling of a 175 metre-deep hole at across the region from digital data sets. Worthington, just west of the Carboniferous Limestone inlier at ● Southern Uplands: in the Leadhills Breedon Cloud. The borehole proved district (Sheet 15E) conodont evidence Lower Coal Measures, down to the has proved three new localities of Arenig Subcrenatum Marine Band, resting on rocks. Detailed revision of the 117 metres of Namurian strata of the Llandovery graptolite biostratigraphy Millstone Grit Group. The resurvey of continues to provide invaluable input to the Melton Mowbray district (Sheet the core mapping programme, particu- 142) commenced at the beginning of larly in understanding the plexus of the year. Mapping in the western and tract-bounding faults within the Gala southern parts of the sheet has consid- Group in the Thornhill (Sheet 9E) and erably refined the complex drift Moffat (Sheet 16W) districts. geology of the Wreake valley; the F I MacTaggart ● Tyne Alston: revision mapping of the Bytham Sand and Gravel of pre- Small-scale compressional fault with Rothbury district (Sheet 9) concen- Anglian age is overlain by interbedded sheared mudstone and disrupted trated mainly on a reinterpretation of tills, glaciolacustrine and glaciofluvial bedding: glaciolacustrine deposits, the outcrops of the Cementstone and deposits of Anglian age. Raitt’s Burn, Spey Valley.
GEOLOGICAL MAPPING OF BRITAIN 3 CORE AND PARTNERSHIP PROGRAMMES Geological Mapping of Britain (continued)
● West Midlands: modelling of the features. Our research, in collaboration Triassic aquifer (right) has benefitted with Royal Holloway, University of from a suite of recently released maps London and the University of Brighton, covering part of the Stafford Basin. The is targeted at determining the prove- integration of seismic data with nance, depositional environment and age ● Yorkshire: The five kilometre- downhole geophysics and surface of these gravels. long Standedge Canal Tunnel mapping has led to a better understand- ● (below), built over 200 years ago, ing of the subsurface structure of the London Basin: mapping west of was formerly an important trans- Basin, and of the distribution of the London has enabled the pre-Anglian Pennine transport route. In Permo-Triassic formations that are an courses of the rivers Blackwater, Kennet advance of remedial work to important source of groundwater for and Thames to be determined. A model reopen the tunnel for use in time public consumption. incorporating outcrop and borehole data for the new millenium, British has led to the determination of dominant ● Waterways provided the BGS an Hampshire Basin: mapping of the north-west-trending faults in the region. unique opportunity to access the Alresford area (Sheet 300) was completed They are thought to be the surface entire tunnel. The section records ahead of schedule. This was greatly expression of basement structures (one an upward transition from the assisted by the interpretation of 1:25 000 underlies the Windsor dome) that may turbidites of the Shale Grit and scale stereo air photography using the have significant implications for assess- Grindslow Shales, deposited in a ImageStation system to produce ‘headup’ ment of the Variscan front. prodelta or delta slope environ- screen images in stereo on which digital linework was interpreted. This new The Quaternary deposits of the ment, to the dominantly fluvio- Reading area (Sheet 268) have been deltaic Kinderscout Grits, approach to field mapping considerably reclassified into a series of river terrace deposited on a delta top. This enhances the production rate in the field deposits relating to the drainage of the work represents part of an ongoing and allows targeting of difficult ground. proto-Kennet and Thames rivers, programme of resurvey of four Work has started on ImageStation pro- together with periglacial weathering 1:50 000 Series maps in West cessing of the photographs for the and mass-movement deposits. Data Yorkshire. The resurvey of the Winchester area (Sheet 299). from two boreholes have allowed con- Wakefield and Bradford sheets is ● Cotswolds: the first detailed survey of siderable refinement of the Palaeogene now complete; Huddersfield is the Moreton-in-Marsh area (Sheet 217) stratigraphy. nearing completion, and Leeds has is nearly complete. Two hitherto been started. ● Cornwall and South Devon: mapping unknown outliers of the Middle Jurassic of the Torquay region (Sheet 350) has Cornbrash and Kellaways formations revealed a ‘high’ at least 20 kilometres have been discovered. The pattern of wide to the north of the Looe Basin in faulting reflects the deep-seated ‘Vale of the Variscan rifted passive margin of Moreton Axis’, on the eastern margin of central Cornwall and south Devon. the Worcester Basin. Cambering and Multiple reef and carbonate complexes gulling are widespread in the district, developed during the Mid to Late and are important in relation to con- Devonian on this ‘high’, where it was struction projects. They have been shielded from clastic sedimentary supply mapped and investigated using geophys- by the formation of a faulted sedimen- ical methods including ground penetrat- tary basin to the north. ing radar and the NERC’s Airborne Thematic Mapper. Collaborative BGS/Durham University CASE research on the Lizard (Sheet ● East Anglia: the Cromer region (Sheet 359) has established that different peri- 131) lies at the interface between dotites of the ophiolite complex are deposits of three ice sheets: the British related to changing pressure and tem- Eastern Ice Sheet, the Scandinavian Ice perature conditions during tectonically Sheet of Anglian age, and the younger controlled mantle uplift. The distribu- Devensian Ice Sheet. Remarkably fresh tion of peridotite types has been C N Waters landforms, such as the Blakeney ‘esker’ mapped out in detail. View of Marsden Portal at the entrance and smaller isolated gravel outcrops in of the Standedge Tunnel. the Glaven valley, are considered by ● Lyme Bay to Bristol Channel: the some to be constructional glacial survey of the Triassic, Cretaceous and landforms, and by others as erosional Tertiary rocks of the Sidmouth area
4 GEOLOGICAL MAPPING OF BRITAIN GEOLOGICAL MAPPING OF BRITAIN (CONTINUED)
● Cardigan: the Moylgrove Group D M Bridge is a poorly known, late Rock strata which comprise part of the Staffordshire Basin Triassic aquifer: the photograph Ordovician, deep-water turbidite shows the junction between the weakly-cemented Wildmoor Sandstone and the overlying basal sequence that is splendidly conglomeratic unit of the Bromsgrove Sandstone, Tong Forge, Staffordshire. exposed in the sea cliffs between Cardigan and Newport in south- west Wales (below). A study of (Sheet 326) continued. Around Beer, an compile digital field information and the architecture and dynamics of extensive layer of partially dissolved other datasets such as mine plans, using this deformed sandy turbidite Chalk is underlain by intact Chalk and PC-based Microstation software. The system is being undertaken as overlain by Tertiary Clay-with-flints. system is fully compatible with that part of the primary survey of the The position of the partially decalcified used by Cartographic Services to Cardigan area (Sheet 193). layer, which is 15 to 20 metres thick, produce 1:10 000 and 1:50 000 scale suggests that it is a Tertiary feature. It maps and will enable the rapid develop- may represent an intermediate stage in ment of customised map-based products the formation of Clay-with-flints. for commercial applications. Similar, large-scale, pervasive, karstic features are preserved beneath chalk ● Continuous revision: the purpose of valleys throughout southern England this programme, which is of consider- and are probably related in origin to the able long-term strategic importance, is Beer occurrences. Their recognition has to address the on-going needs of the important geotechnical and hydrogeo- geoscience map and data-using logical implications. community for areas both within and outside the map sheets designated ● Swanage: mapping of the Swanage area within the 15-year plan. It is carried (Sheet 343) has been completed. The out by a process of focused data acqui- dominant feature of this district is the sition, databasing and subsequent map approximately east – west Purbeck revision at scales of 1:10 000 and Monocline and associated fault, which has resulted in a narrow belt of steeply 1:50 000 for areas, mainly urban, where dipping, locally overturned strata. The the demand is high. Revised maps are Palaeogene basin that lies on the north now available for the Sheffield, side of this structure comprises a thin Bristol/Bath, Beaconsfield/Reigate and London Clay and a much thicker Poole Glasgow areas. Formation. Within the Poole In Scotland, a proactive policy of data R A Waters Formation, a series of clay members acquisition was pursued, with three BGS geologists landing by inflatable to include internationally important ball- BGS boreholes and 30 commercial collect graptolite fossils, necessary for the clay deposits. Close to the monocline boreholes examined and data incorpo- correlation of these Moylgrove sequences. the host clays occupy a narrow, struc- rated in correction copies. In addition, The inaccessibility of the cliffs has turally complex area. 22 non-coal mine plans, 3100 mine precluded a detailed study until now, ● Research and Development: the entries and 14 000 records of quarries but the survey is totally dependent on highlight was the completion of a were researched, validated and entered access from the sea. prototype system to enable geologists to into digital datasets.
GEOLOGICAL MAPPING OF BRITAIN 5 CORE AND PARTNERSHIP PROGRAMMES Geological Mapping of Britain (continued)
PARTNERSHIP PROGRAMME Ground level change in the Thames Estuary: a review was made of potential causes of ground movement and rates of change that may influence the risk of flooding in the next millennium and D G Tragheim and M R Bowker beyond. The study (in the second year of three) is being carried out for the Environment Agency, in collaboration with the Institute of Engineering Survey and Space Geodesy, Nottingham University.
Afon Teifi Catchment Survey: this St Bees area, Lake District: an oblique perspective looking north-east showing Quaternary geology project, co-funded by a consortium draped over a terrain model produced by digital photogrammetry. Drift-free solid geology is in of Local Authorities and the purple, Boulder Clay in light blue, glaciofluvial deposits (sand and gravel) in pink, river alluvium in Environment Agency, was pale yellow, marine alluvium in dark yellow, and peat in orange-brown. The cross section shows completed this year. It has involved imbricate slices of sand and gravel wedges caused by glaciotectonics. The area of the image is 34 km2. the production of 1:25 000 scale maps of the catchment, together with six thematic maps and a Remote Sensing Digital Photogrammetry Technical Report. Most of the effort Remote sensing covers a wide range of Earth focused on the Quaternary deposits. A major focus in recent years has been observation techniques from satellite and The study, together with two deep the development of new applications of airborne imagery (below) to classical photo- boreholes, drilled in abandoned digital photogrammetry aimed at geology and digital photogrammetry. The segments of the Teifi valley, has improving the efficiency of the UK geo- BGS programmes are designed to utilise thrown new light on the Quaternary logical mapping programme. These tech- these techniques to help improve productiv- history of the area (far right). niques enable on-screen interactive geo- ity and cost-effectiveness. morphological interpretation to be carried out of 3-D stereomodels and oblique perspectives derived from high resolution aerial photographs (above). Photogrammetry reduces the amount of time needed for fieldwork and thus can improve the speed and cost-effectiveness of mapping programmes. Inputs have been provided to several mapping projects including Alresford, Melton, Winchester and Huddersfield.
View of an original 1: 5000 scale orthophoto draped over a DTM, near Bourton-on-the- Water, Cotswolds, southern England. It shows an unusual pattern of topographic depressions in Middle Jurassic limestones. Rock exposures in the railway cutting, combined with ground penetrating radar, show that the hollows are related to extensional half-graben faults due to mass movement of the limestones above D G Tragheim weaker clays at depth.
6 GEOLOGICAL MAPPING OF BRITAIN GEOLOGICAL MAPPING OF BRITAIN (CONTINUED)
Namurian Flooding Events and uplift of pre-Permian strata during the (Realising Our Potential Variscan Orogeny. In the southwest and Award) around Milton Green the Warwickshire Group (Erbistock to Ruabon Marl forma- Studies of catastrophically rapid tions) are unconformable on Coal Measures, glacioeustatic marine flooding events in Millstone Grit, Carboniferous Limestone the Namurian of the Central Pennine and older rocks. This relationship persists in Basin reveal that they provide the time the subsurface. Subsurface mapping in framework upon which Namurian Derbyshire shows evidence of Dinantian sequence stratigraphy and lithostratigraphy tilt-blocks dipping southwest. is interpreted. Engineering Behaviour of Graphic correlation indicates that flooding British Rock and Soil surfaces are sensitive to differential subsi- dence, and provides a tool for constraining Formations subtle changes in syndepositional tectonics ● The analysis of the geotechnical and differential compaction. Transgressive database of the Mercia Mudstone for deposits are rare. Many of the fluvial the effects of regional variation, strati- sediments belong to the highstand phase graphical position and weathering grade rather than the early transgressive phase of has been completed. marine flooding; this is contrary to some ● recently published models. A report on the geotechnical shrinking and swelling properties of the Mercia Small-Scale Maps Mudstone has been finalised. ● Regional contour maps at 1:1.5 million The first draft of the monograph on the Glaciolacustrine clays, exhibiting silt scale of the Top Chalk/Base Tertiary of Engineering Geology of the Mercia laminae, soft sediment deformation and the entire UK (onshore and offshore), the Mudstone has been completed. dropstones (pebbles dropped from base Chalk of the North Sea (partial) and ● Compilation of a geotechnical database icebergs), from a cored borehole (67.9 to the base Cretaceous of the North Sea for the Palaeocene Lambeth Group is well 71.65 m depth) near Cardigan. The (partial) have been compiled from a advanced. clays form the lower part of a very thick variety of sources. Preliminary work for ● Field visits to exposures of the Lambeth sequence of glaciolacustine sediments the production of GIS coverages for these deposited in a major proglacial lake, structural surfaces has begun, together Group (below) have yielded disturbed samples for geotechnical testing and ponded by the onshore advance of an with rudimentary procedures for generat- Irish Sea ice sheet during the last ice age. ing cross-sections and fault displacement highlighted the engineering complexity statistics from these coverages. A prelimi- of the group. nary 3-D model of major crustal faults and ● A survey of leading engineering geolo- Moho surfaces in southern England is gists in commerce and academia showed Alum Bay, Isle of Wight. The vertical- nearing completion continuing support for the Engineering dipping Reading Formation of the Properties Project and indicated that Lambeth Group is bounded to the left by Minehead Mapping Lias Clay, Coal Measures Mudrocks London Clay and to the right by Chalk. An earth-flow in the clay of the Reading Following work in the Bristol Channel and the London Clay should be given high priority for future study. Formation is ‘moving’ down the cliff, (1:50 000 Sheet 278 Minehead) an alter- towards the viewer. native explanation has been advanced for a prominent seismic reflector, originally identified as pre-Devonian metamorphic basement. This reflector is interpreted as the top of the Carboniferous Limestone. This interpretation produces geological relationships which are best explained by reviving Ussher’s theory of the Cannington Park Thrust, which has emplaced Devonian and older rocks on Carboniferous Limestone and overlying Silesian, south of Cannington Park and extending westwards offshore. Cheshire-Staffordshire- Derbyshire Project Two unconformities are recognised in the subsurface of the Cheshire Basin. The main regional unconformity lies at the base of the Collyhurst Sandstone, caused by folding K J Northmore
GEOLOGICAL MAPPING OF BRITAIN 7 CORE AND PARTNERSHIP PROGRAMMES
The BGS carries out Minerals and systematic geochemical surveying of the UK and maintains national Geochemistry databases of geochemical, radiometric and mineral Striking the balance between the need for The geochemical atlas for North-west data. a sustainable environment and the need England and North Wales was completed. A for mineral products requires authorita- hydrogeochemical atlas of Wales (the first of tive, systematic information. Technology its kind) is in preparation, containing stream Foresight has identified the problems and water chemistry at a resolution of one sample challenges associated with the stages of the per two square kilometres. A thematic section natural resource cycle, from exploration, to this atlas illustrates how the data may be through the identification, extraction, pro- used to interpret key issues such as regional cessing and industrial use of resources, to controls on trace-element speciation, acid the disposal of waste and the remediation rain and eutrofication. G-BASE data are and aftercare of contaminated land. being used to assist in geological interpreta- Collectively, the projects that make up the tion in Scotland (below left). (Below) Three-component map for Minerals and Geochemistry Core Strategic On the international level, the BGS zirconium (red), strontium (green) and Programme offer the impartial expertise, continued to take the lead in initiatives to rubidium (blue) in stream sediment over knowledge and information on which harmonise geochemical maps and part of the central Highlands of Scotland. sound economic and environmental mapping in Europe and worldwide. The highly evolved Cairngorm Granite decisions can be based at every stage of the cycle. They also provide fundamental data (A) is clearly defined by high levels of MINGOL (Minerals GIS On-Line) rubidium and low strontium and in support of geological mapping. zirconium. The Strath Tummel Basin The basic structure for this minerals infor- (B), part of the Glen Spean–Strath G-BASE mation system is now complete, and a CD- Tummel Subgroup of the Grampian The Geochemical Baseline Survey of the ROM is available for demonstration Group, is marked by high levels of Environment (G-BASE) provides baseline purposes. Data from the DETR-commis- zirconium and rubidium (pink hues), geochemical data for soils, stream sioned county Mineral Resource Planning reflecting the predominance of K-feldspar sediments and waters for economic and maps for Staffordshire and South Wales and detrital mineral assemblages. The environmental applications. In 1997, were successfully incorporated into outcrop of this subgroup to the north-east, suites of geochemical samples (stream MINGOL during the year, and additional the Cromdale Basin (C), has a similar sediments, stream waters and soils) were maps will be added as they are published. signature (the darker colours indicate collected over an area of 5200 square kilo- Maps showing the Economic Planning lower values) but shows less contrast with metres in the East Midlands, including Regions and production data for construc- the geochemistry of the surrounding both rural and urban areas. tion minerals are now available, as well as a rocks. The A9 road is shown in black. national index of mineral exploration data. Revision and updating of the BRITPITS dataset was completed, providing informa- tion for a new edition of the Directory of Mines and Quarries (DMQ). Work continued on the 1:250 000 mineral resource map series: the first map, covering the Lake District, is well advanced. Further commodity chapters and a glossary were drafted for a new publication, Mineral Resources of Britain. Gold in Extensional Basins A new project on the metallogeny of gold in the Dalradian of the Scottish Highlands involves the multidisciplinary study of various types of gold mineralisation in order to understand its distribution in terms of the sedimentary, magmatic and tectonic development of the Dalradian basin. It is planned to develop a unifying predictive model for the identification of prospective targets in this and similar terrains elsewhere in the world.
8 MINERALS AND GEOCHEMISTRY MINERALS AND GEOCHEMISTRY
Trace-element Distributions: a NERS (Natural Environmental New Approach Radioactivity Survey) A novel approach to the measurement of Revised versions of the Liverpool Bay trace-element distributions in soils and 1: 250 000 scale radon potential and gamma- sediments is being developed, which is ray-dose maps were prepared. The radon Basin Maturity simpler to carry out than traditional extrac- sheet now incorporates the effect of uncon- Basin maturity surveys of UK tion schemes and is more flexible and solidated drift deposits as well as the solid Palaeozoic basins have shown that selective in identifying the presence of rocks, a major advance on earlier products. distinctive patterns of metapelitic different physico-chemical components. The Similar revision of the Lake District maps zones indicated by clay-mineral crys- method uses nitric acid as a non-specific was brought close to completion and work tallinity are the result of burial and extractant. Under different experimental con- commenced on the East Midlands sheet. heat flow in different geotectonic ditions, different proportions of metals are Studies were continued into the influence of settings. Deep-burial and low-heat- extracted from different phases. After mineralogy on radon emanation for selected flow conditions are characteristic of chemical analysis of the resulting solutions, rock units, e.g. being the Northampton Sand the Scottish Southern Uplands chemometric processing is used to identify Formation which is known to have relatively terrane and the Windermere and quantify the various components. high radon emanation. Supergroup. The Welsh Basin and the Skiddaw Basin in the Lake District are high-heat-flow exten- PARTNERSHIP PROGRAMME sional basins. The Variscan basin of south-west England represents Interlaboratory comparison: a project Metal-contaminated canal mud: a col- passive-margin sequences which supported by the EU has been set up to laborative study with the University of acquired a pattern of burial metamor- improve collaboration between the geo- Nottingham investigated metal contami- phism prior to the development of a chemical laboratories of geological surveys nation of muds from the Birmingham fold-and-thrust belt . in western and eastern Europe canal system. Cryogenic SEM tech- (Netherlands, Finland, UK, Estonia, niques have been developed to provide Lithuania, Czech Republic, Slovak detailed petrographic information on Republic, Poland, Romania, Russia and the nature of the anthropogenic Cu, Zn, Hungary). The aim of the project is to Pb, Fe and P in the unconsolidated assess the comparability of data provided by sediments. The BGS cryoSEM enables each laboratory for geochemical mapping the muds to be examined wet and purposes, to facilitate data interpretation reduces the disruption of primary fabrics across national borders. During the first associated with sample drying for con- year, each laboratory has provided data for ventional SEM. This approach has an interlaboratory proficiency testing enabled the processes controlling the Metapelitic Zone Kubler Index Late scheme and information on their analytical ‘early diagenetic’ mobilisation and Diagenetic LDZ Tectonic Zone 0.42 °20 transport direction Low LA Younging Anchizone methods as the basis for detailed assessment fixation of the metals to be evaluated. 0.30 direction High HA Anchizone Thrust plane of appropriate analytical strategies. 0.25 Mineral deposit evaluation: the Epizone E UK coal resources: the preparation of a principal aims of this partnership project map of UK coal resources at a scale of between the BGS, who acted as project 1:1 000 000, for completion in 1998, was leaders, DTI, KRJA Systems Ltd and Block diagram showing inverted pattern undertaken with the support of the Coal Anglesey Mining plc were to test a of metapelitic zones developed in a Authority. The map will illustrate the mineral exploration methodology based typical fold-and-thrust belt. Such extent, as projections to surface areas, of on the PIMA (Portable Infrared Mineral patterns are found in low-grade meta- different categories of resources and Analyser) and the VULCAN 3-D morphic terranes on the flanks of major former resources of coal and coal-bed modelling system, and transfer the alpine-type orogenic belts. methane. The map will include coals of all methodology to minerals-sector SMEs. ages, with an indication of the sub-surface The PIMA was successful in detecting geometry of the resources, both onshore distinctive mineral assemblages related to and offshore. The objective of the map is lithology and hydrothermal alteration at to provide a synopsis for the benefit of Parys Mountain (right), and 3-D both initial environmental assessment and modelling with integrated geological and resource management. All the data, geochemical data is assisting in metallo- including detailed information on produc- genetic studies and the delineation of ore tion sites, will be integrated into the BGS zones. The results also indicate that both minerals GIS system (MINGOL). PIMA and VULCAN have more general Midland Valley of Scotland: a digital applicability to mineral exploration in database of Mineral Resources in the other geological environments in Britain. Midland Valley was prepared in collabo- Together they form a powerful combina- ration with Scottish Natural Heritage. tion, with the potential to suggest where T B Colman Data includes sand and gravel, hard rock a borehole has passed close to a buried PIMA analysing altered volcanic rock at aggregate, limestone and coal. ore deposit without intersecting it. outcrop, Parys Mountain.
MINERALS AND GEOCHEMISTRY 9 CORE AND PARTNERSHIP PROGRAMMES
The studies of the physical Geophysics properties of rocks are applied to the solutions of engineering, geotechnical, geomagnetic, and seismic problems, to the exploration for mineral deposits and National Geophysical Mapping packages have all been upgraded. Further and Databank major upgrades have been made to the 3-D hydrocarbons, and to the gravity and magnetic modelling programs understanding of 3-D Gravity measurements were made over the (Gmod/Bmod), including magnetic layer Orkney Islands to bring the coverage of optimisation and experimental, combined crustal structure. this area up to the national standard; the gravity/magnetic optimisation routines. data have been incorporated into the The 3-D software is now being integrated National Gravity Databank. Two maps at into a workstation-based seismic/gravity/ 1:1 500 000 scale were published showing magnetic interpretation package under an gravity and magnetic anomalies over agreement with Ark Geophysics. Britain, Ireland and adjacent areas using colour shaded-relief presentation (left). Geophysical Monitoring Two 1:1 000 000 magnetic anomaly maps were prepared for cartographic enhance- The UK magnetic observatories at ment. A prototype graphical interface was Lerwick, Eskdalemuir and Hartland, and developed to browse information held in the 141-station UK seismic network the Geophysical Surveys databank; this were maintained, and improvements provides access to line-based ground and made to instrumentation and data collec- airborne surveys. tion. Geomagnetic and seismic data were retrieved to Edinburgh automatically Regional Crustal Structure under computer control and data The regional gravity and magnetic data products published in electronic form on acquired over the UK are being interpreted the World-Wide-Web, providing a systematically and the results presented on seven-day, 24-hour service to academia, interactive CD-ROMs. An important government and commerce. Co- input to the interpretation for the current operation with other European institu- Southern Scotland/Northern England tions to promote the rapid exchange of study (below left) has been a model for the seismic data continued and, through the structure of the cover sequence based on INTERMAGNET programme, data I F Smith seismic reflection data and developed from a global set of magnetic observato- Gravity and magnetic maps of Britain, during earlier BGS projects. Integration of ries were exchanged in near real time Ireland and adjacent areas, published seismic, gravity, magnetic and geological with agencies in the US, Canada, Japan as part of the BGS 1:1 500 000 scale data allows the development of a more and France. map series. complete, three-dimensional model for the crust. Work has commenced on the inves- Multicomponent Seismology tigation of the Southern and Eastern England region. Studies of the effects of large faults and fractures on seismic waves have demon- Interpretation strated the potential for the theoretical Software techniques developed to be used to assess The Colmap (geophysical the sealing capacity of faults in hydrocar- imaging), Ararat (track-data pro- bon reservoirs. cessing), Wellog (borehole data Geotechnical Capability processing and display) and Gravmag (2.5-D modelling) ‘Civil Engineering uses of Geophysics’ users’ input is now being incorporated into the second draft of this report for the Construction Industry Research and Information Association (CIRIA) and the (Left) Geophysical data from Geological Society. G S Kimbell southern Scotland and northern England displayed using an A database has been designed to enable interface that allows rapid access geophysical properties to be used in geo- to a wide range of images and logical ground models at the desk study models for the region. phase of geotechnical site investigations.
10 GEOPHYSICS GEOPHYSICS
PARTNERSHIP PROGRAMME
Hi-RES: the BGS is leading an initiative to sortium supported the production of the fly a new airborne High-Resolution Resource 1997 revision of the BGS Global and Environmental Survey (Hi-RES) of the Geomagnetic Model (BGGM) which UK. In collaboration with World incorporates observatory, satellite, land Geoscience, surveying has commenced on survey and marine magnetic data collected the first phase of this project, which involves by organisations world-wide. The BGGM magnetic, radiometric and electromagnetic provides magnetic reference data for direc- measurements along closely spaced (400 tional drilling of oil and gas wells, helping metres) survey lines covering a 200 x 70 kilo- to achieve geological targets and avoid well metres swathe across central England. This collisions. A UK magnetic model was phase of data acquisition is due to be produced, using data from the UK repeat completed during 1998. station network, to provide the magnetic information required for Ordnance Survey Rock mass research: hydrocarbon explo- maps. ration and waste disposal research need to understand the mechanisms of fluid flow Earthquake Monitoring and Information through low-permeability fractured rocks. Service: the UK seismic monitoring and Boreholes provide a detailed one-dimen- information service has been supported for sional examination of the rock mass, but, to nine years by a broadly-based group of determine the distribution of rock proper- customers led by the DETR, including the ties away from boreholes, wireline measure- nuclear, water and oil industries together ments and core sample determinations need with a number of public bodies. Seismic to be linked to the broad data coverage activity is monitored throughout the UK Courtesy of Geophysical Survey of Slovenia provided by seismic surveys. Recent BGS using a network of 141 seismometers with Damage from the 1998 Bovec earth- research has led to new techniques for esti- information about significant earthquakes quake, Slovenia — a reminder that mating porosity and permeability from disseminated rapidly. The data are damaging earthquakes can strike acoustic impedance. compiled into monthly and annual outside areas normally regarded as EUROPROBE: has been supported by the bulletins and reports, which are used to earthquake-prone. European Science Foundation since 1992. develop the database for seismic hazard The BGS provides scientific management assessment. of the TESZ project. Three project Seismic risk for the reinsurance industry: symposia were held. The BGS participates together with Hiscox Syndicates Ltd, the in the ‘PACE’ TMR research network, BGS launched a new system to enable rein- funded by the EC’s Human Capital and surers to assess earthquake risk (above right), Mobility Programme; two teams are in terms of monetary losses, to insurance studying the potential field geophysics and portfolios. The system, called MONICA, isotopic history of the TESZ. Regional consists of a PC-based seismic risk program magnetic, gravity (geoid) and topographic and a set of regional data files for different maps have been generated, and magnetic parts of the world. The reinsurance under- and gravity modelling has been integrated writer can handle the program from the with seismic and structural interpretation insurance viewpoint without needing to with particular emphasis on the East understand the geophysical side of the European Craton/Magnitogorsk volcanic system. arc collision zone. Sea-bottom Seismic URALIDES: this project investigates the Edinburgh Anisotropy Project: the EAP Ural Orogen, and BGS participation in the consortium grew to include 15 operating, ‘URO’ TMR research network is providing service and software companies sponsoring important new information on the research into advanced seismic methods. evolution of the fundamental boundary Processing algorithms and interpretational between the crust of Europe and Asia. techniques were developed for application to data from vertical cable and sea-bed Enterprise Oil (LAMBDA II): the impact sensors (right) and issues affecting the of fine scale sedimentary structure on petro- quality of data acquired on the sea bed physical properties, used to define the were explored. New processing methods reservoir model, has been demonstrated, were devised for application to towed and the need to image downhole core at the streamer data. Ideas on using converted same scale has been established. shear waves to image beneath basalts, Fractured carbonate core: a novel accounting for multiple reflections and technique has been developed for mapping other processing problems, were developed Vertical Cable Seismic connected fractures, and demonstrated and tested. using core from a tight carbonate reservoir. C D MacBeth Magnetic modelling: the UK Health and A report has been completed and a patent Seismic data acquisition using sea-floor Safety Executive and an oil industry con- application filed. and vertical cable sensors.
GEOPHYSICS 11 CORE AND PARTNERSHIP PROGRAMMES
Research into Britain’s Hydrogeology groundwater occurrence, movement and quality is applied to groundwater assessment, development National Groundwater Survey studying the movement of water and solutes from the land surface into the The aim of this survey is to produce a and management. Chalk aquifer. At the field site in series of comprehensive descriptions of the Hampshire, sampling of groundwater for major British aquifers and their ground- pesticides during recharge events has water resources. This is carried out in close continued, and data from a more collaboration with the Environment restricted range of soil instrumentation Agency, water companies and universities has been collected and interpreted in in the study areas. The regional survey relation to the timing and amounts of programme has initiated studies of the preferential flow in the Chalk unsatu- Chalk aquifer in the Wessex Basin and the rated zone. Further unsaturated coring North Downs. The detailed chalk stratig- was undertaken to look for pesticide raphy developed over the last few years in residues and an applied bromide tracer in the core mapping programme is to be the Chalk matrix. In the laboratory, linked to flow horizons in the chalk microcosm experiments by both the BGS aquifer to improve the understanding of and IH to determine the factors control- chalk hydrogeology. ling pesticide degradation in the unsatu- Groundwater Data rated zone have continued. Dissemination Minor Aquifers The BGS is the custodian of several This project on the physical properties of groundwater datasets of national impor- the minor aquifers of England and Wales tance, including 100 000 well records and follows on the success of the manual and data on aquifer properties, water CD-ROM database of major aquifers chemistry, water levels and geophysics. To properties data which was published early provide users of this data with improved in 1998. access, the Groundwater Data Dissemination project concentrated on Geosphere Waste developing an integrated database, Containment bringing together existing digital informa- tion with key elements of the paper A radial array of instrumented boreholes archives. The new WellMaster database is in the Mercia Mudstone Group under the complemented by on-line storage of Keyworth site was successfully used for a scanned images of well records, and forms series of in-situ, gas-injection experiments. the basis both for answering routine High-quality test data have been obtained enquiries and for developing a new genera- which match observations made previously Groundwater – our hidden asset tion of digital hydrogeological maps and in the laboratory. The field results have a booklet to increase awareness of derivative products such as CD-ROMs added to our understanding of how gases groundwater among the public. and on-line databases. move through mudrocks, and have demonstrated that the application of con- Geophysical Logging Activities ventional two-phase flow theory does not Geophysical logs of 93 boreholes have best describe the transport of high-pressure been completed during the year. Nine gases through clay-rich media. boreholes were logged for BGS strati- graphical purposes, and 23 for other Fluid-rock Reactions and purposes, mainly hydrogeology; 61 were Properties completed for water companies (left), envi- The rate and mechanism of reactions ronment agencies and engineering consul- between fluids and minerals have tancies. New software has considerably important consequences for the extractive enhanced interpretation and allowed the (e.g. hydrocarbons, metallic minerals) and group to provide sealed cross-sections disposal (e.g. landfill, nuclear) industries. employing the logging data. New experimental equipment has been D K Buckley developed to study these reactions and Geophysical logging and geochemical Transport and Fate of Pesticides enhance our ability to predict pollution sampling at the Lytchett Minster ASR In this joint project with the Institute of problems and help improve extraction trial, Dorset. Hydrology, work has continued on technologies.
12 HYDROGEOLOGY HYDROGEOLOGY
PARTNERSHIP PROGRAMME Major-aquifer properties: the Aquifer Lowflows, groundwater and wetland Properties Manual has now been interaction: this project (funded by the published. This is the product of a three- EA, UKWIR and NERC) developed a year collaborative study between the BGS framework aimed at achieving environ- and the Environment Agency. It describes mental sustainability based on considera- the physical hydraulic properties of six tion of the driving forces causing river major aquifers in England and Wales, and and wetland degradation and the con- is accompanied by a CD-ROM containing straints on groundwater management. summary data (pumping tests and core Scottish hydrogeology: the BGS, along 100 analyses) for over 2000 sites. Calcium Magnesium with the Scottish Environment Protection Sodium 80 Potassium Chloride Nitrate in the Yorkshire Chalk: a project, Agency and the water authorities, is co- Sulphate Alkalinity co-funded by the BGS and Yorkshire funding both a study of the major Devonian 60 Nitrate as N Water, to predict groundwater nitrate con- aquifer in Fife and the development of a 40
centrations in the Chalk aquifer of East groundwater database for Scotland. Cumulative Frequency % Frequency Cumulative Yorkshire has been completed. 20 Effect of old landfills on groundwater 0 PALAEAUX: this European Union- quality: boreholes into the Middle Chalk 0.1 1 10 100 1000 funded project, involving partners from outside a landfill are sampled bimonthly Concentration (mg l-1 ) Estonia, Denmark, France, Belgium, The and are automatically logged for water
100 Netherlands, United Kingdom, levels and electrical conductivity in order Barium Boron Switzerland, Spain and Portugal, has been to calibrate a contaminant transport Copper 80 Fluoride Iodide investigating the geochemical and other model. The boreholes have been used for Iron (total) Manganese 60 Molybdenum evidence for palaeowater occurrence as pesticide monitoring for the Environment Nickel Phosphorus Silica background to improved management of Agency. 40 Strontium
groundwater resources in coastal regions Zinc Cumulative Frequency % Frequency Cumulative under severe pressure due to human settle- National Groundwater Survey–tracer 20 studies: following a three year project co- ments, industry and tourism. 0 funded by the Environment Agency, a 0.001 0.01 0.1 1 10 100 1000 10000 -1 Natural baseline quality of UK ground- Manual of Tracer Testing has been Concentration (µg l ) waters: phase I of a joint project with the produced. Environment Agency has been completed Cumulative frequency plots are being covering seven areas of the main UK Hydraulic conductivity in tills: in the used to display baseline concentrations of aquifers which should be the pilot project Cottingham area of East Yorkshire, solutes in UK aquifers. for a nationwide study. These regional groundwater is abstracted from adits in the Chalk. The Chalk is overlain by tills, and studies will serve as references against Aquifer Storage Recovery (ASR) utilises work is under way, cofunded by the which current and targeted groundwater the vast capacity of aquifers to store Environment Agency and Yorkshire Water, quality may be measured (right). potable water which is injected during to provide the regulator and operator with periods of excess (winter) for use in times Natural attenuation of organic pollutants information on clay thickness and clay per- of shortage. This technique can use in groundwater: in conjunction with the sistence which will enable an informed aquifers that contain poor quality native University of Sheffield and the Institute of judgment of which areas might be more at water by creating a ‘bubble’ of fresh Freshwater Ecology, redox zones have been risk from pollution near the adits. water in the aquifer for later recovery. mapped out in the contaminant plume in the Triassic sandstone aquifer beneath a coal treated water WATER distillation plant in the Midlands. to supply TREATMENT WORKS UK Groundwater Forum: this forum provides a creative meeting ground to source of raw water promote wider understanding of ground- water recovered to meet 'summer" water issues and identify national priori- demand ASR surplus "winter" ties. The recent publication (left) of the BOREHOLE treated water to book Groundwater – our hidden assetwill groundwater storage increase awareness of groundwater among the public
CONFINING Potential for ASR in Britain: BGS/EA/ CLAY LAYER UKWIR co- funded a study to review the potential for Aquifer Storage Recovery in Britain (right), highlighting the issues "bubble" of treated water poor quality native involved through seminars and wide con- stored in aquifer goundwater displaced SANDSTONE by injected water OR FRACTURE sultation. Regulatory issues were addressed LIMESTONE AQUIFER and generic research needs were identified.