The problem of rock spoil from a proposed underground nuclear waste repository in West Cumbria. David Smythe. 11 October 2011

Similar documents
Why West Cumbria is unsuitable for a deep geological nuclear waste facility

The Ennerdale granite: Implications of a nuclear waste repository development. David Smythe October 2012

Why West Cumbria is unsuitable for a deep geological nuclear waste facility

Why West Cumbria is unsuitable for a deep geological nuclear waste facility: Allerdale

Auckland Transport. Auckland Council. Statement of Evidence of Simon John Ferneyhough

The volunteer process of site selection for radwaste disposal in Canada:

Risks of environmental contamination from proposed fracking in the Fylde, Lancashire

INTRODUCTION. Climate

Mineral Formation & Mining

about GCC

Land at Larchwood Farm, Whitehorse Lane Finchampstead, Berkshire

SOTMAS Geophysical Survey of Norbury Moated Manor house

Illustrator: Vector base Each line/point store some sort of information Mapping Representation of the world

Présentation orale par. Oral Statement from. Peter Ottensmeyer. Peter Ottensmeyer PMD 13-P1.139

The use of Underground Research Facilities in the development of deep geological disposal

Swift Creek Sediment Management Action Plan (SCSMAP)

ENGINEERING EVALUATION OF THE STANLEY MINE ADVENTURE PARK AREA CLEAR CREEK COUNTY, COLORADO. Prepared for:

Urban Planning Word Search Level 1

Presented by: Bryan Bloch GIS Specialist DNREC Division of Watershed Stewardship

What Do You See? FOR 274: Forest Measurements and Inventory. Area Determination: Frequency and Cover

ENGINEER S CERTIFICATION OF FAULT AREA DEMONSTRATION (40 CFR )

Dark Satanic Hills Slate quarries

Land use study of Mellieha Valley

5.11 MINERAL RESOURCES

IMPERIAL COUNTY PLANNING AND DEVELOPMENT

Current Status of Program for Geological Disposal of high-level radioactive waste (HLW) in Japan 1

Would a deep nuclear waste repository in West Cumbria be. Dr Helen Wallace

How we made the maps. By Chris Walker. Map US Coast Survey

Geology and the Aggregate Industry: The Role of Geologists

Initial Borehole Drilling and Testing in Central Huron,

GM POWERTRAIN BEDFORD FACILITY BEDFORD, INDIANA

Initial Borehole Drilling and Testing in or Near Ignace

Bramley Grange, Horsham Road, Bramley, Surrey

RURAL SETTLEMENT PATTERNS AND ACCESS TO DEVELOPMENT LAND: DEVELOPING THE EVIDENCE BASE

Neighborhood Locations and Amenities

Barrow Offshore Wind Farm

Livingston American School 4 th Quarter Curriculum Map

Archaeological Survey and Evaluation at 8954 El Dorado Parkway, El Cajon, San Diego County, California

WATER RESOURCES AND URBANIZATION Vulnerability and Adaptation in the Context of Climate Variability

Directive on the Assessment and Management of Environmental Noise

Geodatabase for Sustainable Urban Development. Presented By Rhonda Maronn Maurice Johns Daniel Ashney Jack Anliker

Measuring connectivity in London

Roman Farm, Nettleden, Hemel Hempstead, Hertfordshire

Different types of maps and how to read them.

DIRECTORY OF COAL MINES IN ILLINOIS

Background. Valley fills Sites in the Area. Construction over Mine Spoil Fills

Appendixx C Travel Demand Model Development and Forecasting Lubbock Outer Route Study June 2014

The outermost container into which vitrified high level waste or spent fuel rods are to be placed. Made of stainless steel or inert alloy.

Clays in Geological Disposal Systems

225 Bush Street Suite 1700 San Francisco, CA phone fax

Warwickshire Geological Conservation Group

Flash flood disaster in Bayangol district, Ulaanbaatar

GIS data classes used within the November 2013 Environmental Statement Engineering Maps

Chapter 5. GIS The Global Information System

Cuyama Basin North Fork Vineyard

Techniques for Science Teachers: Using GIS in Science Classrooms.

Northamptonshire Archaeology

Winning Farm of Winchester

THE CHARACTERIZATION OF ABANDONED URANIUM MINES (AUM) IN NEW MEXICO

presents challenges related to utility infrastructure planning. Many of these challenges

Phase 1 Geoscientific Preliminary Assessment Southern Ontario, Sedimentary Communities

Land adjacent to 103 Pound Lane, Sonning, Berkshire

2267 N o r t h 1500 W C l i n t o n U T 84015

HAZUS-MH: Earthquake Event Report

COPPER KING GOLD COPPER PORPHYRY LARAMIE COUNTY, WYOMING

Navigating to Success: Finding Your Way Through the Challenges of Map Digitization

INDOT Office of Traffic Safety

What is a map? Understanding your map needs

THE MINISTRY OF ENERGY AND ENERGY INDUSTRIES MINERALS DIVISION MINE DESIGN TEMPLATE OPERATOR NAME: OPERATOR ADDRESS: PHONE NUMBER: FACSIMILE:

Transport Planning in Large Scale Housing Developments. David Knight

8 th 12 th Designing a Monitoring Plan Mapping & Analysis (Activities 1 2)

HERON ENTERS OPTION TO PURCHASE A1 GOLD MINE, EASTERN VICTORIA

APPENDIX A GLOSSARY. Appendix A.1

For personal use only

Is It Safe to Frack Beneath Lake Lewisville?

Spatially Connected Government in Great Britain. Peter Hedlund CEO Ordnance Survey International

Why a deep nuclear waste repository should not be sited in Cumbria: a geological review

Figure 1 Major Tectonic Plates. a) What evidence is there that tectonic plates are able to move across the Earth s surface?

Factors Affecting Human Settlement

Koenji. Using ARCGIS Online to explore a place

BASINS RIVER. Luzon. Mekong. Java. Delta. Phraya. Chao. Delta. Malaya. Coast. West. Irrawaddy. Delta

PROBABILISTIC TRANSPORT PATH ANALYSIS THROUGH THREE-DIMENSIONAL DISCRETE FRACTURE NETWORKS FOR UNDERGROUND RADIOACTIVE WASTE DISPOSAL FACILITIES

Landslide susceptibility and landslide hazard zoning in Wollongong. University of Wollongong, NSW, AUSTRALIA

In-situ Experiments on Excavation Disturbance in JNC s Geoscientific Research Programme

APPENDIX B: REPORT ON GEOPHYSICAL SURVEY, JULY 1998

Advanced Algorithms for Geographic Information Systems CPSC 695

Drehid MBT Facility- Waste Licence EIS

An Open-pit Mine Spatial Dataset for Guizhou Province (2015)

Initial Borehole Drilling in the Hornepayne and Manitouwadge Area

MCDR INSPECTION General. Date of Inspection Name of the Mine Bhatbhera Limestone Mine 2 Total Lease Area (Ha)

1. INTRODUCTION, AIMS AND SCOPE

PRELIMINARY WORKING DRAFT Work in Progress

MUG Presentation. Quantifying Habitat Disturbance by Marcellus Shale Drilling Activities in Pennsylvania. Introduction. Previous Work.

APPENDIX N View Impact & Shadow Analysis

Tuesday 6 June 2017 Afternoon

ALDERON IRON ORE CORP. ENVIRONMENTAL IMPACT STATEMENT KAMI IRON ORE MINE AND RAIL INFRASTRUCTURE, LABRADOR. Appendix P

Advancing Geoscientific Capability. Geological Survey of Finland

MAPWORK PRACTICE EXERCISES 13+ ABERDEEN

Big Rivers Electric Corporation Disposal of Coal Combustion Residuals (CCR) from Electric Utilities Final Rule CCR Impoundment Liner Assessment Report

Visual Resources & CPV Valley

Transcription:

The problem of rock spoil from a proposed underground nuclear waste repository in West Cumbria David Smythe 11 October 2011

A letter dated May 2011 from the Nuclear Decommissioning Authority (NDA) to Cumbria County Council states: all of the excavated rock spoil could be stored on the surface and then either re-used in construction and backfilling, or for landscaping and site restoration. Under this scenario there would be no requirement to transport rock spoil off-site. Under different scenarios there may be surplus rock spoil to be taken off-site. In such cases it is likely that bulk spoil transport would be by rail. This statement is completely misleading. In fact the NDA commissioned an environmental report (October 2010) in which precise figures are given. The amounts are considerable, as this slideshow demonstrates.

This is a typical NDA image of what a repository is supposed to look like. It shows idealised green countryside and simple ideal geology (flat homogeneous layers). The picture omits the fact that the surface will be converted into an industrial zone spread over several square kilometres, and in existence for more than a century. The idealised geology shown here has no resemblance to the actual geology of West Cumbria. Image source: NDA Geological disposal. Steps towards implementation. March 2010

The Great Pyramid of Cheops (or Kheops) at Giza, Egypt, has a volume of 2,500,000 cu. m. It is 140 m high. A London Routemaster bus is shown at the foot for scale, as the people in the photo are too small to be seen clearly. In the following slides I have visually modelled the effect of spoil heaps in West Cumbria, by assuming that they are built in the form of the Great Pyramid. Of course, they will not in fact be built to that shape, but rather in the form of low flat-topped mounds called bunds. But the pyramid has the smallest possible footprint that a stable mound of rubble and stone could occupy.

If a repository were to be excavated in the Eskdale granite, the site works might be in the Irt Valley. The spoil which has to be stored for final use as backfill is equivalent to 2 pyramids. The upper view is a 3D GIS view of the valley, on which I have superimposed the two backfill pyramids. Both views are looking south from Sandbank.

Muncaster Fell This is the GIS 3D map, looking east from Irton House (OS grid 308840, 499575). The pyramids are 2.3 km distant.

Google Street View looking east from Irton House, as in the previous graphic, and with the pyramids superimposed.

GIS 3D map, looking north-east from the Ravenglass & Eskdale railway line at the foot of Muncaster Fell.

The two pyramids seen from about 50 m uphill on Muncaster Fell to the south. They are 140 m high. The Blackpool Tower, shown for scale, is 158 m high. The Routemaster bus (4.4 m high) is also shown for scale near the nearest corner of the nearer pyramid.

The Eskdale problem The previous slides illustrate the problem of how and where to store the 4.84 million cu. m. of spoil to be used for backfill. It will be around on the surface for about a century. In addition we have 11 million cu. m. of excess spoil, not to be used for backfilling, which must either be stored permanently as bunds or taken away. This volume is another 3½ pyramids-worth.

Eskdale: Transport off-site of excess spoil Granite spoil does have a commercial value as an aggregate. It would have to be shipped out by rail or road. One possibility would be (compulsory) purchase of the existing miniature railway line, which originally served the haematite mines in the nineteenth century. This line could be reupgraded to a modern gauge, and connects into the national rail network at Ravenglass. Source: wiki Ravenglass & Eskdale Railway

Eskdale: Transport off-site of excess spoil (continued) If removed by road, we have 18 million tonnes to shift. The capacity of a dumper truck on public roads is 44 tonnes, which means 407,000 loads. This means 112 loads per day every day for (say) 10 years. Assuming an 8 hour day, the traffic out will be one truck every 4 minutes, plus an empty truck returning. In comparison, the traffic frequency for the transport of radioactive waste to the repository during its lifetime (which the NDA letter quotes in detail) is insignificant between 10 and 35 loads per week.

Pyramids or bunds? So the NDA can solve the problem of unused and commercially valuable excess spoil in Eskdale ship it out by rail and/or road and sell it. Of course, the two pyramids-worth of backfill spoil to be retained for up to a century will not actually be stored in pyramids. Realistically, it will be stored in flat-topped mounds called bunds. If the bunds are 5 m high, we need 1 sq km to store the spoil. This is the same area as the Drigg low-level waste repository. The problem with the coastal strip of West Cumbria, between Workington and Barrow, is that it is too narrow. Where is such an area to be found?

The Solway problem A proposed repository sited in the Solway plain area would be excavated in so-called lower strength rocks, such as the Mercia Mudstone. In this case we have 15 million cu. m. of excess spoil, which cannot be used for backfilling, nor which has any commercial value. This volume is 6 pyramids-worth, for which permanent storage must be found. Assuming bunds 5 m high, some 2.9 sq km of land would be needed that is 2900 Ha, or 7400 acres.

Conclusion I have demonstrated (elsewhere) that no possible underground repository site can be found within the area of Copeland and Allerdale district councils, that would be geologically safe. In addition to the insurmountable geological problems, the NDA is misleading the elected officials and the general public of West Cumbria as to the scale of environmental blight to be caused, were such a repository to be excavated. The MRWS:Cumbria partners need to ask some searching questions of the NDA; in particular, why the figures from the NDA s own environmental assessments, used herein, have not been presented in a more honest and transparent way.

Appendix Calculations Source: Upper inventory from: Nuclear Decommissioning Authority 2010. Geological Disposal: Generic Environmental and Sustainability Report for a Geological Disposal Facility Assessment Report October 2010. The upper inventory includes Pu/U waste, but no new build waste. Higher strength rocks: 3589000 m3 spoil is stored for backfill, 6640921 m3 excess is taken off-site. Density 2.7 tonnes m-3. Lower strength rocks: 1177500 m3 spoil. Density 2.5 tonnes m-3. Assumed spoil density is 2.0 tonne m-3, so solid rock spoil volumes are multipled by 2.7/2.0 or 2.5/2.0 (higher and lower strength, respectively). Mass calculated for granite transport is the solid rock volume multipled by 2.7.