Geological Survey of Denmark and Greenland Bulletin 28, 2013, 13-16
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Geology, seismic activity and groundwater conditions at six potential disposal sites for radioactive waste from Risø, Denmark Peter Gravesen, Bertel Nilsson, Merete Binderup, Tine B. Larsen and Stig A. Schack Pedersen In 2003 it was decided by the Danish Parliament that low- tential sites and their surroundings were performed by the and intermediate-level radioactive waste from the Danish Geological Survey of Denmark and Greenland aided by the nuclear research facility, Risø, is to be stored at a permanent Danish Nature Agency (Naturstyrelsen), and included drill- disposal site (Ministeriet for Sundhed og Forebyggelse 2008; ing of several new boreholes. Gravesen et al. 2012a). Both the issue of storage and the selec- tion of potential sites have caused considerable public debate. In this paper we report on the most recent geological inves- Geological setting tigations intended to further improve the data base for the The areas that were chosen for further study were selected selection and decision process, although no conclusions have from 22 initial targets (Gravesen et al. 2011) based on com- been drawn at this stage. pliance with specific criteria (see below) that had previously The waste might be deposited on the land surface, partly been established from geological models (Gravesen et al. below surface or totally below surface, and pre-Quaternary 2012a). The six selected areas (Fig. 1) are located in differ- rocks and deposits are the main general targets. In 2011 six ent geological settings. The Østermarie-Paradisbakkerne potential areas were selected for further studyd and evalua- area on Bornholm consists of Precambrian Paradisbakke tion of their suitability for disposal of radioactive waste. The migmatite and Bornholm gneiss. In the Rødbyhavn area on study evaluated local groundwater conditions and earth- Lolland, Palaeocene clay rests on Maastrichtian chalk, while quake hazards, infrastructure, wildlife, environment, water the Kertinge Mark area on Fyn comprises thick Palaeocene supply (especially drinking water) and heritage monuments clay deposits overlying Danian Limestone. In the Hvidbjerg (Gravesen et al. 2011, 2012b). The new studies of the six po- area of north-west Jylland, Palaeocene and Eocene clay for- 10°E 14°E Skagerrak North Sea 57°N Kattegat TThise Hvidbjerg Skive vest Fig. 2 SWEDEN DENMARK Jylland Sjælland KerKertinge Mark Østermarie- Paradisbakkerne Fyn Bornholm Møn Fig. 1. Map of Denmark showing the locations of 55°N Baltic Sea the six areas selected for detailed studies of their Lolland Falster suitability as disposal sites for radioactive waste Rødbyhavn GERMANY from Risø. 50 km © 2013 GEUS. Geological Survey of Denmark and Greenland Bulletin 28, 13–16. Open access: www.geus.dk/publications/bull 13 West (Rettrup) East (Skive) Fig. 2. Geological cross section through Palaeo- 55.1068 gene–Neogene deposits of the Skive vest area, .1072 .1119 .383 .418 .1120 .532 extending from Rettrup in the west to Skive in .311 .657 .1228 .1069 .1022 .507.1229 .533 .503 .152 .85 .180.114 .148A the east. The positions of the boreholes with +40 DGU numbers are indicated along the top of the +30 figure. +20 +10 Vejle Fjord Formation 0 Depth (m) –10 –20 Brejning Formation Skive Clay 1 km –30 Palaeogene–Neogene deposits Clayey till Meltwater sand mations rest on Danian Limestone and are covered by Oli- gocene and Miocene clay formations. Farther to the east and Survey results south-east, at Thise and Skive vest (west), Oligocene and Data from the borehole samples and from the geophysical Miocene clay, respectively, are present. Quaternary clayey till logs have provided important new information on the geo- overlies the pre-Quaternary rocks and sediments at all sites. logical models of the investigated areas, which comprise data on lithology and stratigraphy as well as tectonic and sedi- mentological structures. All the relevant information has Collection of seismic, borehole and been compiled into six technical reports by the Geological groundwater data Survey of Denmark and Greenland, which are available at Part of the new study consisted of an evaluation of earth- GEUS’ website, http://www.geus.dk/program-areas/nature- quake potential. The seismic activity in Denmark has been environment/denmark/radioaktivt_affald/index-dk.htm. recorded instrumentally since 1929, and in later years by an The main topics are: boreholes and logging, seismic activity interconnected network of seismic stations in Denmark and and earthquakes, groundwater and drinking water, climate surrounding countries. Older earthquakes were examined and climate changes and local planning (infrastucture, wild- from descriptions in the literature. For the three potential life, environment, cultural heritage, raw materials, agricul- sites on Bornholm, Lolland and Fyn available seismic data ture and water supply structure). All this information will be within a radius of 50 km were evaluated. For the three areas used in the ongoing evaluation of the areas and identification in north-west Jylland a radius of 75 km was used. of the two most suitable areas. In this paper only selected re- In the new study additional boreholes were drilled in each sults are presented, including geological traverses through of the six selected areas. Sediment samples were collected the six areas. from each metre and analysed, and several types of continu- ous geophysical logs were performed in most boreholes. Such logs are particularly useful for extrapolations between the Geological data samples. On Bornholm, eight existing water abstraction The Precambrian crystalline rocks on Bornholm are thick wells for domestic use were logged for idenfication of frac- and extensive and contain a network of fractures. Knowledge tures in the bedrock. of the fracture systems in the Østermarie-Paradisbakkerne Evaluation of groundwater, drinking water and water sup- area is important for evaluation of groundwater flow and plies was based on new information and existing literature, as storage, and for evaluation of the stability of the host rocks. well as local knowledge of potential groundwater problems. Horizontal and vertical fractures to a depth of 12 m can be The latter was obtained by interviewing local specialists and observed in quarries. The number of horizontal fractures ap- acquisition of written accounts and other information col- pears to decrease downwards, while their spacing increases. lected by the local authorities. This is a normal observation in the uppermost crust. The geophysical borehole logs comprise natural gamma-ray, resis- tivity, sound velocity, fluid temperature, fluid conductivity and flow logs, which can be used to document fractures at various levels from 20 m below the surface down to a depth 14 Fig. 3. Earthquake epicentres in the north-west Jylland Magnitude 1 Kristiansand 9˚E 10˚E 11˚E region. The magnitude on the Richter scale is shown by Magnitude 2 the size of the dots (from Gravesen et al. 2012b). Other Magnitude 3 58˚N earthquake epicentres in the Danish region are not shown Magnitude 4 No Magnitude on this map. Skagerrak Kattegat Aalborg 57˚N 57˚N North Sea Denmark Aarhus 56˚N Horsens 6˚E 7˚E 8˚E 9˚E 10˚E 11˚E of 90 m. Extrapolations of the borehole data suggest that clay of the Kerteminde marl in the northern part of the some fractures are horizontal or subhorizontal and connect- Kertinge Mark peninsula, forming the natural stratigraphi- ed over larger distances. Quaternary clayey and sandy tills on cal sequence. Quaternary clayey till up to 40 m thick is found Bornholm are mostly only a few metres thick. above these formations. Some layers are very sandy and grav- The pre-Quaternary rocks and deposits throughout the elly as shown by samples from the boreholes and from geo- remaining parts of Denmark are fine-grained, have low per- physical logs. meability, and are covered by Quaternary clayey tills. The In the Hvidbjerg area, Palaeocene and Eocene grey clay clay deposits are generally relatively thick and appear to be of the Kerteminde Marl and diatomite from the Fur Forma- of wide horizontal distribution within the selected areas, tion rest on Danian Limestone on the northern flank of the reflecting the fact that the deposits represent marine depo- Uglev salt diapir. The formations are covered by Oligocene sitional environments. Furthermore, the deposits are char- and Miocene black-brown mica clay deposits from the Brej- acterised by low degrees of glaciotectonic disturbance and ning and Vejle Fjord Formations, with a total of up to 100 m pre-Quaternary tectonic movements. These characteristics thickness. Thick Quaternary clayey till comprises the top meet the criteria described by Gravesen et al. (2011, 2012a) 20 m. The new borehole demonstrates a more complex build- based on the guidelines of the International Atomic Energy up of the succession with unconformities caused by tectonic Agency (IAEA 1994). episodes and erosion. At Rødbyhavn, Palaeocene fine-grained deposits and plas- In the Thise area, more than 100 m thick layers of Oligo- tic clay from the Æbelø and Holmehus Formations resting cene mica clay from the Brejning Formation and green-grey, on Maastrichtian chalk have been documented from geo- fine-grained clay from the Branden clay unit are covered by physical surveys and boreholes drilled for bentonite explora- up to 18 m thick Quaternary clayey till. The new borehole tion and geotechnical purposes related to the Femern Bælt penetrated 22 m of Brejning Formation below 19 m of Qua- Fixed Link. The characteristics of the c. 80 m thick clay se- ternary clayey till. The Oligocene deposits form an erosional quence and the overlying up to 40 m thick hard Quaternary inlier bordered by buried valleys filled with Quaternary till clayey till demonstrate that the deposits are in situ, although and meltwater deposits. tectonic disturbances are known to exist outside the area. In the Skive vest area, up to 100 m of Oligocene and Mio- Within and just outside the Kertinge Mark area, up to cene deposits of fine-grained grey Skive Clay unit (to the 75 m thick Palaeocene Kerteminde Marl and Æbelø For- east) and black-brown mica clay from the Brejning and Vejle mation overlying Danian limestone have been documented.