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Article Reference Diurnal variability of turbidity and light attenuation in the southern North Sea from the SEVIRI geostationary sensor.
Located in Library / RBINS Staff Publications
Booklet Reference Assessment of the marine renewables industry in relation to marine mammals: synthesis of work undertaken by the ICES Working Group on Marine Mammal Ecology (WGMME).
Located in Library / RBINS Staff Publications
Article Reference Comments on "Shoreface sand supply and mid- to late Holocene aeolian dune formation on the storm-dominated macrotidal coast of the southern North Sea" by E.J. Anthony, M. Mrani-Alaoui and A. Héquette (Marine Geology 276, 2010, 100-104).
Located in Library / RBINS Staff Publications
Article Reference Reconstructing middle to late Holocene sea-level change: A methodological review with particular reference to 'A new Holocene sea-level curve for the North Sea' as presented by K.-E. Behre': Reply to comments.
Located in Library / RBINS Staff Publications
Inproceedings Reference CCS Directive transposition into national laws in Europe: progress and problems by the end of 2011
The EU CCS Directive transposition process and related issues in 26 European countries, comprising 24 EU member states, Norway and Croatia were studied in the EU FP7 project: “CGS Europe” in 2011-2012. By the end of 2011 the transposition of the Directive into national law had been approved by the European Commission (EC) in Spain only, but had been approved at national/jurisdictional level in 12 other countries (Austria, Denmark, Estonia, France, Greece, Ireland, Italy, Latvia, Lithuania, the Netherlands, Slovakia and Sweden) and two regions of Belgium. By January 2012, the European Commission had assessed and approved national submissions of CCS legal acts transposing the Directive in Denmark, France, Italy, Lithuania, Malta, the Netherlands and Slovenia. Implementation in the UK was completed in February 2012 and by end March 2012, implementation at national level was also complete in Bulgaria, Czech Republic, Portugal and Romania.
Located in Library / RBINS Staff Publications
Article Reference Geologists at the centre of CCS research in Europe - Introduction by the EFG Panel of Experts on the Geological Storage of CO2
Located in Library / RBINS Staff Publications
Article Reference Assessing the impact of the 1498 Meio earthquake and tsunami along the Enshu-nada coast, central japan, using coastal geology.
Located in Library / RBINS Staff Publications
Proceedings Reference Did a major environmental event lead to the Late Bronze Age abandonment of the ancient harbor city of Hala Sultan Tekke? Unraveling the sedimentary record of the Larnaca salt lake, Cyprus.
Located in Library / RBINS Staff Publications
Article Reference The cost of CO2 geological storage is more than a number
CO2 geological storage is the last stage in the CO2 capture and storage process which aims to reduce CO2 emissions into the atmosphere. The cost of storage has frequently been regarded as minor compared to the cost of the whole CCS process. There are however a multitude of cost parameters that will form a unique combination for each storage project, with costs projected from one to several tens of euros per tonne of CO2 stored. Several research efforts have lately been identifying the main cost drivers and relatively wide cost ranges. Reservoir type and location, geological uncertainty, injectivity and capacity are recognised as the main source of cost variation between potential storage projects.
Located in Library / RBINS Staff Publications
Article Reference Vingt siècles d’exploitation des argiles plastiques d’Andenne (Belgique) : du gisement au musée de la céramique.
Arranged in strings, the plastic clay deposits from Andenne are fillings of cryptokarsts of white and colored clays associated with three layers of Dinantian Frasnian limestone oriented EW. Sands, brown coal and Tertiary (Neogene) clays have accumulated according to thekarstic dissolution forming a pocket of up to 100m deep. The sulphuric acid stemming from the oxidation of sulphides of brown coals is the main responsible for the formation of kaolinitic clays at the expense of clay minerals and the feldspathic sands. The circulation of water induced the leaching of the iron and their accumulation in certain horizons. White clays rich in alumina and of low iron and alkali content were the most looked for their refractory properties. Exploitedat first on surface then in subterranean galleries, the extraction reached its maximal development around the 19 and 20th centuries to stop definitively in 1970. The clay and the white sand were used in the industries of fire: glassware, crystal, metallurgy... and fed the pottery, brick, tile, earthenware factory, porcelain factories, pipe factory and the industrial refractories. The white clay first and then the final products have been exported since the Middle Ages in Holland, Germany and France, contributing to the international reputation of the clays from Andenne. Depressions generated by the subsidence as a consequence of the underground extractions form a string of pools and ponds, sources of biodiversity. Finally, the Ceramics Museum preserves the traces of this remarkable geological, mining, industrial and artistic with its outstanding collections of pottery, porcelain and pipes. Living museum holder of memory, it provides educational and cultural functions from its exhibitions.
Located in Library / RBINS Staff Publications