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A new ΔR value for the southern North Sea and its application in coastal research Neth. J. Geosci. (IF 1.891) Pub Date : 2021-01-20 Dirk Enters; Kristin Haynert; Achim Wehrmann; Holger Freund; Frank Schlütz
Accelerator mass spectrometry (AMS) radiocarbon (14C) dating of Cerastoderma edule (Linnaeus 1767) and Mytilus edulis (Linnaeus 1758) shells sampled in AD 1889 near the island of Wangerooge gave a new local correction factor ΔR of −85 ± 17 14C years for the Wadden Sea area. The value is considerably higher than the available scattered data from the North Sea, which were obtained from pre-bomb growth
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Dyke failures in the Province of Groningen (Netherlands) associated with the 1717 Christmas flood: a reconstruction based on geoscientific field data and numerical simulations Neth. J. Geosci. (IF 1.891) Pub Date : 2020-12-23 Björn R. Röbke; Albert Oost; Friederike Bungenstock; Peter Fischer; Bart Grasmeijer; Hanna Hadler; Lea Obrocki; Julia Pagels; Timo Willershäuser; Andreas Vött
The 1717 Christmas flood is one of the most catastrophic storm surges the Frisian coast (Netherlands and Germany) has ever experienced. With more than 13,700 casualties it is the last severe storm surge with a death toll of this order. At the same time, little is known about the hydrodynamic conditions and the morphological effects associated with this storm surge. In this study, 41 potential dyke
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Revealing the past through modelling? Reflections on connectivity, habitation and persistence in the Dutch Delta during the 1st millennium AD Neth. J. Geosci. (IF 1.891) Pub Date : 2020-12-04 Rowin J. van Lanen
This paper focuses on unravelling the 1st millennium AD in the present-day Netherlands and the applicability of modelling when studying the past. By presenting the results of several studies analysing changes (or persistence) in connectivity and habitation patterns, the significance of these findings for (spatial) modelling is derived. The transition between the Roman and early-medieval periods is
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Source-bordering aeolian dune formation along the Scheldt River (southern Netherlands – northern Belgium) was caused by Younger Dryas cooling, high river gradient and southwesterly summer winds Neth. J. Geosci. (IF 1.891) Pub Date : 2020-11-25 Cornelis Kasse; Hessel A.G. Woolderink; Marjan E. Kloos; Wim Z. Hoek
The Younger Dryas cold period caused major changes in vegetation and depositional environments. This study focuses on the aeolian river-connected dunes along the former, Weichselian Late Glacial, course of the Scheldt River in the southern Netherlands. Aeolian dunes along the Scheldt have received little attention, as they are partly covered by Holocene peat and marine deposits. The spatial distribution
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Hydrological disasters in the NW-European Lowlands during the first millennium AD: a dendrochronological reconstruction Neth. J. Geosci. (IF 1.891) Pub Date : 2020-09-29 Esther Jansma
This study presents an annually resolved dendrochronological reconstruction of hydrological impacts on the Roman and early-medieval landscape in the Low Countries of northwestern Europe. Around 600 hydrologically sensitive ring-width patterns, mostly oak (Quercus robur/petraea) as well as some ash (Fraxinus excelsior) and elm (Ulmus sp.), were selected from an initial dataset of >5000 and compiled
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Dark Ages woodland recovery and the expansion of beech: a study of land use changes and related woodland dynamics during the Roman to Medieval transition period in northern Belgium Neth. J. Geosci. (IF 1.891) Pub Date : 2020-09-29 Koen Deforce; Jan Bastiaens; Philippe Crombé; Ewoud Deschepper; Kristof Haneca; Pieter Laloo; Hans Van Calster; Gerben Verbrugghe; Wim De Clercq
The results from analyses of botanical remains (pollen, wood, charcoal, seeds) from several archaeological features excavated in Kluizen (northern Belgium) are presented. The region was largely uninhabited until the Iron Age and Roman period when a rural settlement was established, resulting in small-scale woodland clearance. The site was subsequently abandoned from c. AD 270 till the High Middle Ages
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Review of induced seismicity in geothermal systems worldwide and implications for geothermal systems in the Netherlands – CORRIGENDUM Neth. J. Geosci. (IF 1.891) Pub Date : 2020-08-05 Loes Buijze; Lonneke van Bijsterveldt; Holger Cremer; Bob Paap; Hans Veldkamp; Brecht B.T. Wassing; Jan-Diederik van Wees; Guido C.N. van Yperen; B. Jaarsma; Jan H. ter Heege
Geothermal energy is a viable alternative to gas for the heating of buildings, industrial areas and greenhouses, and can thus play an important role in making the transition to sustainable energy in the Netherlands. Heat is currently produced from the Dutch subsurface through circulation of water between two wells in deep (1.5–3 km) geothermal formations with temperature of up to ∼100 °C. As the number
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The use of geological, geomorphological and soil mapping products in palaeolandscape reconstructions for the Netherlands Neth. J. Geosci. (IF 1.891) Pub Date : 2020-07-15 Harm Jan Pierik; Kim M. Cohen
Geological, geomorphological and soil maps provide important information on the substrate as well as on the past and present physical landscape. For the intensely studied Netherlands coastal plain and Rhine–Meuse delta, many such map datasets have been compiled over the last two centuries. These mapping materials comprise older and younger legacy datasets, often fragmented over regions. They have been
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Fracture characteristics of Lower Carboniferous carbonates in northern Belgium based on FMI log analyses Neth. J. Geosci. (IF 1.891) Pub Date : 2020-06-19 Eva van der Voet; Ben Laenen; Bernd Rombaut; Mourad Kourta; Rudy Swennen
Recently drilled geothermal boreholes in Mol, northern Belgium, provide new information on the Lower Carboniferous carbonates in the Campine–Brabant Basin. Because of low primary porosity, fractures in these limestones and dolostones are of major importance for reservoir permeability. The Fullbore Formation MicroImager (FMI) log of the MOL-GT-01 borehole enabled interpretation of bed boundaries and
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Maximum Holocene groundwater levels and associated extension of peat in the border zone of ‘Het Gooi’ (the Netherlands): a reconstruction based on the study of soil transects Neth. J. Geosci. (IF 1.891) Pub Date : 2020-06-09 Jan Sevink; Sander Koopman
The area ‘Het Gooi’ in the Netherlands is part of a Pleistocene ice-pushed ridge system that partially drowned during the Holocene upon sea level and associated groundwater rise. As a result, the ridge system was gradually encroached by peat. From the late Middle Ages onward, man reclaimed the peatlands surrounding Het Gooi, heavily reducing their extension and lowering the regional groundwater level
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Accelerating geothermal development with a play-based portfolio approach Neth. J. Geosci. (IF 1.891) Pub Date : 2020-06-02 Jan Diederik van Wees; Hans Veldkamp; Logan Brunner; Mark Vrijlandt; Sander de Jong; Nora Heijnen; Corné van Langen; Joris Peijster
Over the past decade in the Netherlands, most operators have only developed a single doublet. The learning effect from these single events is suboptimal, and operators have only been capable of developing doublets in areas with relatively low exploration risk. This ‘stand-alone’ approach can be significantly improved by a collective approach to derisk regions with similar subsurface characteristics
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Ensuring safe growth of the geothermal energy sector in the Netherlands by proactively addressing risks and hazards Neth. J. Geosci. (IF 1.891) Pub Date : 2020-06-02 Graciela Jharap; Laura P. van Leeuwen; Robert Mout; Wouter E. van der Zee; Femke M. Roos; Annemarie G. Muntendam-Bos
The main objective of this paper is to give an overview of the risks seen in the exploration and production of geothermal energy from the viewpoint of the regulator. The risks are categorised as conventional risks, ultra-deep risks and enhancing factors. These risks are similar to those seen in the oil and gas industry, but the maturity of the geothermal sector in terms of managing such risks is much
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Overview of potential geothermal reservoirs in Denmark Neth. J. Geosci. (IF 1.891) Pub Date : 2020-04-17 Rikke Weibel; Mette Olivarius; Henrik Vosgerau; Anders Mathiesen; Lars Kristensen; Carsten M. Nielsen; Lars H. Nielsen
The Danish onshore subsurface contains very large geothermal resources that have the potential to make a significant contribution to transforming Danish energy consumption toward a more sustainable energy mix. Presently, only a minor fraction of this green energy is exploited in three small plants. The main factors that have hampered and delayed larger-scale deployment are related to uncertainties
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Geology of the Upper Jurassic to Lower Cretaceous geothermal aquifers in the West Netherlands Basin – an overview Neth. J. Geosci. (IF 1.891) Pub Date : 2020-03-19 Cees J.L. Willems; Andrea Vondrak; Harmen F. Mijnlieff; Marinus E. Donselaar; Bart M.M. van Kempen
In the past 10 years the mature hydrocarbon province the West Netherlands Basin has hosted rapidly expanding geothermal development. Upper Jurassic to Lower Cretaceous strata from which gas and oil had been produced since the 1950s became targets for geothermal exploitation. The extensive publicly available subsurface data including seismic surveys, several cores and logs from hundreds of hydrocarbon
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Introduction to the geothermal play and reservoir geology of the Netherlands Neth. J. Geosci. (IF 1.891) Pub Date : 2020-03-19 Harmen F. Mijnlieff
The Netherlands has ample geothermal resources. During the last decade, development of these resources has picked up fast. In 2007 one geothermal system had been realised; to date (1 January 2019), 24 have been. Total geothermal heat production in 2018 was 3.7 PJ from 18 geothermal systems. The geothermal sources are located in the same reservoirs/aquifers in which the oil and gas accumulations are