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Get off on the right foot. The importance of initial steps in NGS data analysis
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RBINS Staff Publications
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Getting more out of the marine equipment budget by applying open source technology
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RBINS Staff Publications 2018
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Graphic correlation of the upper Eifelian to lower Frasnian (Middle–Upper Devonian) conodont sequences in the Spanish Central Pyrenees.
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RBINS Staff Publications
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Grey monazite paleoplacers in Lower Cretaceous continental formations in the Mons Basin, Belgium.
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RBINS Staff Publications
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Grey seals Halichoerus grypus choking on common sole Solea solea
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Between 2007 and 2015, we recorded three cases of asphyxiation of grey seals Halichoerus grypus caused by a fish lodged in the respiratory tract. In all cases, the fish involved was a common sole Solea solea, which had found its way to the trachea of the unfortunate seal, as such completely blocking it. That this fish species was involved, is not surprising: it has a very agile body, with a spectacular ability to bend longitudinally into a circular shape, as well as laterally into the form of a cigar - the way it was found in the gluttonous grey seals. The common sole currently occurs abundantly in coastal waters of the southern North Sea, and it constitutes an important part of the diet of grey seals in this area. Asphyxiation due to fish has been described in odontocetes, including in harbour porpoise Phocoena phocoena, bottlenose dolphin Tursiops truncatus, and very recently in long-finned pilot whale Globicephala melas. To our knowledge however, this cause of death has not been described before in grey seals. Furthermore, the significance of this cause of mortality in a single population has not been documented, with in particular aspects of prey abundance, seal behaviour and the limited number of stranded adult grey seals that are being investigated to be considered. Keywords: grey seal; Halichoerus grypus; common sole; Solea solea; asphyxiation; respiratory tract
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RBINS Staff Publications 2016
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Grey seals predating on harbour porpoises: a recent and spreading phenomenon? 27th Conference of the European cetacean society: Interdisciplinary approaches in the study of marine mammals.
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RBINS Staff Publications
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Ground Deformations Observed for Three Decades (1992-2022) above Old and Deep Coal Mines Reused for Deep Gas Storage Sites (Wallonia, Belgium) using PS-InSAR Time-series.
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The coal mining exploitations in Wallonia was gradually phased out till the end of the last century. Groundwater pumping was ceased, implying a groundwater rebound at varying rates that can still be observed by radar interferometry. The sustainability of architectural and technical facilities within those zones must be monitored to reduce environmental concerns during the post-mining phase and their reuse as gas storage reservoir locations. PS-InSAR approach has shown land surface deformations during three decades in a large area (96 km²) covering the cities from Binche to Anderlues (Wallonia, Belgium). Two coal mines are concerned: (i) to the West, the Ressaix-Mariemont-La Louvière concession where a small part was used as the Peronnes Gas Storage (PGS) reservoir; (ii) to the East, the Bois de la Haye concession where about half of the area has been used as the Anderlues Gas Storage (AGS) reservoir. To maintain the PGS reservoir dry, a private company has maintained groundwater pumping activities till 1998 with a dewatering rate of 40 m³/h. After 1998, the water levels raised from 8 m/yr at the beginning to 2.5 m/yr around 2010. The gas storage reservoir of Anderlues is known to be relatively dry. Using a multi-sensor radar dataset including radar images acquired by the European Space Agency’s satellites of ERS1/2, ENVISAT ASAR, and Sentinel-1A, 236 interferograms were constructed. Ground displacements are mapped and subdivided into three successive time intervals showing: (1) during ERS1/2 (1991-2000), a gradient from positive annual average velocities (West) to negative ones (East) across the PGS site and mostly negative values (-0.5 to -3.0 mm/yr) above the AGS site; (2) during ENVISAT ASAR (2003-2010), the positive LOS velocities (0.5 to 2.89 mm/yr) are present along an NW-SE ellipsoid across PGS leaving only negative LOS values in the NW corner while negative LOS velocities were also recorded along the Binche city (-0.5 to -2 mm/yr). During the same period, the AGS is facing negative LOS velocity values and extending to the south as well; (3) during Sentinel-1A (2015-2022), almost all the PGS is affected by positive annual LOS velocities (0.5 to about 4-5 mm/yr) even extending towards the north outside the limits of PGS. AGS is still affected by negative LOS values in the middle and SE parts. Ground displacements measured at the surface of old coal mine concessions and recent gas storage sites allow following the impact of the use of the subsurface through time.
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RBINS Staff Publications 2022 OA
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Ground Deformations Related to an Old Drainage Adit in The Abandoned Coal Concession Around Saint-Vaast (Wallonia, Belgium) Analysed Using PS-InSAR and Piezometric Wells Time Series
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The exploitations of the coal mines in Wallonia were ceased progressively till the end of the last century. Groundwater pumping’s were stopped inducing a groundwater rebound with different rates but still visible today with radar interferometry. To mitigate the threats to the environment during the post-mining period, flooding and outbreak risks, surface ground deformations and the stability of civil engineering infrastructures in the vicinity of those mined areas need to be monitored. The persistent scatterer radar interferometry technique (PS-InSAR) has revealed ground displacements during three decades in Saint-Vaast (Wallonia, Belgium). Under this residential area, an old drainage adit at a depth of approximately 30 m allows mine water discharge to the Haine river. A confined aquifer lies in this Wealdian sandy layer characterized by a weak mechanical resistance and frequent loose sandy pockets. The Saint-Vaast area has so far suffered twice from a clogging rupture in the drainage adit. The clog has induced an underground water pressure increase in the confined aquifer. This water outbreak resulted in a stream of mud, sand and water flowing out during a few days in 2009. This event has induced a displacement at the surface with cracks observed in the walls of several houses nearby. 236 interferograms were produced using images acquired by the ESA’s satellites (ERS1/2, ENVISAT and Sentinel-1A). A time serie of surface displacements from 1991 to 2022 is calculated. Land surface displacements trends before and after both events were recognized. During ERS1/2 (1992–2002) an uplift has a rate exceeding 3 mm/year. The saturation of the Wealdian aquifer sands reduces the effective intergranular stress leading to an uplift. Groundwater recharge slowed down after the uplift and turned to almost stability during ERS (2002-2006) and ENVISAT (2003–2010). The sudden water outbreak in 2009 has resulted in a localized land subsidence. Before and after the second outflow associated to a clog rupture in early 2018, a similar pattern of land surface deformations was observed. After 2018 (Sentinel-1A), the average LOS velocity values are -1.8 mm/year where the 2009 event occured. Piezometric wells drilled after the 2009 event are monitoring the groundwater levels in the Wealdian aquifer. Analysis of piezometric data combined with PS-InSAR allowed to compare the water table evolutions in the confined aquifer and the ground deformations observed at the surface.
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RBINS Staff Publications 2022 OA
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Guide Field book of the international workshop: “About Haematite. Procurement and transformation during recent prehistory.”
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RBINS Staff Publications
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H3O – a better understanding of Campine cross-border Cenozoic stratigraphy
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RBINS Staff Publications 2016
