Skip to content. | Skip to navigation

Personal tools

You are here: Home
2364 items matching your search terms.
Filter the results.
Item type



































New items since



Sort by relevance · date (newest first) · alphabetically
Inproceedings Reference Areas Prone to Land Subsidence and their Evolutions in Belgium During the Last 30 Years
PSInSAR analyses across Belgium using ERS 1-2, ENVISAT, TerraSAR-X and Sentinel 1 allowed to follow several ground movements areas during the last three decades. Several areas of regional importance are affected by land subsidence processes that have been observed during this period (i.e. the alluvial plain of the Schelde estuary in Antwerpen, a large area in the West Flanders province and one around Merchtem area). Other land subsidence areas associated to old coal mining both in Flanders (Campine basin) and Wallonia (Hainaut and Liège province) are affected by progressive uplifting conditions linked to the mining aquifer piezometric rebound. It is extremely important to follow the spatio-temporal behavior of these phenomena to forecast their influences and their effects on the urban developments.
Located in Library / RBINS Staff Publications 2021
Inproceedings Reference Land Subsidence Observed in the Merchtem Area (Flanders) – 30 Years of SAR Data Associated to Groundwater Withdrawal?
A land subsidence affecting several towns at the joining limits of the Belgian Provinces of East Flanders, Antwerp and Flemish Brabant is followed during the last three decades. ERS 1–2, ENVISAT, TerraSAR-X and Sentinel-1A satellites SAR scenes were processed from 1992 till October 2020 to map the land subsidence evolution. The subsidence corresponds to a surface area of 220 km 2 during the ERS 1/2 time interval distributed over three distinct subsidence bowls. During the ENVISAT and TerraSAR-X time interval, only one residual subsidence bowl was mapped affecting a surface area of about 70 km 2 . Several towns (Londerzeel and Steenhuffel) remained in the center of the subsidence bowl. The annual average negative velocity values range between −5.99 and −0.5 mm/year. During the Sentinel-1A period, the subsidence bowl has lost half of its surface reaching 36 km 2 . The LOS velocity values have also decreased during the period 2016–2020.
Located in Library / RBINS Staff Publications 2021
Inproceedings Reference Application of a Bayesian method for investigating the probability and uncertainty of a two-class flocculation kinetic model
Located in Library / RBINS Staff Publications 2019
Inproceedings Reference object code Integrated tracers using genomics, otolith shape and microchemistry to measure sole connectivity at the regional and North-East Atlantic scales
Located in Library / RBINS Staff Publications 2017
Inproceedings Reference A One Health team to improve Monkeypox virus outbreak response: an example from the Democratic Republic of the Congo
Located in Library / RBINS Staff Publications 2017
Proceedings Reference A modelling tool to assess dispersal abilities of Antarctica species
Located in Library / RBINS Staff Publications 2017
Inproceedings Reference A pragmatic at-sea solution to comply with the multisource multibeam backscatter conundrum
Located in Library / RBINS Staff Publications 2023
Unpublished Reference De Odyssee van de Kleine Zwaan, een andere route naar Griekenland
Located in Library / No RBINS Staff publications
Unpublished Reference The results of the use of innovative methods for monitoring and study of migrating anseriformes
Located in Library / No RBINS Staff publications
Unpublished Reference Les résultats de la saison 2016
Located in Library / No RBINS Staff publications