Surface movement above old coal longwalls after mine closure

Although most subsidence occurs in the months and years after mining by the longwall method, surface movement is still occurring many decades after the mining. The aim of the study is to quantify the long term behavior. Satellite data (radar-interferometry) were analyzed to study an area of about 2 ...

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Main Authors: André Vervoort, Pierre-Yves Declercq
Format: Article
Language:English
Published: Elsevier 2017-05-01
Series:International Journal of Mining Science and Technology
Online Access:http://www.sciencedirect.com/science/article/pii/S2095268617302306
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author André Vervoort
Pierre-Yves Declercq
author_facet André Vervoort
Pierre-Yves Declercq
author_sort André Vervoort
collection DOAJ
description Although most subsidence occurs in the months and years after mining by the longwall method, surface movement is still occurring many decades after the mining. The aim of the study is to quantify the long term behavior. Satellite data (radar-interferometry) were analyzed to study an area of about 2 km2 during the 18 years following the closure of the underground infrastructure and the flooding of the underground workings and rock mass. It was observed that, on average, a residual downward movement took place till 7–12 years after the closure, followed by a clear uplift. However, the first signs of an uplift occurred in certain sub-areas 3–4 years after the closure. Zones within the area studied were identified with either larger or smaller movements. However, the spatial variation of the surface subsidence or uplift could not be directly explained by the characteristics of mining. Keywords: Coal mining, Surface movement, Subsidence, Uplift, Radar-interferometry
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spelling doaj.art-eb415d69cb6c443e99b075ee3029de902022-12-21T19:52:43ZengElsevierInternational Journal of Mining Science and Technology2095-26862017-05-01273481490Surface movement above old coal longwalls after mine closureAndré Vervoort0Pierre-Yves Declercq1Department of Civil Engineering, KU Leuven, Leuven 3001, Belgium; Corresponding author.Geological Survey of Belgium, Royal Belgian Institute of Natural Sciences, Brussels 1000, BelgiumAlthough most subsidence occurs in the months and years after mining by the longwall method, surface movement is still occurring many decades after the mining. The aim of the study is to quantify the long term behavior. Satellite data (radar-interferometry) were analyzed to study an area of about 2 km2 during the 18 years following the closure of the underground infrastructure and the flooding of the underground workings and rock mass. It was observed that, on average, a residual downward movement took place till 7–12 years after the closure, followed by a clear uplift. However, the first signs of an uplift occurred in certain sub-areas 3–4 years after the closure. Zones within the area studied were identified with either larger or smaller movements. However, the spatial variation of the surface subsidence or uplift could not be directly explained by the characteristics of mining. Keywords: Coal mining, Surface movement, Subsidence, Uplift, Radar-interferometryhttp://www.sciencedirect.com/science/article/pii/S2095268617302306
spellingShingle André Vervoort
Pierre-Yves Declercq
Surface movement above old coal longwalls after mine closure
International Journal of Mining Science and Technology
title Surface movement above old coal longwalls after mine closure
title_full Surface movement above old coal longwalls after mine closure
title_fullStr Surface movement above old coal longwalls after mine closure
title_full_unstemmed Surface movement above old coal longwalls after mine closure
title_short Surface movement above old coal longwalls after mine closure
title_sort surface movement above old coal longwalls after mine closure
url http://www.sciencedirect.com/science/article/pii/S2095268617302306
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