Laurent Chalumeau
University of Reims Champagne-Ardenne
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Featured researches published by Laurent Chalumeau.
Geological Society, London, Special Publications | 2014
Aurélie Turmel; Gilles Fronteau; Céline Thomachot-Schneider; Claire Moreau; Laurent Chalumeau; Vincent Barbin
Abstract Reims Cathedral is a major monument in the NE of France originally built with local Lutetian limestone. The recent closure of the last quarries has made restoration using the same stone more complicated. The restoration stones used currently are Lutetian limestones from the centre of the Paris Basin (Saint-Pierre-Aigle and Saint-Maximin stones). Mapping of the Cathedrals façades confirmed the data from ancient manuscripts: Courville stone was the original building stone, but several other local stones from various quarries and beds were also used. As a follow-up to this mapping, Lutetian limestones from five disused quarries were sampled for petrophysical characterization tests: thin section analyses, porosimetry, capillary and drying kinetics. The petrophysical properties of the limestones showed differences between the two main local stone types (Ditrupa limestone and miliolids limestone) and also between the quarries. This study addresses the difficulty of selecting new stone for restoration. Should ancient quarries be re-opened? If so, which ones?
Geological Society, London, Special Publications | 2016
Aurélie Turmel; Gilles Fronteau; Laurent Chalumeau; J.-P. Deroin; S. Eyssautier-Chuine; Céline Thomachot-Schneider; T. De Kock; Veerle Cnudde; Vincent Barbin
Abstract The Pays rémois in the eastern Paris Basin is an administrative area of 1394 km2; in the surroundings of Reims (France). Two main geological substrata are separated by the Île-de-France cuesta: the Tertiary substratum in the western part is composed of various types of geomaterials (clay, sandstone, limestone, burrstone), whereas the substratum in the eastern part is composed only of Cretaceous Chalk. A field survey in each commune of the Pays rémois identified 26 building materials documented in a Geographic Information System database (GIS-database) that includes information about them (lithology, petrographical and petrophysical data, weathering) and the corresponding buildings (e.g. town, georeferenced data, building type, position on the façade). The spatial analysis of the building materials’ distribution (Standard Deviational Ellipse) with GIS identifies their uses and the criteria established for the selection of the materials: availability, efficiency, workability and durability. Some lithologies were preferred for particular buildings or selected for their efficiency in specific positions. The study also defines the relation between the stones’ origin (local and non-local stones) and their application. This database is useful to establish stone replacement strategies in the Pays rémois.
revue internationale de géomatique | 2016
Anne Combaud; Alain Devos; Laurent Chalumeau; Pierre Taborelli; Nicolas Bollot
Le theme de la Grande Guerre a fait l’objet de nombreuses publications dans le cadre du centenaire dans lesquelles l’approche est generalement historique ou sociale mais pas spatiale. Pourtant, l’archeologie de la Grande Guerre, les recherches genealogiques, les travaux des associations et le devoir de memoire utilisent de nombreux extraits de cartes militaires de la zone de front ou de plans directeurs. L’objectif de cette contribution est double. D’une part, elle replace les plans directeurs dans le contexte des cartes francaises existantes avant la Grande Guerre, demontrant ainsi la necessite d’innover du fait de l’adoption de la guerre de position par les differents belligerants, marquee par plusieurs rideaux defensifs de tranchees. Et d’autre part, elle propose de presenter les clefs de lecture des plans directeurs (systeme de coordonnees, construction, echelles, projection, legende).
Geodinamica Acta | 2015
Alain Devos; Nicolas Bollot; Laurent Chalumeau; Gilles Fronteau; Olivier Lejeune
Spatial disparity of run-off conditions during low-water period in homogeneous watersheds depends on the degree of incision of valleys, but may also be influenced by a structural partitioning or some lateral variations in the aquifer lithology. For small basins (area <300 km2), often hydrometrically unsupervised, campaigns of serial flow measurements, gauging, conductivity and temperature are achieved. The Ardre basin, localised in the Tertiary formations of the Paris Basin is used as a workshop basin. Results validated by hydrological and physico-chemical profiles show increased hydrological yields in the basin which correspond to the increase in the thickness of aquifers and their porosity. These lateral variations of facies and of aquifer thicknesses are related to Eocene sedimentary conditions (Lutetian) for homogeneous basins, which explain the spatial disparity of water resources.
Geomorphologie-relief Processus Environnement | 2014
Nicolas Bollot; Alain Devos; Guillaume Pierre; Laurent Chalumeau; Olivier Lejeune
Karstologia | 2011
Alain Devos; Laurent Chalumeau; Gilles Fronteau; Cristelle Sosson; Aurélie Turmel; Olivier Lejeune
Physio-Géo. Géographie physique et environnement | 2015
Alain Devos; Pierre Taborelli; Mylène Dodici; Laurent Chalumeau; Jérôme Buridant; Nicolas Bollot; Anne Combaud; Yves Desfossés
Physio-Géo. Géographie physique et environnement | 2016
Pierre Taborelli; Laurent Chalumeau; Guillaume Pierre; Alain Devos; Jonathan Lenoir; Gilles Fronteau; Olivier Lejeune; Nicolas Bollot
Geomorphologie-relief Processus Environnement | 2015
Thibaud Damien; Mylène Briquet; Nicolas Bollot; Alain Devos; Laurent Chalumeau; Guillaume Pierre; Olivier Lejeune
Physio-Géo. Géographie physique et environnement | 2012
Laurent Chalumeau; Anne Combaud; Nicole Plumettaz; Gianna Reginelli-Servais