Bruno Phalip
Blaise Pascal University
Network
Latest external collaboration on country level. Dive into details by clicking on the dots.
Publication
Featured researches published by Bruno Phalip.
Geological Society, London, Special Publications | 2014
Marie-Françoise André; Olivier Voldoire; Franck Vautier; Erwan Roussel; Bruno Phalip; David Morel
Abstract Three Romanesque churches of the Bourbonnais region in the French Massif Central have been investigated. These date back to the twelfth century, and are mainly built of red and white sandstones. Their ashlar blocks were extensively repointed in the mid-twentieth century with cement-rich mortar. In order to quantitatively assess the impact of repointing on the decay rates of the sandstones, the following methods have been used: dating of reference surfaces (‘zero datum levels’) based on stone-dressing marks, stone-by-stone and terrestrial LiDAR (Light Detection And Ranging) surveys, and petrographical analyses including on-site non-destructive tests. This study reveals that, between the twelfth century and the mid-twentieth century, intrinsic geological factors have been a key control on weathering rates. Stone surface recession has proceeded, on average, 500 times faster in the poorly cemented soft white sandstone compared to the iron-cemented red sandstone (4 mm/century v. 0.008 mm/century). Since the mid-twentieth century, the replacement of the original lime mortar with a cement-rich mortar has resulted in a marked increase in weathering rates and resulting surface recession of the poorly cemented white sandstone: this increase is fivefold where cement-lime mortar (‘bastard mortar’) has been used and 10-fold where harder cement-rich mortar has been applied. By contrast, the application of cement-lime mortar between the ashlars composed of iron-cemented red sandstone had no deleterious effects. This study confirms that the use of cement-based mortar should be avoided on soft and porous masonries. It also stresses the fact that accelerated stone surface recession rates are systematically associated with heritage sites that are subject to significant anthropogenic effects caused by inappropriate interventions or excessive pressure on the monuments or their environment.
Earth Surface Processes and Landforms | 2012
Marie-Françoise André; Olivier Voldoire; Erwan Roussel; Franck Vautier; Bruno Phalip; Hang Peou
Environmental Earth Sciences | 2011
Marie-Françoise André; Bruno Phalip; Olivier Voldoire; Franck Vautier; Yves Géraud; Mhammed Benbakkar; Christophe Constantin; Fabienne Huber; Gilles Morvan
Bulletin de l'Association de géographes français | 2008
Marie-Françoise André; Bruno Phalip; Julia Bonneau; Murielle Robert
Archive | 2012
Bruno Phalip; Olivier Voldoire; Marie-Françoise André; Franck Vautier; Erwan Roussel
8th International Conference on Geomorphology | 2012
Marie-Françoise André; Bruno Phalip; Erwan Roussel; Franck Vautier; Olivier Voldoire
l International Co-ordinating Committee for the Safeguarding and Development of the Historic Site of Angkor, 18th Plenary session | 2011
Marie-Françoise André; Franck Vautier; Olivier Voldoire; Bruno Phalip; Erwan Roussel
12th International Congress on the Deterioration and Conservation of Stone | 2011
Marie-Françoise André; Bruno Phalip; Olivier Voldoire; Erwan Roussel; Franck Vautier; David Morel
Archive | 2010
Marie-Françoise André; Franck Vautier; Bruno Phalip; Olivier Voldoire; Samuel Etienne; Denis Mercier; Erwan Roussel
Archive | 2009
Marie-Françoise André; Bruno Phalip; Olivier Voldoire; Franck Vautier; Erwan Roussel