Muriel Gasc-Barbier

Dr. Muriel Gasc-Barbier

CEREMA, Aix-en-Provence, Provence-Alpes-Côte d’Azur, France
orcid

Research Focus & Metrics

Academic Career Length

27Years (2000-Present)

(Calculated once Scilit publication data is synced: current year − year of first publication + 1)

Representative Publications

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1 August 2004 in Applied Clay Science
Verified
Journal Article
Closed access
MGMuriel Gasc-Barbier
Muriel Gasc-Barbier
SCS Chanchole
S Chanchole
PBP Bérest
P Bérest

1 September 2012 in Applied Clay Science
Verified
Journal Article
Closed access
JAJ.E. Aubert
J.E. Aubert
MGMuriel Gasc-Barbier
Muriel Gasc-Barbier

1 October 2014 in Building and Environment
Verified
Journal Article
Closed access
RDR. Delinière
R. Delinière
JAJ.E. Aubert
J.E. Aubert
FRF. Rojat
F. Rojat
MGMuriel Gasc-Barbier
Muriel Gasc-Barbier

1 September 2018 in International Journal of Rock Mechanics and Mining Sciences
Verified
Journal Article
Closed access
CVC.J. Villarraga
C.J. Villarraga
MGMuriel Gasc-Barbier
Muriel Gasc-Barbier
JVJ. Vaunat
J. Vaunat
José DarrozesJosé Darrozes
José Darrozes

18 February 2023 in Applied Sciences
Verified
Journal Article
Open access
PDF file
RRRosa María Ruiz
Rosa María Ruiz
Roberto  SarroRoberto Sarro
Roberto Sarro
Andres Diez-HerreroAndres Diez-Herrero
Andres Diez-Herrero
CRCristina Reyes-Carmona
Cristina Reyes-Carmona
JLJuan López-Vinielles
Juan López-Vinielles
Oriol MonserratOriol Monserrat
Oriol Monserrat
Coastal regions in Southwest Europe have experienced major interventions and transformations of the territory with unprecedented urban development, primarily related to growing tourism activity. The coast is the place where marine and terrestrial processes converge, making it highly vulnerable to the effects of climate change. However, the lack of information on the frequency of these extreme weather events and their impacts on the coast hampers an accurate analysis of the consequences of global change. This paper provides a detailed analysis of the extreme weather events (EWE) that have affected the Atlantic and Mediterranean coasts of Southwest Europe during the period from 1 January 2009 to 28 February 2020, as well as a quantification of their impacts: fatalities, injuries and economic damage. Official sources from France, Portugal and Spain were consulted, along with technical reports, scientific articles, etc., to generate a unified database. A total of 95 significant extreme events have caused 168 fatalities, 137 injuries and almost €4000 M in direct economic losses. Cyclone Xynthia (February 2010) on the French Atlantic coast stands out, having caused 47 fatalities, 79 injuries and substantial economic losses valued at €3000 M. The study shows a slight upward trend in the number of events recorded, especially during the last three years of the analysis, as well as in human losses and damages. The results reveal a higher exposure of the Mediterranean coast of Southwest Europe when compared to the Atlantic, especially the Spanish Mediterranean coast, with 61% of the fatalities recorded there during the study period. This is primarily due to a model of exponential tourism growth on the Mediterranean coast, with an enormous urban and infrastructure development during the last decades. Traditionally, the Mediterranean coast is less prepared to reduce the effects of marine storms, extreme events that are becoming more frequent and virulent in the context of climate and global change. This work highlights the need to create a continuous monitoring system–at the European level–of the impacts of extreme weather events on the coast, where 40% of the European population is concentrated. This observatory should serve as a source of information for risk mitigation policies (predictive, preventive and corrective), as well as for emergency management during disasters.

1 May 2007 in International Journal of Geomechanics
Verified
Journal Article
Closed access
MGMuriel Gasc-Barbier
Muriel Gasc-Barbier
DTD. Tessier
D. Tessier
Wetting/drying tests including cycling effects were performed on an argillaceous deep rock coming from a Callovo–Oxfordian deposit in eastern France. Bulk volume and water content were measured in order to estimate the importance of physical changes. Then, mercury intrusion porosimetry (MIP) was performed on dry and moist samples in order to quantify the influence of hydraulic history on fracture. Results showed that shrinkage and swelling caused microcracks, which led to volume variations thus altering the structures of the rock. MIP tests performed on moist samples equilibrated with different hygrometric saline solutions allow unsaturated pores and classic water retention curves to be described so as to explain changes in the microstructure.