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Modelling of Eruptive Fire Occurrence and Behaviour

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Journal of Environmental Science and Engineering(B) 2014年第3期3卷 115-132页

作者： Jacques-Henri Balbi Frangois Joseph Chatelon jean louis rossi Albert Simeoni Domingos Xavier Viegas Carlos Rossa Research Laboratory 6134 National Center for Scientific Research University of Corsica Corte 20250 France Building Research Establisment Centre for Fire Safety Engineering University of Edinburgh Edinburgh EH93JL Scotland Centre of Studies on Forest Fires Association for the Development of the Industrial Aerodynamics University of CoimbraCoimbra 3030-790 Portugal Department of Mechanical Engineering University of Coimbra Coimbra 3030-790 Portugal School of Technology and Management Polytechnic Institute of Leiria Leiria 2411-901 Portugal

Eruptive fires are one of the main causes of human losses in forest fire fighting. The sudden change in fire behaviour due to a fire eruption is extremely dangerous for fire-fighters because it is unpredictable. Very little literature is available to support either modelling or occurrence prediction for this phenomenon. In this study, an unsteady physical model of fire spread is detailed, which describes the initiation and development of eruptive fires with an induced wind sub-model. The latter phenomenon is proposed as the mainspring of fire eruptions. Induced wind is proportional to the rate of spread and the rate of spread is in a non-linear relationship with induced wind. This feedback can converge or diverge depending on the conditions. The model allows both explaining why an eruption can occur and predicting explicitly its occurrence according to meteorological conditions, topographic parameters, fuel bed properties and fire front width. The model is tested by comparing its results to a set of experiments carried out at laboratory scale and during an outdoor wildfire, the Kornati accident.

关键词： Eruptive fire unsteady solutions fire spread physical model.

Surface Fires： No Wind, No Slope, Marginal Burning

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Journal of Environmental Science and Engineering(A) 2014年第2期3卷 73-86页

作者： Jacques-Henry Balbi Domingos Xavier Viegas jean-louis rossi Carlos Rossa Francois Joseph Chatelon Dominique Cancellieri Albert Simeoni Thierry Marcelli Research Laboratory 6134 National Center for Scientific Research University of Corsica Corte 20250 France Centre of Studies on Forest Fires~Association for the Development of the Industrial Aerodynamics University of CoimbraCoimbra 3030-790 Portugal Department of Mechanical Engineering University of Coimbra Coimbra 3030-790 Portugal School of Technology and Management Polytechnic Institute of Leiria Leiria 2411-901 Portugal Building Research Establisment Centre for Fire Safety Engineering University of Edinburgh Edinburgh EH9 3JL Scotland

The first aim of this work is to provide an analytical expression to calculate the rate of spread of surface fires under no wind and no slope conditions. A previous simplified model was improved for this particular case of fire propagation. The test of this proposed model was performed by using two complete sets of experimental results with several fuel beds and variable parameters such as moisture content or bulk density. The second aim of this article is to highlight two conditions that allow stopping a fire： the low leaf area and the high value of the moisture content.

关键词： Surface fire spread marginal burning extinction conditions

Textures and melt-crystal-gas interactions in granites

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Geoscience Frontiers 2015年第5期6卷 635-663页

作者： jean-louis Vigneresse GeoRessources UMR 7339Universite de Lorraine

Felsic intrusions present ubiquitous *** result from the differential interactions between the magma components(crystal,melt,gas phase) while it flows or when the flow is perturbed by a new magma *** most obvious structure consists in fabrics caused by the interactions of rotating grains in a flowing viscous *** magma inputs through dikes affect the buk massif flow,considered as global within each mineral facies.A review of the deformation and flow types developing in a magma chamber identifis the patterns that could be *** determines their controlling parameters and summarizes the tools for their ***,a brief review of the theology of a complex multiphase magma identifies and suggests interactions between the different *** specific responses each component presents lead to instability *** particular,the change in vorticity orientation,associated with the switch between monoclinic to triclinic flow is a cause of many *** are preferentially *** include fabric development,shear zones and flow *** depend of the underlying rheology of interacting ***,enclaves,schlieren and ladder dikes result from the interactions between the magma components and changing boundary ***,pegmatites,unidirectional solidification textures and miarolitic cavities result from the interaction of the melt with a gaseous *** illustrations examine what is relevant to the bulk flow,local structures or boundary *** each case a field observation illustrates the *** discussion reformulates instability observations,suggesting new trails for ther description and interpretation in terms of local departure to a bulk flow.A brief look at larger structures and at their evolution tries to relate these instabilities on a broader *** helical structures of the Ricany pluton,Czech Republic and by the multiple granitic intrusions of Dolbe

关键词： Granitic magma Instabilities Triclinic flow Struct

Addressing ore formation and exploration

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Geoscience Frontiers 2019年第4期10卷 1613-1622页

作者： jean-louis Vigneresse GéoRessources UMR 7339Université de Lorraine

Common base and noble metals represent an important economic factor in the actual industrial *** instance the world resources for copper are actually estimated for about the next 30 years *** situation requires rethinking the way major ore deposits form,leading to new guides for *** present paper briefly examines the processes leading to ore formation,in relation with granitic or granodioritic *** identifies the importance of metal enrichment during the magmatic *** the magma chamber that forms porphyry intrusions,metals may incorporate to first formed crystals,becoming inert;concentrate into the residual melt of a mush;or segregate by diffusion into the exsolved magmatic volatile phase(MVP)into which they are transported and precipitated.A competition results between elements partitioning and ***,a specific Peclet number for each metal(Cu,Au,Ag,Mo,W,Sn,and REE)controls the ratio between the diffusive and the advective *** diffusivity in the melt shows differential behavior relative to a threshold of about10 13 m2/*** with slower diffusivity values(***)will not ***,fast diffusive metals(Au,Ag,Cu)may rapidly incorporate the MVP,provided an adequate component(halogens or S)is attractive for *** chemistry of the MVP escaping the magma induces different alteration *** relative content in F,Cl or S,attested by the composition of biotites and apatites,links with the preferential content of metals in o re deposits,representing a valuable tool for *** the model is replaced in a set of coupled mechanical-chemical instabilities,within a three phase material.

关键词： Porphyry ore deposits Metals concentration processes Exploration Alteration pattern

Phase coexistence properties of liquid mercury:a simulation study

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Rare Metals 2006年第5期25卷 567-571页

作者： jean-louis Bretonnet jean-Marc Bomont Laboratoire de Physique des Milieux Denses Université Paul Verlaine1bd F.D.Arago57078 MetzCedex 3France

The thermophysical properties of expanded liquid mercury have been investigated along the liquid-vapor coexistence curve by using Monte Carlo and Molecular Dynamic simulations. For the purpose, an empirical state dependent interatomic potential for the region of dense metallic liquid is used, while the state dependence is not necessary near the cliffcal point. In order to test the validity of this potential, we determine the surface layering and the sound velocity, two properties very sensitive to the choice of the potential. Our results are in quite good agreement with other theoretical results and to the experimental data available in the literature.

关键词： mercury simulation phase coexistence liquid state

Homogenization of Hyperbolic Damped Stochastic Wave Equations

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Acta Mathematica Sinica,English Series 2018年第2期34卷 233-254页

作者： Aurelien FOUETIO jean louis WOUKENG Department of Mathematics and Computer Science University of Dschang P.O. Box 67 Dschang Cameroon Interdisciplinary Center for Scientific Computing ( IWR) University of Heidelberg Im Neuenheimer Feld 205 69120 Heidelberg Germany

For a family of linear hyperbolic damped stochastic wave equations with rapidly oscillating coefficients, we establish the homogenization result by using the sigma-convergence method. This is achieved under an abstrac... 详细信息

关键词： Algebras with mean value stochastic hyperbolic partial differential equations Wiener process sigma-convergence

MULTISCALE HOMOGENIZATION OF NONLINEAR HYPERBOLIC EQUATIONS WITH SEVERAL TIME SCALES

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Acta Mathematica Scientia 2011年第3期31卷 843-856页

作者： jean louis Woukeng David Dongo Department of Mathematics and Computer Science Faculty of Science University of Dschang

We study the multiscale homogenization of a nonlinear hyperbolic equation in a periodic *** obtain an accurate homogenization *** also show that as the nonlinear term depends on the microscopic time variable,the global homogenized problem thus obtained is a system consisting of two hyperbolic *** is also shown that in spite of the presence of several time scales,the global homogenized problem is not a reiterated one.

关键词： hyperbolic multiscale nonlinear

Multiscale Analysis of Semilinear Damped Stochastic Wave Equations

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Acta Mathematica Sinica,English Series 2023年第7期39卷 1305-1331页

作者： Aurelien FOUETIO Gabriel NGUETSENG jean louis WOUKENG Department of Mathematics Higher Teacher Training CollegeUniversity of NgaoundereP.O.Box 652BertouaCameroon Department of Mathematics University of Yaounde IP.O.Box 812YaoundeCameroon Department of Mathematics and Computer Science University of DschangP.O.Box 67DschangCameroon

In this paper we proceed with the multiscale analysis of semilinear damped stochastic wave motions. The analysis is made by combining the well-known sigma convergence method with its stochastic counterpart, associated to some compactness results such as the Prokhorov and Skorokhod theorems. We derive the equivalent model, which is of the same type as the micro-model. One of the novelties of the work is that the corrector problem is solved in the classical sense of distributions,thereby allowing numerical computations of the homogenized coefficients.

关键词： Hyperbolic stochastic equations Wiener Process sigma convergence tightness of probability measures

The Séchilienne (France) Landslide:a Non-typical Progressive Failure Implying Major Risks

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Journal of Mountain Science 2011年第2期8卷 117-123页

作者： jean-louis DURVILLE Christophe BONNARD Pierre POTHERAT Conseil général de l'environnement et du développement durable Paris France Independent expert PBBG SA Lausanne Switzerland Centred'études techniques de l'équipement Lyon France

The National Road RN 91 has been threatened for about twenty-five years by a huge landslide, located 25 km south-east to the town of Grenoble (France). If several million cubic meters of rock fall down, the debris will dam the valley. Then the failure of the dam by overtopping and rapid erosion might result in a catastrophic flood and dramatic consequences for human life, environment and economy throughout the valley. The paper presents the hazard assessment based on geological and hydrological surveys, including small scale hydraulic tests, as well as the risk evaluation that has been performed. The risk management relies first upon a high level monitoring and an emergency plan; various mitigation strategies have been considered.

关键词： Landslide Progressive failure Séchilienne France