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Hysteresis Loops and Phase Diagrams of the Spin-1 Ising Model in a Transverse Crystal Field

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Chinese Physics Letters 2012年第1期29卷 194-197页

作者： S.Bouhou I.Essaoudi A.Ainane M.Saber J.J.de Miguel M.Kerouad Laboratoire de physique des Materiaux et Modelisations des Systemes Unite Associee au CNRST-URAC 08Department of PhysicsFaculty of SciencesUniversity of Moulay IsmailB.P.11201MeknesMorocco Max-Planck-institut fur Physik Complexer Systeme Nohnitzer Str.38D-01187 DresdenGermany Dpto.Fisica de la Materia Condensada C-3 and Institut of Materials Sciences“Nicolas Cabrera”Univ.AutonomaCantoblanco E-28049-MadridSpain

Within the framework of the effective-field theory with a probability distribution technique,which accounts for the self-spin correlation functions,the ferromagnetic spin-1 Ising model with a transverse crystal field on honeycomb,square and simple cubic lattices is *** have investigated the effect of the transverse crystal field on the phase diagrams,magnetization,hysteresis loops and χ_(z,h) of the system.A number of interesting phenomena of the system are discussed.

关键词： transverse Ising crystal

Extreme multiexciton emission from deterministically assembled single-emitter subwavelength plasmonic patch antennas

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Light(Science & Applications) 2020年第1期9卷 1697-1705页

作者： Amit Raj Dhawan Cherif Belacel Juan Uriel Esparza-Villa Michel Nasilowski Zhiming Wang Catherine Schwob Jean-Paul Hugonin Laurent Coolen Benoit Dubertret Pascale Senellart Agnes Maitre institute of Fundamental and Frontier Sciences University of Electronic Science and Technology of ChinaChengdu 610054People’s Republic of China Sorbonne Universite CNRSInstitut des Nanosciences de ParisUMR 758875005 ParisFrance Centre de Nanosciences et de Nanotechnologies et de Nanostructures CNRS UMR9001Universite Paris-Saclay10 boulevard Thomas Gobert91120 MarcoussisFrance Laboratoire de physique et d’Etude des Materiaux ESPCI-ParisTechPSL Research UniversitySorbonne UniversiteCNRS UMR 821310 rue VauquelinParis 75005France Laboratoire Charles Fabry Institut d’Optique Graduate SchoolCNRS UMR 8501Universite Paris Saclay2 avenue Augustin Fresnel91127 Palaiseau CedexFrance

Coupling nano-emitters to plasmonic antennas is a key milestone for the development of nanoscale quantum light *** challenge,however,is the precise nanoscale positioning of the emitter in the ***,we present a laser etching protocol that deterministically positions a single colloidal CdSe/CdS core/shell quantum dot emitter inside a subwavelength plasmonic patch antenna with three-dimensional nanoscale *** exploiting the properties of metal–insulator–metal structures at the nanoscale,the fabricated single-emitter antenna exhibits a very high-Purcell factor(>72)and a brightness enhancement of a factor of *** to the unprecedented quenching of Auger processes and the strong acceleration of the multiexciton emission,more than 4 photons per pulse can be emitted by a single quantum dot,thus increasing the device *** technology can be applied to a wide range of photonic nanostructures and emitters,paving the way for scalable and reliable fabrication of ultracompact light sources.

关键词： patch precise acceleration

Construction of New Surface Wave Solutions of the Modified KdV Equation

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Open Journal of Applied Sciences 2022年第2期12卷 196-215页

作者： Clovis Taki Djeumen Tchaho Jean Pierre Ngantcha Thierry Blanchard Ekogo Bruno Rodin Mbock Um Hugues Martial Omanda Hugues Martial Omanda Jean Roger Bogning African Centre for Advanced Studies Yaoundé Cameroon Lycée Technique Fulbert Bongotha Moanda Gabon Laboratoire de Mécanique des matériaux école Polytechnique Université des Sciences et Techniques de Masuku Franceville Gabon Département de physique Université des Sciences et Techniques de Masuku Franceville Gabon institut International de Recherches Biomédicales et de Biotechnologies Carl Kambangoye (IRBK) Université Internationale de Li-breville (UIL) Libreville Gabon Laboratoire Pluridisciplinaire des Sciences école Normale Supérieure Libreville Gabon department of Physics Higher Teacher Training College University of Bamenda Bamenda Cameroon

The major concern of this work is to propose new prototypes of surface hybrid waves, in particular waves propagating without sprawl or deformation on the surface of a fluid. The model considered for this purpose is the modified KdV (Korteweg-de Vries) equation. A peculiarity of the obtained solutions is that they form packages constituted by combinations of waves belonging to the two main families of well-known bright and dark solitary waves. This putting together creates competitions between the different components of the considered packages which, following the values assigned to the parameters of the considered system and in relation to those of the wave parameters, generate hybrid or multi-form structures. The direct method of resolution which made possible the obtained results is that of Bogning-Djeumen Tchaho-Kofane extended to the new implicit Bogning functions. The existence conditions of some solutions are obtained. The numerical simulations carried out with a view to testing the observable and applicable characters of the obtained solutions revealed their stabilities over a relatively long time, and at the same time, confirmed the recommended theoretical forecasts. We are convinced that the solutions proposed as part of this work will make it possible to detect, understand and explain some physical phenomena linked to fluid molecular interactions, former or new, which constantly occur on the fluid surfaces, mainly at the shallow water surface.

关键词： Surface Hybrid Waves Modified Korteweg-de Vries Equation Bogning-Djeumen Tchaho-Kofané Method Hybrid Prototypes Multi-Form Structures

Composition and evolution of the continental crust:Retrospect and prospect

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Geoscience Frontiers 2022年第5期13卷 1-15页

作者： J.L.R.Touret M.Santosh J.M.Huizenga institut de Minéralogie Physique des MatériauxCosmochimieSorbonne Universités4 Place JussieuF-75005 ParisFrance 121 Rue de la Réunion 75020 ParisFrance School of Earth Sciences and Resources China University of GeosciencesBeijing 100083China department of Earth Science University of AdelaideAdelaideSA 5005Australia Faculty of Environmental Sciences and Natural Resource Management Norwegian University of Life SciencesP.O.Box 5003NO-1432ÅsNorway EGRU(Economic Geology Research Centre) James Cook UniversityTownsvilleQueensland 4811Australia department of Geology University of JohannesburgPO Box 524Auckland Park 2006South Africa

Until the middle of the 20th century,the continental crust was considered to be dominantly *** hypothesis was revised after the Second World War when several new studies led to the realization that the continental crust is dominantly made of metamorphic *** rocks were emplaced at peak metamorphic conditions in domains,which can be defined by geophysical *** to medium-grade metamorphic rocks constitute the upper crust,granitic migmatites and intrusive granites occur in the middle crust,and the lower crust,situated between the Conrad and Moho discontinuities,comprises charnockites and *** continental crust acquired its final structure during metamorphic episodes associated with mantle upwelling,which mostly occurred in supercontinents prior to their disruption,during which the base of the crust experienced ultrahigh temperatures(>1000℃,ultrahigh temperature granulite-facies metamorphism).Heat is provided by underplating of mantle-derived mafic magmas,as well as by a massive influx of low H_(2)O activity mantle fluids,***-density CO_(2) and highsalinity *** fluids are initially stored in ultrahigh temperature domains,and subsequently infiltrate the lower crust,where they generate anhydrous granulite mineral *** brines can reach upper crustal levels,possibly even the surface,along major shear zones,where granitoids are generated through brine streaming in addition to those formed by dehydration melting in upper crustal levels.

关键词： Brines CO_(2) Continental crust Granulite Lower crust

Origin of pit chains in the floor of lunar Copernican craters

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Science China(Physics,Mechanics & Astronomy) 2010年第12期53卷 2145-2159页

作者： XIAO ZhiYong ZENG ZuoXun XIAO Long FA WenZhe HUANG Qian Faculty of Earth Sciences China University of GeosciencesWuhan 430074China Research Center for Space Science and Technology China University of GeosciencesWuhan 430074China institut de physique du Globe de Paris 4 Avenue de NeptuneSaint Maur des Fosse’s94100France Shanghai Astronomical Observatory Chinese Academy of SciencesShanghai 200030China

There are small pit chains in the floor of lunar Copernican craters. They are usually so small in scale that there are few lunar spacecrafts to detect their detailed morphology. Combining camera data from Lunar Orbiter, Lunar Reconnaissance Orbiter (LRO), Kaguya and Chang’e-1 missions, 5 representative large Copernican craters on various terrains of the lunar surface are chosen to study the origin of the pit chains in the crater floor. The morphology and distribution characteristic of the pit chains are referred by the high resolution images in this research. It is suggested that it is the magma activities from the subsurface magma layer combining with the existence of fractures and faults under the crater floor that leaded the formation of the pit chains. The model is further verified and discussed using the regolith thickness data in the crater floor. Our model suggests that the pit chains are still developing in the floor of the Copernican craters and the Moon may not be totally cold. Finally, the model limitation and potential future work are discussed based on available data.

关键词： lunar Copernican crater pit chains LRO LROC Kaguya Chang’e-1

Geochemistry of the volcanic rocks from Bioko Island(“Cameroon Hot Line”)： Evidence for plume-lithosphere interaction

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Geoscience Frontiers 2016年第5期7卷 743-757页

作者： Fadimatou Ngounouno Yamgouot Bernard Déruelle Isaac Bertrand Gbambié Mbowou Ismaila Ngounouno Daniel demaiffe departement des Sciences de la Terre Faculte des Sciences Universite de Ngaoundere B.P. 454 Ngaoundere Cameroon Laboratoire de Magmatologie et Ceochimie lnorganique et Experimentale (MAGIE) Institut de Physique du Globe de Paris UMR 7154 Universite Pierre et Marie Curie 4 place Jussieu 75252 Paris cedex 05 France departement des Mines et de la Geologie Ecole de Geologie et d'Exploitation Miniere (EGEM) Universite de Ngaoundere B.R 115 Meiganga Cameroon Laboratoire de Geochimie lsotopique et Geodynamique Chimique DSTE (CP 160/02) Universite Libre de Bruxelles 50 av. Roosevelt 1050 BruxellesBelgium

Bioko Island（3008 m a.s.l） is located in the presently more active volcanic zone of the Cameroon Line and composed essentially of alkaline basalts and hawaiites, and lesser mugearites. The rocks show microlitic porphyritic texture with phenocrysts of olivine（83% 〈 Fo 〈 87%） and clinopyroxene in a matrix of plagioclase, clinopyroxene and oxides. Hawaiites and mugearites also include phenocrysts of plagioclase（An62-67Ab35-32Or3-1）. Major element variation diagrams show an increase in Si O2, Al2O3, Na2 O and K2 O with increasing Mg O for the studied rock groups. The rocks are characterized by low（^86Sr/^87Sr）i ratios（0.70320e0.70406）, high 3Nd（t） values（2.56e4.33） and high（^206Pb/^204Pb）i ratios（20.032e20.035） *** are enriched in LILE and LREE, and have（Hf/Sm）N= 0.57e1.16. These geochemical signatures are similar to those of the Mount Cameroon rocks, and might be attributed to low degrees of partial melting from a garnet-amphibole-bearing mantle source. The trace elements and isotopic compositions suggest that the parental magma source might have involved HIMU- and EM1-components.

关键词： Geochemistry HIMU-EM1 Volcanic rocks Bioko Cameroon Hot Line

Vasarely painting at the nanoscale on sapphire crystals

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Nano Research 2020年第9期13卷 2512-2516页

作者： Caroline Matringe Elsa Thune Rémy Cavalotti Ahmad Fakih Stephan Amaud Nils Blanc Nathalie Boudet Alessandro Coati Yves Garreau David Babonneau René Guinebretière IRCER UMR CNRS 7315Centre Europeen de la CeramiqueUniversite de Limoges12 rue Atlantis87068 LimogesFrance institut Neel UPR CNRS 2940 CRG D2AM BeamlineESRFUniversite Grenoble Alpes38042 GrenobleFrance SixS Beamline Synchrotron SOLEILBP4891192 Gifsur YvetteFrance Laboratoire Materiaux et Phenomenes Quantiques UMR CNRS 7162Universite de Paris75013 ParisFrance institut Pprime Departement Physique et Mecanique des Materiauxf UPR CNRS 3346Universite de PoitiersSP2MITSA 4112386073 Poitiers Cedex 9France

We demonstrate that convenient thermal treatment of a specific sapphire vicinal surface can induce the formation of a fully two-dimensional(2D)ordered surface made of a periodic assembly of(006)*** simiarity between the resuting surface topography and pattemns represented in the hexagon series"of paintings by Vasarely is really striking!We thus propose to call these surfaces as"nanoscaled Vasarely surfaces".We also show that the self-organization process,which is driven by the minimization of the free energy of a closed system,results in a quasi-linear isothermal growth of the facets'surface area over time.

关键词： nanoscaled Vasarely surfaces two-dimensional(2D)-self-organization sapphire vicinal surfaces

Microwave Synthesis of Large Few-Layer Graphene Sheets in Aqueous Solution of Ammonia

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Nano Research 2010年第2期3卷 126-137页

作者： Izabela Janowska Kambiz Chizari Ovidiu Ersen Spyridon Zafeiratos Driss Soubane Victor Da Costa Virginie Speisser Christine Boeglin Matthieu Houllé Dominique Bégin Dominique Plee Marc-Jacques Ledoux Cuong Pham-Huu Laboratoire des Matériaux Surfaces et Procédés pour la Catalyse(LMSPC)UMR7515 CNRS-Universitéde Strasbourg 25rue Becquerel67087 Strasbourg Cedex 08France institut de physique et Chimie des Matériaux de Strasbourg(IPCMS) UMR7504 CNRS-Universitéde Strasbourg 23rue du Loess67037 Strasbourg Cedex 02France Arkema Groupement de Recherche de Lacq(GRL)BP 3464170 LACQFrance

Few-layer graphene (FLG) sheets with sizes exceeding several micrometers have been synthesized by exfoliation of expanded graphite in aqueous solution of ammonia under microwave irradiation, with an overall yield approaching 8 wt.%. Transmission electron microscopy (in bright-field and dark-field modes) together with electron diffraction patterns and atomic force microscopy confirmed that this graphene material consisted mostly of mono-, bi- or few-layer graphene (less than ten layers). The high degree of surface reduction was confirmed by X-ray photoelectron and infrared spectroscopies. In addition, the high stability of the FLG in the liquid medium facilitates the deposition of the graphene material onto several substrates via low-cost solution-phase processing techniques, opening the way to subsequent applications of the material.

关键词： Graphene transmission electron microscopy(TEM) expanded graphite exfoliation microwaves

design of Fe(3–x)O4 raspberry decorated graphene nanocomposites with high performances in lithium-ion battery

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Journal of Energy Chemistry 2016年第2期25卷 270-275页

作者： Olivier Gerber Sylvie Bégin-Colin Benoit P.Pichon Elodie Barraud Sébastien Lemonnier Cuong Pham-Huu Barbara Daffos Patrice Simon Jeremy Come Dominique Bégin institut de physique et Chimie des Materiaux de Strasbourg UMR 7504 - CNRS Universite de Strasbourg 23 rue du Loess 67034 Strasbourg Cedex 08France RS2E - FR CNRS n 3459 Universite Paul Sabatier Toulouse III CIRIMAT 118 route de Narbonne 31062 Toulouse Cedex 9 France French-German Research institute of Saint-Louis 5 rue du General Cassagnou 68300 Saint-Louis France institut de Chimie et Procedes pour l'Energie l'Environnement et la Sante UMR 7515-CNRS Universite de Strasbourg 25 rue Becquerel 67087 Strasbourg Cedex 02 France

Fe（3–x）O4 raspberry shaped nanostructures/graphene nanocomposites were synthesized by a one-step polyol-solvothermal method to be tested as electrode materials for Li-ion battery（LIB）. Indeed, Fe（3–x）O4 raspberry shaped nanostructures consist of original oriented aggregates of Fe（3–x）O4 magnetite nanocrystals, ensuring a low oxidation state of magnetite and a hollow and porous structure, which has been easily combined with graphene sheets. The resulting nanocomposite powder displays a very homogeneous spatial distribution of Fe（3–x）O4 nanostructures at the surface of the graphene sheets. These original nanostructures and their strong interaction with the graphene sheets resulted in very small capacity fading upon Li＋ion intercalation. Reversible capacity, as high as 660 m Ah/g, makes this material promising for anode in Li-ion batteries application.

关键词： Graphene Fe3–xO4 raspberry shaped nanostructures Fe3–xO4/graphene nanocomposites Lithium-ion battery Reversible capacity