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Institution

University of Rennes

EducationRennes, France
About: University of Rennes is a education organization based out in Rennes, France. It is known for research contribution in the topics: Population & Crystal structure. The organization has 18404 authors who have published 40374 publications receiving 995327 citations.


Papers
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Journal ArticleDOI
TL;DR: In this article, the singular solutions of time-harmonic Maxwell equations in a domain which has edges and polyhedral corners are investigated, and simple and explicit formulas based on (generalized) Dirichlet and Neumann singularities for the Laplace operator are presented.
Abstract: In this paper, we investigate the singular solutions of time-harmonic Maxwell equations in a domain which has edges and polyhedral corners. It is now well known that in the presence of non-convex edges, the solution fields have no square integrable gradients in general and that the main singularities are the gradients of singular functions of the Laplace operator [4,–5]. We show how this type of result can be derived from the classical Mellin analysis, and how this analysis leads to sharper results concerning the singular parts which belong to H 1. For the singular functions, we exhibit simple and explicit formulas based on (generalized) Dirichlet and Neumann singularities for the Laplace operator. These formulas are more explicit than the results announced in our note [10].

339 citations

Journal ArticleDOI
Anny Cazenave, Benoit Meyssignac, Michael Ablain, Magdalena Balmaseda1, Jonathan L. Bamber2, Valentina R. Barletta3, Brian D. Beckley4, Jérôme Benveniste5, Etienne Berthier, Alejandro Blazquez, Timothy P. Boyer6, Denise Cáceres7, Don P. Chambers8, Nicolas Champollion9, Ben Chao10, Jianli Chen11, Lijing Cheng12, John A. Church13, Stephen Chuter2, J. Graham Cogley14, Soenke Dangendorf15, Damien Desbruyères16, Petra Döll7, Catia M. Domingues17, Ulrike Falk9, James S. Famiglietti18, Luciana Fenoglio-Marc19, René Forsberg3, Gaia Galassi20, Alex S. Gardner18, Andreas Groh21, Benjamin D. Hamlington22, Anna E. Hogg23, Martin Horwath21, Vincent Humphrey24, Laurent Husson25, Masayoshi Ishii, A. Jaeggi26, Svetlana Jevrejeva27, Gregory C. Johnson6, Nicolas Kolodziejczyk, Jürgen Kusche19, Kurt Lambeck28, Felix W. Landerer18, P. W. Leclercq29, Benoit Legresy17, Eric Leuliette6, William Llovel, Laurent Longuevergne30, Bryant D. Loomis4, Scott B. Luthcke4, Marta Marcos31, Ben Marzeion9, Christopher J. Merchant32, Mark A. Merrifield33, Glenn A. Milne34, Gary T. Mitchum8, Yara Mohajerani35, Maeva Monier, Didier Monselesan17, Steve Nerem36, Hindumathi Palanisamy, Frank Paul37, Begoña Pérez, Christopher G. Piecuch38, Rui M. Ponte, Sarah G. Purkey33, John T. Reager18, Roelof Rietbroek19, Eric Rignot35, Riccardo Riva39, Dean Roemmich33, Louise Sandberg Sørensen3, Ingo Sasgen40, E.J.O. Schram39, Sonia I. Seneviratne24, C. K. Shum41, Giorgio Spada20, Detlef Stammer42, Roderic van de Wal43, Isabella Velicogna44, Karina von Schuckmann, Yoshihide Wada43, Yiguo Wang45, Christopher Watson46, David N. Wiese18, Susan Wijffels17, Richard M. Westaway2, Guy Wöppelmann47, Bert Wouters43 
TL;DR: In this paper, the authors present estimates of the altimetry-based global mean sea level (average variance of 3.1 +/- 0.3 mm/yr and acceleration of 0.1 mm/r2 over 1993-present), as well as of the different components of the sea level budget over 2005-present, using GRACE-based ocean mass estimates.
Abstract: Global mean sea level is an integral of changes occurring in the climate system in response to unforced climate variability as well as natural and anthropogenic forcing factors. Its temporal evolution allows detecting changes (e.g., acceleration) in one or more components. Study of the sea level budget provides constraints on missing or poorly known contributions, such as the unsurveyed deep ocean or the still uncertain land water component. In the context of the World Climate Research Programme Grand Challenge entitled “Regional Sea Level and Coastal Impacts”, an international effort involving the sea level community worldwide has been recently initiated with the objective of assessing the various data sets used to estimate components of the sea level budget during the altimetry era (1993 to present). These data sets are based on the combination of a broad range of space-based and in situ observations, model estimates and algorithms. Evaluating their quality, quantifying uncertainties and identifying sources of discrepancies between component estimates is extremely useful for various applications in climate research. This effort involves several tens of scientists from about fifty research teams/institutions worldwide (www.wcrp-climate.org/grand-challenges/gc-sea- level). The results presented in this paper are a synthesis of the first assessment performed during 2017-2018. We present estimates of the altimetry-based global mean sea level (average rate of 3.1 +/- 0.3 mm/yr and acceleration of 0.1 mm/yr2 over 1993-present), as well as of the different components of the sea level budget (http://doi.org/10.17882/54854). We further examine closure of the sea level budget, comparing the observed global mean sea level with the sum of components. Ocean thermal expansion, glaciers, Greenland and Antarctica contribute by 42%, 21%, 15% and 8% to the global mean sea level over the 1993-present. We also study the sea level budget over 2005-present, using GRACE-based ocean mass estimates instead of sum of individual mass components. Results show closure of the sea level budget within 0.3 mm/yr. Substantial uncertainty remains for the land water storage component, as shown in examining individual mass contributions to sea level.

338 citations

Journal ArticleDOI
TL;DR: In this paper, the degradation mechanism of a cyclic and linear carbonate-based electrolyte mixtures was investigated using NMR, FTIR and high resolution mass spectrometry (ESI-HRMS) analysis.

338 citations

Journal ArticleDOI
TL;DR: The goal is not to replace software user guides, but to provide key concepts, principles, and procedures to be applied during geomodeling tasks, with a specific focus on quality control.
Abstract: Building a 3D geological model from field and subsurface data is a typical task in geological studies involving natural resource evaluation and hazard assessment. However, there is quite often a gap between research papers presenting case studies or specific innovations in 3D modeling and the objectives of a typical class in 3D structural modeling, as more and more is implemented at universities. In this paper, we present general procedures and guidelines to effectively build a structural model made of faults and horizons from typical sparse data. Then we describe a typical 3D structural modeling workflow based on triangulated surfaces. Our goal is not to replace software user guides, but to provide key concepts, principles, and procedures to be applied during geomodeling tasks, with a specific focus on quality control.

337 citations

Journal ArticleDOI
TL;DR: Arylation at C 3 and C 4 positions of a C-H bond activation has become a popular method for generating carbon-carbon bonds as mentioned in this paper, and a wide variety of hetero-aromatics, such as furans, thiophenes, pyrroles, thiosoles, thiazoles, oxazoles, imidazoles and pyrazoles can be employed.
Abstract: In recent years, palladium-catalyzed direct C2 or C5 arylation of heteroaromatic compounds with aryl halides by C-H bond activation has become a popular method for generating carbon-carbon bonds For this reaction, a wide variety of heteroaromatics, such as furans, thiophenes, pyrroles, thiazoles, oxazoles, imidazoles, pyrazoles, indoles, triazoles, or even pyridines, can be employed C3 and C4 arylations of heteroaromatics by C-H bond activation have also been described Such reactions initially attracted much less attention than the C2 or C5 arylations due to the lower reactivity of the C3 and C4 positions However, in more recent years, several results from using modified and improved catalysts and reaction conditions have been reported, which permit C3 and C4 arylations in synthetically useful yields Several intramolecular cyclizations of 2-substituted heterocycles have been described, with formation of a C—C bond on C3 resulting in the formation of five- to nine-membered rings incorporating pyrroles, indoles, thiophenes, furans, isoxazoles, or pyridines Intermolecular C3 or C4 direct arylations are still quite rare for some heteroaromatics and are in several cases not highly regioselective For such reactions, the best results have been obtained using pyrroles, thiophenes, or furans For selected substrates, regioselective arylation at C3 or C4 of the heteroaromatic compounds took place under appropriate reaction conditions Only a few examples of intermolecular couplings using oxazoles, thiazoles, imidazoles, isoxazoles, pyrazoles, triazoles, or pyridines have been reported For most of these reactions, aryl iodides or bromides have been used as coupling partners, although a few examples with aryl chlorides are also known This method allows the synthesis of complex molecules in only a few steps, and will provide access to a very wide variety of new heteroaryl derivatives in the next years

337 citations


Authors

Showing all 18470 results

NameH-indexPapersCitations
Philippe Froguel166820118816
Bart Staels15282486638
Yi Yang143245692268
Geoffrey Burnstock141148899525
Shahrokh F. Shariat118163758900
Lutz Ackermann11666945066
Douglas R. MacFarlane11086454236
Elliott H. Lieb10751257920
Fu-Yuan Wu10736742039
Didier Sornette104129544157
Stefan Hild10345268228
Pierre I. Karakiewicz101120740072
Philippe Dubois101109848086
François Bondu10044069284
Jean-Michel Savéant9851733518
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Performance
Metrics
No. of papers from the Institution in previous years
YearPapers
202321
2022176
20212,655
20202,735
20192,670
20182,378