Porosity and fluid velocities in the upper continental crust (2 to 4 km) inferred from injection tests at the Soultz-sous-Forêts geothermal site     

Luc Aquilina  Jean-Raynald de Dreuzy  Philippe Davy 《Geochimica et cosmochimica acta》2004,68(11):2405-2415

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Crystallization in flow – I. Palaeocirculation track by texture analysis and magnetic fabrics     

Stanislas Sizaret  Yan Chen  Luc Barbanson  Bernard Henry  Pierre Camps  Eric Marcoux 《Geophysical Journal International》2006,167(2):605-612

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Crystallization in flow – II. Modelling crystal growth kinetics controlled by boundary layer thickness     

Stanislas Sizaret  Ivan Fedioun  Luc Barbanson  Yan Chen 《Geophysical Journal International》2006,167(2):1027-1034

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Changes in channel size at river confluences with coarse bed material     

Andre G. Roy  Ren Roy 《地球表面变化过程与地形》1988,13(1):77-84

A field survey of thirty stream junctions from a small watershed, together with data collected by Miller (1958), allowed us to investigate morphometric adjustments occurring at confluences. The model proposed by Roy and Woldenberg (1986) was slightly modified and used as a tool for morphometric analysis. Two parameters are necessary in order to evaluate the rate of change in channel size at a confluence: the area ratio (channel capacity above the confluence: channel capacity below the confluence) and the discharge ratio (discharge of the minor tributary: discharge of the major tributary). Our data show that total channel capacity tends to decline below most confluences. A reduction in cross-sectional area implies an increase in average flow velocity. This interpretation is consistent with Lyell's observations and with results from recent flume experiments (Best and Reid, 1984).  相似文献   

Magma genesis in a battered Moon: Effects of basin-forming impacts     

Norman Hubbard  Constance G. Andre 《Earth, Moon, and Planets》1983,29(1):15-37

Magma genesis in the Moon could have been significantly altered by large impacts if they melted solidified residual liquids and late cumulates from the ‘magma ocean’. Calculations of the heat required to melt these materials, under different assumed conditions, are compared to estimates of the total kinetic energy of the Imbrium impact. For a significant amount of these materials to have been melted, they must have been near their solidus temperatures, the impacts must have been very large, and the lunar lithosphere must have been locally heated at depths of 70 to 140 km. Unless the Imbrium impact released at least the maximum estimated kinetic energy, only larger impacts, e.g., the proposed ‘Gargantuan’ impact, could have augmented the intrinsic lunar heat budget enough to locally alter the abundance, timing of eruption, and chemical compositions of lunar magmas. The mechanical and thermal energy generated by such an impact could have been critical in creating (1) the higher concentrations of radioactive elements in the Imbrium/Procellarum area by migration of residual liquids driven by differential lithospheric thickness; and (2) hybrid mare basalts (representing varying proportions of late cumulates and/or residual liquids incorporated into primitive magmas rising from the partially molten lunar interior). Complete compositional spectra of lunar basalts are to be expected, from primitive mare basalts to pure KREEP and to Ti-rich varieties. Comparison of the Gargantuan/Imbrium area with ancient basins in the eastern nearside area suggests that the interplay between the Moon's internal heat engine and the timing of large impacts was a crucial factor in determining the time of tunar volcanism and the chemical composition of the lavas.  相似文献   

Short-Term Ozone Forecasting with a Network Model System during Summer 1999     

Hermann J. Jakobs  Stefan Tilmes  Andre Heidegger  Klaus Nester  Gerhard Smiatek 《Journal of Atmospheric Chemistry》2002,42(1):23-40

Within the framework of the Tropospheric Research Programme (TFS) four working groups in Germany (University of Stuttgart, University of Cologne, Research Center Karlsruhe, German Weather Service) formed a network developing a model system for chemistry transport calculations on different scales. The network was optimized, based on each module and combined for the different interfaces in order to perform daily preoperational ozone forecasts and its precursors at the German Weather Service in summer 1999 (May through September). The setup of the model system, the interfaces and changes of each module are described. The results of the whole preoperational episode are displayed and discussed. Main efforts were done analyzing the model climate statistics and the verification of the predictions with an extensive data base of observations at stations in Germany. The results of this extensive verification demonstrate the relatively good performance of the entire forecast system.  相似文献   

Holocene paleoenvironmental change inferred from two sediment cores collected in the Tibetan lake Taro Co     

Laug  Andreas  Haberzettl  Torsten  Pannes  Andre  Schwarz  Anja  Turner  Falko  Wang  Junbo  Engels  Stefan  Rigterink  Sonja  Börner  Nicole  Ahlborn  Marieke  Ju  Jianting  Schwalb  Antje 《Journal of Paleolimnology》2021,66(3):171-186

Journal of Paleolimnology - The Tibetan Plateau, also known as the “Water Tower of Asia” because of its function as a water storage and supply region, responds dramatically to modern...  相似文献   

Significance of a combined approach for replacement stones in the heritage buildings’ conservation frame     

Olivier Rozenbaum  Luc Barbanson  Fabrice Muller  Ary Bruand   《Comptes Rendus Geoscience》2008,340(6):345-355

Stone substitution is a conventional operation during heritage buildings’ restoration, but becomes problematic for architects and restorers when the quarry is mined out. The compatibility of the substitution stones with the original ones has been for long mainly based on the aesthetical aspect, this resulting too often in a patchwork of original and substitution stones with different patina after several years because of differences of properties. In this study, the objective is to show how substitution stones can be selected by combining aesthetic criteria and stones properties that are relevant for analyzing their compatibility. A couple of French limestones with their potential substitution stones were selected for the study. Our results showed that potential substitution stones selected on their aesthetic criteria require to be rejected because of their differences of physical properties. On the other hand, our results showed also the possibility to select substitution stones with satisfactory aesthetic aspect and properties that enable to expect a satisfactory compatibility with the original stone.  相似文献   

A geomorphologic kinematic‐wave (GKW) model for estimation of floods from small alpine watersheds     

Dominique D. Brod  Vijay P. Singh  Andre Musy 《水文研究》1999,13(9):1391-1416

A geomorphologic kinematic‐wave (GKW) model was developed for simulation of extreme floods from small alpine catchments. The GKW model couples the kinematic‐wave theory and the geomorphologic representation of the catchment based on the Horton–Strahler ordering scheme. The model was tested on two small alpine catchments in Switzerland, and the agreement between simulated and observed floods was good. Care must however be taken with the computation of slope and roughness parameters. Copyright © 1999 John Wiley & Sons, Ltd.  相似文献   

Parameter identification in fresh-saltwater flow based on borehole resistivities and freshwater head data     

Luc Lebbe 《Advances in water resources》1999,22(8):107

By means of a series of borehole resistivity measurements and a resistivity–salinity relation, a particular salt-freshwater inversion was found under the shore with semi-diurnal tides at the French–Belgian border. These resistivity data provide valuable information about the vertical variation of the saltwater percentage in different boreholes. At different places and depths fluctuations of freshwater heads are observed. A regression modelling procedure is proposed in which the hydraulic parameters for density dependent flow and solute transport can be simultaneously considered with the parameters of the resistivity–salinity relation. The object function comprises resistivity residuals and freshwater head residuals along with saltwater percentage residuals and parameter residuals. First, a synthetic problem is elaborated with this regression modelling procedure. It is followed by the application of the procedure on the observed fresh-saltwater flow problem under the shore. In the synthetic problem the identification of the hydraulic parameters was demonstrated without the inclusion of prior information about these parameters. The resistivity–salinity relation was slightly adjusted in this regression. During the regression modelling of the observations made in one of the shore-normal cross sections, the horizontal and vertical conductivity are identified along with the effective porosity and the longitudinal and transverse dispersivity. The optimal values of the dispersivities are very small. Finally, it is shown that the high waters on the back shore forms the main threat of saltwater enchroachment from the sea side of the dunes and that the isolated fresh-brackish lens under the lower part of the shore before the build up area of De Panne can be explained by overexploitation.  相似文献