Multi-method assessment of connectivity between surface water and shallow groundwater: the case of Limarí River basin,north-central Chile   总被引：2，自引：1，他引：1  

Ricardo Oyarzún  Felisa Barrera  Pamela Salazar  Hugo Maturana  Jorge Oyarzún  Evelyn Aguirre  Pablo Alvarez  Hervé Jourde  Nicole Kretschmer 《Hydrogeology Journal》2014,22(8):1857-1873

A study that tests the applicability and consistency of independent but complementary approaches in the assessment of interactions between surface water and shallow groundwater within a water-stressed basin is described. The mostly agricultural Limarí basin in arid north-central Chile was chosen as a suitable case study. The analyses involved: (1) a connectivity index method, (2) hydrochemistry, and (3) water isotopic geochemistry. Chemical and isotopic data were obtained from two sampling campaigns conducted in April (fall) and December (summer) of 2011 in 22 sampling locations, which included surface water and groundwater. The results obtained by each of the methodologies were mutually consistent and indicate high connectivity conditions. Additionally, the relative contribution by different sources was assessed through end-member mixing analysis, and for reaches of the river that showed gaining conditions, the contribution of groundwater inflow to stream discharge was estimated. It is suggested that this multi-method approach is useful for the characterization of surface-water–groundwater interactions, since it at least represents a suitable starting point for obtaining basic information on these relationships. Thus, it may become the base for further studies in arid and semi-arid basins facing water management challenges.  相似文献   

Holocene environmental changes and human impact in the northern Swiss Jura as reflected by data from the Delémont valley     

Michel Guélat  Hervé Richard 《Swiss Journal of Geoscience》2014,107(1):1-21

The construction of the A16-Transjurane motorway revealed evidence of Holocene sediment sequences in the Delémont valley (Canton of Jura, Switzerland). Certain processes begin during the Younger Dryas. Pine forests dominate this cold period, which was unfavourable for pedogenesis; they remain throughout the first half of the Holocene. The meandering river system then becomes stable for more than four millennia. The first signs of human impact on the vegetal cover begin to appear around 3,500 cal BC (Middle Neolithic). An increase in hydric activity occurs between 3,600 and 2,500 cal BC. However, the earliest evidence of the cultivation of cereals dates only to about 2,000 cal BC (Early Bronze Age). Extensive forest clearing and the emergence of cultivated plants occur after 1,400 cal BC. On the cleared slopes the soil erodes and at their foot colluvium deposits accumulate. The densification of the settlement from the Late Bronze Age (1,350–800 cal BC) until the beginning of the Iron Age (800–650 cal BC) contributes to alluvial destabilization. A palaeosol has been identified in all of the Holocene deposits in the valley. The deforestation intensifies between 400 and 100 cal BC while hydric activity decreases. The first centuries of our era record very limited pedo-sedimentary phenomena. However, human presence becomes less marked after 350 cal AD. The slopes are stabilized and the soil develops. From 550 cal AD, an important increase in hydric activity takes place, a probable consequence of a wet fluctuation in the climate. Contemporary forest clearing causes deep gullies. After 750 cal AD, drier conditions set in. This period of stability, marked by occasional rises in the water level, continues until 1,250–1,300 cal AD (Late Middle Ages). Then superficial flows resume and entrenchment of the main waterways occurs, combined consequences of the Little Ice Age and the upsurge in human activity.  相似文献   

European temperatures in CMIP5: origins of present-day biases and future uncertainties     

Julien Cattiaux  Hervé Douville  Yannick Peings 《Climate Dynamics》2013,41(11-12):2889-2907

European temperatures and their projected changes under the 8.5 W/m² Representative Concentration Pathway scenario are evaluated in an ensemble of 33 global climate models participating in the fifth phase of the Coupled Model Intercomparison Project (CMIP5). Respective contributions of large-scale dynamics and local processes to both biases and changes in temperatures, and to the inter-model spread, are then investigated from a recently proposed methodology based on weather regimes. On average, CMIP5 models exhibit a cold bias in winter, especially in Northern Europe. They overestimate summer temperatures in Central Europe, in association with a greater diurnal range than observed. The projected temperature increase is stronger in summer than in winter, with the highest summer warming occurring over Mediterranean regions. Links between biases and sensitivities are evidenced in winter, suggesting a potential influence of snow cover biases on the projected surface warming. A brief analysis of daily temperature extremes suggests that the intra-seasonal variability is projected to decrease (slightly increase) in winter (summer). Then, in order to understand model discrepancies in both present-day and future climates, we disentangle effects of large-scale atmospheric dynamics and regional physical processes. In particular, in winter, CMIP5 models simulate a stronger North-Atlantic jet stream than observed and, in contrast with CMIP3 results, the majority of them suggests an increased frequency of the negative phase of the North-Atlantic Oscillation under future warming. While large-scale circulation only has a minor contribution to ensemble-mean biases or changes, which are primarily dominated by non-dynamical processes, it substantially affects the inter-model spread. Finally, other sources of uncertainties, including the North-Atlantic warming and local radiative feedbacks related to snow cover and clouds, are briefly discussed.  相似文献   

Photometric evolution of N-body + SPH + star formation simulations of isolated disc galaxies     

Léo Michel-Dansac  Hervé Wozniak 《Astrophysics and Space Science》2003,284(2):921-924

We have calibrated self-consistent simulations of isolated disc galaxies including star, gas and star formation with the spectro-photometric evolutionary model GISSEL2000 (Bruzual and Charlot, 1993). With this approach we can compare morphologies studying mass and luminous distributions. We present an example about the evolution of bar ellipticity, which is simultaneously governed by dynamic and spectro-photometric evolution. This revised version was published online in August 2006 with corrections to the Cover Date.  相似文献   

Kinematics of disc galaxies using photometrically calibrated N-body models     

Hervé Wozniak  Léo Michel-Dansac 《Astrophysics and Space Science》2003,284(2):707-710

We have studied the evolution of isolated galaxies over several Gyr using a self-consistent N-body code including stars, gas and star formation. The results of our simulations are calibrated using spectrophotometric evolution models. We thus simultaneously analyse kinematical and photometrical evolution of the various stellar populations born during the successive bursts of star formation. Our calibrated simulations show that the properties of stellar velocity dispersion drops observed in the centre of three barred active galaxies by Emsellem et al. (2001) could depend on the observational wavelength. This revised version was published online in August 2006 with corrections to the Cover Date.  相似文献   

Formation of the Upper Pleistocene terraces of Lake Van (Turkey)     

Catherine Kuzucuoğlu  Aurélien Christol  Damase Mouralis  Ali‐Fuat Doğu  Ebru Akköprü  Monique Fort  Daniel Brunstein  Halil Zorer  Michel Fontugne  Mustafa Karabiyikoğlu  Stéphane Scaillet  Jean‐Louis Reyss  Hervé Guillou 《第四纪科学杂志》2010,25(7):1124-1137

Sedimentological and geomorphological studies of terraces around Lake Van (1647 m) provided a preliminary framework for lake‐level variations. The elevations of terraces and past lake level were measured with a differential global positioning system. A chronology is developed using ²³⁴U/²³⁰Th dating of travertines, ³⁹Ar/⁴⁰Ar dating of pyroclastites and ¹⁴C dating of organic matter. Facies and stratigraphic correlations identify four transgressions (C1′, C1″, C2′ and C2″), each followed by a regression which ended with low lake levels that caused river incision and terrace formation. Evidence of the oldest transgression (C1′) is found in the uppermost reaches of valleys up to 1755 m, an altitude higher than the present lake threshold (1736 m). This C1′ transgression may be related to pyroclastic flows which dammed an outlet located in the western part of the lake basin and which is dated to before 105 ka. After 100 ka, a second transgression (C1″) reached 1730/1735 m, possibly related to a younger ignimbrite flow, in association with high water inflow (warm and/or wetter conditions). The two younger transgressions reached 1700–1705 m. The first one (C2′) is dated to 26–24.5 cal. ka BP and the second one (C2″) to 21–20 cal. ka BP. Available data suggest that the long‐term lake‐level changes responded mainly to climate oscillations. Additional events such as river captures caused by volcanic falls filling valleys, tectonism, erosion and karstic diversion may have impacted these long‐term lake‐level changes. Copyright © 2010 John Wiley & Sons, Ltd.  相似文献   

SATELLITE IMAGE ANALYSIS OF CIRCULAR ANOMALIES AND FRACTURING NETWORKS IN THE ARMORICAN MASSIF,FRANCE     

Joël Rolet  Hervé Yésou  Yves Besnus 《地理信息系统科学与遥感》2013,50(1):21-43

This paper describes results from a detailed study of circular anomalies—related to outcrops of granitic domes over the western part of the Armorican Massif—using SPOT, Landsat TM, Seasat, and composite imagery in conjunction with aerial photographs. Two types of features have been distinguished: (1) simple and circular, related to small granitic bodies or to hidden domes, which correspond with concentric networks of fractures formed during the cooling of the granite, and (2) complex and composite of the onion skin type, related to the larger plutonic domes. This type of feature could also be related to the concentric cooling networks but would more probably correspond to the magmatic foliation planes. Semi-circular features of the “half-moon” type, derived from these described structures, are located on the periphery of plutonic domes. These could correspond to preliminary intrusions cross cut by the major structures. From the lineament maps and based on the relationship between regional foliation fracturing networks and circular features, the following networks can be distinguished: (1) radial networks centered on plutonic diapirs, which seem to be contemporary with the granitic intrusions; (2) transverse networks that pass around or across circular features, creating fan-shaped forms and which are late with respect to the granitic intrusions; (3) post-tectonic fracturing networks that cross all previously described structures; and (4) a network, parallel to the regional foliation N070, which crosses or twists the circular features. This system documents the syntectonic pattern of the granites. Translated by Judit Ozoray, Chicoutimi, Quebec from: “Structures circulaires et réseaux de fractures en pays granitique. Analyse de données SPOT, Landsat TM et Seasat sur le Massif armoricain,” Bull. Soc. géol. France, 1993, Vol. 164, No. 2, pp. 199-214, with permission of the Société Gèologique de France (please cite original paper).  相似文献   

Effect of the steel material variability on the seismic capacity design of steel-concrete composite structures: a parametric study     

Hugues Somja  Srour Nofal  Mohammed Hjiaj  Hervé Degee 《Bulletin of Earthquake Engineering》2013,11(4):1099-1127

Modern seismic codes recommend the design of ductile structures able to absorb seismic energy through high plastic deformation. Since seismic ductile design relies on an accurate control of plastic hinges formation, which mainly depends on the distribution of plastic resistances of structural elements, efficiency of the design method strongly depends on the actual mechanical properties of materials. The objective of the present contribution is therefore to assess the impact of material variability on the performance of capacity-designed steel-concrete composite moment resisting frames.  相似文献   

Miocene to recent alkaline volcanism between Al Haruj and Waw an Namous (southern Libya)   总被引：1，自引：0，他引：1  

Jacques-Marie Bardintzeff  Catherine Deniel  Hervé Guillou  Bernard Platevoet  Philippe Télouk  Khaled M. Oun 《International Journal of Earth Sciences》2012,101(4):1047-1063

Unspiked K–Ar ages, petrological, geochemical and isotopic data are reported on samples from southern Libya (Wan an Namous—Al Haruj area). The Wan an Namous intracaldera cone dated at 0.2?Ma consists of unusually undersaturated foidite, representing the most extreme compositions among Libyan and Tibestian lavas. A basanitic and a basaltic lava flow located north-west of Wan an Namous, and probably belonging to the Al Haruj volcanic field, were dated at 5.1?Ma and 8.1?Ma. These data extend the range of ages previously reported for Al Haruj lavas. REE and multi-element patterns are typical of alkaline intraplate magmas. Sr ratios range from 0.70314 to 0.70812, whereas Nd ratios are very homogeneous (0.51290–0.51293). Pb ratios (19.231?<?²⁰⁶Pb/²⁰⁴Pb?<?19.547, 15.607?<?²⁰⁷Pb/²⁰⁴Pb?<?15.641 and 38.859?<?²⁰⁸Pb/²⁰⁴Pb?<?39.242) are typical of HIMU-FOZO compositions. Such isotope characteristics are very similar to those available on two Gharyan (northern Libya) lavas and largely overlap those of Hoggar and Cameroon Line alkaline rocks. These lavas were produced by low and variable degrees of partial melting of a garnet- and amphibole-bearing mantle source, constraining the depth of melting between 80 and 150?km. Crustal contamination was also probably involved for the oldest sample. Mineral compositions of a dunite–harzburgite xenolith clearly indicate that the lithospheric mantle was affected by partial melting and metasomatic processes by magmatic liquids, probably associated with the genesis of Cenozoic lavas. Lithospheric delamination and asthenospheric upwelling, due to the reactivation of lithospheric megastructures induced by the Africa-Europe convergence, could represent a model for the genesis of Libyan lavas, as in Hoggar.  相似文献   

Experimental study on the bioaccumulation of oxytetracycline and oxolinic acid by the blue mussel (Mytilus edulis). An evaluation of its ability to bio-monitor antibiotics in the marine environment   总被引：1，自引：0，他引：1  

Le Bris H  Pouliquen H 《Marine pollution bulletin》2004,48(5-6):434-440

The ability of blue mussel (Mytilus edulis) to act as a potential antibiotic bioindicator in marine waters was experimentally tested by the study of the kinetics of two veterinary antibiotics (oxolinic acid: OA and oxytetracycline: OTC). Antibiotic uptake was fast in the soft parts of the mussels. OA was quickly eliminated while OTC was released more slowly (half-life in viscera=3.9 days). OA and OTC were preferentially accumulated in gills and in viscera, respectively. Bio-accumulation factors were low (maximum: 2 for OTC in viscera) in accordance with the low K(ow)s. It was assumed that the higher OTC bioaccumulation pattern was related to its binding to mineral and organic compounds that led to its activity inhibition (62%). The antibiotics were persistent in shells (OTC half-life=8.3 days). Most veterinary and human antibiotics such as tetracyclines and sulphonamides have low log K(ow)(<2) and should weakly accumulate in mussel. This might limit the use of blue mussel to bio-monitor antibiotics in the marine environment.  相似文献