Ambient vertical flow in long-screen wells: a case study in the Fontainebleau Sands Aquifer (France)

A tritium (H-3) profile was constructed in a long-screened well (LSW) of the Fontainebleau Sands Aquifer (France), and the data were combined with temperature logs to gain insight into the potential effects of the ambient vertical flow (AVF) of water through the well on the natural aquifer stratification. AVF is commonly taken into account in wells located in fracture aquifers or intercepting two different aquifers with distinct hydraulic heads. However, due to the vertical hydraulic gradient of the flow lines intercepted by wells, AVF of groundwater is a common process within any type of aquifer. The detection of 3H in the deeper parts of the studied well ( approximate depth 50m), where H-3-free groundwater is expected, indicates that shallow young water is being transported downwards through the well itself. The temperature logs show a nearly zero gradient with depth, far below the mean geothermal gradient in sedimentary basins. The results show that the age distribution of groundwater samples might be biased in relation to the age distribution in the surroundings of the well. The use of environmental tracers to investigate aquifer properties, particularly in LSWs, is then limited by the effects of the AVF of water that naturally occurs through the well.

Origin of Early Carboniferous pseudo-adakites in northern Brittany (France) through massive amphibole fractionation from hydrous basalt

P>The first Variscan pseudo-adakites were identified in close association with the Saint-Jean-du-Doigt (SJDD) mafic intrusion (Brittany, France) in a geodynamic context unrelated to subduction. These rocks are trondhjemites emplaced 347 +/- 4 Ma ago as 2-3 km2 bodies and dykes. Trace-element concentrations and Sr-Nd-Pb isotope ratios indicate that the SJDD pseudo-adakites probably resulted from extreme differentiation of an SJDD-type hydrous basaltic magma in a lower continental crust of normal thickness (0.8 GPa). Modelling shows that garnet is not a required phase, which was commonly believed to be the case for continental arc-derived adakite-like rocks. A massive fractionation of amphibole fits the data much better and does not require high pressures, in agreement with the inferred extensional tectonic regime at the time of pluton emplacement. Alternatively, the SJDD pseudo-adakites could have resulted from the melting of newly underplated SJDD mafic precursors, but thermal considerations lead us to believe that this was not the case.

Collaboration entre cliniciens et chercheurs autour de la «consultation systémique» : une situation de violence intrafamiliale

Cet article vise à illustrer la collaboration et l'enrichissement mutuel qu'apportent aux chercheurs et aux cliniciens l'utilisation de la «consultation systémique». Cette dernière, demandée soit spontanément par les parents, soit par le(s) thérapeute(s) qui suive(nt) la famille, a pour but l'évaluation des interactions familiales. Lors d'une première rencontre, les questions qui motivent les parents et/ou thérapeute(s) à consulter sont formulées et la famille est invitée à faire des jeux familiaux semi-standardisés qui sont filmés. Lors d'une deuxième rencontre réunissant les mêmes personnes, un visionnement d'extraits des films sert de base à une discussion ainsi qu'à l'élaboration de réponses aux questions posées, en partant des observations des chercheurs. Après une description de la consultation systémique standard (principes, objectifs, procédure et situations d'observation), une vignette clinique atypique, concernant des violences intrafamiliales, illustrera la variété et la richesse de ces consultations. Les observations micro et macro-analytiques des interactions données par les chercheurs, auxquelles s'ajoute la compréhension clinique des thérapeutes, montrent qu'une collaboration entre eux est fructueuse pour toutes les parties concernées.