Flux and composition of settling particles across the continental margin of the Gulf of Lion: the role of dense shelf water cascading

Settling particles were collected using sediment traps deployed along three transects in the Lacaze-Duthiers and Cap de Creus canyons and the adjacent southern open slope from October 2005 to October 2006. The settling material was analyzed to obtain total mass fluxes and main constituent contents (organic matter, opal, calcium carbonate, and siliciclastics). Cascades of dense shelf water from the continental shelf edge to the lower continental slope occurred from January to March 2006. They were traced through strong negative near-bottom temperature anomalies and increased current speeds, and generated two intense pulses of mass fluxes in January and March 2006. This oceanographic phenomenon appeared as the major physical forcing of settling particles at almost all stations, and caused both high seasonal variability in mass fluxes and important qualitative changes in settling material. Fluxes during the dense shelf water cascading (DSWC) event ranged from 90.1 g m(-2) d(-1) at the middle Cap de Creus canyon (1000 m) to 3.2 g m(-2) d(-1) at the canyon mouth (1900 m). Fractions of organic matter, opal and calcium carbonate components increased seaward, thus diminishing the siliciclastic fraction. Temporal variability of the major components was larger in the canyon mouth and open slope sites, due to the mixed impact of dense shelf water cascading processes and the pelagic biological production. Results indicate that the cascading event remobilized and homogenized large amounts of material down canyon and southwardly along the continental slope contributing to a better understanding of the off-shelf particle transport and the internal dynamics of DSWC events.

Nitrogen dynamics in soil management systems. I - flux of inorganic nitrogen (NH4+ and NO3-)

In agricultural systems the N-NH4+ and N-NO3- contents is significantly affected by soil management. This study investigated the dynamics of inorganic nitrogen (N; NH4+ and NO3-) in an experimental evaluation of soil management systems (SMSs) adopted in 1988 at the experimental station of the ABC Foundation in Ponta Grossa, in the Central South region of the State of Paraná. The objective of this study was to evaluate the changes in N-NH4+ and N-NO3- flux in the surface layer of a Red Latosol arising from SMSs over a 12-month period. The experiment was arranged in a completely randomized block design in split plots, in three replications. The plots consisted of the following SMSs: 1) conventional tillage (CT); 2) minimum tillage (MT); 3) no-tillage with chisel plow every three years (NT CH); and 4) continuous no-tillage (CNT). To evaluate the dynamics of inorganic N, the subplots represented samplings (11 sampling times, T1 - T11). The ammonium N (N-NH4+) and nitric N (N-NO3-) contents were higher in systems with reduced tillage (MT and NT CH) and without tillage (CNT) than in the CT system. In the period from October 2003 to February 2004, the N-NH4+ was higher than the N-NO3- soil content. Conversely, in the period from May 2004 to July 2004, the N-NO3- was higher than the N-NH4+ content. The greatest fluctuation in the N-NH4+ and N-NO3- contents occurred in the 0-2.5 cm layer, and the highest peak in the N-NH4+ and N-NO3- concentrations occurred after the surface application of N. Both N-NH4+ and N-NO3- were strongly correlated with the soil organic C content, which indicated that these properties vary together in the system.

Prise en charge du traumatisme cranio-cérébral sévère [Update on the management of severe traumatic brain injury]

Prognosis after severe traumatic brain injury (TBI) is determined by the severity of initial injury and secondary cerebral damage. The main determinants of secondary cerebral damage are brain ischemia and oedema. Traumatic brain injury is a heterogeneous disease. Head CT-scan is essential in evaluating initial type of injury and severity of brain oedema. A standardised approach based on prevention and treatment of secondary cerebral damage is the only effective therapeutic strategy of severe TBI. We review the classification, pathophysiology and treatment of secondary cerebral damage after severe TBI and discuss the management of intracranial hypertension, cerebral perfusion pressure and brain ischemia.

Seasonal dependence in the solar neutrino flux

Mikheyev-Smirnov-Wolfenstein (MSW) solutions of the solar neutrino problem predict a seasonal dependence of the zenith angle distribution of the event rates, due to the nonzero latitude at the Super-Kamiokande site. We calculate this seasonal dependence and compare it with the expectations in the no-oscillation case as well as just-so scenario, in the light of the latest Super-Kamiokande 708-day data. The seasonal dependence can be sizable in the large mixing angle MSW solution and would be correlated with the day-night effect. This may be used to discriminate between MSW and just-so scenarios and should be taken into account in refined fits of the data.

Soil CO2 flux: a method comparison of closed static chambers in a sugarcane field

A large variety of techniques have been used to measure soil CO2 released from the soil surface, and much of the variability observed between locations must be attributed to the different methods used by the investigators. Therefore, a minimum protocol of measurement procedures should be established. The objectives of this study were (a) to compare different absorption areas, concentrations and volumes of the alkali trapping solution used in closed static chambers (CSC), and (b) to compare both, the optimized alkali trapping solution and the soda-lime trapping using CSC to measure soil respiration in sugarcane areas. Three CO2 absorption areas were evaluated (7; 15 and 20 % of the soil emission area or chamber); two volumes of NaOH (40 and 80 mL) at three concentrations (0.1, 0.25 and 0.5 mol L-1). Three different types of alkaline traps were tested: (a), 80 mL of 0.5 mol L-1 NaOH in glass containers, absorption area 15 % (V0.5); (b) 40 mL of 2 mol L-1 NaOH retained in a sponge, absorption area 80 % (S2) and (c) 40 g soda lime, absorption area 15 % (SL). NaOH concentrations of 0.5 mol L-1 or lower underestimated the soil CO2-C flux or CO2 flux. The lower limit of the alkali trap absorption area should be a minimum of 20 % of the area covered by the chamber. The 2 mol L-1 NaOH solution trap (S2) was the most efficient (highest accuracy and highest CO2 fluxes) in measuring soil respiration.

Contribution of macroporosity to water flux of a soil under different tillage systems

In view of the importance of the macroporosity for the water transport properties of soils, its quantitative assessment is a challenging task. Measurements of hydraulic conductivity (K) at different soil water tensions and the quantification of water-conducting macropores (θM) of a soil under different tillage systems could help understand the effects on the soil porous system and related hydraulic properties. The purpose of this study was to assess the effects of Conventional Tillage (CT), Chisel Plow (CP) and No Tillage (NT) on θM and on K; and to quantify the contribution of macroporosity to total water flux in a loam soil. A tension disc infiltrometer was used at two soil water pressure heads (-5 cm, and 0) to infer θM and K, during fallow. Macroporosity was determined based on the flow contribution between 0 and -5 cm water potentials (K0, K5, respectively), according to the Hagen-Poiseuille equation. The K0 values were statistically higher for CT than for NT and CP. The K5 values did not differ statistically among treatments. The mean K values varied between 0.20 and 3.70 cm/h. For CT, θM was significantly greater than for CP and NT, following the same trend as K0. No differences in θM were detected between CP and NT. With CT, the formation of water-conducting macropores with persistence until post-harvest was possible, while under CP preparation, the water-conducting macropores were not persistent. These results support the idea that tillage affects the soil water movement mainly by the resulting water-conducting macropores. Future studies on tillage effects on water movement should focus on macroporosity.

Effets sur le métabolisme cérébral par PET au 18F-FDG de la stimulation du nerf vague chez les patients épileptiques

Contexte : La stimulation du nerf vague est une technique neurochirurgicale qui consiste en l'implantation d'une électrode envoyant des impulsions autours de celui-ci. Depuis l'approbation de la FDA en 1997 aux Etats-Unis, elle est utilisée chez certains patients épileptiques pharmaco-résistants et dont la chirurgie classique n'est pas envisageable [1], Par exemple lorsque qu'aucun foyer épileptique n'est identifiable, qu'une zone éloquente du cortex est atteinte ou encore qu'il y a de multiples points de départ. On parle généralement de patient « répondeur » lorsqu'une diminution de plus de 50% des crises est observée après l'opération. La proportion de patients répondeurs est estimée entre 20 à 50% [2], avec une action positive sur l'éveil [3]. Le mécanisme d'action de cette thérapie reste largement inconnu même si quelques ébauches d'hypothèses ont été formulées, notamment une action inhibitrice sur le noyau solitaire du nerf vague qui pourrait avoir comme effet de moduler des projections ascendantes diffuses via le locus coeruleus [3, 4]. Objectifs : Le but de ce travail est d'observer les effets de la stimulation du nerf vague sur le métabolisme cérébral et potentiellement d'élaborer des hypothèses sur le mécanisme d'action de ce traitement. Il faudra plus précisément s'intéresser au tronc cérébral, contenant le locus coeruleus (métabolisme de la noradrénaline) et aux noyaux du raphé (métabolisme de la sérotonine), deux neurotransmetteurs avec effet antiépileptique [5]. Le but sera également d'établir des facteurs prédictifs sur la façon de répondre d'un patient à partir d'une imagerie cérébrale fonctionnelle avant implantation, notamment au niveau du métabolisme cortical, particulièrement frontal (éveil) sera intéressant à étudier. Méthodes : Un formulaire d'information ainsi que de consentement éclairé sera remis à chaque patient avant inclusion dans l'étude. Les informations de chaque patient seront également inscrites dans un cahier d'observation (Case Report Form, CRF). Le travail s'organisera essentiellement sur deux populations. Premièrement, chez les patients déjà opérés avec un stimulateur en marche, nous réaliserons qu'une imagerie PET au F-18-fluorodeoxyglucose (FDG) post-opératoire qui seront comparés à une base de données de patients normaux (collaboration Dr E. Guedj, AP-HM, La Timone, Marseille). Nous confronterons également les images de ces patients entre elles, en opposant les répondeurs (diminution des crises de ≥50%) aux non-répondeurs. Deuxièmement, les patients non encore opérés auront un examen PET basal avant implantation et 3-6 mois après la mise en marche du stimulateur. Nous évaluerons alors les éventuelles modifications entre ces deux imageries PET, à la recherche de différences entre les répondeurs et non-répondeurs, ainsi que de facteurs prédictifs de bonne réponse dans l'imagerie de base. Toutes les comparaisons d'images seront effectuées grâce avec le programme d'analyse SPM08. Résultats escomptés : Nous espérons pouvoir mettre en évidence des modifications du métabolisme cérébral au FDG sur la base de ces différentes images. Ces constatations pourraient nous permettre de confirmer ou d'élargir les hypothèses physiologiques quant aux effets du traitement par stimulation vagale. Nous aimerions, de plus, amener à définir des facteurs prédictifs sur la façon de répondre d'un patient au traitement à l'aide du PET au F-18-FDG de départ avant implantation. Plus value escomptée : Ces résultats pourront donner des pistes supplémentaires quant au fonctionnement de la stimulation vagale chez les patients avec épilepsie réfractaire et servir de base à de nouvelles recherches dans ce domaine. Ils pourraient aussi donner des éléments pronostics avant l'implantation pour aider la sélection des patients pouvant bénéficier de ce type de thérapie.

Threading dislocation lines in two-sided flux-array decorations

Two-sided flux decoration experiments indicate that threading dislocation lines (TDLs), which cross the entire film, are sometimes trapped in metastable states. We calculate the elastic energy associated with the meanderings of a TDL. The TDL behaves as an anisotropic and dispersive string with thermal fluctuations largely along its Burgers vector. These fluctuations also modify the structure factor of the vortex solid. Both effects can, in principle, be used to estimate the elastic moduli of the material.

Relation entre glucose cérébral et systémique chez le sujet neurolésé: une étude par microdialyse cérébrale

Introduction: Le glucose est le principal substrat énergétique cérébral. Sa concentration dans le cerveau est étroitement liée à la glycémie. Chez le patient neurolésé, du fait de l'augmentation des besoins énergétiques, les réserves cérébrales de glucose sont limitées. Une glycémie suffisamment élevée paraît nécessaire pour assurer un apport adéquat de glucose au cerveau. Objectifs : Le but de cette étude est de mieux comprendre la relation entre glucose cérébral et glycémie lors de lésion cérébrale en analysant la physiologie cérébrale chez des patients neurolésés. Plus précisément nous investiguerons: La relation entre le glucose cérébral et le glucose systémique et son association avec le pronostic vital, l'association entre la neuroglucopénie et différents paramètres cérébraux tel que l'hypertension intracrânienne (HTIC) ou la dysfonction énergétique et finalement l'effet d'une perfusion de glucose 10% sur le glucose cérébral lors d'état de neuroglucopénie. Méthodologie : Analyse d'une base de données prospective comportant des patients souffrant d'un traumatisme crânio-cérébral (TCC) ou une hémorragie sous- arachnoïdienne (HSA) sévères. Les patients comateux sont monitorés par un dispositif intra-parenchymateux avancé, comprenant un cathéter de microdialyse cérébrale et un capteur de PbO2. Résultats : 34 patients consécutifs (moyenne d'âge 42 ans, moyenne de temps jusqu'au début du monitoring : 1.5 jours ± 1 ; moyenne de la durée maximale du monitoring : 6 jours ± 3) ont été étudiés, 25 patients souffrant d'un TCC et 9 patients avec une HSA. Nous avons obtenu une corrélation individuelle entre le glucose cérébral et la glycémie chez 52.9 % des patients. Lorsque la glycémie est inférieure à 5 mmol/l, on observe plus fréquemment des épisodes de neuroglucopénie en comparaison aux valeurs intermédiaires de glycémie (5 - 9.9 mmol/l). Les épisodes d'HTIC (pression intracrânienne (PIC) > 20 mmHg) sont plus fréquemment associés à des épisodes de neuroglucopénie que lorsque la pression intracrânienne est normale 75 % vs. 35%. La dysfonction énergétique est plus souvent associés à des épisodes de neuroglucopénie que lorsque le LPR est normal: 55% contre 36%. Un coefficient de corrélation entre glucose cérébral et glycémie significativement plus élevé a été obtenu chez les survivants que chez les non-survivants (0.1 [interquartile range 0.02- 0.3] contre 0.32 [0.17-0.61]). Chez les patients neuroglucopéniques ayant une corrélation entre glucose cérébral et glycémie, la perfusion de glucose i.v. fait monter le glucose cérébral jusqu'à l'arrêt de la perfusion. Conclusion : Malgré une étroite relation entre glycémie et glucose cérébral en conditions stables, cette relation peut être altérée par des causes cérébrales chez les patients neurolésés montrant que la diminution de la disponibilité du glucose extracellulaire ne résulte pas uniquement d'une hypoglycémie relative mais également de causes cérébrales tel que l'hypoperfusion, l'HTIC ou la dysfonction énergétique.

Vortices and extreme black holes: The question of flux expulsion

It has been claimed that extreme black holes exhibit a phenomenon of flux expulsion for Abelian Higgs vortices, irrespective of the relative width of the vortex to the black hole. Recent work by two of the authors showed a subtlety in the treatment of the event horizon, which cast doubt on this claim. We analyze in detail the vortexextreme black hole system, showing that, while flux expulsion can occur, it does not do so in all cases. We give analytic proofs for both expulsion and penetration of flux, in each case deriving a bound for that behavior. We also present extensive numerical work backing up, and refining, these claims, and showing in detail how a vortex can end on a black hole in all situations. We also calculate the back reaction of the vortex on the geometry, and comment on the more general vortexblack hole system.

The roles of flux- and decompression melting and their respective fractionation lines for continental crust formation: Evidence from the Kohistan arc

Delamination and foundering of the lower continental crust (LCC) into the mantle is part of the crust-forming mechanism. However, knowledge of the composition and mineralogy of the preserved or delaminated LCC over geological timescales remains scarce. We provide a synopsis of recent research within the Kohistan arc (Pakistan) and demonstrate that hydrous and less hydrous liquid lines of descent related to flux assisted and decompression mantle melting, respectively, produce compositionally different lower crustal rocks. The argument refers to two lower crustal sections exposed in Kohistan, the older Southern Plutonic Complex (SPC) and the younger Chilas Complex. The SPC typifies a hydrous, high-pressure fractionation sequence of olivine-pyroxenes-garnet-Fe/Ti-oxide-amphibole-plagioclase. The Chilas Complex illustrates a less hydrous fractionation sequence of olivine-clinopyroxene-orthopyroxene-plagioclase-amphibole. Despite the similarity of the Chilas Complex rocks to proposed lower crust compositions, the less hydrous fractionation results in unrealistically small volumes of silica-rich rocks, precluding the Chilas Complex gabbros to represent the magmatic complement to the upper crust. The composition of the SPC lower crust differs markedly from bulk lower crust estimates, but is complementary to silica-rich rocks exposed along this section and in the Kohistan batholith. These observations inspire a composite model for the formation of continental crust (CC) where the negatively buoyant delaminated and the buoyant preserved lower continental crusts (LCC) differ in genesis, mineralogy, and composition. We propose that the upper, non-sedimentary subsequent removal of the complementary, negatively buoyant garnet-pyroxene-amphibole-plagioclase-rich cumulates. In contrast, the LCC, which is buoyant and preserved over geological timescales, is formed by less hydrous parental mantle melts. We suggest that the bulk continental crust composition is related to mixing of these petrologically not directly related end members. Published by Elsevier B.V.

Effets de la perfusion de facteurs natriurétiques auriculaires synthétiques sur quelques flux régionaux chez le volontaire sain [Effect of synthetic atrial natriuretic factors on various regional blood flows in the healthy subject]

The effects of continuous infusions of 2 synthetic atrial natriuretic peptides Ile12-(3-28) (rANP) and Meth12-(3-28) (hANP) eicosahexapeptides on blood pressure, heart rate, skin blood flow, glomerular filtration rate, renal plasma flow, apparent hepatic blood flow, and carotid blood flow were evaluated in normal volunteers. A rANP infusion at increasing rates (1-40 micrograms/min) induced a decrease in blood pressure, an increase in heart rate and in skin blood flow linearly related to the dose administered. In contrast, hANP infusion at 1 microgram/min for 4 hours induced an initial increase followed by a secondary fall in skin blood flow without blood pressure changes. A 4-hour rANP infusion at 0.5 and 5 mcg/min did not alter glomerular filtration rate but induced a delayed and dose-related fall in renal plasma flow from 531 to 461 (p less than 0.05), and from 554 to 342 ml/min (p less than 0.001) respectively, with a consequential rise in the filtration fraction. The 5 mcg/min dose furthermore significantly reduced blood pressure following a latency period of 2.5 hours. A 2-hours rANP infusion at 0.5 micrograms/min induced a fall in apparent hepatic blood flow from 1,087 to 863 ml/min (p less than 0.01), without simultaneously altering blood pressure. Similarly, a 2-hour hANP infusion at 2 micrograms/min altered neither blood pressure nor carotid blood flow. In conclusion, ANP infusion induced changes in systemic and regional hemodynamics varying in direction, intensity and duration.

Surface-dependent strategies and energy flux in benthic marine communities or, why corals do not exist in the Mediterranean

Most structure-building organisms in rocky benthic communities are surface-dependent because their energy inputs depend mainly on the surface they expose to water. Two photosynthetic strategies, divided into calcareous and non calcareous algae, strict suspension-feeders and photosynthetic suspension feeders (e.g. hermatypic corals) are the four main strategies evolutively acquired by benthic organisms. Competition between those strategies occur in relation to productivity of the different species, in such a way that, for given environmental conditions, species with a higher growth (P/B ratio) would dominate. At a worldwide scale, littoral marine benthos can he considered to fit into the four fields defined by two main axes: the first, relates to productivity and relies atrophic and oligotrophic waters and the second is defined by the degree of environmental variability or seasonality (from high to low). Coral reefs (marine ecosystems dominated by photosynthetic suspension feeders) develop in the space of oligotrophic areas with low variability, while kelp beds (marine ecosystem dominated by large, non calcareous algae) are to be found only in eutrophic places with a high variability. The space of eutrophic waters with a low variability do not has specially adapted, high structured, benthic marine ecosystems, and in these conditions opportunistic algae and animals predominate. Finally, photophilic mediterranean benthos -devoid of kelps and without hermatypic corals- typifies the field of oligotrophic areas with high variability; in its more genuine aspect, Mediterranean benthos is represented by small algae with a high percentage of calcareous thallii. In all cases strict suspension-feeders compete successfully with photosynthetic organisms only in situations of low irradiances or very high inputs of POM. In its turn, Mediterranean rocky benthos, in spite of its relative uniformity, is geographically organized along the same axes. The Gulf of Lions and the insular bottoms (Balearic Islands, for example) would correspond to the extremes of eutrophic-high variability areas and oligotrophic-low variability areas, respectively. Irradiance, nutrient and POM concentration, and hydrodynamism are the three variables which mainly affect the distribution of the different surface-dependent strategies, and thus, these parameters are of paramount interest for understanding the trophic structure of Mediterranean benthic communities. In environments non limited by light, nutrient availability, defined as the product between nutrient -POM concentration and hydrodynamism, states the dominance of calcareous versus non calcareous algae. Calcareous algae dominate in oligotrophic waters while non-calcareous algae dominate in moderately eutrophic waters. In light-limited environments, passive suspension feeders (octocorallaria, gorgonians) become dominant species if POM availability is enhanced by a high hydrodynamism (strong currents); in waters with a low charge of POM organisms of other groups, mainly active suspension feeders, predominate (sponges, bryozoans, scleractiniarians). In any case, there always exists a very variable bathymetric zone, depending on light attenuation and nutrient-POM availability, where encrusting calcareous algae strongly compete with suspension feeders (coralligenous).