Salinisation | EPFL Graph Search

thumb|upright=1.2|Un exemple de salinisation dans le Colorado La salinisation est l'accumulation des sels hydrosolubles (potassium, magnésium, calcium, chlore, sulfate, carbonate, bicarbonate) dans les sols à des niveaux toxiques pour la plupart des plantes, animaux et champignons. La sodification est l'augmentation dans les sols de sels à haute teneur en sodium. La salinisation et la sodification sont devenue une cause importante de désertification, d'érosion et de dégradation des sols et de l'agriculture et plus largement de la biodiversité. C'est aussi une . Ses causes sont diverses avec notamment le réchauffement climatique, la surexploitation ou la dérivation de ressources en eau douce, le défrichement, les incendies de forêt, l'irrigation, certaines effluents miniers salés, l'élévation du niveau marin, le recul du trait de côte, les ondes de tempête, l'utilisation de sels de déglaçage... Et les propectivistes annoncent une aggravation des modifications anthropiques du cycle h

Effects of deep pools on salinization in coastal reservoirs

David Andrew Barry, Jing Xu

Coastal reservoir contributes to alleviating the freshwater shortage in stressed areas, and the salinization of reservoir water is one of the most important challenges that coastal reservoir faced. Field-investigation indicates that there are many deep pools located at reservoir bed, and a large amount of high-salinity water was found within a deep pool which was hardly be desalted. Laboratory experiments and numerical simulations with different depth and locations of deep pools were conducted to further discuss the influence of deep pool on the salinization of reservoir and adjacent aquifer. Results showed that deep pool has greatly increased the salinity of reservoir water due to high-salinity water stored in the deep pool, which may act as an extra source of saltwater to the coastal reservoir during the dry season. The increasing depth of the deep pool was found to have negative impacts on the salinity of reservoir water, and as the distance from the deep pools to dam increased, the salinization extent in coastal reservoir decreased. Salinity data from the numerical simulations in coastal reservoirs and adjacent aquifer were matched the experimental data well. Flow field indicates that there is a high exchange capacity zone occurred from the deep pool to the seaward boundary, which gave the reasonable reasons for the existence of high-salinity water within deep pools. Those findings highlight the significant influence of deep pool on the salinization of the coastal reservoir, and explain the increased salinization by the deep pool.

2019

Comparative 16S rDNA and 16S rRNA sequence analysis indicates that Actinobacteria might be a dominant part of the metabolically active bacteria in heavy metal-contaminated bulk and rhizosphere soil

Fabienne Gremion

Bacterial diversity in 16S ribosomal DNA and reverse-transcribed 16S rRNA clone libraries originating from the heavy metal-contaminated rhizosphere of the metal-hyperaccumulating plant Thlaspi caerulescens was analysed and compared with that of contaminated bulk soil. Partial sequence analysis of 282 clones revealed that most of the environmental sequences in both soils affiliated with five major phylogenetic groups, the Actinobacteria, alpha-Proteobacteria, beta-Proteobacteria, Acidobacteria and the Planctomycetales. Only 14.7% of all phylotypes (sequences with similarities >97%), but 45% of all clones, were common in the rhizosphere and the bulk soil clone libraries. The combined use of rDNA and rRNA libraries indicated which taxa might be metabolically active in this soil. All dominant taxa, with the exception of the Actinobacteria, were relatively less represented in the rRNA libraries compared with the rDNA libraries. Clones belonging to the Verrucomicrobiales, Firmicutes, Cytophaga-Flavobacterium-Bacteroides and OP10 were found only in rDNA clone libraries, indicating that they might not represent active constituents in our samples. The most remarkable result was that sequences belonging to the Actinobacteria dominated both bulk and rhizosphere soil libraries derived from rRNA (50% and 60% of all phylotypes respectively). Seventy per cent of these clone sequences were related to the Rubrobacteria. subgroups 2 and 3, thus providing for the first time evidence that this group of bacteria is probably metabolically active in heavy metal-contaminated soil.

Wiley-Blackwell2003

Freshwater Flux and Spatiotemporal Simulated Runoff Variability into Ilulissat Icefjord, West Greenland, Linked to Salinity and Temperature Observations near Tidewater Glacier Margins Obtained Using Instrumented Ringed Seals

Konrad Steffen

The distribution of terrestrial surface runoff to Ilulissat Icefjord, west Greenland, is simulated for the period 2009-13 to better emphasize the spatiotemporal variability in freshwater flux and the link between runoff spikes and observed hydrographic conditions at theGreenland Ice Sheet tidewater glacier margins. Runoffmodel simulations were forced with automatic weather station data and verified against snow water equivalent depth, equilibrium line altitude, and quasi-continuous salinity and temperature observations obtained by ringed seals. Instrumented seals provide a novel platform to examine the otherwise inaccessible waters beneath the dense ice melange within the first 0-10 km of the calving front. The estimated mean freshwater flux from land was 70.6 +/- 4.2 km(3) yr(-1), with an 85% contribution of ice discharge from Jakobshavn Isbrae (also known as SermeqKujalleq), 14% from runoff, and the remaining 1% from precipitation on the fjord surface area, subglacial geothermal melting, and frictional melting due to basal ice motion. Runoff was simulated to be present from May to November and to vary spatially according to glacier cover and individual catchment size. Salinity and temperature observations correlate (significantly) with simulated runoff for the upper part of both the main fjord and southern fjord arm. Also, at the tidewater glacier margins in the northern and southern arm of Ilulissat Icefjord, salinity changes in the upper water column (upper 50 m) are significant after temporal spikes in runoff during late summer, while small-amplitude runoff variability during the recession of runoff did not create a clear signal in observed salinity variability. Also, in the southern arm near the glacier margin (between 100- and 150-m depth), the heterogeneous distribution in salinity could be because of the mixing of meltwater going upward from passing the grounding line. The effect of runoff spikes on observed salinity is less pronounced near the ice margin of Jakobshavn Isbrae than in the north and south arms.

Amer Meteorological Soc2015

Konrad Steffen

Amer Meteorological Soc2015