A xenon gas purity monitor for EXO

We discuss the design, operation, and calibration of two versions of a xenon gas purity monitor (GPM) developed for the EXO double beta decay program. The devices are sensitive to concentrations of oxygen well below 1 ppb at an ambient gas pressure of one atmosphere or more. The theory of operation of the GPM is discussed along with the interactions of oxygen and other impurities with the GPM's tungsten filament. Lab tests and experiences in commissioning the EXO-200 double beta decay experiment are described. These devices can also be used on other noble gases.Comment: 41 pages, 26 figure

The marine cyanobacterium <i>Crocosphaera watsonii</i> WH8501 synthesizes the compatible solute trehalose by a laterally acquired OtsAB fusion protein

Compatible solutes are small organic molecules that are involved in the acclimation to various stresses such as temperature and salinity. Marine or moderate halotolerant cyanobacteria accumulate glucosylglycerol, while cyanobacteria with low salt tolerance (freshwater strains) usually accumulate sucrose or trehalose as the main compatible solutes. The screening of the genome of the marine, unicellular N2-fixing cyanobacterium Crocosphaera watsonii WH8501 revealed that instead of genes for glucosylglycerol biosynthesis, a fusion protein for the synthesis of trehalose was found that displayed similarities to trehalose-phosphate-synthase and -phosphatase (OtsAB pathway) from enterobacteria. Accordingly, cells of Crocosphaera showed salt-stimulated expression of the otsAB gene as well as a salt-dependent trehalose accumulation. The biochemical characterization of recombinant full-length OtsAB and truncated OtsB versions revealed that the otsAB gene in Crocosphaera encodes for an active trehalose-phosphate-synthase/phosphatase fusion protein. Genes coding for such proteins were not found in the genomes of other cyanobacteria but were present in many other, non-related marine bacteria, suggesting that otsAB might have been acquired by lateral gene transfer into the Crocosphaera genome

Modelling Freshwater Resources at the Global Scale: Challenges and Prospects

Quantification of spatially and temporally resolved water flows and water storage variations for all land areas of the globe is required to assess water resources, water scarcity and flood hazards, and to understand the Earth system. This quantification is done with the help of global hydrological models (GHMs). What are the challenges and prospects in the development and application of GHMs? Seven important challenges are presented. (1) Data scarcity makes quantification of human water use difficult even though significant progress has been achieved in the last decade. (2) Uncertainty of meteorological input data strongly affects model outputs. (3) The reaction of vegetation to changing climate and CO2 concentrations is uncertain and not taken into account in most GHMs that serve to estimate climate change impacts. (4) Reasons for discrepant responses of GHMs to changing climate have yet to be identified. (5) More accurate estimates of monthly time series of water availability and use are needed to provide good indicators of water scarcity. (6) Integration of gradient-based groundwater modelling into GHMs is necessary for a better simulation of groundwater-surface water interactions and capillary rise. (7) Detection and attribution of human interference with freshwater systems by using GHMs are constrained by data of insufficient quality but also GHM uncertainty itself. Regarding prospects for progress, we propose to decrease the uncertainty of GHM output by making better use of in situ and remotely sensed observations of output variables such as river discharge or total water storage variations by multi-criteria validation, calibration or data assimilation. Finally, we present an initiative that works towards the vision of hyper resolution global hydrological modelling where GHM outputs would be provided at a 1-km resolution with reasonable accuracy