Taxation of sugar-sweetened beverages for reducing their consumption and preventing obesity or other adverse health outcomes:protocol

This is a protocol for a Cochrane Review (Intervention). The objectives are as follows: To assess the effects of taxation of sugar‐sweetened beverages (SSBs) on SSB consumption, energy intake, overweight, obesity, and other adverse health outcomes in the general population

Taxation of unprocessed sugar or sugar-added foods for reducing their consumption and preventing obesity or other adverse health outcomes

No abstract available

Identification of intermediates formed during anaerobic benzene degradation by an iron-reducing enrichment culture.

Anaerobic benzene degradation is an important process in contaminated aquifers but is poorly understood due to the scarcity of microbial cultures for study. We have enriched a ferric iron-reducing culture that completely mineralizes benzene to CO2. With 13C6-labelled benzene as the growth substrate, ring-labelled benzoate was identified as a major intermediate by liquid chromatography/tandem mass spectrometry (LC/MS/MS) analysis of culture supernatants. With increasing incubation time, 13C7-labelled benzoate appeared, indicating that the carboxyl group of benzoate derived from CO2 that was produced from mineralization of labelled benzene. This was confirmed by growing the culture in 13C-bicarbonate-buffered medium with unlabelled benzene as the substrate, as the label appeared in the carboxyl group of benzoate produced. Phenol was also identified as an intermediate at high concentration. However, it was clearly shown that phenol was formed abiotically by autoxidation of benzene during the sampling and analysis procedure as a result of exposure to air. The results suggest that, in our culture, anaerobic benzene degradation proceeds via carboxylation and that caution should be exercised in interpreting hydroxylated benzene derivatives as metabolic intermediates of anaerobic benzene degradation

High resolution monitoring above and below the groundwater table uncovers small-scale hydrochemical gradients.

Hydrochemical solute concentrations in the shallow subsurface can be spatially highly variable within small scales, particularly at interfaces. However, most monitoring systems fail to capture these small scale variations. Within this study, we developed a high resolution multilevel well (HR-MLW) with which we monitored water across the interface of the unsaturated and saturated zone with a vertical resolution of 0.05-0.5 m. We installed three of these 4 m deep HR-MLWs in the riparian zone of a third-order river and analyzed for hydrochemical parameters and stable water isotopes. The results showed three distinct vertical zones (unsaturated zone, upper saturated zone, lower saturated zone) within the alluvial aquifer. A 2 m thick layer influenced by river water (upper saturated zone) was not captured by existing monitoring wells with higher screen length. Hydrochemical data (isotopes, total ions) were consistent in all HR-MLWs and showed similar variation over time emphasizing the reliability of the installed monitoring system. Further, the depths zones were also reflected in the NO3-N concentrations; with high spatial variabilities between the three wells. The zonation was constant over time, with seasonal variability in the upper saturated zone due to the influence of river water. This study highlights the use of high resolution monitoring for identifying the spatial and temporal variability of hydrochemical parameters present in many aquifer systems. Possible applications range from riparian zones, agricultural field sites to contaminated site studies, wherever an improved understanding of biogeochemical turnover processes is necessary