<p>Global industrial sulphur (S) dioxide emissions between 1900 to 1980 led to excessive S deposition and associated soil acidification.  However, since introducing effective mitigation strategies, industrial S emissions have been significantly reduced, with concurrent reductions in S deposition. This has resulted in S deficiency in many croplands which now require supplementary S applications via fertilisers. We examined if such past differential atmospheric S inputs (‘legacy’) influence organic (or inorganic) S dynamics in current agricultural soils. We used a 62-year chronosequence of the reclaimed agricultural field after brown-coal mining (Inden, Germany) to sample topsoil (0-30 cm) from seven sites (representing the years 1956, 1971, 1985, 1995, 2005, 2011, and 2018). The dynamics of sulphur transformation were determined by adding <sup>35</sup>S labelled methionine (Met) at 6, 24 and 48 h in an incubation experiment. The <sup>35</sup>S-Met and <sup>35</sup>S-SO<sub>4</sub><sup></sup>derived from labelled Met<sup></sup>were determined by measuring CaCl<sub>2</sub>-extractable <sup>35</sup>S with or without BaCl<sub>2</sub>, the difference between the total added <sup>35</sup>S-Met and the CaCl<sub>2</sub>-extractable <sup>35</sup>S was recognized as the <sup>35</sup>S immobilised in the microbial biomass. Results showed that soil S concentrations declined in a curvilinear pattern over the full chronosequence, from 0.27 (in 1956) to 0.11 g S kg<sup>-1</sup> soil (in 2018). In contrast, soil C peaked in 1995 at 16 g C kg<sup>-1</sup> soil, with the lowest values in 1956 at 10 g C kg<sup>-1</sup> soil. For the site recultivated in 1985, transformation and S dynamics obviously differed from others. Here, compared with other sites, the <sup>35</sup>S-SO<sub>4</sub><sup></sup>(inorganic S) concentrations (as % of the total <sup>35</sup>S-Met added) peaked at 12, 29, 38% respectively, and <sup>35</sup>S-Met (organic S) was the lowest at 35, 23, and 16%, respectively (at sampling times, 6, 24, and 48 h). The microbial biomass immobilized 53% of <sup>35</sup>S-Met added to the soils in less than 6 h, and gradually released it as <sup>35</sup>S-SO<sub>4</sub> as incubation time increased. We conclude that organic S transformation in the soils was driven by the C rather S content, possible through differences in microbial C biomass, As such the effect of the S legacy in the soils could not be confirmed. </p>
Microdialysis‐based soil sampling offers a potential alternative to traditional soil core extractions that better informs about the availability of nitrogen (N) for plant nutrition. This study compared soil N status, as estimated using 0.5 M K 2 SO 4 and distilled water extractions, with microdialysis‐derived diffusive flux measurements in eight grassland soils up an altitudinal gradient. Soil extracts and microdialysis samples were analyzed for plant‐available N: total free amino acids, NH 4 + , and NO 3 − . In terms of the percentage contribution that amino acids, NH 4 + , and NO 3 − made to total plant‐available N, the microdialysis‐derived diffusive flux measurements were most similar to distilled water extractions. However, the relative magnitude of the diffusive flux measurements did not always reflect the pool sizes as estimated by the soil extractions, which suggests that the availability of N to plants, via diffusion, may be decoupled from concentration in these soils. The potential and limitations of microdialysis sampling and the implications of the results for soil N management are discussed.
Routine bacterial monitoring of shellfish beds using indicator species is a common global practice designed to prevent human consumption of contaminated shellfish products. However, current bacteriological monitoring procedures which focus on the quantification of faecal indicator organisms (FIOs) as a proxy for microbial pollution may not be representative of total bacterial contamination levels present in shellfish harvesting areas. The objective of this study was to critically assess the accuracy of current monitoring strategies by quantifying the spatial (lateral and longitudinal distance) and temporal (seasonality and tidal state) concentrations of FIOs (Escherichia coli and total coliforms) within a single intertidal commercially harvested shellfish bed. Spatial and temporal FIO dynamics, including the effects of tidal state and seasonality, were quantified in mussel flesh and sediment samples from a single intertidal mussel (Mytilus edulis) bed. Our results confirmed that FIO concentrations across a shellfish bed were heterogeneous over larger spatial and temporal scales, but showed no relation to the concentrations of autochthonous bacteria, such as Vibrio spp., or the physico-chemical parameters of the sediment. These results have important implications for both public health and the economic prosperity of the shellfish industry, and demonstrate the importance of accommodating both spatial and temporal fluctuations in routine bacteriological monitoring protocols. We conclude that current FIO monitoring procedures may not accurately represent levels of microbial contamination within shellfish harvesting areas and that more robust microbiological testing procedures need developing.
Dune slacks are biodiverse seasonal wetlands within sand dune systems, strongly influenced by the dynamics of the local groundwater regime. Future climate predictions indicate strong adverse impact on the hydrology and therefore ecology of these wetland ecosystems. In this study we aimed to find the most appropriate hydrological and ecological indicators to summarise dune slack plant community responses to hydrology over multiple years. We evaluated 80 hydrological metrics (weighted and un-weighted median, mean, minimum, maximum, mean spring level, averaged over 1–8 year duration, and 5 additional 1-year metrics) against plant community responses (variants of Ellenberg EbF moisture indicator). The data were drawn from 453 relevées in 17 dune slacks, using permanent quadrats and co-located piezometers, set up in 2010 with vegetation monitoring repeated six times until 2019. Within our study we found a strong relationship between multiple hydrology metrics and the plant community response, but this displayed inter-annual variation with different patterns and correlations between years. The best performing hydrology metric was the unweighted 5-year average mean spring water level (MSL), linked to unweighted mean EbF using vascular plant species only. Maximum water level (MAX) also performed well, but MSL was preferred as MAX can be enhanced or truncated by topography leading to anomalies for individual slacks. MSL is also flexible to implement within manual monitoring programmes, which could be targeted to 3-months per year over the spring as a minimum requirement. These findings provide simpler metrics for site managers to monitor potential hydrology and vegetation responses to climate change.
Selling of damaged chicken wings (those with bone protrusion) for human consumption is prohibited in the European Union on the grounds of possible risks to human health arising from microbial contamination. Standard food industry tests were used to assess different categories of chicken wings (undamaged, farm damaged and factory damaged; n = 264) for, coliforms, Enterobacteriaceae, total viable counts, Pseudomonas spp., Staphylococcus aureus and Salmonella spp. No significant differences in bacterial numbers existed among wings belonging to the three categories. Only low numbers of bacteria were found throughout, and 97% of all results would pass the standards of a leading UK retailer. These results were strengthened by a longitudinal survey of wing breakage, which showed almost all wing puncturing occurred during the de-feathering process, limiting the likelihood of microbial contamination. Combined, these results indicate there is no increased health risk from consumption of damaged, compared to undamaged, chicken wings. The existing imposed regulations may therefore be an unnecessary burden on the poultry industry.
Two beam coupling is the process whereby two beams of light at similar frequencies are coupled together resulting in energy transfer from one beam to the other. The mechanism responsible for the coupling is a diffraction grating written within a photorefractive crystal.
Parent material greatly influences pedogenesis and soil nutrient availability and consequently we hypothesized that it would significantly affect the amount of organic solutes in soil, many of which have been implicated in rhizosphere processes linked to plant nutrient uptake. Consequently, we investigated the influence of two contrasting parent materials in which calcite was present or absent (alkaline and non-alkaline soils) on the concentrations of dissolved organic carbon (DOC), low-molecular weight organic acids (LMWOA) and glucose in soil solution. Both soils were under Norway spruce. The dynamics of LMWOAs in soil were also investigated using 14C-labelled citrate and oxalate. Some of the mineral horizons of the alkaline soils showed significantly higher concentrations of DOC, phenolics, and fumarate in soil solution and also a higher basal respiration. No major differences were seen in organic solute status in the organic horizons of the two soil types. LMWOAs were present at low concentrations in soil solution (<1 to 25 µM). Their mineralization rate significantly decreased with soil depth, however, overall neither their concentration or half-life in soil was markedly affected by parent material. The alkaline soils had significantly higher CO2-to-soil organic C (SOC) ratios, and consequently SOC in the alkaline soils did not seem more chemically stable against mineralization. Considering possible DOC and CO2 efflux rates it was suggested that the equal or larger SOC stocks in alkaline mineral soils were most likely linked to a higher net primary productivity. In conclusion, our study found that parent material exerted only a small effect on the concentration and dynamics of organic solutes in soil solution. This suggests that in comparison to other factors (e.g. vegetation cover, climate etc) parent material may not be a major regulator of the organic solute pool in soil.