A comparison of match demands using ball-in-play versus whole match data in professional soccer players of the English Championship

This is the first study to report the Whole Match, ball-in-play (BiP), ball-out-of-play (BoP), and Max BiP (worst case scenario phases of play) demands of professional soccer players competing in the English Championship. Effective playing time per soccer game is typically 90 s) providing precise peak match demands. Whole-match demands recorded were compared to BiP and Max BiP, and BiP data excluded data from all match stoppages, providing a more precise analysis of match demands. Whole-match metrics were significantly lower than BiP metrics (p 90 s. No significant differences were found between positions. Ball-in-play analysis allows an accurate representation of the game and physical demands imposed on professional soccer players. Through having a clearer understanding of maximum game demands in professional soccer, will enable practitioners to design highly specific training methods

A comparison of match demands using ball-in-play vs. whole match data in elite male youth soccer players

Effective playing time in soccer is typically 90 seconds. This data allows practitioners to gain a deeper understanding of the physical demands imposed on players and plan sessions using targets that better represent match demands

Stakeholders' collaboration in defining scenarios relating to agricultural soils, on the basis of trends in relevant drivers

Trabajo presentado en Internation Union of Soil Science (IUSS)-100 Years of Soil Science, celebrado en Florencia (Italia) del 19 al 21 de mayo de 2024.The SERENA Project (EJP SOIL) aims to improve the effectiveness of European environmental policies, and in particular those on soil health, through the analysis of soil threats and soil-based ecosystem services in European agricultural landscapes. The need for good agro-management practices and techniques to contribute to the improvement of soil health and to mitigate the effects of and adapt to anticipated global change scenarios have been widely recognized. The predicted effects of global changes make it necessary to properly inform stakeholders about risks under future scenarios. To contribute to the improvement of soil health and to mitigate and adapt to the effects of global changes, it is important that people are made aware of the benefits of sustainable cropping systems and the implementation of beneficial for the soil agromanagement practices and techniques. With information taken from literature and in collaboration with stakeholders, this study focuses on defining the relevant scenarios for agricultural soils. The main drivers of change considered are climate change, demographic trends, changes in land use/land cover as well as land management. Stakeholders have been asked to identify potential mitigation entry points and have been offered the possibility to share their opinions and expertise on the outcome of the scenario analysis and the resulting implications for soil health and ecosystem services. The results indicate that further consideration must be given to how best to raise awareness among stakeholders on aspects of soil health. Here especially, the importance of soil threats and soil ecosystem services in maintaining soil health should be acknowledged. The scenario co-creation process with stakeholders plays a key role in evaluating the effectiveness of soil related policies in striving to achieve national and global environmental targets, including Agenda 2030 and its Sustainable Development Goals, the provisions given in the Rio Conventions, in the European Green Deal, and the proposals contained in the new EU Soil Law

Groundwater geochemistry, hydrogeology and potash mineral potential of the Lake Woods region, Northern Territory, Australia

We collected 38 groundwater and two surface-water samples in the semi-arid Lake Woods region of the Northern Territory to better understand the hydrogeochemistry of this system, which straddles the Wiso, Tennant Creek and Georgina geological regions. Lake Woods is presently a losing waterbody feeding the underlying groundwater system. The main aquifers comprise mainly carbonate (limestone and dolostone), siliciclastic (sandstone and siltstone) and evaporitic units. The water composition was determined in terms of bulk properties (pH, electrical conductivity, temperature, dissolved oxygen, redox potential), 40 major, minor and trace elements, and six isotopes (δ18Owater, δ2Hwater, δ13CDIC, δ34SSO42–, δ18OSO42–, 87Sr/86Sr). The groundwater is recharged through infiltration in the catchment from monsoonal rainfall (annual average rainfall ∼600 mm) and runoff. It evolves geochemically mainly through evapotranspiration and water–mineral interaction (dissolution of carbonates, silicates and to a lesser extent sulfates). The two surface waters (one from the main creek feeding the lake, the other from the lake itself) are extraordinarily enriched in 18O and 2H isotopes (δ18O of +10.9 and +16.4‰ VSMOW, and δ2H of +41 and +93‰ VSMOW, respectively), which is interpreted to reflect evaporation during the dry season (annual average evaporation ∼3000 mm) under low humidity conditions (annual average relative humidity ∼40%). This interpretation is supported by modelling results. The potassium (K) relative enrichment (K/Cl– mass ratio over 50 times that of sea water) is similar to that observed in salt-lake systems worldwide that are prospective for potash resources. Potassium enrichment is believed to derive partly from dust during atmospheric transport/deposition, but mostly from weathering of K-silicates in the aquifer materials (and possibly underlying formations). Further studies of Australian salt-lake systems are required to reach evidence-based conclusions on their mineral potential for potash, lithium, boron and other low-temperature mineral system commodities such as uranium.This project was undertaken as part of the salt-lake mineral prospectivity project at Geoscience Australia during 2012–2013, which was supported by appropriation funding from the Commonwealth of Australi

A comparison of match demands using ball-in-play vs. whole match data in elite male youth soccer players

© 2019 Informa UK Limited, trading as Taylor & Francis Group. Instruction: Effective playing time in soccer is typically 90 seconds.Conclusion: This data allows practitioners to gain a deeper understanding of the physical demands imposed on players and plan sessions using targets that better represent match demands

Strong physical constraints on sequence-specific target location by proteins on DNA molecules

Sequence-specific binding to DNA in the presence of competing non-sequence-specific ligands is a problem faced by proteins in all organisms. It is akin to the problem of parking a truck at a loading bay by the side of a road in the presence of cars parked at random along the road. Cars even partially covering the loading bay prevent correct parking of the truck. Similarly on DNA, non-specific ligands interfere with the binding and function of sequence-specific proteins. We derive a formula for the probability that the loading bay is free from parked cars. The probability depends on the size of the loading bay and allows an estimation of the size of the footprint on the DNA of the sequence-specific protein by assaying protein binding or function in the presence of increasing concentrations of non-specific ligand. Assaying for function gives an ‘activity footprint’; the minimum length of DNA required for function rather than the more commonly measured physical footprint. Assaying the complex type I restriction enzyme, EcoKI, gives an activity footprint of ∼66 bp for ATP hydrolysis and 300 bp for the DNA cleavage function which is intimately linked with translocation of DNA by EcoKI. Furthermore, considering the coverage of chromosomal DNA by proteins in vivo, our theory shows that the search for a specific DNA sequence is very difficult; most sites are obscured by parked cars. This effectively rules out any significant role in target location for mechanisms invoking one-dimensional, linear diffusion along DNA

Quantifying defects in graphene via Raman spectroscopy at different excitation energies.

We present a Raman study of Ar(+)-bombarded graphene samples with increasing ion doses. This allows us to have a controlled, increasing, amount of defects. We find that the ratio between the D and G peak intensities, for a given defect density, strongly depends on the laser excitation energy. We quantify this effect and present a simple equation for the determination of the point defect density in graphene via Raman spectroscopy for any visible excitation energy. We note that, for all excitations, the D to G intensity ratio reaches a maximum for an interdefect distance ∼3 nm. Thus, a given ratio could correspond to two different defect densities, above or below the maximum. The analysis of the G peak width and its dispersion with excitation energy solves this ambiguity

High resolution footprinting of a type I methyltransferase reveals a large structural distortion within the DNA recognition site.

The type I DNA methyltransferase M.EcoR124I is a multi-subunit enzyme that binds to the sequence GAAN6RTCG, transferring a methyl group from S-adenosyl methionine to a specific adenine on each DNA strand. We have investigated the protein-DNA interactions in the complex by DNase I and hydroxyl radical footprinting. The DNase I footprint is unusually large: the protein protects the DNA on both strands for at least two complete turns of the helix, indicating that the enzyme completely encloses the DNA in the complex. The higher resolution hydroxyl radical probe shows a smaller, but still extensive, 18 bp footprint encompassing the recognition site. Within this region, however, there is a remarkably hyper-reactive site on each strand. The two sites of enhanced cleavage are co-incident with the two adenines that are the target bases for methylation, showing that the DNA is both accessible and highly distorted at these sites. The hydroxyl radical footprint is unaffected by the presence of the cofactor S-adenosyl methionine, showing that the distorted DNA structure induced by M.EcoR124I is formed during the initial DNA binding reaction and not as a transient intermediate in the reaction pathway