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High-quality soils are an important resource affecting the quality of life of human societies, as well as terrestrial ecosystems in general. Thus, soil erosion and soil loss are a serious issue that should be managed, in order to conserve both artificial and natural ecosystems. Predicting soil erosion has been a challenge for many years. Traditional field measurements are accurate, but they cannot be applied to large areas easily because of their high cost in time and resources. The last decade, satellite remote sensing and predictive models have been widely used by scientists to predict soil erosion in large areas with cost-efficient methods and techniques. One of those techniques is the Revised Universal Soil Loss Equation (RUSLE). RUSLE uses satellite imagery, as well as precipitation and soil data from other sources to predict the soil erosion per hectare in tons, in a given instant of time. Data acquisition for these data-demanding methods has always been a problem, especially for scientists working with large and diverse datasets. Newly emerged online technologies like Google Earth Engine (GEE) have given access to petabytes of data on demand, alongside high processing power to process them. In this paper we investigated seasonal spatiotemporal changes of soil erosion with the use of RUSLE implemented within GEE, for Pindos mountain range in Greece. In addition, we estimated the correlation between the seasonal components of RUSLE (precipitation and vegetation) and mean RUSLE values.

F0F1-ATPase has been isolated from the marine alkali-resistant bacterium Vibrio alginolyticus. The enzyme subunits cross-reacted with antibodies against subunits alpha, beta, gamma, epsilon, and b of E. coli ATPase. The purified ATPase was reconstituted into liposomes effecting an ATP-dependent uptake of H+. Proton transport was inhibited by the ATPase blockers DCCD, triphenyltin, and venturicidin. Na+ ions had no effect on ATP-dependent proton transport. No ATP-dependent transport of Na+ was detected in proteoliposomes.