Abstract:<p>It is shown that in the area of sandy steppe in a nature reserve "Dnieper-Orelsky" the soil temperature has been changed from 17.2 to 31.0 ° C. Loci with higher temperatures are on the left and right ends of the landfill, whereas the plot with lower temperature was located in the central region. There is a tendency of spatial variability of soil temperature, which could be explained by vegetation location and edaphic characteristics. We calculated the indicators of spatial dependence and the radius of… Show more
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