The first monograph of Ukrainian soil scientists on the Holocene evolution of soilsReview of the first monograph of Ukrainian
soil scientists on Holocene evolution of
soils Changes in status of soil salinity in North Crimea since 2013, as detected by Landsat 8 OLI data and objective information about the modern state of
soil secondary salinization
processes. Comparison
The place of soil formation values in the problem of rate setting soil loss toleranc tolerance), which are based on the choice of the scenario of optimal
soil use, on the estimation of the
main Soil organic matter priming: The pH effects carbon (C) cycling.
Soil pH is a
main factor defining priming effects (PEs) because it (i) controls
Strength of frozen soils during thawing subject to load, in order to determine the
main parameters affecting the stability of
soils during thawing
The selection of energy-efficient main processing of the soil for sugar sorghum processing of
soil are given great attention, as it largely affects the water-physical, biological
Universality of priming effect: An analysis using thirty five soils with contrasted properties sampled from five continentsPerveen N.,
Barot S.,
Maire V.,
Cotrufo M.F.,
Shahzad T.,
Blagodatskaya E.,
Stewart C.E.,
Ding W.,
Siddiq M.R.,
Dimassi B.,
Mary B.,
Fontaine S. soils are more prone to PE induced by cellulose addition. Variations in PE were
mainly explained by
soil