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Two fire-affected soils were studied usingmicromorphological methods. The objective of the paper is to assess andcompare fire effects on the micropedological organisation of soils in a forest-steppe zone of central Russia (Volga Basin, Togliatti city). Sampleswere collected in the green zone of Togliatti city. The results showed thatboth soils were rich in quartz and feldspar. Mica was highly present in soilsaffected by surface fires, while calcium carbonates were identified in thesoils affected by crown fires. The type of plasma is humus–clay, but the soilassemblage is plasma–silt with a prevalence of silt. Angular andsubangular grains are the most dominant soil particulates. No evidence ofintensive weathering was detected. There was a decrease in the porosity of soils affected by fires as a consequence of soil pores filled with ash andcharcoal

Micromorphological characteristics of sandy forest soils recently impacted by wildfires in Russia