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The Development of Chernozems on the Dniester-Prut Interfluve in the Holocenepedogenesis

Petromagnetic Properties of Fallow Soils as an Indicator of the Organic-Matter Content the pedogenesis processes. A statistically significant relationship between the humus content on the one hand

Heochemical preconditions of resistace and degradation the ferralythic soils, moist and changeable moist of Angola tropics of convergence of pedogenesis. The influence of the lithological factor is most dramatic in such specific

Soils with the second humus horizon, paleochernozems, and the history of pedogenesis at the border between forest and steppe areasSoils with the second humus horizon, paleochernozems, and the history of pedogenesis at the border

Soils with the second humus horizon, paleochernozems, and the history of pedogenesis at the border between forest and steppe areasSoils with the second humus horizon, paleochernozems, and the history of pedogenesis at the border

Plant–soil–microbial interactions mediate vegetation succession in retreating glacial forefieldsInitial pedogenesis

Dual nature of soil structure: The unity of aggregates and poresPedogenesis

LATE GLACIAL EROSION AND PEDOGENESIS DYNAMICS: EVIDENCE FROM HIGH-RESOLUTION LACUSTRINE ARCHIVES AND PALEOSOLS IN CENTRAL EUROPELATE GLACIAL EROSION AND PEDOGENESIS DYNAMICS: EVIDENCE FROM HIGH-RESOLUTION LACUSTRINE ARCHIVES

One more challenge for study of anthropogenic pedogenesis: soil change in peri-urban environment (Belgorod case study)One more challenge for study of anthropogenic pedogenesis: soil change in peri-urban environment

Technosols on mining wastes in the subarctic: Efficiency of remediation under Cu-Ni atmospheric pollution communities. The Technosol development in its early stage of pedogenesis indicates the efficiency of applied

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