Eurasian Soil Science is an international peer reviewed journal that publishes original articles on global and regional theoretical and experimental studies of the genesis, geography, physics, chemistry, biology, fertility, management, conservation, and remediation of soils. The journal welcomes manuscripts from all countries in the English or Russian language. PEER REVIEW Eurasian Soil Science is a peer reviewed journal. We use a double blind peer review format. Our team of reviewers includes over 190 experts from 8 coutntries (USA, Austria, Germany, Hungary, Georgia, etc.). The average period from submission to first decision in 2018 was 25 days, and that from first decision to acceptance was 60 days. The rejection rate for submitted manuscripts in 2018 was 15%. The final decision on the acceptance of an article for publication is made by the Editorial Board. Any invited reviewer who feels unqualified or unable to review the manuscript due to the conflict of interests should promptly notify the editors and decline the invitation. Reviewers should formulate their statements clearly in a sound and reasoned way so that authors can use reviewer’s arguments to improve the manuscript. Personal criticism of the authors must be avoided. Reviewers should indicate in a review (i) any relevant published work that has not been cited by the authors, (ii) anything that has been reported in previous publications and not given appropriate reference or citation, (ii) any substantial similarity or overlap with any other manuscript (published or unpublished) of which they have personal knowledge.
Eurasian Soil Science
Description
Identifiers
ISSN | 1064-2293 |
e-ISSN | 1556-195X |
DOI | 10.1134/11475.1556-195X |
Publisher
Pleiades Publishing
Additional information
Data set: Springer
Articles
Eurasian Soil Science > 2019 > 52 > 11 > 1447-1455
Under the influence of perennial dynamics of soil thawing depth, the upper layer of permafrost periodically thaws and becomes a part of the soil profile in the permafrost zone. In this case, the horizon, which is either frozen or thawed and has a thickness of several tens of centimeters, displays an elevated ice content (moisture). This horizon between the lower boundary of the active layer and the...
Eurasian Soil Science > 2019 > 52 > 11 > 1429-1438
The studies were performed at the long-term stationary experiment on crusty hydromorphic solonetzes of the Baraba Plain during 1986–2017. In the humid year of 2013, the ground water level drastically rose from a depth of 250 cm to 50 cm, and secondary salinization was recorded. The content of soluble salts increased, their composition changed, the soil pH shifted to higher values, and the exchangeable...
Eurasian Soil Science > 2019 > 52 > 11 > 1414-1421
— The seasonal dynamics of the structure of microbial biomass in a soddy-podzolic soil under fallow was assessed using luminescent microscopy. Samples from three soil horizons (P, 5‒15 cm, BEL, 30‒40 cm, and BT2, 50‒60 cm) were sampled monthly from March, 2017 to February, 2018, in the territory of Eldigino experimental station (Moscow oblast). In addition to microbial biomass measurement, soil temperature...