Please use this identifier to cite or link to this item:https://hdl.handle.net/20.500.12259/89466
Type of publication: Straipsnis Clarivate Analytics Web of Science ar/ir Scopus / Article in Clarivate Analytics Web of Science or / and Scopus (S1)
Field of Science: Agronomija / Agronomy (A001)
Author(s): Volungevičius, Jonas;Jukna, Laurynas;Veteikis, Darijus;Vaisvalavičius, Rimantas;Amalevičiūtė, Kristina;Šlepetienė, Alvyra;Skorupskas, Ričardas;Jankauskaitė, Margarita
Title: The problem of soil interpretation according to the WRB 2014 classification system in the context of anthropogenic transformations
Is part of: Acta Agriculturae Scandinavica. Section B, Soil and plant science. OSLO : Taylor & Francis, Vol. 66, Issue 5 (2016)
Extent: p. 452-460
Date: 2016
Keywords: Agroecosystem;Anthropogenic transformation;Arenosols;Cambisols;Planosols;Regosols;Soil classification;Soils of Lithuania;Stagnosols
Abstract: Evaluation of soil transformations and degradation is important not only for agriculture, but also for fundamental research on identification of new features for classification. In 1999, new Lithuanian soil classification (LTDK-99) was developed by adopting the diagnostic principles of WRB 1998. Together with new knowledge, it highlighted some relevant soil research and classification problems. Not only new terms but also diagnostic features of several newly distinguished first-level soils groups are being discussed, especially for the identification of cambisols, planosols, arenosols, and regosols. Additionally, a group of stagnosols is suggested for inclusion into this classification. The presence of glaciogenic secondary clay minerals in Lithuanian cambisols does not imply unambiguous brownification involvement, neither any study shows cambisols having specific to brownification iron minerals. The intensively occurring lesive in these soils questions correctness of identification of cambisols additionally aggravated by strong and deep anthropogenization of the soil profiles within the territorial range. Complex glaciogenesis makes it difficult to identify Lithuanian planosols. WRB 2014 (update 2015) identifies planosols according to the pedogenesis in old, strongly weathered binomial deposits using examples mostly from South American, South and East African plateaus of the subtropical zone. The same classification assigns planosols identified in Lithuania to stagnosols, that is, to the soils characterized by binomial genesis and stagnification. The diagnostic features of arenosols and regosols are similar in both groups and are related to primitive pedogenesis. Difficulties in distinguishing between the two groups in Lithuania are strengthened by the intensive cultivation of the ecosystems in their territorial range
Internet: https://www.tandfonline.com/doi/full/10.1080/09064710.2016.1164231
Affiliation(s): Gamtos tyrimų centras
Lietuvos agrarinių ir miškų mokslų centro filialas Žemdirbystės institutas
Lietuvos agrarinių ir miškų mokslų centro Žemdirbystės institutas
Vilniaus universitetas
Vytauto Didžiojo universitetas
Žemės ūkio akademija
Appears in Collections:Universiteto mokslo publikacijos / University Research Publications

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