ANALIZA MODELI DYNAMIKI TRANSFORMACJI MATERII ORGANICZNEJ GLEBY
Liubov Shostak
National University of Water and Environmental Engineering, Department of Applied Mathematics (Ukraina)
http://orcid.org/0000-0002-7881-7366
Mykhailo Boiko
National University of Water and Environmental Engineering, Department of Applied Mathematics (Ukraina)
http://orcid.org/0000-0002-0962-8625
Olha Stepanchenko
o.m.stepanchenko@nuwm.edu.uaNational University of Water and Environmental Engineering, Department of Applied Mathematics (Ukraina)
http://orcid.org/0000-0001-6033-7404
Olena Kozhushko
National University of Water and Environmental Engineering, Department of Applied Mathematics (Ukraina)
http://orcid.org/0000-0001-9934-1013
Abstrakt
W tym artykule rozważamy modele opisujące dynamikę transformacji materii organicznej w glebie. Przedstawiono wyniki praktycznej realizacji modeli ROMUL, CENTURY i ROTHAMSTED. Modele te proponują teoretyczne podejścia do modelowania transformacji szczątków organicznych oparte na opisie procesów fizykochemicznych podczas formowania się próchnicy z zależnościami różnicowymi. W wyniku analizy wyróżniono ich mocne i słabe strony.
Słowa kluczowe:
model, mineralizacja, materia organiczna gleby, tworzenie się próchnicy, glebaBibliografia
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Autorzy
Liubov ShostakNational University of Water and Environmental Engineering, Department of Applied Mathematics Ukraina
http://orcid.org/0000-0002-7881-7366
Autorzy
Mykhailo BoikoNational University of Water and Environmental Engineering, Department of Applied Mathematics Ukraina
http://orcid.org/0000-0002-0962-8625
Autorzy
Olha Stepanchenkoo.m.stepanchenko@nuwm.edu.ua
National University of Water and Environmental Engineering, Department of Applied Mathematics Ukraina
http://orcid.org/0000-0001-6033-7404
Autorzy
Olena KozhushkoNational University of Water and Environmental Engineering, Department of Applied Mathematics Ukraina
http://orcid.org/0000-0001-9934-1013
Statystyki
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Licencja
Utwór dostępny jest na licencji Creative Commons Uznanie autorstwa – Na tych samych warunkach 4.0 Miedzynarodowe.