The temporal dynamics of readily available soil moisture for plants in the technosols of the Nikopol Manganese Ore Basin

• Published in: Biosystems diversity Vol. 27; no. 2; pp. 156 - 162
• Main Authors: Kunah, O. М, Zelenko, Y.V, Fedushko, M.P, Babchenko, A.V, Sirovatko, V.O, Zhukov, O. V
• Format: Journal Article
• Language: English
• Published: Дніпропетровський національний університет імені Олеся Гончара 01.01.2019; Oles Honchar Dnipropetrovsk National University; Oles Honchar Dnipro National University
• Subjects: Environmental interactions; Evaluation research; reclamation; water regime; albedo; evapotranspiration; penman-monteith equation; evapotranspiration; reclamation; PenmanMonteith equation; water regime; albedo
• ISSN: 2519-8513; 2520-2529
• DOI: 10.15421/011921

The restoration of a stable and productive ecosystem after drastic disturbances to the natural environment due to mining and open-cast mining may be achieved by means of reclamation. Investigation of the hydrological budget of technosols is important task in developing adequate approaches to reclamation. Sod lithogenic soils on red-brown clay, on grey-green clay were chosen as the objects of the investigation. The simulation of moisture content in Nikopol Manganese Ore Basin technosols was performed using the Penman-Monteith approach and evaluated the role of the dependence of soils’ surface albedo on the humidity in the intensity of evapotranspiration. The research was conducted during 2013–2015 at the station for research on reclaimed land within the Nikopol Manganese Ore Basin (city Pokrov, Ukraine). The experimental area for the study of optimal modes of agricultural reclamation was created in 1968–1970. Precipitation in the investigated area was found to fall very unevenly in time. In 2013, the duration of the rainless period was 259 days, in 2014 – 264 days, in 2015 – 261 days. The maximum daily rainfall varies within 18–49 mm. There are significant interannual differences in the intensity of rainfall. The minimum total annual precipitation in 2014 was due to a decrease in atypical rainfall in late winter and early winter.