PREDICTION OF THE HYDROCHEMICAL REGIME OF SURFACE WATER USING SIMULATION MATHEMATICAL MODELLING

Journal Title: Biuletyn Państwowego Instytutu Geologicznego - Year 2012, Vol 453, Issue 453

Abstract

Mathematical simulation models of the hydrochemical regime of Velykyi Lyubin pond (Vereshchytsya River basin) and the pond of the Pidhaytsi town (Koropets River basin) have been constructed to clarify the possibilities of using such models in the practice of managing the quality of water resources in small rivers. To evaluate the ecological state of the Vereshchytsya and Koropets river basins – left tributaries of the Dniester – the expedition method was applied, i.e. collecting information on natural conditions and the content of nitrogen compounds (determined directly on-site) as well as Cl[sup]–[/sup] and SO[sub]4[/sub][sup]2–[/sup] ions in water. Information processing was performed by mathematical modelling of the hydrochemical regime of surface waters – calculation models to study the changes in the concentration of biogenic substances and chloride, and sulphate ions in the ponds have been developed. The simulation mathematical models of the hydrochemical regime of surface waters of the ponds were developed for different seasons by a direct construction of the chamber model based on the spatial averaging of the processes and compilation of balance equations. Mathematical models of the change in content of biogenic substances and sulphate, and chloride ions testify to partial purification of waters from pollutants, which is facilitated by the processes taking place within them (sedimentation, sorption–adsorption processes, dissolution).

Authors and Affiliations

Olha NIKOLENKO

Keywords

Related Articles

Hydrogeological conditions of the Latosówka-Rudniki limestone and marl deposit in Rudniki near Częstochowa

Rudniki Cement Plant at Rudniki village is supplied with carbonates by the nearby located Latosówka open pit. Intense drainage of the upper Jurassic aquifer due to limestone and marl exploitation has changed the hydrodyn...

UDZIAŁ WÓD Z CIEKÓW W ZASILANIU POZIOMU WODONOŚNEGO JURY GÓRNEJ NA OBSZARZE WYŻYNY KRAKOWSKIEJ

W artykule przedstawiono zjawisko infiltracji wód z cieków na obszarach krasowych Wyżyny Krakowskiej na tle hydrograficznym wyżyny. Na podstawie 8 serii badań scharakteryzowano dynamikę zmian sezonowych infiltracji wód z...

SEASONAL CHANGES OF NITROGEN LOAD IN PRECIPITATION IN THE KRAKÓW AREA

The results of the precipitation quality measurements which have been realized for a few years in two locations in Kraków are presented. Nitrogen compounds are analyzed in details. The seasonal changes in nitrate, ammoni...

Pleistocene fauna in the Sucha Wieś (Ełk Lakeland) and Czarnucha (Augustów Plain) sections, northeastern Poland

Samples collected from the Sucha Wieś borehole (Ełk Lakeland) from a depth interval of 153.60–178.00 and from the Czarnucha borehole (Augustów Plain) from a depth interval of 96.05–118.85 m were analysed for faunal conte...

OBRAZOWANIE ELEKTROOPOROWE WARUNKÓW HYDROGEOLOGICZNYCH STREFY BRZEGOWEJ WYSPY WOLIN

W artykule zaprezentowano problematykę złożonych warunków hydrogeologicznych w strefie brzegowej wyspy Wolin, które można obrazować za pomocą metod geoelektrycznych. Wody podziemne warstw wodonośnych strefy brzegowej zna...

Download PDF file
  • EP ID EP63656
  • DOI -
  • Views 84
  • Downloads 0

How To Cite

Olha NIKOLENKO (2012). PREDICTION OF THE HYDROCHEMICAL REGIME OF SURFACE WATER USING SIMULATION MATHEMATICAL MODELLING. Biuletyn Państwowego Instytutu Geologicznego, 453(453), 23-28. https://europub.co.uk/articles/-A-63656