<abstract xmlns="http://www.w3.org/1999/xhtml"><p>This paper presents an analysis of thermal and oxygen conditions of the Charzykowskie Lake in the years 2014-2016 in the period from May to August. The measurements were carried out once a month, at points representing three different basins in the lake, and the temperatures and oxygen content dissolved in the water were recorded every 1m from the surface to the bottom at the deepest point of each basin. The changes in temperatures and content of dissolved oxygen were analysed in each of the representative measurement points for particular parts of the lake. It has been shown that the deficit of oxygen dissolved in the bottom layers of the water starts occurring by the beginning of the summer stagnation period, whereas at its peak (August) the anaerobic zone includes hypolimnion and part of the metalimnion. The hypothesis that the thickness of the thermal layers varies within the lake basin was confirmed. It was also shown that the oxygen content curve at representative points, in all years of research, evolves to the form of a clinograde at the peak of summer stagnation, where the concentration of dissolved oxygen decreases with the depth.</p></abstract>

This paper presents an analysis of thermal and oxygen conditions of the Charzykowskie Lake in the years 2014-2016 in the period from May to August. The measurements were carried out once a month, at points representing three different basins in the lake, and the temperatures and oxygen content dissolved in the water were recorded every 1m from the surface to the bottom at the deepest point of each basin. The changes in temperatures and content of dissolved oxygen were analysed in each of the representative measurement points for particular parts of the lake. It has been shown that the deficit of oxygen dissolved in the bottom layers of the water starts occurring by the beginning of the summer stagnation period, whereas at its peak (August) the anaerobic zone includes hypolimnion and part of the metalimnion. The hypothesis that the thickness of the thermal layers varies within the lake basin was confirmed. It was also shown that the oxygen content curve at representative points, in all years of research, evolves to the form of a clinograde at the peak of summer stagnation, where the concentration of dissolved oxygen decreases with the depth.

Thermal and Oxygen Conditions of Lake Charzykowskie in the Years 2014-2016

University of Technology and Life Sciences in Bydgoszcz

Faculty of Civil Engineering; Architecture and Environmental Engineering, Department of Eco-Engineering and Environmental Physical Chemistry

Polish Hyperbaric Research

This work is licensed under the Creative Commons Attribution-NonCommercial-NoDerivatives 4.0 License.

{"article-title":"Thermal and Oxygen Conditions of Lake Charzykowskie in the Years 2014-2016"}

This paper presents an analysis of thermal and oxygen conditions of the Charzykowskie Lake in the years 2014-2016 in the period from May to August. The...

Thermal and Oxygen Conditions of Lake Charzykowskie in the Years 2014-2016

Published Online: Jul 07, 2018

Page range: 85 - 96

DOI: https://doi.org/10.2478/phr-2018-0007

Keywords
water stratification, oxygen deficit, Lake Charzykowskie

© 2018 Jerzy K. Garbacz et al., published by Sciendo

This work is licensed under the Creative Commons Attribution-NonCommercial-NoDerivatives 4.0 License.

Thermal and Oxygen Conditions of Lake Charzykowskie in the Years 2014-2016

Published Online: Jul 07, 2018

Page range: 85 - 96

DOI: https://doi.org/10.2478/phr-2018-0007

Keywordswater stratification, oxygen deficit, Lake Charzykowskie

© 2018 Jerzy K. Garbacz et al., published by Sciendo

This work is licensed under the Creative Commons Attribution-NonCommercial-NoDerivatives 4.0 License.

Keywords
water stratification, oxygen deficit, Lake Charzykowskie