Dissolved oxygen and water temperature dynamics in lowland rivers over various timescales

The impact of floodplain hydrology on the in-stream dissolved oxygen dynamics and the relation between dissolved oxygen and water temperature are investigated. This has been done by examining the time series of dissolved oxygen and water temperature coupled with meteorological and hydrological data...

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Main Authors: Rajwa-Kuligiewicz Agnieszka, Bialik Robert J., Rowiński Paweł M.
Format: Article
Language:English
Published: Sciendo 2015-12-01
Series:Journal of Hydrology and Hydromechanics
Subjects:
Online Access:https://doi.org/10.1515/johh-2015-0041
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author Rajwa-Kuligiewicz Agnieszka
Bialik Robert J.
Rowiński Paweł M.
author_facet Rajwa-Kuligiewicz Agnieszka
Bialik Robert J.
Rowiński Paweł M.
author_sort Rajwa-Kuligiewicz Agnieszka
collection DOAJ
description The impact of floodplain hydrology on the in-stream dissolved oxygen dynamics and the relation between dissolved oxygen and water temperature are investigated. This has been done by examining the time series of dissolved oxygen and water temperature coupled with meteorological and hydrological data obtained from two lowland rivers having contrasting hydrological settings. Spectral analysis of long-term oxygen variations in a vegetated river revealed a distinct scaling regime with slope ‘–1’ indicating a self-similar behaviour. Identical slopes were obtained for water temperature and water level. The same power-law behaviour was observed for an unvegetated river at small timescales revealing the underlying scaling behaviour of dissolved oxygen regime for different types of rivers and over various time scales. The results have shown that the oxygenation of a vegetated river is strongly related to its thermal regime and flow conditions. Moreover, analysis of short-term fluctuations in the unvegetated river demonstrated that physical factors such as rainfall and backwaters play a substantial role in the functioning of this ecosystem. Finally, the results show that the relation between water temperature and dissolved oxygen concentration at the diurnal timescale exhibits a looping behaviour on the variable plot. The findings of this study provide an insight into the sensitivity of rivers to changing hydro-physical conditions and can be useful in the assessment of environmental variability.
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spelling doaj.art-856c67179fe041639273e862a1e4a1492022-12-22T03:13:33ZengSciendoJournal of Hydrology and Hydromechanics0042-790X2015-12-0163435336310.1515/johh-2015-0041johh-2015-0041Dissolved oxygen and water temperature dynamics in lowland rivers over various timescalesRajwa-Kuligiewicz Agnieszka0Bialik Robert J.1Rowiński Paweł M.2Institute of Geophysics, Polish Academy of Sciences, Centre for Polar Studies, Ks. Janusza 64, 01-452 Warsaw, Poland.Institute of Geophysics, Polish Academy of Sciences, Centre for Polar Studies, Ks. Janusza 64, 01-452 Warsaw, Poland.Institute of Geophysics, Polish Academy of Sciences, Centre for Polar Studies, Ks. Janusza 64, 01-452 Warsaw, Poland.The impact of floodplain hydrology on the in-stream dissolved oxygen dynamics and the relation between dissolved oxygen and water temperature are investigated. This has been done by examining the time series of dissolved oxygen and water temperature coupled with meteorological and hydrological data obtained from two lowland rivers having contrasting hydrological settings. Spectral analysis of long-term oxygen variations in a vegetated river revealed a distinct scaling regime with slope ‘–1’ indicating a self-similar behaviour. Identical slopes were obtained for water temperature and water level. The same power-law behaviour was observed for an unvegetated river at small timescales revealing the underlying scaling behaviour of dissolved oxygen regime for different types of rivers and over various time scales. The results have shown that the oxygenation of a vegetated river is strongly related to its thermal regime and flow conditions. Moreover, analysis of short-term fluctuations in the unvegetated river demonstrated that physical factors such as rainfall and backwaters play a substantial role in the functioning of this ecosystem. Finally, the results show that the relation between water temperature and dissolved oxygen concentration at the diurnal timescale exhibits a looping behaviour on the variable plot. The findings of this study provide an insight into the sensitivity of rivers to changing hydro-physical conditions and can be useful in the assessment of environmental variability.https://doi.org/10.1515/johh-2015-0041dissolved oxygenwater temperaturehysteresisspectral analysisself-similarityanastomosing riverbackwaters
spellingShingle Rajwa-Kuligiewicz Agnieszka
Bialik Robert J.
Rowiński Paweł M.
Dissolved oxygen and water temperature dynamics in lowland rivers over various timescales
Journal of Hydrology and Hydromechanics
dissolved oxygen
water temperature
hysteresis
spectral analysis
self-similarity
anastomosing river
backwaters
title Dissolved oxygen and water temperature dynamics in lowland rivers over various timescales
title_full Dissolved oxygen and water temperature dynamics in lowland rivers over various timescales
title_fullStr Dissolved oxygen and water temperature dynamics in lowland rivers over various timescales
title_full_unstemmed Dissolved oxygen and water temperature dynamics in lowland rivers over various timescales
title_short Dissolved oxygen and water temperature dynamics in lowland rivers over various timescales
title_sort dissolved oxygen and water temperature dynamics in lowland rivers over various timescales
topic dissolved oxygen
water temperature
hysteresis
spectral analysis
self-similarity
anastomosing river
backwaters
url https://doi.org/10.1515/johh-2015-0041
work_keys_str_mv AT rajwakuligiewiczagnieszka dissolvedoxygenandwatertemperaturedynamicsinlowlandriversovervarioustimescales
AT bialikrobertj dissolvedoxygenandwatertemperaturedynamicsinlowlandriversovervarioustimescales
AT rowinskipawełm dissolvedoxygenandwatertemperaturedynamicsinlowlandriversovervarioustimescales