Gas Pressure Dynamics in Small and Mid-Size Lakes

Dissolved gases produce a gas pressure. This gas pressure is the appropriate physical quantity for judging the possibility of bubble formation and hence it is central for understanding exchange of climate-relevant gases between (limnic) water and the atmosphere. The contribution of ebullition has wi...

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Main Authors: Bertram Boehrer, Sylvia Jordan, Peifang Leng, Carolin Waldemer, Cornelis Schwenk, Michael Hupfer, Martin Schultze
Format: Article
Language:English
Published: MDPI AG 2021-06-01
Series:Water
Subjects:
Online Access:https://www.mdpi.com/2073-4441/13/13/1824
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spelling doaj-6e1759d9a6da4241943aae2ee6f18be52021-07-15T15:48:31ZengMDPI AGWater2073-44412021-06-01131824182410.3390/w13131824Gas Pressure Dynamics in Small and Mid-Size LakesBertram Boehrer0Sylvia Jordan1Peifang Leng2Carolin Waldemer3Cornelis Schwenk4Michael Hupfer5Martin Schultze6Helmholtz-Centre for Environmental Research—UFZ, 39114 Magdeburg, GermanyLeibniz-Institute of Freshwater Ecology and Inland Fisheries—IGB, 12587 Berlin, GermanyHelmholtz-Centre for Environmental Research—UFZ, 39114 Magdeburg, GermanyHelmholtz-Centre for Environmental Research—UFZ, 39114 Magdeburg, GermanyHelmholtz-Centre for Environmental Research—UFZ, 39114 Magdeburg, GermanyLeibniz-Institute of Freshwater Ecology and Inland Fisheries—IGB, 12587 Berlin, GermanyHelmholtz-Centre for Environmental Research—UFZ, 39114 Magdeburg, GermanyDissolved gases produce a gas pressure. This gas pressure is the appropriate physical quantity for judging the possibility of bubble formation and hence it is central for understanding exchange of climate-relevant gases between (limnic) water and the atmosphere. The contribution of ebullition has widely been neglected in numerical simulations. We present measurements from six lacustrine waterbodies in Central Germany: including a natural lake, a drinking water reservoir, a mine pit lake, a sand excavation lake, a flooded quarry, and a small flooded lignite opencast, which has been heavily polluted. Seasonal changes of oxygen and temperature are complemented by numerical simulations of nitrogen and calculations of vapor pressure to quantify the contributions and their dynamics in lacustrine waters. In addition, accumulation of gases in monimolimnetic waters is demonstrated. We sum the partial pressures of the gases to yield a quantitative value for total gas pressure to reason which processes can force ebullition at which locations. In conclusion, only a small number of gases contribute decisively to gas pressure and hence can be crucial for bubble formation.https://www.mdpi.com/2073-4441/13/13/1824dissolved gasHenry lawtotal gas pressureebullitiongreenhouse gaseslacustrine waters
collection DOAJ
language English
format Article
sources DOAJ
author Bertram Boehrer
Sylvia Jordan
Peifang Leng
Carolin Waldemer
Cornelis Schwenk
Michael Hupfer
Martin Schultze
spellingShingle Bertram Boehrer
Sylvia Jordan
Peifang Leng
Carolin Waldemer
Cornelis Schwenk
Michael Hupfer
Martin Schultze
Gas Pressure Dynamics in Small and Mid-Size Lakes
Water
dissolved gas
Henry law
total gas pressure
ebullition
greenhouse gases
lacustrine waters
author_facet Bertram Boehrer
Sylvia Jordan
Peifang Leng
Carolin Waldemer
Cornelis Schwenk
Michael Hupfer
Martin Schultze
author_sort Bertram Boehrer
title Gas Pressure Dynamics in Small and Mid-Size Lakes
title_short Gas Pressure Dynamics in Small and Mid-Size Lakes
title_full Gas Pressure Dynamics in Small and Mid-Size Lakes
title_fullStr Gas Pressure Dynamics in Small and Mid-Size Lakes
title_full_unstemmed Gas Pressure Dynamics in Small and Mid-Size Lakes
title_sort gas pressure dynamics in small and mid-size lakes
publisher MDPI AG
series Water
issn 2073-4441
publishDate 2021-06-01
description Dissolved gases produce a gas pressure. This gas pressure is the appropriate physical quantity for judging the possibility of bubble formation and hence it is central for understanding exchange of climate-relevant gases between (limnic) water and the atmosphere. The contribution of ebullition has widely been neglected in numerical simulations. We present measurements from six lacustrine waterbodies in Central Germany: including a natural lake, a drinking water reservoir, a mine pit lake, a sand excavation lake, a flooded quarry, and a small flooded lignite opencast, which has been heavily polluted. Seasonal changes of oxygen and temperature are complemented by numerical simulations of nitrogen and calculations of vapor pressure to quantify the contributions and their dynamics in lacustrine waters. In addition, accumulation of gases in monimolimnetic waters is demonstrated. We sum the partial pressures of the gases to yield a quantitative value for total gas pressure to reason which processes can force ebullition at which locations. In conclusion, only a small number of gases contribute decisively to gas pressure and hence can be crucial for bubble formation.
topic dissolved gas
Henry law
total gas pressure
ebullition
greenhouse gases
lacustrine waters
url https://www.mdpi.com/2073-4441/13/13/1824
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AT sylviajordan gaspressuredynamicsinsmallandmidsizelakes
AT peifangleng gaspressuredynamicsinsmallandmidsizelakes
AT carolinwaldemer gaspressuredynamicsinsmallandmidsizelakes
AT cornelisschwenk gaspressuredynamicsinsmallandmidsizelakes
AT michaelhupfer gaspressuredynamicsinsmallandmidsizelakes
AT martinschultze gaspressuredynamicsinsmallandmidsizelakes
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