Aquatic eddy correlation: quantifying the artificial flux caused by stirring-sensitive O2 sensors.

In the last decade, the aquatic eddy correlation (EC) technique has proven to be a powerful approach for non-invasive measurements of oxygen fluxes across the sediment water interface. Fundamental to the EC approach is the correlation of turbulent velocity and oxygen concentration fluctuations measu...

Full description

Bibliographic Details
Main Authors: Moritz Holtappels, Christian Noss, Kasper Hancke, Cecile Cathalot, Daniel F McGinnis, Andreas Lorke, Ronnie N Glud
Format: Article
Language:English
Published: Public Library of Science (PLoS) 2015-01-01
Series:PLoS ONE
Online Access:https://doi.org/10.1371/journal.pone.0116564
id doaj-912f41a1a1a449418a88e0913b36122b
record_format Article
spelling doaj-912f41a1a1a449418a88e0913b36122b2021-03-04T08:36:17ZengPublic Library of Science (PLoS)PLoS ONE1932-62032015-01-01101e011656410.1371/journal.pone.0116564Aquatic eddy correlation: quantifying the artificial flux caused by stirring-sensitive O2 sensors.Moritz HoltappelsChristian NossKasper HanckeCecile CathalotDaniel F McGinnisAndreas LorkeRonnie N GludIn the last decade, the aquatic eddy correlation (EC) technique has proven to be a powerful approach for non-invasive measurements of oxygen fluxes across the sediment water interface. Fundamental to the EC approach is the correlation of turbulent velocity and oxygen concentration fluctuations measured with high frequencies in the same sampling volume. Oxygen concentrations are commonly measured with fast responding electrochemical microsensors. However, due to their own oxygen consumption, electrochemical microsensors are sensitive to changes of the diffusive boundary layer surrounding the probe and thus to changes in the ambient flow velocity. The so-called stirring sensitivity of microsensors constitutes an inherent correlation of flow velocity and oxygen sensing and thus an artificial flux which can confound the benthic flux determination. To assess the artificial flux we measured the correlation between the turbulent flow velocity and the signal of oxygen microsensors in a sealed annular flume without any oxygen sinks and sources. Experiments revealed significant correlations, even for sensors designed to have low stirring sensitivities of ~0.7%. The artificial fluxes depended on ambient flow conditions and, counter intuitively, increased at higher velocities because of the nonlinear contribution of turbulent velocity fluctuations. The measured artificial fluxes ranged from 2-70 mmol m(-2) d(-1) for weak and very strong turbulent flow, respectively. Further, the stirring sensitivity depended on the sensor orientation towards the flow. For a sensor orientation typically used in field studies, the artificial flux could be predicted using a simplified mathematical model. Optical microsensors (optodes) that should not exhibit a stirring sensitivity were tested in parallel and did not show any significant correlation between O2 signals and turbulent flow. In conclusion, EC data obtained with electrochemical sensors can be affected by artificial flux and we recommend using optical microsensors in future EC-studies.https://doi.org/10.1371/journal.pone.0116564
collection DOAJ
language English
format Article
sources DOAJ
author Moritz Holtappels
Christian Noss
Kasper Hancke
Cecile Cathalot
Daniel F McGinnis
Andreas Lorke
Ronnie N Glud
spellingShingle Moritz Holtappels
Christian Noss
Kasper Hancke
Cecile Cathalot
Daniel F McGinnis
Andreas Lorke
Ronnie N Glud
Aquatic eddy correlation: quantifying the artificial flux caused by stirring-sensitive O2 sensors.
PLoS ONE
author_facet Moritz Holtappels
Christian Noss
Kasper Hancke
Cecile Cathalot
Daniel F McGinnis
Andreas Lorke
Ronnie N Glud
author_sort Moritz Holtappels
title Aquatic eddy correlation: quantifying the artificial flux caused by stirring-sensitive O2 sensors.
title_short Aquatic eddy correlation: quantifying the artificial flux caused by stirring-sensitive O2 sensors.
title_full Aquatic eddy correlation: quantifying the artificial flux caused by stirring-sensitive O2 sensors.
title_fullStr Aquatic eddy correlation: quantifying the artificial flux caused by stirring-sensitive O2 sensors.
title_full_unstemmed Aquatic eddy correlation: quantifying the artificial flux caused by stirring-sensitive O2 sensors.
title_sort aquatic eddy correlation: quantifying the artificial flux caused by stirring-sensitive o2 sensors.
publisher Public Library of Science (PLoS)
series PLoS ONE
issn 1932-6203
publishDate 2015-01-01
description In the last decade, the aquatic eddy correlation (EC) technique has proven to be a powerful approach for non-invasive measurements of oxygen fluxes across the sediment water interface. Fundamental to the EC approach is the correlation of turbulent velocity and oxygen concentration fluctuations measured with high frequencies in the same sampling volume. Oxygen concentrations are commonly measured with fast responding electrochemical microsensors. However, due to their own oxygen consumption, electrochemical microsensors are sensitive to changes of the diffusive boundary layer surrounding the probe and thus to changes in the ambient flow velocity. The so-called stirring sensitivity of microsensors constitutes an inherent correlation of flow velocity and oxygen sensing and thus an artificial flux which can confound the benthic flux determination. To assess the artificial flux we measured the correlation between the turbulent flow velocity and the signal of oxygen microsensors in a sealed annular flume without any oxygen sinks and sources. Experiments revealed significant correlations, even for sensors designed to have low stirring sensitivities of ~0.7%. The artificial fluxes depended on ambient flow conditions and, counter intuitively, increased at higher velocities because of the nonlinear contribution of turbulent velocity fluctuations. The measured artificial fluxes ranged from 2-70 mmol m(-2) d(-1) for weak and very strong turbulent flow, respectively. Further, the stirring sensitivity depended on the sensor orientation towards the flow. For a sensor orientation typically used in field studies, the artificial flux could be predicted using a simplified mathematical model. Optical microsensors (optodes) that should not exhibit a stirring sensitivity were tested in parallel and did not show any significant correlation between O2 signals and turbulent flow. In conclusion, EC data obtained with electrochemical sensors can be affected by artificial flux and we recommend using optical microsensors in future EC-studies.
url https://doi.org/10.1371/journal.pone.0116564
work_keys_str_mv AT moritzholtappels aquaticeddycorrelationquantifyingtheartificialfluxcausedbystirringsensitiveo2sensors
AT christiannoss aquaticeddycorrelationquantifyingtheartificialfluxcausedbystirringsensitiveo2sensors
AT kasperhancke aquaticeddycorrelationquantifyingtheartificialfluxcausedbystirringsensitiveo2sensors
AT cecilecathalot aquaticeddycorrelationquantifyingtheartificialfluxcausedbystirringsensitiveo2sensors
AT danielfmcginnis aquaticeddycorrelationquantifyingtheartificialfluxcausedbystirringsensitiveo2sensors
AT andreaslorke aquaticeddycorrelationquantifyingtheartificialfluxcausedbystirringsensitiveo2sensors
AT ronnienglud aquaticeddycorrelationquantifyingtheartificialfluxcausedbystirringsensitiveo2sensors
_version_ 1714807802687389696