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  • 1
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    American Society of Limnology and Oceanography
    In:  Limnology and Oceanography: Methods, 11 . pp. 425-437.
    Publication Date: 2018-09-17
    Description: Eddy-correlation measurements of sediment oxygen uptake rates in aquatic systems are increasingly used to obtain areal-averaged fluxes with a high temporal resolution. Here we discuss the effects of coordinate rotation and averaging time scale for Reynolds decomposition on flux estimates. Using 119 hours of continuous eddy-correlation measurements of sediment oxygen fluxes in an impounded river, we demonstrate that rotation of measured current velocities into streamline coordinates can be a crucial and necessary step in data processing under complex flow conditions in non-flat environments with complex topography. We found that under these conditions neither time series detrending nor coordinate rotation can remove low-frequency velocity variations completely. These variations result in spurious flux contributions and in a pronounced dependence of the derived fluxes on averaging time scales. Application of the planar fit transformation was found to provide an alternative means for transforming measured velocities into streamline coordinates for longer-term observations. The observed sensitivity of estimated fluxes to coordinate transformation and selection of averaging time scale is discussed in the context of the theoretical concepts underlying eddy-correlation measurements and a set of recommendations for planning and analyses of flux measurements are derived.
    Type: Article , PeerReviewed
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  • 2
    Publication Date: 2018-08-15
    Description: The aquatic application of the eddy correlation (EC) technique is growing more popular and is gradually becoming a standard method for resolving benthic O2 fluxes. By including the effects of the local hydrodynamics, the EC technique provides greater insight into the nature of benthic O2 exchange than traditional methods (i.e., benthic chambers and lander microprofilers). The growing popularity of the EC technique has led to a greater demand for easily accessible and robust EC instrumentation. Currently, the EC instrumentation is limited to two commercially available systems that are still in the development stage. Here, we present a robust, open source EC picoamplifier that is simple in design and can be easily adapted to both new and existing acoustic Doppler velocimeters (ADV). The picoamplifier has a response time of 〈 0.1 ms and features galvanic isolation that ensures very low noise contamination of the signal. It can be adjusted to accommodate varying ranges of microelectrode sensitivity as well as other types of amperometric microelectrodes. We show that the extracted flux values are not sensitive to reduced microelectrode operational ranges (i.e., lower resolution) and that no signal loss results from using either a 16- or 14-bit analog-to-digital converter. Finally, we demonstrate the capabilities of the picoamplifier with field studies measuring both dissolved O2 and H2S EC fluxes. The picoamplifier presented here consistently acquires high-quality EC data and provides a simple solution for those who wish to obtain EC instrumentation. The schematic of the amplifier’s circuitry is given in the Web Appendix.
    Type: Article , PeerReviewed , info:eu-repo/semantics/article
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  • 3
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    American Society of Limnology and Oceanography
    In:  Limnology and Oceanography: Methods, 8 . pp. 610-627.
    Publication Date: 2018-08-15
    Description: Sedimentwater fluxes are influenced by both hydrodynamics and sediment biogeochemical processes. However, fluxes at the sediment–water interface (SWI) are almost always analyzed from either a water- or sediment-side perspective. This study expands on previous work by comparing water-side (hydrodynamics and resulting diffusive boundary layer thickness, δDBL) and sediment-side (oxygen consumption and resulting sediment oxic zone) approaches for evaluating diffusive sediment oxygen uptake rate (JO2) and δDBL fro microprofiles. Dissolved oxygen microprofile and current velocity data were analyzed using five common methods to estimate JO2 and δDBL and to assess the robustness of the approaches. Comparable values for JO2 and δDBL were obtained (agreement within 20%), and turbulence-induced variations in these parameters were uniformly characterized with the five methods. JO2 estimates based on water-side data were consistently higher (+1.8 mmol m–2 d–1 or 25% on average) and δDBL estimates correspondingly lower (–0.4 mm or 35% on average) than those obtained using sediment-side data. This deviation may be attributed to definition of the sediment–water interface location, artifacts of the methods themselves, assumptions made on sediment properties, and/or variability in sediment oxygen-uptake processes. Our work emphasizes that sediment-side microprofile data may more accurately describe oxygen uptake at a particular location, whereas water-side data are representative of oxygen uptake over a broader sediment area. Regardless, our overall results show clearly that estimates of JO2 and δDBL are not strongly dependent on the method chosen for analysis.
    Type: Article , PeerReviewed
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