2016
DOI: 10.3791/54098
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The Benthic Exchange of O<sub>2</sub>, N<sub>2</sub> and Dissolved Nutrients Using Small Core Incubations

Abstract: The measurement of sediment-water exchange of gases and solutes in aquatic sediments provides data valuable for understanding the role of sediments in nutrient and gas cycles. After cores with intact sediment-water interfaces are collected, they are submerged in incubation tanks and kept under aerobic conditions at in situ temperatures. To initiate a time course of overlying water chemistry, cores are sealed without bubbles using a top cap with a suspended stirrer. Time courses of 4-7 sample points are used to… Show more

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Cited by 11 publications
(11 citation statements)
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“…Water was stirred throughout the whole pre-incubation and incubation periods. Intact sediment cores were incubated in a batch mode according to standardized protocols developed for the measurement of benthic fluxes of gases and nutrients [28,29]. Incubations were performed in the laboratory at 25 • C, simulating the typical middle summer conditions in the Po River Delta.…”
Section: Measurement Of Benthic Fluxes and Denitrification Ratesmentioning
confidence: 99%
“…Water was stirred throughout the whole pre-incubation and incubation periods. Intact sediment cores were incubated in a batch mode according to standardized protocols developed for the measurement of benthic fluxes of gases and nutrients [28,29]. Incubations were performed in the laboratory at 25 • C, simulating the typical middle summer conditions in the Po River Delta.…”
Section: Measurement Of Benthic Fluxes and Denitrification Ratesmentioning
confidence: 99%
“…Hourly rates of NO 3 − removal (mg N m −2 h −1 ) were determined from NO 3 − concentration‐time linear regression in each mesocosm, according to the equation (Owens & Cornwell, ): NO3removalrate=αVAwhere α is the slope of regression line obtained by plotting the NO 3 − concentration as a function of incubation time, V is the water volume of each mesocosm, and A is the area of the sediment surface.…”
Section: Methodsmentioning
confidence: 99%
“…Summer and winter experiments consisted of 12 incubations each: six NO 3 − levels (0.7, 1.4, 2.8, 4.2, 7.0, 11.2 mg N L −1 ) under both dark and light conditions to discriminate the effect of photosynthetic processes on N removal. Mesocosms were incubated in a batch mode according to standard protocols developed for the measurement of benthic fluxes of gases and nutrients (Dalsgaard et al., ; Owens & Cornwell, ). The gradient of NO 3 − concentrations captured the common range found in lowland drainage waters, receiving diffuse (agricultural runoff) and point‐source pollution (discharges from wastewater treatment plants) (Pierobon et al., ; Soana et al., ).…”
Section: Methodsmentioning
confidence: 99%
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“…Cores were sealed and stored in a cooler filled with water from respective sites and transported to Horn Point Laboratory at the University of Maryland Center for Environmental Science for analysis. Incubation methods described in Owens and Cornwell (2016) were used to perform light/dark core incubation and MIMS for N 2 and O 2 dissolved gas flux measurement.…”
Section: Denitrification and Nutrient Fluxesmentioning
confidence: 99%