2021
DOI: 10.5194/hess-25-2159-2021
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A novel analytical approach for the simultaneous measurement of nitrate and dissolved organic carbon in soil water

Abstract: Abstract. In this paper, we present a novel approach, enabling the measurement of nitrate concentrations in natural soil porewater containing natural soil dissolved organic carbon (DOC). The method is based on UV absorbance spectroscopy, combined with fluorescence spectroscopy, for simultaneous analysis of DOC and nitrate concentrations. The analytical procedure involves deduction of the absorption caused by the DOC from the total absorbance in the UV range that is attributed to both DOC and nitrate in the wat… Show more

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Cited by 5 publications
(2 citation statements)
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“…Although the spectrophotometer can measure absorbances from 325 to 1100 nm, only 330 to 700 nm absorbance data were utilized in this study to minimize matrix interference from compounds such as nitrates, which absorb at wavelengths < 340 nm. 3,54 These absorbance measurements were further utilized to calculate absorption properties, specifically, mass absorption efficiency (MAE WS-BrC- λ ) and solar-weighted total absorbance for WS-BrC from 330 to 500 nm. The MAE of WS-BrC, expressed in m 2 g −1 -C, at a given wavelength (MAE WS-BrC- λ ) was calculated using eqn (1) 19 where A WS-BrC- λ is the absorbance of WS-BrC at a given wavelength ( λ ), l is the path length of the spectrophotometer ( i.e.…”
Section: Experimental Methodologymentioning
confidence: 99%
“…Although the spectrophotometer can measure absorbances from 325 to 1100 nm, only 330 to 700 nm absorbance data were utilized in this study to minimize matrix interference from compounds such as nitrates, which absorb at wavelengths < 340 nm. 3,54 These absorbance measurements were further utilized to calculate absorption properties, specifically, mass absorption efficiency (MAE WS-BrC- λ ) and solar-weighted total absorbance for WS-BrC from 330 to 500 nm. The MAE of WS-BrC, expressed in m 2 g −1 -C, at a given wavelength (MAE WS-BrC- λ ) was calculated using eqn (1) 19 where A WS-BrC- λ is the absorbance of WS-BrC at a given wavelength ( λ ), l is the path length of the spectrophotometer ( i.e.…”
Section: Experimental Methodologymentioning
confidence: 99%
“…High-frequency water quality sensors are part of the greater “high-frequency wave of the present” 10 in which high-frequency measurements of key elements, e.g., C, N, and P, are becoming readily available for different environments and media such as gases, 197 soils, 198 and biological samples with environmental DNA. 199 Ultimately, using multisensor technologies simultaneously to measure key biogeochemical cycles across Earth subsystems (i.e., atmosphere, soils, waters, biosphere) can lead to new discoveries of elemental and ecosystem interactions and fundamentally improve our estimates of fluxes and turnover rates from river networks.…”
Section: Future Directions and Challengesmentioning
confidence: 99%