2019
DOI: 10.1016/j.envint.2019.105126
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Temporal variation in riverine organic carbon concentrations and fluxes in two contrasting estuary systems: Geum and Seomjin, South Korea

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Cited by 29 publications
(18 citation statements)
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“…Those facts give us some added confidence about the robustness of our conclusion. Our conclusion may also be supported by the results of Kang et al [36], who found that DOC fluxes were, in general, controlled by the water discharge in estuary systems. 5:00 9:00 13:00 17:00 .…”
Section: Resultssupporting
confidence: 90%
“…Those facts give us some added confidence about the robustness of our conclusion. Our conclusion may also be supported by the results of Kang et al [36], who found that DOC fluxes were, in general, controlled by the water discharge in estuary systems. 5:00 9:00 13:00 17:00 .…”
Section: Resultssupporting
confidence: 90%
“…The observed δ 13 C values in riverine and estuarine-channel POM may be indicative of a considerable contribution of riverine algae to the estuarine POM pool. Previous studies, in the lowest reach of the Seomjin River, reported freshwater δ 13 C POM values (−26.5 ± 1.4 ) very close to our estuarine δ 13 C POM values and very low SPM concentrations (mean: 1.9-4.3 mg L −1 ) with restricted load delivery (28 ± 40 g C s −1 POC flux in the Seomjin River compared with 1122 ± 1007 g C s −1 in the adjacent Geum River with a diked estuary) (Yang and Choi, 2003;Kang et al, 2019). Based on the C:N (7.4-17.1) and POC:Chla (195 ± 156) ratios, and the positive correlations of both POM proxies with water discharge, those authors described an increased proportion of allochthonous (terrestrial) POC to the river-water POC pool and hydrological influence over POM concentrations in the Seomjin River.…”
Section: Dominance Of Phytoplankton-derived Pomsupporting
confidence: 79%
“…Previous studies have reported that particulate matter derived from erosion of soil may have low OC adsorption due to the low clay content of surface soils in the Jinsha River Basin (Wu et al, 2020), which agrees with the results of this study. Conversely, the POC/Chl-a threshold ratio of 300 indicates the dominance of phytoplankton in the POC pool (Suzuki et al, 2014;Kang et al, 2019;De Castro Bueno et al, 2020), and more than half of the samples in the surface water were classified with the origin of phytoplankton dominance (Figure S4), which is similar to the results of stable isotope mixing models.…”
Section: Particulate Organic Matter and Stable Isotopic Signaturessupporting
confidence: 71%