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In contrast, larger wetlands (>100 ha) with long hydraulic residence times (>10 days) resulted in higher dissolved organic carbon and bromide levels, increasing disinfection byproduct formation by factors ranging between 1.7 and 10.2 compared to agricultural return flows.
The requirement of high dissolved oxygen in submerged fermentation of polyketide compounds natamycin (Liang et al. 2008), lovastatin (Rodriguez-Porcel et al. 2006) and erythromycin (Zou et al. 2008) to achieve high productivity has been reported and supports our findings in the case of bikaverin production.
Here we investigate the temporal and spatial variation in dissolved Fe redox state in a high dissolved organic matter (DOM) estuarine system, the River Beaulieu.
That is, cornea accumulates water as a result of high dissolved solute levels in the stroma (1, 2).
In principle, high dissolved CO concentrations throughout the column are desirable since CO is the primary carbon source for growth.
The water composition is consistent with this interpretation, as it is suboxic, near-neutral in pH, contains high dissolved Fe2+ and As.3+ With the exception of the mine adit, the seep sites (LL1, LL10) have the highest sulfate values of all sites.
During the investigation period, the highest TDS of 1184 mg/l in 2011 and 1401 mg/l in 2014 has been obtained which indicate high dissolved mineral content in groundwater of Dhanbad Township.
High dissolved solids in the River causes substantial damages to users, primarily in reduced agricultural crop yields and corrosion.
The high dissolved solid content in shallow groundwater in the area renders it unsuitable for domestic and irrigation purposes.
This scenario could also explain why in situ profiling measurements obtained during ebb tide in CB sediments (Figure 5a) display high dissolved sulfide concentrations near the sediment surface but not deeper in the sediment, while the deep porewaters are, in contrast, dominated by large soluble organic-Fe(III) signals.
Previous studies of the dissolved Fe released from glacier and sea-ice report concentrations typically in the range of 5 to 50 nM [6, 15 17], which were suggested to originate either from aeolian dust or from sea-ice formed in coastal waters with relatively high dissolved Fe [6, 7].
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