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Continuous measurement of spectrophotometric absorbance in peatland streamwater in northern England: implications for understanding fluvial carbon fluxes

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Figure

Table 1. Wavelengths used in the analysis of DOC/DOM in natural waters. The majorityof wavelengths are used as proxies whereas both 660 nm and 665 nm have been used
Table 2. Correlation matrix demonstrating the relationships (Pearson correlation r values) between the temporal response ofabsorbance at those wavelengths previously used as proxies for or to characterise DOC
Table 3. Storm event details including the start and end time of the hydrograph, the meanE/E ratio, total rainfall and total storm discharge.
Figure 10.25
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