2010
DOI: 10.1007/s10967-010-0735-x
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Fluorescence characterization of the natural organic matter in deep ground waters from the Canadian Shield, Ontario, Canada

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Cited by 7 publications
(2 citation statements)
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“…RGW fluorescence was essentially similar to that of our laboratory water used as a blank, water that has been extensively purified to remove DOM. A PARAFAC fluorescence model of deep groundwater (>600 m) taken from a borehole in the Canadian Shield (Ontario, Canada) showed substantially reduced intensity compared to shallow groundwater, especially in humic‐like components matching C1 and C4 from the La Selva model in this study (Caron et al, ). While the residence time in that study was not reported, the presence of fluorescent DOM, albeit at low intensities, suggests that RGW feeding streams at La Selva were far more altered than bedrock groundwater analyzed by Caron et al ().…”
Section: Discussionmentioning
confidence: 49%
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“…RGW fluorescence was essentially similar to that of our laboratory water used as a blank, water that has been extensively purified to remove DOM. A PARAFAC fluorescence model of deep groundwater (>600 m) taken from a borehole in the Canadian Shield (Ontario, Canada) showed substantially reduced intensity compared to shallow groundwater, especially in humic‐like components matching C1 and C4 from the La Selva model in this study (Caron et al, ). While the residence time in that study was not reported, the presence of fluorescent DOM, albeit at low intensities, suggests that RGW feeding streams at La Selva were far more altered than bedrock groundwater analyzed by Caron et al ().…”
Section: Discussionmentioning
confidence: 49%
“…A PARAFAC fluorescence model of deep groundwater (>600 m) taken from a borehole in the Canadian Shield (Ontario, Canada) showed substantially reduced intensity compared to shallow groundwater, especially in humic‐like components matching C1 and C4 from the La Selva model in this study (Caron et al, ). While the residence time in that study was not reported, the presence of fluorescent DOM, albeit at low intensities, suggests that RGW feeding streams at La Selva were far more altered than bedrock groundwater analyzed by Caron et al (). Altogether, these results strongly suggest that RGW's residence time of about 3,000 years in the regional volcanic bedrock aquifer system and upslope of La Selva (Genereux et al, ) affords ample time to remove DOM's fluorescence properties as well as produce DOM exhibiting SUVA 254 values <1 L mg C −1 m −1 and S R values >5.…”
Section: Discussionmentioning
confidence: 49%