TY - JOUR
T1 - Organic characterisation of cave drip water by LC-OCD and fluorescence analysis
AU - Rutlidge, Helen
AU - Andersen, Martin S.
AU - Baker, Andy
AU - Chinu, Khorshed J.
AU - Cuthbert, Mark O.
AU - Jex, Catherine N.
AU - Marjo, Christopher E.
AU - Markowska, Monika
AU - Rau, Gabriel C.
N1 - Funding Information:
We thank the staff at Wellington Caves for their support. Funding for this research was provided by the National Centre for Groundwater Research and Training , an Australian Government initiative, supported by the Australian Research Council and the National Water Commission, and Mark Wainwright Analytical Centre at UNSW Australia. Mark Cuthbert was supported by Marie Curie Research Fellowship funding from the European Community’s Seventh Framework Programme [FP7/2007–2013] under grant agreement n°299091. We also acknowledge the anonymous reviewers that provided helpful feedback.
Publisher Copyright:
© 2015 Elsevier Ltd.
PY - 2015/10/1
Y1 - 2015/10/1
N2 - Cathedral Cave, Wellington, Australia, is a natural laboratory for studying water movement and geochemical processes in the unsaturated zone by using artificial irrigation to activate drip sites within the cave. Water sampled from two drip sites activated by irrigations carried out in summer 2014 was analysed for dissolved inorganic ions and fluorescent organic matter. The analysis allowed the development of a conceptual flow path model for each drip site. DOM analysis was further complemented by liquid chromatography with organic carbon detection (LC-OCD), applied for the first time to karst drip waters, allowing the characterisation of six organic matter fractions. The differences in organic matter fractions at each drip site are interpreted as a signature of the proposed flow paths. LC-OCD was also compared with parallel factor analysis (PARAFAC) of the fluorescence and good correlations were observed for high molecular weight organic matter. Strong positive correlations were also observed for high molecular weight matter and Cu and Ni. This is suggestive of colloidal transport of Cu and Ni by organic matter with high molecular weight, while small molecular weight colloids were not efficient transporters. LC-OCD uniquely provides information on non-fluorescent organic matter and can be used to further quantify drip water organic matter composition.
AB - Cathedral Cave, Wellington, Australia, is a natural laboratory for studying water movement and geochemical processes in the unsaturated zone by using artificial irrigation to activate drip sites within the cave. Water sampled from two drip sites activated by irrigations carried out in summer 2014 was analysed for dissolved inorganic ions and fluorescent organic matter. The analysis allowed the development of a conceptual flow path model for each drip site. DOM analysis was further complemented by liquid chromatography with organic carbon detection (LC-OCD), applied for the first time to karst drip waters, allowing the characterisation of six organic matter fractions. The differences in organic matter fractions at each drip site are interpreted as a signature of the proposed flow paths. LC-OCD was also compared with parallel factor analysis (PARAFAC) of the fluorescence and good correlations were observed for high molecular weight organic matter. Strong positive correlations were also observed for high molecular weight matter and Cu and Ni. This is suggestive of colloidal transport of Cu and Ni by organic matter with high molecular weight, while small molecular weight colloids were not efficient transporters. LC-OCD uniquely provides information on non-fluorescent organic matter and can be used to further quantify drip water organic matter composition.
UR - http://www.scopus.com/inward/record.url?scp=84934942843&partnerID=8YFLogxK
U2 - 10.1016/j.gca.2015.05.042
DO - 10.1016/j.gca.2015.05.042
M3 - Article
AN - SCOPUS:84934942843
SN - 0016-7037
VL - 166
SP - 15
EP - 28
JO - Geochimica et Cosmochimica Acta
JF - Geochimica et Cosmochimica Acta
ER -