Fluorescence Indices and Their Interpretation
337
Mladenov, N., Zheng, Y., Miller, M.P., Nemergut, D.R., Legg, T., Simone, B., Hageman,
C., Rahman, M.M., Ahmed, K.M., and McKnight, D.M. (2010). Dissolved organic
matter sources and consequences for iron and arsenic mobilization in Bangladesh
aquifers. Environ. Sci. Technol., 44(1), 123–128.
Mobed, J., Hemmingsen, S., Autry, J., and McGown, L. (1996). Fluorescence characterization of IHSS humic substances: Total luminescence spectra with absorbance correction. Environ. Sci. Technol., 30(10), 3061–3065.
Murphy, K., Butler, K., Spencer, R., Stedmon, C., Boehme, J., and Aiken, G. (2010).
Measurement of dissolved organic matter fluorescence in aquatic environments: An
interlaboratory comparison. Environ. Sci. Technol., 44(24), 9405–9412.
Naden, P.S., Old, G.H., Eliot-Laize, C., Granger, S.J., Hawkins, J.M.B, Bol, R., and
Haygarth, P. (2010). Assessment of natural fluorescence as a tracer of diffuse agricultural pollution from slurry spreading on intensely-farmed grasslands. Water Res,
44(6), 1701–1712.
Ohno, T. (2002a). Fluorescence inner-filtering correction for determining the humification
index of dissolved organic matter. Environ. Sci. Technol., 36(4), 742–746.
Ohno, T. (2002b). Response to comment on “fluorescence inner-filtering correction
for determining the humification index of dissolved organic matter.” Environ. Sci.
Technol., 36(19), 4196.
Ohno, T., Fernandez, I., Hiradate, S., and Sherman, J. (2007). Effects of soil acidification
and forest type on water soluble soil organic matter properties. Geoderma, 140(1–2),
176–187.
Parlanti, E., Wörz, K., Geoffroy, L., and Lamotte, M. (2000). Dissolved organic matter
fluorescence spectroscopy as a tool to estimate biological activity in a coastal zone
submitted to anthropogenic inputs. Org. Geochem., 31(12), 1765–1781.
Perrette, Y., Delannoy, J., Desmet, M., Lignier, V., and Destombes, J. (2005). Speleothem
organic matter content imaging: The use of a fluorescence index to characterise the
maximum emission wavelength. Chem. Geol., 214(3–4), 193–208.
Proctor, C., Baker, A., Barnes, W., and Gilmour, M. (2000). A thousand year speleothem
proxy record of North Atlantic climate from Scotland. Clim. Dyn., 16(10), 815–820.
Scott, D.T., McKnight, D.M., Blunt-Harris, E.L., Kolesar, S.E., and Lovley, D.R. (1998).
Quinone moieties act as electron acceptors in the reduction of humic substances by
humics-reducing microorganisms. Environ. Sci. Technol., 32(19), 2984–2989.
Senesi, N., Miano, T., Provenzano, M., and Brunetti, G. (1989). Spectroscopic and compositional comparative characterization of IHSS reference and standard fulvic and
humic acids of various origin. Sci. Total Environ., 81, 143–156.
Senesi, N., Miano, T., Provenzano, M., and Brunetti, G. (1991). Characterization, differentiation, and classification of humic substances by fluorescence spectroscopy. Soil Sci.,
152(4), 259–271.
Spencer, R.G.M., Bolton, L., and Baker, A. (2007). Freeze/thaw and pH effects on freshwater dissolved organic matter fluorescence and absorbance properties from a number of
UK locations. Water Res., 41(13), 2941–2950.
Stewart, A. and Wetzel, R. (1980). Fluorescence: Absorbance ratios – a molecular-weight
tracer of dissolved organic matter. Limnol. Oceanogr., 25(3), 559–564.
Stewart, A. and Wetzel, R. (1981). Asymmetrical relationships between absorbance, fluorescence, and dissolved organic carbon. Limnol. Oceanogr., 26(3), 590–597.
Trouet, V., Esper, J., Graham, N.E., Baker, A., Scourse, J.D., and Frank, D.C. (2009).
Persistent positive North Atlantic oscillation mode dominated the medieval climate
anomaly. Science, 324(5923), 78–80.
337
Mladenov, N., Zheng, Y., Miller, M.P., Nemergut, D.R., Legg, T., Simone, B., Hageman,
C., Rahman, M.M., Ahmed, K.M., and McKnight, D.M. (2010). Dissolved organic
matter sources and consequences for iron and arsenic mobilization in Bangladesh
aquifers. Environ. Sci. Technol., 44(1), 123–128.
Mobed, J., Hemmingsen, S., Autry, J., and McGown, L. (1996). Fluorescence characterization of IHSS humic substances: Total luminescence spectra with absorbance correction. Environ. Sci. Technol., 30(10), 3061–3065.
Murphy, K., Butler, K., Spencer, R., Stedmon, C., Boehme, J., and Aiken, G. (2010).
Measurement of dissolved organic matter fluorescence in aquatic environments: An
interlaboratory comparison. Environ. Sci. Technol., 44(24), 9405–9412.
Naden, P.S., Old, G.H., Eliot-Laize, C., Granger, S.J., Hawkins, J.M.B, Bol, R., and
Haygarth, P. (2010). Assessment of natural fluorescence as a tracer of diffuse agricultural pollution from slurry spreading on intensely-farmed grasslands. Water Res,
44(6), 1701–1712.
Ohno, T. (2002a). Fluorescence inner-filtering correction for determining the humification
index of dissolved organic matter. Environ. Sci. Technol., 36(4), 742–746.
Ohno, T. (2002b). Response to comment on “fluorescence inner-filtering correction
for determining the humification index of dissolved organic matter.” Environ. Sci.
Technol., 36(19), 4196.
Ohno, T., Fernandez, I., Hiradate, S., and Sherman, J. (2007). Effects of soil acidification
and forest type on water soluble soil organic matter properties. Geoderma, 140(1–2),
176–187.
Parlanti, E., Wörz, K., Geoffroy, L., and Lamotte, M. (2000). Dissolved organic matter
fluorescence spectroscopy as a tool to estimate biological activity in a coastal zone
submitted to anthropogenic inputs. Org. Geochem., 31(12), 1765–1781.
Perrette, Y., Delannoy, J., Desmet, M., Lignier, V., and Destombes, J. (2005). Speleothem
organic matter content imaging: The use of a fluorescence index to characterise the
maximum emission wavelength. Chem. Geol., 214(3–4), 193–208.
Proctor, C., Baker, A., Barnes, W., and Gilmour, M. (2000). A thousand year speleothem
proxy record of North Atlantic climate from Scotland. Clim. Dyn., 16(10), 815–820.
Scott, D.T., McKnight, D.M., Blunt-Harris, E.L., Kolesar, S.E., and Lovley, D.R. (1998).
Quinone moieties act as electron acceptors in the reduction of humic substances by
humics-reducing microorganisms. Environ. Sci. Technol., 32(19), 2984–2989.
Senesi, N., Miano, T., Provenzano, M., and Brunetti, G. (1989). Spectroscopic and compositional comparative characterization of IHSS reference and standard fulvic and
humic acids of various origin. Sci. Total Environ., 81, 143–156.
Senesi, N., Miano, T., Provenzano, M., and Brunetti, G. (1991). Characterization, differentiation, and classification of humic substances by fluorescence spectroscopy. Soil Sci.,
152(4), 259–271.
Spencer, R.G.M., Bolton, L., and Baker, A. (2007). Freeze/thaw and pH effects on freshwater dissolved organic matter fluorescence and absorbance properties from a number of
UK locations. Water Res., 41(13), 2941–2950.
Stewart, A. and Wetzel, R. (1980). Fluorescence: Absorbance ratios – a molecular-weight
tracer of dissolved organic matter. Limnol. Oceanogr., 25(3), 559–564.
Stewart, A. and Wetzel, R. (1981). Asymmetrical relationships between absorbance, fluorescence, and dissolved organic carbon. Limnol. Oceanogr., 26(3), 590–597.
Trouet, V., Esper, J., Graham, N.E., Baker, A., Scourse, J.D., and Frank, D.C. (2009).
Persistent positive North Atlantic oscillation mode dominated the medieval climate
anomaly. Science, 324(5923), 78–80.