Physicochemical Effects
273
Kumke, M.U., Specht, C.H., Brinkmann, T., and Frimmel, F.H. (2001). Alkaline hydrolysis of humic substances – spectroscopic and chromatographic investigations.
Chemosphere, 45(6–7), 1023–1031.
Laane, R. (1982). Influences of pH on the fluorescence of dissolved organic matter. Mar.
Chem., 11(4), 395–401.
Lakowicz, J. (2006). Principles of Fluorescence Spectroscopy. New York: Springer
Science+Business Media.
Lakshman, S., Mills, R., Patterson, H., and Cronan, C. (1993). Apparent differences in
binding site distributions and aluminum(III) complexation for three molecular weight
fractions of a coniferous soil fulvic acid. Anal. Chim. Acta, 282(1), 101–108.
Lead, J.R., De Momi, A., Goula, G., and Baker, A. (2006). Fractionation of freshwater
colloids and particles by SPLITT: Analysis by electron microscopy and 3D excitationemission matrix fluorescence. Anal. Chem., 78(11), 3609–3615.
Leenheer, J.A., Noyes, T.I., Rostad, C.E., and Davisson, M.L. (2004). Characterization and
origin of polar dissolved organic matter from the Great Salt Lake. Biogeochemistry,
69(1), 125–141.
Levesque, M. (1972). Fluorescence and gel filtration of humic compounds. Soil Sci.,
113(5), 346–353.
Liu, X. and Millero, F.J. (2002). The solubility of iron in seawater. Mar. Chem., 77(1),
43–54.
Liu, R.X., Lead, J.R., and Baker, A. (2007). Fluorescence characterization of cross flow
ultrafiltration derived freshwater colloidal and dissolved organic matter. Chemosphere,
68(7), 1304–1311.
Lochmuller, C.H. and Saavedra, S.S. (1986). Conformational changes in soil fulvic
acid measured by time-dependent fluorescence depolarization. Anal. Chem., 58(9),
1978–1981.
Lu, X.Q. and Jaffe, R. (2001). Interaction between Hg(II) and natural dissolved organic
matter: A fluorescence spectroscopy based study. Water Res., 35(7), 1793–1803.
Luster, J., Lloyd, T., Sposito, G., and Fry, I.V. (1996). Multi-wavelength molecular fluorescence spectrometry for quantitative characterization of copper(II) and aluminum(III)
complexation by dissolved organic matter. Environ. Sci. Technol., 30(5), 1565–1574.
Ma, J.H., Del Vecchio, R., Golanoski, K.S., Boyle, E.S., and Blough, N.V. (2010). Optical
properties of humic substances and CDOM: Effects of borohydride reduction. Environ.
Sci. Technol., 44(14), 5395–5402.
Ma, X.D. and Green, S.A. (2004). Photochemical transformation of dissolved organic carbon in Lake Superior – An in-situ experiment. J. Great Lakes Res., 30, 97–112.
Mac, M. and Wirz, J. (1993). Deriving intrinsic electron-transfer rates from nonlinear SternVolmer dependencies for fluorescence quenching of aromatic molecules by inorganic
anions in acetonitrile. Chem. Phys. Lett., 211(1), 20–26.
Mac, M. (1995). Fluorescence quenching of aromatic molecules by inorganic anions in
polar solvents. J. Luminesc., 65(3), 143–151.
Maloney, K.O., Morris, D.P., Moses, C.O., and Osburn, C.L. (2005). The role of iron and
dissolved organic carbon in the absorption of ultraviolet radiation in humic lake water.
Biogeochemistry, 75(3), 393–407.
Mantoura, R.F.C. and Woodward, E.M.S. (1983). Conservative behavior of riverine dissolved organic carbon in the Severn Estuary – Chemical and geochemical implications. Geochim. Cosmochim. Acta, 47(7), 1293–1309.
Maranger, R. and Pullin, M.J. (2002). Elemental complexation by dissolved organic matter in lakes: Implications for Fe speciation and the bioavailability of Fe and P. In
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