Geoscience Reference
In-Depth Information
Kumke, M.U., Specht, C.H., Brinkmann, T., and Frimmel, F.H. (2001). Alkaline hydroly-
sis 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 excitation-
emission 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 fluores-
cence 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 car-
bon 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 Stern-
Volmer 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 dis-
solved organic carbon in the Severn Estuary - Chemical and geochemical implica-
tions.
Geochim. Cosmochim. Acta
,
47
(7), 1293-1309.
Maranger, R. and Pullin, M.J. (2002). Elemental complexation by dissolved organic mat-
ter in lakes: Implications for Fe speciation and the bioavailability of Fe and P. In S.