Behaviour of the optical properties of coloured dissolved organic matter under conservative mixing

The optical properties of coloured dissolved organic matter (CDOM) can be used, in some environments, to trace water masses and provide information about the dynamics of the dissolved organic fraction in natural waters. This work presents the results from a modelling exercise, laboratory experiment and field data, which describe the variations in the optical properties of CDOM during mixing. The exponential slope coefficient (S) is frequently used to characterise different CDOM pools; however, its behaviour during conservative mixing of two different CDOM types is often misunderstood. Identification of a theoretical conservative mixing line allows the rapid identification of non-conservative processes (e.g. in situ production, flocculation and degradation) acting on the pool during mixing. The results suggest that some of the patterns reported in the literature could purely be a result of conservative mixing rather than a product of non-conservative processes.

[1]  M. DeGrandpre,et al.  Seasonal variation of CDOM and DOC in the Middle Atlantic Bight: Terrestrial inputs and photooxidation , 1997 .

[2]  C. Stedmon,et al.  Optical properties and signatures of chromophoric dissolved organic matter (CDOM) in Danish coastal waters , 2000 .

[3]  Warwick F. Vincent,et al.  Spectral light attenuation and the absorption of UV and blue light in natural waters , 2000 .

[4]  N. K. Højerslev urface water‐quality studies in the interior marine environment of Denmark , 1989 .

[5]  J. Morell,et al.  Analysis of the optical properties of the Orinoco River plume by absorption and fluorescence spectroscopy , 1999 .

[6]  K. Kramer,et al.  Natural fluorescence in the north sea and its major estuaries , 1990 .

[7]  P. Given Book Review: Humic substances in soil, sediment and water. edited by G.R. Aiken, D.M. McKnight, R.L. Wershaw and P. MacCarthy, 1985, Wiley-Interscience, 692 p., £61.35 , 1986 .

[8]  C. Stedmon,et al.  The optics of chromophoric dissolved organic matter (CDOM) in the Greenland Sea: An algorithm for differentiation between marine and terrestrially derived organic matter , 2001 .

[9]  Synchronous fluorescence spectra of natural waters: tracing sources of dissolved organic matter , 1987 .

[10]  P. Hall,et al.  Early diagenetic production and sediment-water exchange of fluorescent dissolved organic matter in the coastal environment , 1996 .

[11]  J. Wikner,et al.  Dynamics of Dissolved Organic Carbon in a Coastal Ecosystem. , 1995 .

[12]  J. R. Nelson,et al.  Particulate and dissolved spectral absorption on the continental shelf of the southeastern United States , 1995 .

[13]  G. Ferrari,et al.  The relationship between chromophoric dissolved organic matter and dissolved organic carbon in the European Atlantic coastal area and in the West Mediterranean Sea (Gulf of Lions) , 2000 .

[14]  K. Carder,et al.  Marine humic and fulvic acids: Their effects on remote sensing of ocean chlorophyll , 1989 .

[15]  Neil V. Blough,et al.  Optical absorption spectra of waters from the Orinoco River outflow : terrestrial input of colored organic matter to the Caribbean , 1993 .

[16]  G. Ferrari,et al.  Influence of pH and heavy metals in the determination of yellow substance in estuarine areas , 1991 .

[17]  C. D. Castillo,et al.  Seasonal variability of the colored dissolved organic matter during the 1994 95 NE and SW Monsoons in the Arabian Sea , 2000 .

[18]  Claire Hughes,et al.  Non‐conservative mixing behavior of colored dissolved organic matter in a humic‐rich, turbid estuary , 2001 .

[19]  L. Prieur,et al.  Absorption by dissolved organic matter of the sea (yellow substance) in the UV and visible domains1 , 1981 .

[20]  Murray T. Brown,et al.  Transmission spectroscopy examinations of natural waters: C. Ultraviolet spectral characteristics of the transition from terrestrial humus to marine yellow substance , 1977 .