emoto
Serra
ipais
asil,
asil,
LASER FLUORESCENT DIAGNOSTIC OF DISSOLVED
ORGANIC MATTER IN NATURAL WATER.
Elena M. Filippova
Quantum Radiophysics Chair,
Department of Physics, Moscow State University,
Moscow 119899 GSP, Russia.
Comission: VII.
ABSTRACT:
Important problems of environment control demand
elaboration of remote methods for dissolved
organic matter (DOM) diagnostics in natural water.
Currently fluorescent methods using Raman,
scattering signal as an internal standard are
widely applied for environment control DOM in
water.
In this paper temperature variations and
ultraviolet irradiation (both lamp and laser
sources) influence on fluorescence excitation and
emission spectra of water samples have been
investigated. Photo chemical processes under laser
excitation and effect of fluorescence saturation
have been studied. The obtained results give a
chance to support the hypothesis of the nature of
fluorescence band of dissolved organic matter in
water.
KEY WORDS: Remote Sensing, Water, Fluorescence
Spectra.
1. INTRODUCTION.
The dissolved organic matter is a
significantingredient of natural water systems and
determines its ecological state. That is why the
creation of the precise and sensitive methods to
control the presence of DOM total quantity in
water is now as the actual problem as before. One
of such method is the fluorescent analysis based
on the hypothesis that the correlation between
fluorescent intensity (Ig1) and DOM concentration
(C) exists. However, more careful investigation of
DOM spectral characteristics led us to conclusion
that the relation between Ici and C is practically
much more complex that one could anticipate a
priori. There are many factors which break this
correlation. These factors are:
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1) random changes of the fluorescent source
intensity;
2) dependence of fluorescent signal level on
the experimental conditions and as well as the
conditions of the waves propagation;
3) temperature changes of the water;
4) changes of pH values in water;
5) presence of metal ions in water;
6) ultraviolet (UV) radiation from the Sun
and excitation radiation of laser or lamp sources.
The first two factors can be removed using the
method with calibration of fluorescent signal
according to Raman scattering (RS) signal of
water and parallel detection of these signals
(Fadeev, 1983). Parameter F=l RS doesn’t depend
on fluctuations of radiation source power,
experimental conditions and is used in our case as
a parameter correlating with concentration of
organic pollutions (DOM in our case).
It is important to emphasize that the use of RS
signal as an internal standard is the basic
principle for remote sensing, when some parameters
can not be controlled.
Influence of metal ions on fluorescence spectra of
DOM has been studied in (Safronova, 1989). Changes
of the fluorescent intensity connected with
variations of pH values and temperature ( in range
8...42 C) have been investigated in detail in
(Smart, 1976). Influence of UV sunlight radiation
on fluorescence spectra of DOM are described in
(Samokhina, 1989).
The goal of this paper is to study the general
appropriateness of the spectral characteristic of
DOM under temperature variations ( in wide range
0...30°C) and UV radiation excitation by both lamp
and laser sources. During these experiments we
supposed to estimate an influence of factors
mentioned above on the spectral characteristics of
DOM (to correct fluorescence spectra obtained in
situ). Moreover new experimental results extend
our knowledge about the nature fluorescence band
of DOM.