The light intensity in water decreases exponentially with depth and it is usually estimated by the equation as
Iz=
Io⋅
e-k⋅z, in which
Iz is the intensity at
z.
Io is intensity at the surface, and
k is extinction coefficient (
m-1) in water. The extinction coefficient is affected by presence of dissolved and suspended substances. In this study, this relation is shown by the equation
k=
ko+α (
SSchl) + β (
SSdet) in which
k is the total apparent extinciion coefficient, k
o is the light extinction of water with no suspended solids,
SSchl is the phytoplankton concentration (
g⋅m-3),
SSdet is concentration of suspended substances other than phytoplankton (
g⋅m-3), and α and β are constant (
m3⋅g
-1⋅m
-1) .
SSchl, and
SSdet be computed by using the following equations:
SSchl=
250 (chl-a) in brown water,
SSchl=
150 (chl-a) in green water, and
SSdet=
SS-
SSchl in which
chl-a is chlorophyll-
a concentration (
g⋅m-3) and
SS is the total concentration of suspended substances. Field work to gain data on water quality was performed in kuruma prawn culture ponds of Kumamoto Prefecture. The α value obtained from analysis of experimental data is 0.091 and 0.15 in brown and green waters, respectively. The values of β and
ko were found to be 0.060 and 0.076, respectively, regardless of the color of the water. Concerning with
k values, mean occupation rates of
SSchl and
SSdet per
SS are 59.6 ± 18.3 % and 35.9 ± 17.1 %, respectively. The ratio of
ko + β (
SSdet) per
k is 40.4 % in kuruma prawn ponds, and this result was shown to be higher value than 2-16 % in offshore waters obtained by Riley's works. From these results, the extinction coefficient was calculated by the above equation and experimental data. A comparison of the observed and calculated coefficients yielded a satisfactory result.
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