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Seasonal variation in the
physicochemistry of a small tropical reservoir (Aiba
Reservoir, Iwo, Osun, Nigeria)
Atobatele, Oluwatosin
Ebenezer1 and Ugwumba, O. Alex2
1Department
of Biological Sciences, Bowen University, Iwo, Osun,
Nigeria.
2Department
of Zoology, University of Ibadan, Ibadan, Nigeria.
*Corresponding author. E-mail:
tosine_ben@yahoo.com.
Tel: +2348033667983.
Accepted 8
May, 2008 |
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Aiba Reservoir was sampled between March, 2004 and February,
2005 for physico-chemical studies. Air temperatures ranged
from 20.00 – 30.50oC (mean ± s.e: 26.33 ± 0.26oC),
water temperature ranged from 25.00 – 35.00oC
(mean ± s.e: 29.26 ± 0.19oC), pH ranged from 5.53
- 9.48 (mean ± s.e: 7.98 ± 0.11), dissolved oxygen ranged
from 1.75 – 11.20 mgO2/l (mean ± s.e: 7.23 ± 0.20
mgO2/l), alkalinity ranged from 42.50 – 85.00
mg/l (mean ± s.e: 65.20 ± 0.85 mg/l), total hardness ranged
from 12.00–59.00 mg/lCaCO3 (mean ± s.e: 45.13 ±
0.90 mg/lCaCO3), conductivity ranged from 6.80 –
126.40 mV (mean ± s.e: 67.03 ± 4.04 mV), and turbidity
ranged from 12.50 – 143.75 FTU (mean ± s.e: 40.74 ± 3.60 FTU).
The physico-chemistry of Aiba Reservoir exhibited spatio-temporal
variation. Two-way analysis of variance of physico-chemical
parameters showed obvious seasonality for pH, conductivity
and turbidity, suggesting that these parameters play major
roles in the limnology of the reservoir. Factor analysis
shows pH, conductivity, temperature and dissolved oxygen as
important parameters contributing to the annual variability.
Dissolved oxygen is a more important parameter during the
wet season, while alkalinity is more important during the
dry season for the reservoir. Hardness and alkalinity values
suggest that the reservoir water is good for aquaculture.
Key words:
Reservoir, physicochemical parameters, seasonality, factor
analysis, limnology. |