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Introduction

The Kaliasote reservoir is situated near the Water and Land Management Institute (WALMI) Bhopal, and was constructed as a storage dam to conserve excess water of Upper Lake, discharged through the Bhadbhada spill gates of the lake for irrigation purposes. The reservoir is having a catchment of 381.38 Km²and the gross capacity is 35.387 Mecum. The reservoir is also facing the problem of siltation due to rapid change in land use pattern from agriculture to housing. The catchment area is surrounded by agriculture land where fertilizers and pesticides are being used. Under present investigation two sampling stations were identified one at Near Bhadbhada where Chemical Fertilizers are being used and the other one at Reference sample i.e. Behind MACT.

Material and Methods

Water samples were collected in fresh 2.5 L plastic containers previously washed with 1:3 HNO₃during the post monsoon months i.e. September-2010 from surface and bottom water.

使用数字酸度计pH值确定。Conductivity was measured using digital conductivity meter. Dissolved Oxygen was determined by the Wrinkler’s method with Azide modification. Biological Oxygen Demand was determined by five days method. Chemical Oxygen Demand determined by Potassium Dichromate Pen Reflux method. Nitrate & phosphate were estimated by UV-visible Spectrophotometer. Potassium was determined by using Flame Photometer.

Results and Discussion

水质量标准and guidelines corresponding to the ISI, WHO, CPCB have been compared with the results under the given tables and graphs.

pH and Conductivity

pH is largely depend on carbonates_,bicarbonates, CO₂.The results of pH ranged in between 7.1-7.6 indicating that the lake water is slightly alkaline. Desirable pH range is 7.0-8.5 as per WHO, ISI. Conductivity is depended on SO₄,Cl,PO₄and heavy metals and total concentration of dissolved ions. The results of analysis in between 269-768 micro-ohms/cm. The conductivity standard value is 50-1500 micro-ohms/ cm.

Dissolved Oxygen (DO)

DO in water is of great importance to all aquatic organism and is considered to be the factor that reflects the biological activity taking place in a water body and influences the biological changes. In the present study DO values were found in between 3.2-8.8 mg/L against the standard value of 6.0 mg/L.

Biological Oxygen Demand (BOD)

BOD is directly linked with decomposition of dead organic matter present in the lake and hence the higher values of BOD can be directly co-related with pollution status and has an inverse relation with DO concentration. The BOD values were observed in between 1.2-7.2 mg/L . The permissible limit is 3-6 mg/L.

Chemical Oxygen demand (COD)

The range of COD was observed in between 30-52 mg/L while the permissible limit is 10.0 mg/L.

Nitrate (NO₃), phosphate (PO₄) and Potassium

Nitrate and phosphate are two important nutrients in the lake for eutrophication process. These nutrients support the fast growth of aquatic plant. In the present study, the results of nitrate in between 1.16-2.69 mg/L. and results of phosphate was in between 1.33-2.56 mg/L. This range were observed exceeds the permissible limit because excessive use of chemical Fertilizers. Potassium ranged in between 18.0-35.0 mg/L. The values were observed beyond the permissible limit.

Table 1: Concentration of physicochemical parameters of different Sampling stations of Kaliashote reservoir in the given table and graphs Click here to View table

Figure 1: Variation in pH in different stations of Kaliashote resevoir Click here to View figure

Figure 2: Variation in conductivity in different stations of Kaliashote resevoir Click here to View figure

Figure 3: Variation in DO and BOD in different stations of Kaliashote resevoir Click here to View figure

Figure 4: Variation in COD in different stations of Kaliashote resevoir Click here to View figure

Figure 5: Variation in Nitrate and Phosphate in different stations of Kaliashote resevoir Click here to View figure

Figure 6: Variation in Potassium in different stations of Kaliashote resevoir Click here to View figure

Conclusion

The comparative analysis depicts that, higher concentration of nutrients both nitrates as well as phosphates in the water samples of near Bhadbhada which is being predominantly cultivated with chemical fertilizers especially with Urea, DAP, Super Phosphate etc. The availability of the higher concentration of nutrients in water due to intensive use of chemical fertilizer in the catchment area of the reservoir would accelerate the process of eutrophication. The water samples collected from Reference sample i.e. behind MACT, Kaliasote reservoir has comparatively lower concentration of nutrients. Thus, the present study recommends the use of organic fertilizer in place of chemical fertilizer which would not only improve the soil fertility but also help in reducing the enrichment of nutrients the reservoir water because of chemical fertilizer.

Acknowledgements

The authors are thankful to Principal, Sadhu Vaswani college Bhopal for providing me Laboratory Facilities and encouragement.

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