Evolution Of Phycocyanin

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3.6. Evolution of Phycocyanin The evolution of Phycocyanin during the summer is presented from Fig. 13. Cyanobacteria occurrence and dominance have increased from June to September. It is found that the southern part of the lake has the highest concentration of Phycocyanin (approximately 50 µg/L), and Phycocyanin presents relatively highly over the lake. At the surface In June, there was little presence of Phycocyanin on the surface of the lake. Phycocyanin was not present until July 30th in the middle-east and north sections of the lake. On September 10th most of the surface is covered with a low concentration except for a small section in the far north. Early October on the lake had the highest concentration of Phycocyanin. The whole …show more content…

Comparing the Fig. 14 and 15, it is clear that Nitrates do not have as fast an effect on the chlorophyll-a as TP does. The level of Nitrate starts at 0 mg/L (again, initial value of the study after winter season), and the predicted value of chlorophyll-a is 12 µg/L. The concentration of chlorophyll-a increases slowly until the value of Nitrate is 0.6 mg/L. At this point, the value of chlorophyll-a increases at a steeper slope until Nitrate reaches 1.6 mg/L. Temperature has a decreasing linear effect on chlorophyll-a concentration. For the model, it should be noted that predictions could not be done for temperatures lower than 15 degrees Celsius or higher that 30 degrees Celsius. This is because such low/high temperature is out of the real local conditions. However, we can see from the simulation is that if the temperature goes higher and higher (beyond 30 degrees), the chlorophyll-a decreases. As temperature increases from 16 degrees Celsius, there is a sharp decrease in the value of chlorophyll-a …show more content…

Figure 17 show the relationship between DO and chlorophyll-a. DO starts at approximately 2 mg/L and chlorophyll-a at 30. As the value of DO is increased, the chlorophyll-a concentration slowly decreases until DO reaches 8 mg/L. Once the value of DO surpasses 8mg/L, chlorophyll-a starts to increase with DO until the maximum predicted value of 37 µg/L is reached when DO is around mg/L. This ‘win-win’ relationship between DO and Chlorophyll-a showed also an inverse effect, that means when DO can increase by the fact that when the algae develop (Chlorophyll-a increasing), the photosynthesis of diverse species of algae release more oxygen to the waterbody. The prediction for pH appears to have an error starting out (Fig. 18). The value of chlorophyll-a is in the negative numbers until pH reaches the value of 7. Out of all the single effect parameters, pH appears to be one of the top parameters to effect chlorophyll-a concentration, next to temperature. When the pH value exceeds 7, the chlorophyll-a concentration sharply increases. This increase stopped once the pH reaches 9, and once that value is exceeded, the chlorophyll-a concentration slightly decreases to a plateau of 80 µg/L (Fig.

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