Abstract
Assessment of physicochemical parameters of Chilika lagoon water is of vital importance as it guides to monitor the pollution status and formulate a management plan. Mixing of water from river and sea with different nutrient levels makes an ideal condition of salinity and nutrient stoichiometry supporting a unique benthic and pelagic biodiversity including fishery. The hydrology of the lagoon undergoes a significant change during the switchover between seasons as well as years. The rainfall pattern influences the discharge with different nutrient concentration and stoichiometry which ultimately alters the lagoon biogeochemistry. Apart from these, the spatiotemporal variability is also controlled by the exchange of seawater through the lagoon mouth which undergoes drastic change over time with respect to the cross-sectional area and its position. Overall brackish nature of the lagoon was sustained in most of the lagoon throughout the year due to the adequate inflow of saline water from the sea and fresh water from major Rivers.
The present study showed that the physicochemical parameters such as pH, dissolved oxygen (DO), biochemical oxygen demand (BOD), nitrite nitrogen (NO2), nitrate nitrogen (NO3), and phosphate phosphorous (PO4) were within the threshold range suitable for the propagation of wildlife and fishery. The primary source of PO4 and NO2 were mostly from in situ mineralisation processes whereas, NO3 and silicate (SiO2) from the riverine influx. The overall nutrient stoichiometry indicated NO3 and PO4 were limiting with respect to SiO2 throughout the year which favoured the growth of diatoms. During the monsoon period, PO4 remained limiting due to dilution by fresh water from northeast rivers. Shallow regions of the lagoon get turbid during monsoon due to the inflow of river water with high SPM but during summer, the wind-induced bottom sediment churning becomes the key influencing variable. The variability of the flux of nutrients and suspended particulate matter (SPM) with respect to different rivers and season, re-suspension of sediment, and autochthonous processes had a significant influence on the lagoon’s biogeochemical cycle. Despite least photic depth (transparency), the appropriate condition of light and nutrient stoichiometry enabled highest primary productivity (PP) in the northern sector (NS) while southern sector (SS) had the lowest rate due to low nutrient content, even though it maintained the highest water clarity throughout the year.
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Acknowledgments
The authors are thankful to the World Bank for the funding support to the “Integrated Coastal Zone Management Project” through the State Project Management Unit, Odisha, India. to the authors also thank the scientific and supporting staff for the help during the sample collection as well as analysis in the laboratory. We also wish to thank Mr. Abhijit Das, CDA for data compilation and Mrs. Jagnyaseni Rout for preparation of the GIS map.
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Muduli, P.R., Pattnaik, A.K. (2020). Spatio-Temporal Variation in Physicochemical Parameters of Water in the Chilika Lagoon. In: Finlayson, C., Rastogi, G., Mishra, D., Pattnaik, A. (eds) Ecology, Conservation, and Restoration of Chilika Lagoon, India. Wetlands: Ecology, Conservation and Management, vol 6. Springer, Cham. https://doi.org/10.1007/978-3-030-33424-6_9
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