ABSTRACT The study aimed to monitor the water quality status of Ashtamudi estuary – a Ramsar wetland situated along south west coast of India. Surface water samples collected were analysed to evaluate the spatio-temporal variability in water quality parameters. Riverine sites exhibited a relative lowering of total dissolved solids due to dilution effect via runoff, substantiated by rainfall and river discharge data. Increased average salinity during non-monsoon (23.84 ± 1.02 ppt) and subsequent enriched levels of major ions at sites near to Arabian Sea was attributed to seawater intrusion. The conservative nature of major ions was established through Theoretical Dilution Line. Relatively higher biochemical oxygen demand (average = 6.54 ± 0.82 mg/L ) during monsoon was due to allochthonous organic matter input and subsequent biodegradation, substantiated by depleted Eh values (range: −105.70 to −12 mV). Concentration of dissolved inorganic phosphate (range: 0.32–2.58 µM) and nitrate (range: 1.43–182.14 µM) during non-monsoon was comparable with already published data. Decline in phosphate content during non-monsoon was due to decreased runoff, adsorption to sediments, and phytoplankton uptake. Increased silicate concentration during non-monsoon (average = 28.73 ± 0.5 µM) could be related to biodegradation of phytoplankton detritus. In general, no drastic variations in water quality were noted compared to that of the earlier investigations.
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