Department of Chemistry, Council of Scientific and Industrial Research (CSIR)-National Institute of Oceanography (NIO), Regional Centre, Kochi-682018, India
 Research Article   
								
																Biogeochemical Cycling of Phosphorus in the Cochin Backwaters:
Southwest Coast of India 
																Author(s): Rejomon George*, Martin GD, Gerson VJ and Nair M             
								
																
						 Here we studied total phosphorus and its fractions in sediments from the Cochin backwaters along with dissolved 
  inorganic phosphate, tidal currents, pH, and salinity during the monsoon and pre-monsoon periods. During the 
  monsoon, sediments function as a sink for phosphate derived from land-based pollutant sources, whereas, during 
  the pre-monsoon, sediment re-suspension provides a source of phosphate to the overlying water column, both with 
  the capacity to alter eutrophication events. The heavy river runoff during the monsoon lowers the pH and salinity of 
  the water column, thereby enhancing adsorption of phosphorus from water to sediments. In contrast, seawater 
  incursion during the pre-monsoon increases the pH and salinity of the water column to enhance the desorption of 
  phosphorus from sediments to the water. Iron-bound inorganic (0.48-0.78 mg g-1.. Read More»
						  
															  
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