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<p>Geochemical partitioning of phosphorous (P) in surface sediments of Ashtamudi wetland was undertaken to assess the nutrient mobility, bioavailability and ecological risks. The fraction composition implied the dominance of calcium carbonate–bound P (326.92 ± 26.61&#xa0;mg/kg) during non-monsoon and alkali-bound organic P (439.25 ± 11.54&#xa0;mg/kg) during monsoon. Iron-bound P was the major component of bioavailable P; its retention, mobility, and bioavailability in sediments was controlled by iron (oxyhydr) oxides, pH, redox, and salinity. The elevated alkali-bound P content during monsoon highlights the allochthonous contribution of humic associated P via run-off. Increased salinity favours the formation of carbonate minerals (adsorption sites for P in sediments), resulting in dominance of calcium-bound P during non-monsoon. Sedimentary OP was relatively higher and the microbially mediated remineralisation triggers the transformation of organic P to bioavailable form. Enriched levels of total P in sediments were substantiated by relatively lower average organic carbon to total P [70.45 (non-monsoon) and 25.74 (monsoon)] and organic nitrogen/total P ratios [4.53 (non-monsoon) and 1.68 (monsoon)]. Estimated bioavailable P (~ 34–60%) indicated the possibility for rise in P content of the water column and may induce eutrophication risk if nutrient release occurs from sediments. Total P concentration &gt; 700&#xa0;mg/kg at majority of sites implied P contamination due to anthropogenic sources. Severe pollution at ~ 50% of the sites (as per phosphorous pollution index) endorses the fact that the wetland sediments are susceptible to eutrophication.</p>

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Sedimentary phosphorous fraction composition in Ashtamudi wetland: implications on nutrient mobility, bioavailability, trophic state, and pollution

  • 期刊论文

  • 发表日期：

    2026年6月24日

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  • Roshni Mohan,
  • Ratheesh Kumar C. S.,
  • Sudha A.,
  • Sreejisha U

摘要

Geochemical partitioning of phosphorous (P) in surface sediments of Ashtamudi wetland was undertaken to assess the nutrient mobility, bioavailability and ecological risks. The fraction composition implied the dominance of calcium carbonate–bound P (326.92 ± 26.61 mg/kg) during non-monsoon and alkali-bound organic P (439.25 ± 11.54 mg/kg) during monsoon. Iron-bound P was the major component of bioavailable P; its retention, mobility, and bioavailability in sediments was controlled by iron (oxyhydr) oxides, pH, redox, and salinity. The elevated alkali-bound P content during monsoon highlights the allochthonous contribution of humic associated P via run-off. Increased salinity favours the formation of carbonate minerals (adsorption sites for P in sediments), resulting in dominance of calcium-bound P during non-monsoon. Sedimentary OP was relatively higher and the microbially mediated remineralisation triggers the transformation of organic P to bioavailable form. Enriched levels of total P in sediments were substantiated by relatively lower average organic carbon to total P [70.45 (non-monsoon) and 25.74 (monsoon)] and organic nitrogen/total P ratios [4.53 (non-monsoon) and 1.68 (monsoon)]. Estimated bioavailable P (~ 34–60%) indicated the possibility for rise in P content of the water column and may induce eutrophication risk if nutrient release occurs from sediments. Total P concentration > 700 mg/kg at majority of sites implied P contamination due to anthropogenic sources. Severe pollution at ~ 50% of the sites (as per phosphorous pollution index) endorses the fact that the wetland sediments are susceptible to eutrophication.