Data for: HIGH RESOLUTION EVIDENCE OF IRON-PHOSPHORUS-SULPHUR MOBILITY AT HYPOXIC SEDIMENT WATER INTERFACE: AN INSIGHT TO PHOSPHORUS REMOBILIZATION USING DGT-INDUCED FLUXES IN SEDIMENTS MODEL.

Name: Data for: HIGH RESOLUTION EVIDENCE OF IRON-PHOSPHORUS-SULPHUR MOBILITY AT HYPOXIC SEDIMENT WATER INTERFACE: AN INSIGHT TO PHOSPHORUS REMOBILIZATION USING DGT-INDUCED FLUXES IN SEDIMENTS MODEL.
Creator: Eyram Norgbey
Published: 2020-04-09T03:51:36.853Z
Keywords: Bioavailability, Heavy Metal, Iron, Water Quality, Phosphorus, Sulphate Reducer

Norgbey, Eyram

doi:10.17632/4jdm8fbhts.1

Data for: HIGH RESOLUTION EVIDENCE OF IRON-PHOSPHORUS-SULPHUR MOBILITY AT HYPOXIC SEDIMENT WATER INTERFACE: AN INSIGHT TO PHOSPHORUS REMOBILIZATION USING DGT-INDUCED FLUXES IN SEDIMENTS MODEL.

Published: 9 April 2020| Version 1 | DOI: 10.17632/4jdm8fbhts.1

Contributor:

Eyram Norgbey

Description

The diffusive gradient in thin films (DGT) technique, high-resolution dialysis, DGT-computer imaging densitometry (CID), DGT-induced fluxes in sediments (DIFS) and planar optode (PO) device were used to describe the dynamics Fe-P-S in SWI during hypoxia.The DGT-CID-PO-DIFS provided a deep insight on the mechanism of Fe-P-S and remobilization of P at SWI leading to Blackwater event and eutrophication affecting reservoir water quality.

Data for: HIGH RESOLUTION EVIDENCE OF IRON-PHOSPHORUS-SULPHUR MOBILITY AT HYPOXIC SEDIMENT WATER INTERFACE: AN INSIGHT TO PHOSPHORUS REMOBILIZATION USING DGT-INDUCED FLUXES IN SEDIMENTS MODEL.

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