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- W2358637524 abstract "The clay mineral composition of sediments from Dianchi Lake mainly constituted kaolinite, followed, by illite, and small amounts of vermiculite, chlorite and montmorillonite. The adsorption on surface of the sediments mainly occurred within 0~ 6 hour, and then reached a dynamic equilibrium after 6 h, thus the adsorption rate within 0~ 30 minutes was bigger than 5.0 mg· g- 1· h- 1. P adsorption amount on the sediments enhanced with the increasing initial phosphate concentration. The adsorption isotherms of phosphate indicated that the adsorbed capacity was about 5.0 mg· g- 1 on surface of the sediments. In acidic condition, the adsorption ability was bigger than that in alkaline condition, and declined gradually with the increasing pH." @default.
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- W2358637524 date "2004-01-01" @default.
- W2358637524 modified "2023-09-25" @default.
- W2358637524 title "Adsorption of Phosphate and Mineral Characteristic in Sediment in Dianchi Lake" @default.
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