[Phosphate adsorption characteristics on the desert particulates of inflow Yellow River].

Adsorption behaviors of phosphate on the desert particulates of inflow Yellow River were investigated in natural water (river water and sea water) and the experimental data was fitted by both the improved Langmuir and Freundlich isotherm adsorption models. The results show that (1) With more clear physical meaning and more reasonable fitting parameters, the improved Langmuir isotherm adsorption model is much better for describing phosphate adsorption on the desert particulates than the improved Freundlich isotherm adsorption model; (2) The maximum phosphorus (P) adsorption capacity Qmac is in the range of 41.322-357.143 mg x kg(-1), which is the biggest in Y2 (Juyanhai Lake particulates). There is remarkable positive correlation between Qmax and organic matter of the particulates (Y1-Y5); (3) Except for Y1 (Badain Jaran Desert particulates), the EPC0 (zero equilibrium P concentration) of the particulates are higher than the concentration of P in corresponding water. The EPC0 of P adsorption on Y1 in Yellow River is lower than P concentration in corresponding water (0.010 mg x L(-1) < 0.053 mg x L(-1)), while the EPC0 of P adsorption on Y1 in Bohai Sea water is higher than the P concentration in their corresponding water (0.109 mg x L(-1) > 0.074 mg x L(-1)), which shows that Y1 adsorbs P from the water of the Yellow River, then it releases its NAP (native adsorbed exchangeable phosphorus) into Bohai Seawater. However, in the process of the P exchange between other desert particulates and their corresponding water, only desorption phenomenon were observed, which means all other desert particulates release P to their corresponding water; (4) The adsorption isotherms of phosphate on the desert particulates of inflow Yellow River are cross-axis-type with over 0.00, a new cross-axis-type adsorption-desorption model, which provide a better explanation for adsorption characteristics of P and for the dual role of natural particulates.