黄河入河沙漠颗粒物对磷酸盐的吸附特征

研究了黄河入河沙漠颗粒物在天然水(河水和海水)中对磷酸盐的吸附行为,用改进的Langmuir和Freundlich等温吸附模型对实验数据进行了拟合.结果表明,①改进的Langmuir等温吸附模型更适用于描述黄河入河沙漠颗粒物对磷酸盐的吸附特征,其物理意义更明确,得到的拟合参数更合理;②颗粒物对磷的最大吸附容量Qmax变化范围为41.322～357.143mg.kg-1,其中居延海颗粒物Y2的Qmax最大.Qmax与颗粒物(Y1～Y5)的有机质有着极显著的正相关关系;③除巴丹吉林沙漠颗粒物Y1外,颗粒物的临界磷平衡浓度EPC0值均大于其相应水体的磷浓度.Y1在黄河水中吸附磷的EPC0小于相应水体的磷浓度0.0100.053 mg.L-1,而在渤海海水中却大于相应水体的磷浓度0.1090.074 mg.L-1,表明Y1吸附了黄河水中的磷,进入渤海后Y1原有吸附可交换态磷NAP转移到海水中.其它颗粒物与相应水体进行磷交换的过程中存在着解吸磷的现象,具有向相应水体释放磷的能力;④黄河入河沙漠颗粒物对磷酸盐的吸附等温线是过溶液浓度轴0.00的交叉型等温线,这种新型交叉型吸附-解吸模型较好地解释了其吸附特征和天然粒子的双重性作用.

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.