Zhu Jia-mei, Cao Xiao-yan, Liu Su-mei, Wang Li-sha, Yang Gui-peng, Ge Cheng-feng, Lu Min
Huan Jing Ke Xue. 2016 Feb 15;37(2):558-64.
Kinetic curves and isotherms were investigated to study the sorption mechanism of phosphorus onto the sediments of Sanggou Bay, together with the surface charge properties of sediments and the forms of phosphorus studied. The results showed that the sorption including a fast process and a slow one, and could be described by a two-compartment first order equation. The thermodynamic isotherms were well fitted with a modified Langmuir equation. The maximum adsorption capacity was larger in summer than in spring, and the smaller particle size was favorable to the sorption. The maximum adsorption capacities (Qm) were 0.0471-0.1230 mg x g(-1), and the zero equilibrium phosphorus concentration (EPC0) of the sediments ranged from 0.0596 mg x L(-1) to 0.1927 mg x L(-1), which indicated that the sediments from Sanggou Bay were sources of phosphorus. Inorganic phosphorus (IP) was the main form of total phosphorus (TP). The contents of exchangeable or loosely absorbed P and Fe-bound P increased significantly in the samples after sorption. The sorption process involved physical sorption and chemical sorption, with the former being the predominant.
通过研究动力学曲线和等温线,结合沉积物的表面电荷性质及磷的形态,探讨了桑沟湾沉积物对磷的吸附机制。结果表明,吸附过程包括快速过程和慢速过程,可用双室一级方程描述。热力学等温线与修正的朗缪尔方程拟合良好。夏季的最大吸附容量大于春季,较小的粒径有利于吸附。最大吸附容量(Qm)为0.0471 - 0.1230 mg·g⁻¹,沉积物的零平衡磷浓度(EPC0)范围为0.0596 mg·L⁻¹至0.1927 mg·L⁻¹,这表明桑沟湾的沉积物是磷的源。无机磷(IP)是总磷(TP)的主要形态。吸附后样品中可交换态或松散吸附态磷以及铁结合态磷的含量显著增加。吸附过程涉及物理吸附和化学吸附,其中物理吸附占主导。