Arai Yuji, Sparks D L, Davis J A
U.S. Geological Survey, Water Resource Division, MS 465, 345 Middlefield Road, Menlo Park, California 94025, USA.
Environ Sci Technol. 2004 Feb 1;38(3):817-24. doi: 10.1021/es034800w.
Effects of dissolved carbonate on arsenate [As(V)] reactivity and surface speciation at the hematite-water interface were studied as a function of pH and two different partial pressures of carbon dioxide gas [P(CO2) = 10(-3.5) atm and approximately 0; CO2-free argon (Ar)] using adsorption kinetics, pseudo-equilibrium adsorption/titration experiments, extended X-ray absorption fine structure spectroscopic (EXAFS) analyses, and surface complexation modeling. Different adsorbed carbonate concentrations, due to the two different atmospheric systems, resulted in an enhanced and/or suppressed extent of As(V) adsorption. As(V) adsorption kinetics [4 g L(-1), [As(V)]0 = 1.5 mM and I = 0.01 M NaCl] showed carbonate-enhanced As(V) uptake in the air-equilibrated systems at pH 4 and 6 and at pH 8 after 3 h of reaction. Suppressed As(V) adsorption was observed in the air-equilibrated system in the early stages of the reaction at pH 8. In the pseudo-equilibrium adsorption experiments [1 g L(-1), [As(V)]0 = 0.5 mM and I = 0.01 M NaCI], in which each pH value was held constant by a pH-stat apparatus, effects of dissolved carbonate on As(V) uptake were almost negligible at equilibrium, but titrant (0.1 M HCl) consumption was greater in the air-equilibrated systems (P(CO2) = 10(-3.5) atm) than in the CO2-free argon system at pH 4-7.75. The EXAFS analyses indicated that As(V) tetrahedral molecules were coordinated on iron octahedral via bidentate mononuclear ( 2.8 A) and bidentate binuclear (approximately equal to 3.3 A) bonding at pH 4.5-8 and loading levels of 0.46-3.10 microM m(-2). Using the results of the pseudo-equilibrium adsorption data and the XAS analyses, the pH-dependent As(V) adsorption under the P(CO2) = 10(-3.5) atm and the CO2-free argon system was modeled using surface complexation modeling, and the results are consistent with the formation of nonprotonated bidentate surface species at the hematite surfaces. The results also suggest that the acid titrant consumption was strongly affected by changes to electrical double-layer potentials caused by the adsorption of carbonate in the air-equilibrated system. Overall results suggest that the effects of dissolved carbonate on As(V) adsorption were influenced by the reaction conditions [e.g., available surface sites, initial As(V) concentrations, and reaction times]. Quantifying the effects of adsorbed carbonate may be important in predicting As(V) transport processes in groundwater, where iron oxide-coated aquifer materials are exposed to seasonally fluctuating partial pressures of CO2(g).
研究了溶解碳酸盐对赤铁矿 - 水界面上砷酸盐[As(V)]反应活性和表面形态的影响,该影响是pH值以及两种不同二氧化碳气体分压[P(CO₂)= 10⁻³·⁵ atm和约0;无CO₂的氩气(Ar)]的函数,采用了吸附动力学、准平衡吸附/滴定实验、扩展X射线吸收精细结构光谱(EXAFS)分析以及表面络合模型。由于两种不同的大气系统,不同的吸附碳酸盐浓度导致As(V)吸附程度增强和/或受到抑制。As(V)吸附动力学[4 g L⁻¹,[As(V)]₀ = 1.5 mM且I = 0.01 M NaCl]表明,在pH为4和6以及反应3小时后pH为8的空气平衡系统中,碳酸盐增强了As(V)的吸收。在pH为8的反应早期,在空气平衡系统中观察到As(V)吸附受到抑制。在准平衡吸附实验[1 g L⁻¹,[As(V)]₀ = 0.5 mM且I = 0.01 M NaCl]中,每个pH值通过pH计装置保持恒定,在平衡时溶解碳酸盐对As(V)吸收的影响几乎可以忽略不计,但在pH为4 - 7.75时,空气平衡系统(P(CO₂)= 10⁻³·⁵ atm)中的滴定剂(0.1 M HCl)消耗量比无CO₂的氩气系统中的大。EXAFS分析表明,在pH为4.5 - 8且负载水平为0.46 - 3.10 μmol m⁻²时,As(V)四面体分子通过双齿单核(2.8 Å)和双齿双核(约等于3.3 Å)键合与铁八面体配位。利用准平衡吸附数据和XAS分析的结果,采用表面络合模型对P(CO₂)= 10⁻³·⁵ atm和无CO₂的氩气系统下pH依赖的As(V)吸附进行了建模,结果与赤铁矿表面形成非质子化双齿表面物种一致。结果还表明,在空气平衡系统中,酸滴定剂的消耗受到碳酸盐吸附引起的双电层电位变化的强烈影响。总体结果表明,溶解碳酸盐对As(V)吸附的影响受反应条件[例如可用表面位点、初始As(V)浓度和反应时间]的影响。量化吸附碳酸盐的影响对于预测地下水中As(V)的迁移过程可能很重要,在地下水中,氧化铁包覆的含水层材料会暴露于季节性波动的CO₂(g)分压下。