首页> 外文期刊>Geochimica et Cosmochimica Acta: Journal of the Geochemical Society and the Meteoritical Society >Isopiestic measurement of the osmotic and activity coefficients for the NaOH-NaAl(OH)(4)-H2O system at 313.2 K
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Isopiestic measurement of the osmotic and activity coefficients for the NaOH-NaAl(OH)(4)-H2O system at 313.2 K

机译:NaOH-NaAl(OH)(4)-H2O系统在313.2 K时的渗透压和活度系数的同量测量

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摘要

By using a specially designed and constructed isopiestic apparatus, we measured the osmotic coefficients at 313.2 K for the NaOH-NaAl(OH)(4)-H2O system with the total alkali molality, m(NaOHT) (m(NaOH) + m(NaAl[OH]4)), from 0.05 mol/kg H2O to 12 mol/kg H2O and alpha(K) (m(NaOHT)/m(NaAl(OH)4)) from 1.64 to 5.53. The mean standard deviation of the measurements is 0.0038. Several sets of the Pitzer model parameters for NaOH-NaAl(OH)(4)-H2O system were then obtained by regressing the measured osmotic coefficients with the Pitzer model and the Pitzer model parameters for NaOH(aq). One set of the results is as follows: beta(NaOH)((0)): 0.08669, beta(NaOH)((1)): 0.31446, beta(NaOH)((2)). -0.00007367, C-NaOH(Phi): 0.003180, beta(NaAl(OH)4)((0)): 0.03507, beta(NaAl(OH)4)((1)): 0,02401, C-NaAl(OH)4(Phi): -0.001066, theta(OH)-(Al(OH)4)-: 0.08177, Psi(Na)+(OH)-(Al(OH)4)-: -0.01162. The mean standard difference between the calculated and the measured osmotic coefficients is 0.0088. With the obtained Pitzer model parameters, we calculated the values of K-1 = (gamma(NaAl(OH)4,cal2)(.)m(Al(OH)4)-(,exp))/(gamma(NaOH,cal2)(.)m(OH)-(,ex p)) for the gibbsite solubility. The results show that the obtained Pitzer model parameters are reliable, and the relative error of the calculated activity coefficients should be < 2.1%. We also compared the calculated gibbsite solubility data among several activity coefficients models over a range of m(NaOHT) at various temperatures. The comparison indicates that our activity coefficients model may be approximately applied in the ranges of temperature from 298.2 to 323.2 K and m(NaOHT) from 0 to 8 mol/kg H2O. We also calculated the stoichiometric activity coefficients of NaOH and NaAl(OH)(4) and the activity of H2O for the NaOH-NaAl(OH)(4)-H2O system, and these calculations establish their variations with M-NaOHT and alpha(K). These variations imply that the strengths of the repulsive interactions among various anions are in the following sequence: Al(OH)(4)(-)-Al(OH)(4)(-) < Al(OH)(4)(-)-OH- < OH--OH-, and the attractive interaction between Al(OH)(4)(-) and H2O is weaker than that between OH- and H2O. Copyright (C) 2003 Elsevier Ltd. [References: 41]
机译:通过使用专门设计和构造的等渗仪器,我们测量了总碱摩尔比为m(NaOHT)(m(NaOH)+ m()的NaOH-NaAl(OH)(4)-H2O系统在313.2 K的渗透系数NaAl [OH] 4))从0.05 mol / kg H2O到12 mol / kg H2O,α(K)(m(NaOHT)/ m(NaAl(OH)4))从1.64到5.53。测量的平均标准偏差为0.0038。然后,通过将测得的渗透系数与Pitzer模型和NaOH(aq)的Pitzer模型参数进行回归,获得几套NaOH-NaAl(OH)(4)-H2O系统的Pitzer模型参数。一组结果如下:β(NaOH)((0)):0.08669,β(NaOH)((1)):0.31446,β(NaOH)((2))。 -0.00007367,C-NaOH(Phi):0.003180,β(NaAl(OH)4)((0)):0.03507,β(NaAl(OH)4)((1)):0,02401,C-NaAl( OH)4(Phi):-0.001066,θ(OH)-(Al(OH)4)-:0.08177,Psi(Na)+(OH)-(Al(OH)4)-:-0.01162。计算和测得的渗透系数之间的平均标准差为0.0088。利用获得的Pitzer模型参数,我们计算出K-1 =(γ(NaAl(OH)4,cal2)(。)m(Al(OH)4)-(,exp))/(γ(NaOH, cal2)(。)m(OH)-(,ex p))的三水铝石溶解度。结果表明,所获得的Pitzer模型参数是可靠的,计算出的活度系数的相对误差应小于2.1%。我们还比较了在不同温度下在m(NaOHT)范围内的几个活度系数模型中计算出的三水铝石溶解度数据。比较表明,我们的活度系数模型可以近似应用于温度范围为298.2至323.2 K和m(NaOHT)为0至8 mol / kg H2O的情况。我们还计算了NaOH-NaAl(OH)(4)-H2O系统的NaOH和NaAl(OH)(4)的化学计量活度系数和H2O的活度,这些计算确定了它们与M-NaOHT和α( K)。这些变化表明,各种阴离子之间的排斥相互作用强度按以下顺序排列:Al(OH)(4)(-)-Al(OH)(4)(-)

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