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Calculation of the equilibrium pH in a multiple-buffered aqueous solution based on partitioning of proton buffering: a new predictive formula

机译:基于质子缓冲分配的多重缓冲水溶液中平衡pH的计算:一个新的预测公式

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摘要

Upon the addition of protons to an aqueous solution containing multiple buffers, the final H+ concentration ([H+]) at equilibrium is determined by the partitioning of added H+ among the various buffer components. In the analysis of acid-base chemistry, the Henderson-Hasselbalch equation and the Stewart strong ion formulation can only describe (rather than predict) the equilibrium pH following a proton load since these formulas calculate the equilibrium pH only when the reactant concentrations at equilibrium1 are already known. In this regard, it is simpler to directly measure the equilibrium pH rather than measure the equilibrium reactant concentrations to calculate the equilibrium pH. As these formulas cannot predict the final equilibrium [H+] following a proton load to a multiple-buffered aqueous solution, we developed a new quantitative approach for predicting the equilibrium [H+] that is based on the preequilibrium2 concentrations of all buffers in an aqueous solution. The mathematical model used to derive our equation is based on proton transfer buffer equilibria without requiring the incorporation of electroneutrality considerations. The model consists of a quartic polynomial equation that is derived based solely on the partitioning of H+ among the various buffer components. We tested the accuracy of the model using aqueous solutions with various buffers and measured the equilibrium pH values following the addition of HCl. Our results confirmed the accuracy of our new equation (r2 = 1; measured pH vs. predicted pH), indicating that it quantitatively accounts for the underlying acid-base phenomenology.
机译:在将质子添加到含有多种缓冲剂的水溶液中时,平衡时的最终H +浓度([H +])由添加的H +在各种缓冲剂成分之间的分配确定。在酸碱化学分析中,Henderson-Hasselbalch方程和Stewart强离子公式只能描述(而不是预测)质子载荷后的平衡pH,因为这些公式仅在平衡物1处的反应物浓度为1时才计算平衡pH。已经知道了。在这方面,直接测量平衡pH值比测量平衡反应物浓度来计算平衡pH值更简单。由于这些公式无法预测质子加载到多缓冲水溶液后的最终平衡[H +],因此我们开发了一种新的定量方法来预测平衡[H +],该方法基于水溶液中所有缓冲液的preequilibrium2浓度。用于推导我们方程的数学模型基于质子转移缓冲液平衡,而无需考虑电子中性。该模型由一个四次多项式方程组成,该方程仅基于H +在各个缓冲区分量之间的分配而得出。我们使用具有各种缓冲液的水溶液测试了模型的准确性,并在加入HCl后测量了平衡pH值。我们的结果证实了我们新方程式的准确性(r2 = 1;测量的pH与预测的pH),表明它定量地解释了潜在的酸碱现象。

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