首页> 外文期刊>Journal of Applied Polymer Science >Kinetics of Release of Particulate Solutes lncorporated in Cellulosic Polymer Matrices as a Function of Solute Solubility and Polymer Swellability.II.Highly Soluble Solute
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Kinetics of Release of Particulate Solutes lncorporated in Cellulosic Polymer Matrices as a Function of Solute Solubility and Polymer Swellability.II.Highly Soluble Solute

机译:溶质溶解度和聚合物溶胀度的函数,结合在纤维素聚合物基质中的溶质释放出来的动力学。II。高溶质溶质

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摘要

The kinetics of release into water of particulate NaCl (used here as an example of a highly water-soluble solute) incorproated in a cellulose acetate (CA)matrix was investigated in correlation with the concurrent variation of the water content of the matrix.To ensure comparability with the kinetic behavior of sparingly soluble solutes reported in part I,a CA of the same composition,and identical filmforming procedures were employed.In contrast to this sparingly soluble solute behavior,deviations from t~(1/2) release kinetics and temporary osmotically induced retention of excess imbibed water were observed.Both these effects became more noticeable with decreasing salt loads.At the same time the observed release rates were far in excess of what could be expected from measurements of the NaCl transport properties of the particle-depleted matrix or what could be predicted on the basis of model calculations assuming homogeneous and instantaneously reversible osmotically induced excess water uptake.Such a marked enhancement of release rate is commonly attributed to the formation of a pore network in the particle-depleted matrix by mechanical rupture of the "walls" separating neighboring particle-containing cavities,due to osmotically induced ingress of water therein. However, it was shown that such a mechanism is unsustainable in the present context.A new,more general mechanism is proposed that can successfully account for all the salient kinetic features of the combined solute release and water absorption-desorption processes noted here.Additionally,slow molecular relaxation processes were also shown to play a significant role in the mechanism of solute release.
机译:研究了结合在醋酸纤维素(CA)基质中的颗粒状氯化钠(此处用作高水溶性溶质的例子)释放到水中的动力学,并与基质中水含量的同时变化相关联。与第一部分中报道的难溶性溶质的动力学行为具有可比性,采用相同组成的CA,采用相同的成膜程序。与这种难溶性溶质的行为相反,与t〜(1/2)释放动力学和暂时性的偏差渗透诱导的过量吸水的滞留现象被观察到,随着盐负荷的降低,这两种作用变得更加明显;同时,观察到的释放速率远远超过了通过测量贫化后的颗粒的NaCl传输特性所预期的释放速率。矩阵或在假设均质且瞬时可逆渗透引起的过量水的模型计算的基础上可以预测的结果这种释放速率的显着提高通常归因于由于渗透诱导的水进入其中,通过将相邻的含颗粒腔分开的“壁”的机械破裂,在贫颗粒的基质中形成了孔网络。然而,事实证明这种机制在当前情况下是不可持续的。提出了一种新的,更通用的机制,该机制可以成功解决本文所述溶质释放和吸水-解吸过程相结合的所有显着动力学特征。缓慢的分子弛豫过程在溶质释放机理中也显示出重要作用。

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