Department of Chemical and Environmental Engineering, University of California, Riverside, CA 92521, USA.
Water Res. 2010 Feb;44(4):1213-23. doi: 10.1016/j.watres.2009.09.041. Epub 2009 Sep 22.
The coupled role of solution ionic strength (IS), hydrodynamic force, and pore structure on the transport and retention of viable Cryptosporidium parvum oocyst was investigated via batch, packed-bed column, and micromodel systems. The experiments were conducted over a wide range of IS (0.1-100 mM), at two Darcy velocities (0.2 and 0.5 cm/min), and in two sands (median diameters of 275 and 710 microm). Overall, the results suggested that oocyst retention was a complex process that was very sensitive to the solution IS, the Darcy velocity, and the grain size. Increasing IS led to enhanced retention of oocysts in the column, which is qualitatively consistent with predictions of Derjaguin-Landau-Verwey-Overbeek theory. Conversely, increasing velocity and grain size resulted in less retention of oocysts in the column due to the difference in the fluid drag force and the rates of mass transfer from the liquid to the solid phase and from high to low velocity regions. Oocyst retention was controlled by a combined role of low velocity regions, weak attractive interactions, and/or steric repulsion. The contribution of each mechanism highly depended on the solution IS. In particular, micromodel observations indicated that enhanced oocyst retention occurred in low velocity regions near grain-grain contacts under highly unfavorable conditions (IS=0.1 mM). Oocyst retention was also found to be influenced by weak attractive interactions (induced by the secondary energy minimum, surface roughness, and/or nanoscale chemical heterogeneity) when the IS=1 mM. Reversible retention of oocysts to the sand in batch and column studies under favorable attachment conditions (IS=100 mM) was attributed to steric repulsion between the oocysts and the sand surface due to the presence of oocyst surface macromolecules. Comparison of experimental observations and theoretical predictions from classic filtration theory further supported the presence of this weak interaction due to steric repulsion.
采用批式、填充床柱和微模型系统研究了溶液离子强度(IS)、水动力和孔隙结构对活的隐孢子虫卵囊传输和保留的偶联作用。实验在很宽的 IS 范围内(0.1-100 mM)、两个达西速度(0.2 和 0.5 cm/min)和两种砂中(中值粒径为 275 和 710 微米)进行。总体而言,结果表明卵囊保留是一个复杂的过程,对溶液 IS、达西速度和粒度非常敏感。增加 IS 会导致卵囊在柱中得到增强保留,这与德加古林-朗道-韦尔韦尔-奥弗贝克理论的预测定性一致。相反,由于流体阻力和质量从液相向固相以及从高速区向低速区转移的速率的差异,增加速度和粒度会导致卵囊在柱中保留减少。卵囊保留受到低速区、弱吸引力和/或空间排斥的综合作用的控制。每种机制的贡献高度取决于溶液 IS。特别是,微模型观察表明,在高度不利的条件下(IS=0.1 mM),在颗粒-颗粒接触附近的低速区会发生增强的卵囊保留。当 IS=1 mM 时,还发现卵囊保留受弱吸引力(由二次能量最小值、表面粗糙度和/或纳米级化学不均匀性引起)的影响。在有利的附着条件下(IS=100 mM),在批式和柱研究中,卵囊可逆保留在砂中归因于卵囊表面大分子的存在导致卵囊和砂表面之间的空间排斥。经典过滤理论的实验观察和理论预测的比较进一步支持了由于空间排斥而存在这种弱相互作用。