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Method to determine van der Waals potential energy of particle interactions for soil clay by dynamic light scattering

机译:动态光散射法测定土壤黏土颗粒相互作用范德华势能的方法

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摘要

Soil particle interaction forces/energies control aggregation and breakup/dispersion processes, which further profoundly affect a series of soil micro- and macro-processes. For soils with complex compositions, it is the interaction energy of different particles that determines particle aggregation and aggregate breakdown/dispersion. However, measuring the interaction energy for complex systems remains a challenge. In this study we proposed a method to measure this van der Waals potential energy using the dynamic light scattering technique. Firstly, the mathematic relationship between the mean aggregation rate and van der Waals potential energy was established. The mean aggregation rates of particles for either simple or complex systems can be facilely determined by the dynamic light scattering technique. Secondly, for verifying the availability of the suggested method, montmorillonite suspensions in four different electrolyte solutions (NaCl, KCl, MgCl2 and CaCl2) were respectively employed to measure the van der Waals potential energy, which equals -17,817 +/- 857 J mol(-1) or -7.22 +/- 0.304 kT with an average deviation of 4.22; this directly verified the reliability of the suggested method. Thirdly, the proposed method was also verified indirectly and independently by the ratio of the electrostatic potential energy of particles to the presence of K+ and Na+, as compared with the ratios from the determined van der Waals potential energy of this study and from cation adsorption selectivity. Considering the dynamic light scattering technique has been widely applied for characterizing soil/clay/humus/microbe aggregation, the proposed method should be appropriate for measuring the van der Waals potential energy for all those systems.
机译:土壤颗粒相互作用力/能量控制着聚集和破碎/扩散过程,进而深刻影响着土壤的一系列微观和宏观过程。对于成分复杂的土壤,不同颗粒的相互作用能决定了颗粒聚集和团聚体的分解/分散。然而,测量复杂系统的相互作用能量仍然是一个挑战。在这项研究中,我们提出了一种使用动态光散射技术测量范德华势能的方法。首先,建立了平均聚集率与范德华势能的数学关系;简单或复杂系统的粒子平均聚集速率可以通过动态光散射技术轻松确定。其次,为了验证所提方法的可用性,分别采用4种不同电解质溶液(NaCl、KCl、MgCl2和CaCl2)中的蒙脱石悬浮液测量范德华势能,其等于-17,817 +/- 857 J mol(-1)或-7.22 +/- 0.304 kT,平均偏差为4.22%;这直接验证了所提方法的可靠性。然后,通过颗粒静电势能与K+和Na+存在的比值,与本研究确定的范德华势能和阳离子吸附选择性的比值,间接和独立地验证了所提方法。考虑到动态光散射技术已被广泛用于表征土壤/粘土/腐殖质/微生物聚集,所提出的方法应适用于测量所有这些系统的范德华势能。

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