Univ Lyon, Université Claude Bernard Lyon 1, CNRS, Institut Lumière Matière, F-69622, VILLEURBANNE, France.
Dipartimento di Chimica, Materiali ed Ingegneria Chimica "G. Natta", Politecnico di Milano, Piazza Leonardo da Vinci 32, 20133 Milano, Italy.
Soft Matter. 2017 Mar 8;13(10):2014-2023. doi: 10.1039/c6sm02607a.
We address the mechanical characterization of a calcite paste as a model system to investigate the relation between the microstructure and macroscopic behavior of colloidal suspensions. The ultimate goal is to achieve control of the elastic and yielding properties of calcite which will prove valuable in several domains, from paper coating to paint manufacture and eventually in the comprehension and control of the mechanical properties of carbonate rocks. Rheological measurements have been performed on calcite suspensions over a wide range of particle concentrations. The calcite paste exhibits a typical colloidal gel behavior, with an elastic regime and a clear yield strain above which it enters a plastic regime. The yield strain shows a minimum when increasing the solid concentration, connected to a change in the power law scaling of the storage modulus. In the framework of the classical fractal elasticity model for colloidal suspensions proposed by Shih et al. [Phys. Rev. A, 1990, 42, 4772], we interpret this behavior as a switch with the concentration from the strong-link regime to the weak-link regime, which had never been observed so far in one well-defined system without external or chemical forcing.
我们研究了方解石糊作为模型系统的力学特性,以探讨胶体悬浮液的微观结构和宏观行为之间的关系。最终目标是控制方解石的弹性和屈服特性,这将在多个领域具有重要意义,从纸张涂料到油漆制造,最终应用于理解和控制碳酸盐岩的力学性能。我们在很宽的颗粒浓度范围内对方解石悬浮液进行了流变学测量。方解石糊表现出典型的胶体凝胶行为,具有弹性区和明显的屈服应变,超过该应变后进入塑性区。屈服应变随着固体浓度的增加而最小化,与储能模量的幂律标度的变化有关。在 Shih 等人提出的胶体悬浮液经典分形弹性模型的框架内[Phys. Rev. A, 1990, 42, 4772],我们将这种行为解释为随着浓度从强键合区到弱键合区的转变,这在没有外部或化学强制的情况下,在一个明确定义的系统中从未观察到过。