Effective charges along the melting line of colloidal crystals.

Effective charges along the melting line of colloidal crystals.
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沿胶体晶体熔线的有效电荷。

DOI:
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发表时间:
2006
影响因子:
4.4
通讯作者:
T. Palberg
T. Palberg
中科院分区:
化学2区
文献类型:
--
作者:
L. Shapran;H. Schöpe;T. Palberg

文献摘要

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带电胶体晶体的剪切模量G测量在几个恒定的颗粒密度n和不同的盐浓度c的熔融盐浓度cM使用扭转共振光谱。远离相边界的样品是多晶的,并且剪切模量作为c的函数大致保持恒定。在接近熔化转变时,围绕收缩的多晶芯形成增加量的壁基晶体材料,并且G几乎线性地下降。当跃迁完成时,G又保持不变。形态过渡可以在单个主曲线上缩放。对于多晶形态,弹性数据根据成对加性屏蔽库仑相互作用产生颗粒有效电荷Z(G)* 来评估。在去离子条件下,Z(0,G)* 与n无关,并且显著低于电荷重整化理论的预期。随着盐浓度的增加,Z(G)* 增加。在较大的n时,增加变得更加明显。通过外推,我们进一步得到了熔点有效弹性电荷Z(M,G)*。Z(M,G)* 随nM和cM的增加呈阶梯状增加,达到与电荷重整化理论一致的值。有趣的是,增加符合半定量与一个预期从通用的熔融线带电球,从而促进了一致的描述相行为和弹性在一个扩展的范围内的相图。
The shear modulus G of charged colloidal crystals was measured at several constant particle densities n and varying salt concentrations c up to the melting salt concentration cM using torsional resonance spectroscopy. Far from the phase boundary the samples are polycrystalline and the shear modulus stays roughly constant as a function of c. Upon approaching the melting transition an increasing amount of wall based crystal material is formed surrounding a shrinking polycrystalline core and G drops nearly linearly. When the transition is complete G again stays constant. The morphologic transitions may be scaled upon a single master curve. For the polycrystalline morphology, the elastic data are evaluated in terms of a pairwise additive screened Coulomb interaction yielding a particle effective charge Z(G)*. Under de-ionized conditions Z(0,G)* is independent of n and significantly lower than expected from charge renormalization theory. With increasing salt concentration Z(G)* increases. The increase becomes more pronounced at larger n. By extrapolation we further obtain the melting line effective elasticity charge Z(M,G)*. Z(M,G)* shows a steplike increase with increasing nM and cM to values consistent with charge renormalization theory. Interestingly, the increase coincides semi-quantitatively with the one expected from the universal melting line for charged spheres, thus facilitating a consistent description of phase behavior and elasticity over an extended range of the phase diagram.