Institute for Atmospheric and Climate Science, ETH Zurich, Zurich, Switzerland.
Phys Chem Chem Phys. 2011 Feb 28;13(8):3514-26. doi: 10.1039/c0cp01273d. Epub 2011 Jan 13.
We present measurements of water uptake and release by single micrometre-sized aqueous sucrose particles. The experiments were performed in an electrodynamic balance where the particles can be stored contact-free in a temperature and humidity controlled chamber for several days. Aqueous sucrose particles react to a change in ambient humidity by absorbing/desorbing water from the gas phase. This water absorption (desorption) results in an increasing (decreasing) droplet size and a decreasing (increasing) solute concentration. Optical techniques were employed to follow minute changes of the droplet's size, with a sensitivity of 0.2 nm, as a result of changes in temperature or humidity. We exposed several particles either to humidity cycles (between ∼2% and 90%) at 291 K or to constant relative humidity and temperature conditions over long periods of time (up to several days) at temperatures ranging from 203 to 291 K. In doing so, a retarded water uptake and release at low relative humidities and/or low temperatures was observed. Under the conditions studied here, the kinetics of this water absorption/desorption process is controlled entirely by liquid-phase diffusion of water molecules. Hence, it is possible to derive the translational diffusion coefficient of water molecules, D(H(2)O,) from these data by simulating the growth or shrinkage of a particle with a liquid-phase diffusion model. Values for D(H(2)O)-values as low as 10(-24) m(2) s(-1) are determined using data at temperatures down to 203 K deep in the glassy state. From the experiment and modelling we can infer strong concentration gradients within a single particle including a glassy skin in the outer shells of the particle. Such glassy skins practically isolate the liquid core of a particle from the surrounding gas phase, resulting in extremely long equilibration times for such particles, caused by the strongly non-linear relationship between concentration and D(H(2)O). We present a new parameterization of D(H(2)O) that facilitates describing the stability of aqueous food and pharmaceutical formulations in the glassy state, the processing of amorphous aerosol particles in spray-drying technology, and the suppression of heterogeneous chemical reactions in glassy atmospheric aerosol particles.
我们展示了对单个微米级水合蔗糖颗粒水吸收和释放的测量。实验是在电动力学天平中进行的,在那里,颗粒可以在温度和湿度可控的腔室中无接触储存数天。水合蔗糖颗粒会通过从气相中吸收/解吸水来响应环境湿度的变化。这种水吸收(解吸)导致液滴尺寸增加(减小)和溶质浓度降低(增加)。我们采用光学技术来跟踪液滴尺寸的微小变化,其灵敏度为 0.2nm,这是由于温度或湿度的变化。我们将几个颗粒暴露在相对湿度循环(2%至 90%之间)下,温度为 291K,或在温度为 203 至 291K 的长时间(长达数天)内处于恒定相对湿度和温度条件下。这样,我们观察到在低相对湿度和/或低温下,水的吸收和释放会延迟。在研究的条件下,水分子的液相扩散完全控制了这种水吸收/解吸过程的动力学。因此,通过用液相扩散模型模拟颗粒的生长或收缩,可以从这些数据中推导出水分子的扩散系数 D(H(2)O)。在温度低至 203K 的玻璃态深处,使用数据确定的 D(H(2)O)值低至 10(-24)m(2)s(-1)。从实验和建模中,我们可以推断出单个颗粒内存在强烈的浓度梯度,包括颗粒外壳的玻璃化层。这种玻璃化层实质上将颗粒的液相核心与周围的气相隔离,导致这种颗粒的平衡时间非常长,这是由于浓度与 D(H(2)O)之间的强非线性关系所致。我们提出了一种新的 D(H(2)O)参数化方案,有助于描述水合食品和药物制剂在玻璃态下的稳定性、喷雾干燥技术中无定形气溶胶颗粒的处理以及抑制玻璃态大气气溶胶颗粒中的多相化学反应。