Larson Ben H, Swanson Brian D
Department of Earth and Space Sciences, Box 351310, University of Washington, Seattle, Washington 98195, USA.
J Phys Chem A. 2006 Feb 9;110(5):1907-16. doi: 10.1021/jp054270l.
We have measured the light scattering intensity and homogeneous ice nucleation temperatures from water droplets containing 0-33 wt % ammonium sulfate. In these laboratory experiments, we used a free-fall freezing tube technique to determine the fraction of frozen droplets at a particular droplet temperature by measuring the depolarized light scattering intensity from the droplets in free-fall. Previously reported freezing temperatures for solution concentrations greater than 5 wt % display a larger spread than can be accounted for by the reported experimental errors. We find freezing temperatures in good agreement with the lowest temperature freezing results reported by previous experiments. Our ammonium sulfate freezing temperature data set with water activity less than 0.98 is consistent with a curve that deviates in activity shift by about 5% from the best-fit ice nucleation temperature versus water activity curve found by Koop et al. in 2000, but the significance of this deviation will only be known with further high-precision ice nucleation temperature measurements for other aqueous solutions.
我们测量了含有0 - 33 wt%硫酸铵的水滴的光散射强度和均匀冰核形成温度。在这些实验室实验中,我们使用自由落体冷冻管技术,通过测量自由落体中水滴的去偏振光散射强度,来确定特定水滴温度下的冷冻水滴比例。先前报道的溶液浓度大于5 wt%时的冷冻温度显示出比报道的实验误差所能解释的更大的离散度。我们发现冷冻温度与先前实验报道的最低温度冷冻结果高度一致。我们的硫酸铵冷冻温度数据集,其水活度小于0.98,与一条曲线相符,该曲线在活度偏移方面比库普等人在2000年发现的最佳拟合冰核形成温度与水活度曲线偏离约5%;但只有通过对其他水溶液进行进一步的高精度冰核形成温度测量,才能知晓这种偏差的意义。