Richards Simon D, Leighton Timothy G, Brown Niven R
Marine & Acoustics Centre, QinetiQ, Winfrith Technology Centre, Dorchester Dorset DT2 8XJ, United Kingdom.
J Acoust Soc Am. 2003 Oct;114(4 Pt 1):1841-50. doi: 10.1121/1.1610449.
Knowledge of the particle size distribution is required in order to predict ultrasonic absorption in polydisperse particulate suspensions. This paper shows that the method used to measure the particle size distribution can lead to important differences in the predicted absorption. A reverberation technique developed for measuring ultrasonic absorption by suspended particles is used to measure the absorption in suspensions of nonspherical particles. Two types of particulates are studied: (i) kaolin (china clay) particles which are platelike in form; and (ii) calcium carbonate particles which are more granular. Results are compared to theoretical predictions of visco-inertial absorption by suspensions of spherical particles. The particle size distributions, which are required for these predictions, are measured by laser diffraction, gravitational sedimentation and centrifugal sedimentation, all of which assume spherical particles. For a given sample, each sizing technique yields a different size distribution, leading to differences in the predicted absorption. The particle size distributions obtained by gravitational and centrifugal sedimentation are reinterpreted to yield a representative size distribution of oblate spheroids, and predictions for absorption by these spheroids are compared with the measurements. Good agreement between theory and measurement for the flat kaolin particles is obtained, demonstrating that these particles can be adequately represented by oblate spheroids.
为了预测多分散颗粒悬浮液中的超声吸收,需要了解颗粒尺寸分布。本文表明,用于测量颗粒尺寸分布的方法可能会导致预测吸收出现重大差异。一种为测量悬浮颗粒的超声吸收而开发的混响技术被用于测量非球形颗粒悬浮液中的吸收。研究了两种类型的颗粒:(i)呈片状的高岭土(瓷土)颗粒;(ii)更呈颗粒状的碳酸钙颗粒。将结果与球形颗粒悬浮液的粘弹性吸收理论预测进行比较。这些预测所需的颗粒尺寸分布通过激光衍射、重力沉降和离心沉降来测量,所有这些方法都假定颗粒为球形。对于给定的样品,每种尺寸测量技术都会产生不同的尺寸分布,从而导致预测吸收的差异。对通过重力沉降和离心沉降获得的颗粒尺寸分布进行重新解释,以得出扁球体的代表性尺寸分布,并将这些扁球体的吸收预测与测量结果进行比较。对于扁平的高岭土颗粒,理论与测量结果取得了良好的一致性,表明这些颗粒可以用扁球体充分表示。