吉林大学学报(地球科学版) ›› 2019, Vol. 49 ›› Issue (2): 380-393.doi: 10.13278/j.cnki.jjuese.20180055
袁红旗1, 王蕾1, 于英华1, 张冬杰1, 许凤鸣2, 刘海涛3
Yuan Hongqi1, Wang Lei1, Yu Yinghua1, Zhang Dongjie1, Xu Fengming2, Liu Haitao3
摘要: 文章回顾了粒度分析的历史,总结了常用的粒径类型,介绍了粒度标准和目前沉积学中常用的5种粒度分析方法,并对其中的沉降法、场干扰分析法、图像法作了详细的分类说明。此外,对每一种粒度分析方法的适用范围、测定原理以及其存在的优缺点也进行了详细的介绍。其中:直接测量法简单易行,但精度较差;筛析法较为普遍,但只限于松散或弱胶结沉积物,且不能反映颗粒形状;沉降法适用于松散样、弱胶结样和液体样的分析,可对细砂、粉砂或泥等细粒沉积物进行测量;场干扰法主要依据碎屑颗粒的衍射、散射及电压脉冲响应进行,固体样和液体样均可,精度高,适用性广;图像法手段多样,简单直观,操作性强。总体上,未来的几十年内,粒度分析方法仍将是新旧技术并存,多种方法共用的状况。
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