Buck E C, Dietz N L, Bates J K
Chemical Technology Division, Argonne National Laboratory, Illinois 60439-4837, USA.
Microsc Res Tech. 1995 Jun 1;31(2):174-81. doi: 10.1002/jemt.1070310208.
Uranium-contaminated soils from the U.S. Department of Energy (DOE) Fernald Site, Ohio, have been examined by a combination of backscattered electron imaging (BSE) and analytical electron microscopy with electron diffraction (AEM). The inhomogeneous distribution of particulate uranium phases in the soil required the development of a method for using ultramicrotomy to prepare transmission electron microscopy (TEM) thin sections from the SEM mounts. A water-miscible resin was selected that allowed comparison between SEM and TEM images, permitting representative sampling of the soil. Uranium was found in iron oxides, silicates (soddyite), phosphates (autunites), and uraninite (UO2 + x). No uranium was detected in association with phyllosilicates in the soil.
美国能源部(DOE)位于俄亥俄州的弗纳尔德场址受铀污染的土壤,已通过背散射电子成像(BSE)与带电子衍射的分析电子显微镜(AEM)相结合的方法进行了检测。土壤中颗粒状铀相的分布不均匀,因此需要开发一种方法,利用超薄切片技术从扫描电子显微镜(SEM)载物台上制备透射电子显微镜(TEM)薄片。选择了一种与水混溶的树脂,以便能够比较SEM和TEM图像,从而对土壤进行代表性取样。在铁氧化物、硅酸盐(硅钙铀矿)、磷酸盐(钙铀云母)和晶质铀矿(UO2 + x)中发现了铀。在土壤中未检测到与层状硅酸盐相关的铀。