摘要
常规的非铁矿床识别主要通过显微镜下对其物理性质、形貌、共生特征以及它们之间的相关性进行识别,而许多矿床都具有“质同像”的特征。在此基础上,利用X-荧光光谱区对矿石进行现场分析,充分发挥了设备的潜力,提高了设备的利用率;将X射线荧光光谱法用于矿物成分的测定,不仅可以极大提高测定的敏感性,而且能够有效地克服不均匀性,确保测定的准确性。因此,本文以理论实际为依据,通过对X射线荧光光谱法的基本原理及结构构成进行简单介绍,并对其在实际工作中的使用进行了详细的分析,以期对从事矿物检验工作的人员起到借鉴作用。
The conventional identification of non iron deposits mainly relies on the identification of their physical properties,morphology,symbiotic characteristics,and their correlations under a microscope,and many deposits have the characteristic of"isomorphism".On this basis,on-site analysis of the ore was carried out using X-ray fluorescence spectroscopy,fully tapping into the potential of the equipment and improving its utilization rate;Applying X-ray fluorescence spectroscopy to the determination of mineral composition can not only greatly improve the sensitivity of the measurement,but also effectively overcome non-uniformity and ensure the accuracy of the measurement.Therefore,based on theoretical practice,this article provides a brief introduction to the basic principle and structural composition of X-ray fluorescence spectroscopy,and a detailed analysis of its use in practical work,in order to provide reference for personnel engaged in mineral inspection work.
作者
陈振雄
CHEN Zhen-xiong(Yunnan Gold Mining Group Precious Metals Testing Co.,Ltd,Kunming 650000,China)
出处
《世界有色金属》
2024年第2期58-60,共3页
World Nonferrous Metals
关键词
X射线荧光光谱分析法
矿石检测
应用
实践
X-ray fluorescence spectroscopy analysis method
Mineral testing
Application
practice