X-射线岩心扫描系统对海洋沉积物成分测定质量的综合评价和校正
The calibration and quality evaluation of elemental analysis results of marine sediment measured by an X-ray fluorescence core scanner
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摘要: 基于采自东海内陆架泥质区的沉积物岩心,利用X-射线岩心扫描系统对其进行高分辨成分扫描,同时利用台式偏振X射线荧光光谱仪对该岩心进行元素测定,通过对比研究评价了X-射线岩心扫描系统元素扫描分析质量。研究表明:(1)X-射线岩心扫描系统对海洋沉积物元素分析质量可以分为四类,Ⅰ类元素分析结果可信度高、可以直接作为含量对待,Ⅱ类具有重要的参考价值,Ⅲ类具有一定参考价值,而Ⅳ类无参考价值。(2)海洋沉积物的X-射线岩心扫描元素分析受到压实作用的影响,其中钙、铁、钾、钛、硅等5种元素压实效应明显,通过压实校正可以有效消除压实作用造成的元素垂向上的系统波动。(3)对钙、铁、钾、钛、硅等5种元素,X-射线岩心扫描强度与传统的XRF元素含量之间具有良好的线性关系,相关系数在0.47~0.87,可以据此进行扫描强度和元素含量的换算。Abstract: Based on Core C0702 in the East China Sea mud area, an elemental analysis quality was appraised by comparing the results of two analysis methods, which are an X-ray fluorescence core scanner (X-ray core scanner) and an X-ray fluorescence spectrometer (XRF). The results show that: (1) The elements detected by the X-ray core scanner can be divided into four classes. Elements in Class Ⅰ show a high detecting quality, and the intensities of these elemente measured by the X-ray core scanner can be taken as contents directly. The measuring intensities of elements in Class Ⅱ are great significance, and those in Class Ⅲ are small significance. However,the measured intensities of elements in Class Ⅳ are worthless and minor significant. (2) The analysis results of element itensities in marine sediments detected by the X-ray core scanner affected by compaction, especially, Ca,Fe,K,Ti,Si are more vulnerable. A formula for eliminating this effect via calibration is proposed. (3) The measuring results of Ca,Fe,K,Si,Ti detected by the two methods show a good linear relationship (with correlation coefficients of 0.46-0.87), so the element intensities of Ca,Fe,K,Si,Ti detected by the X-ray core scanner could be converted into the chemical content according to the relationship.
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