X-射线荧光光谱法定量分析海山富钴结壳中MnO2与MnO的含量之比值
Quantitative analysis on ratio of MnO2 content to MnO one in cobalt-rich manganese crusts on seamounts by X-ray fluorescence spectrometer
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摘要: 通过普通X-射线荧光光谱仪,结合PeakFit谱峰处理软件,对不同比例的MnO和MnO2的混合样品的Kβ谱峰参数进行了研究,用数学方法将实测的谱峰分解为各个单一的谱峰参数(峰位、峰高、半高宽、子峰面积),找出了各个谱峰参数与不同价态锰的含量之间的关系,并据此确定了中太平洋海山区大量富钴结壳样品中不同价态锰的相对含量.分析结果显示,富钴结壳中+4价锰从核心向外有增高的趋势,可以认为这与该区第三纪以来南极底流活动的增强有关.
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关键词:
- X-射线荧光光谱 /
- MnO2与MnO的含量之比值 /
- 富钴结壳 /
- 南极底流
Abstract: The spectral peak parameters of mixed samples with different ratios of MnO content to MnO2 one were analysed by X-ray fluorescence spectrometer and processing software Peak Fit.Various single spectral peak parameters such as peak position,peak intensity and full width at half marimal were obtained by deconvolution of over lapped spectral peaks.The relationship between the peak parameters and the ratio of MnO2 content to MnO one was determined.According to the refation,the ratio of MnO2 content of MnO one in a number of cobalt-rich manganese crusts from the central Pacific seamounts was quantitatively calculated.The results show that MnO2 content in cobalt-rich manganese crusts increases from the core outwards.It is believed that this tendency has been related to the enhancing activity of Antarctic Bottom Water in this area since Tertiary. -
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