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School of Engineering and Science - Jacobs University

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Figure 5. Diagram depicting various types <strong>of</strong> precision that may be defined for sample decompositions<br />

<strong>and</strong> ICPMS analyses. Note that sample precision reflects raw uncorrected intensities (cps), while run<br />

<strong>and</strong> method precision are calculated from corrected concentration data.<br />

that <strong>of</strong> the sample precision for many elements, <strong>and</strong> also varies as function <strong>of</strong> rock<br />

type (Fig. 7). Shales display slightly poorer run precision (3-5%), though this might<br />

reflect the limited number <strong>of</strong> analyses where these CRMs were measured repeatedly.<br />

For purposes <strong>of</strong> long term reproducibility, the method precision is the most suitable<br />

measure <strong>of</strong> the st<strong>and</strong>ard deviation expected for a complete sample decomposition <strong>and</strong><br />

ICPMS analyses, as it describes the variability expected in concentration data when a<br />

sample powder is dissolved numerous times over a period <strong>of</strong> months or years.<br />

Comparisons <strong>of</strong> the three types <strong>of</strong> precision discussed here (sample, run, <strong>and</strong> method)<br />

are presented in Figure 8 for CRMs <strong>of</strong> four different rock types. Of the 32 elements<br />

analyzed, the method precision RSD is better than 5% for 25 elements in BHVO-2<br />

(basalt), 31 elements in SGR-1b, 26 elements in FeR-2 (iron-formation), <strong>and</strong> 22<br />

elements in JDo-1 (dolomite). The method precision is also comparable to the sample<br />

<strong>and</strong> run precision, suggesting that any error associated with the HF-HClO 4 sample<br />

decomposition method (e.g., weighing <strong>and</strong>/or dilution errors) is small compared to the<br />

error inherent in the ICPMS analysis.<br />

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