2021
DOI: 10.1016/j.talanta.2021.122785
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Comparison of single pulse, multiple dosage, and 2D oversampling / deconvolution LA-ICPMS strategies for mapping of (ultra)low-concentration samples

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Cited by 8 publications
(11 citation statements)
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“…Both the orthogonal and hexagonal grids can be contracted to yield a smooth post-ablation surface for all crater profiles ( n (□) and n (○) in the range 2–20) with a normalized average depth of one, although more contraction is necessary for lower super-Gaussian orders. Smooth, deeper ablation layers are associated with overlapping craters and may be responsible for blurring in LA–ICP–MS image maps . Nevertheless, for the orthogonal grid (Figure A), 2D overlapping of square spots still yields smooth depth layers at a normalized depth of approximately four for all crater profiles n (□), whereas deeper, smooth layers can only be generated at extreme overlapping of ablation craters with super-Gaussian orders less than 10.…”
Section: Resultsmentioning
confidence: 99%
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“…Both the orthogonal and hexagonal grids can be contracted to yield a smooth post-ablation surface for all crater profiles ( n (□) and n (○) in the range 2–20) with a normalized average depth of one, although more contraction is necessary for lower super-Gaussian orders. Smooth, deeper ablation layers are associated with overlapping craters and may be responsible for blurring in LA–ICP–MS image maps . Nevertheless, for the orthogonal grid (Figure A), 2D overlapping of square spots still yields smooth depth layers at a normalized depth of approximately four for all crater profiles n (□), whereas deeper, smooth layers can only be generated at extreme overlapping of ablation craters with super-Gaussian orders less than 10.…”
Section: Resultsmentioning
confidence: 99%
“…Smooth, deeper ablation layers are associated with overlapping craters and may be responsible for blurring in LA−ICP−MS image maps. 8 Nevertheless, for the orthogonal grid (Figure 4A), 2D overlapping of square spots still yields smooth depth layers at a normalized depth of approximately four for all crater profiles n(□), whereas deeper, smooth layers can only be generated at extreme overlapping of ablation craters with super-Gaussian orders less than 10. For the hexagonal grid (Figure 4B), the overall post-ablation surface smoothness seems less affected by pinpoint accuracy in the selection of the contraction parameters, as can be seen from the much broader purple regions compared to the orthogonal grid, and the fact that the overall depth range is narrower, as visible from the limited color range.…”
Section: ■ Results and Discussionmentioning
confidence: 99%
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