Barely Significant
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Dynamics of volcanic ash remobilisation by wind through the Patagonian steppe after the eruption of Cordón Caulle, 2011.

Sci Rep · 2017 · PMC5368570 · PMID 28349929

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a clear trendno p-value reported
Approaching the end of the sampling period, a clear trend towards a more homogeneous distribution of the mass flux across the height was consistently observed at all the sampling sites.

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