Whilst these relationships are not statistically significant ( R 2 = 0.4149, p = 0.0657 and R 2 = 0.3809, p = 0.0508, respectively; figure 5 ) they provide an interesting trend, and the data are complicated by lack of seasonal catchment records, which is likely to be causing the lack of a significant relationship.
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Silicon isotopes in Arctic and sub-Arctic glacial meltwaters: the role of subglacial weathering in the silicon cycle.
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