Fig. 2: Partitioning of the dissolved K+ budget into five end-members, i.e. | Nature Communications

Fig. 2: Partitioning of the dissolved K+ budget into five end-members, i.e.

From: K isotopes trace temporal silicate weathering intensity

Fig. 2: Partitioning of the dissolved K+ budget into five end-members, i.e.

evaporites, rain, anthropogenic, carbonates, and silicates. The weathering of silicates dominates the dissolved K+ budget (an annual average of 73.3 ± 6.3%), while another significant contributor is evaporites (25.8 ± 6.3%), whereas the other contributions are negligible. See supplementary text for the calculations.

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