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. 2022 Feb 2;158(1):39–72. doi: 10.1007/s10533-021-00884-7

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Fig. 11 — Contents of titanium (Ti, index element for chemical weathering intensity) and phosphorus (P) (left axis) and ratio of soil P/bedrock P (right axis) in different soil horizons of Cambisols formed on carbonate bedrock (Mangfall Mts. N1, Bärenthal; upper panels) and silicate bedrock (Bad Brückenau, Conventwald; lower panels). Dashed line indicates 1:1 ratio of soil P to bedrock P