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

Fig. 5.

Fig. 5

Comparison of mineral soil stocks of different Hedley P fractions at temperate beech forest sites with carbonate (left panels) and silicate parent material (right panels; data from Lang et al. (2017). Shown are absolute and relative contributions of different Hedley P fractions in the investigated profiles