The spatial heterogeneity of chemical properties in acid forest soils and its importance for tree nutrition

Abstract

For two sites in the Black Forest, presence, extent and ecological significance of structure-dependent chemical. heterogeneity in the rhizosphere of acid forest soils is discussed. The heterogeneity is demonstrated by two independent methods. First, by comparison of soil solution composition in (quasi-) equilibrium with undisturbed soil cores and sieved soil samples. Water soluble K, Ca and Mg show a selective depletion on aggregate surfaces. Second, by comparison of cumulated amounts of exchangeable ions obtained from percolated homogenized soil samples and undisturbed soil cores. The release of exchangeable K, Ca and Mg is less, if soil structure is not destroyed. The finding that aggregate surfaces are more depleted of exchangeable and water-soluble K, Ca and Mg is common in aggregated acid forest soils. As aggregate surfaces bind soil water with low suction, that is where the roots preferentially grow. Consequently, a considerable underestimation of chemical stress in the rhizosphere is possible, if soil structure is destroyed for analysis.