J. Hruska et al., Relationship between Norway spruce status and soil water base cations/aluminum ratios in the Czech Republic, WATER A S P, 130(1-4), 2001, pp. 983-988
There is a concern that soil acidification by acidic deposition, along with
the resulting depletion of the labile pool of nutrient cations (e.g. Ca, M
g) and enhanced leaching of Al from soil may contribute to forest dieback.
The molar ratios of Ca/Al or (Ca+Mg+K)/Al in the soil solution have been wi
dely used as a criterion for risk of tree damage due to acidification. Inte
nsity and quality of the crown and branch structure transformation due to f
ormation of secondary shoots in successive series is a very sensitive indic
ator of long-term tree damage, and the subsequent regenerative processes. S
oil water chemistry and crown structure transformation of Norway spruce wer
e observed at 16 forest plots within the Czech Republic with the following
results: parameters, expressing degradation processes in the crown (defolia
tion of primary structure), regeneration processes (percentage of secondary
shoots) or synthetic stages of crown structure transformation showed high
correlation with soil water (Ca+Mg+K)/Al ratio in organic horizons. No rela
tionships were found for mineral horizons. The correlations between soil wa
ter and crown status parameters were considerably stronger when using the (
Ca+Mg+K)/Al ratio rather than the Ca/Al ratio.