Extraction of soils by leaching 20 g in 50 ml of unbuffered 1 M NH4NO3 for
2 h has become the standard German protocol (DIN 19730) to estimate mobile
and potentially hazardous forms of trace elements. This protocol was examin
ed using soil controls of chernozem and podzol character collected in the C
anadian Prairies and Ontario. It was found that this procedure was not robu
st with respect to change in sample weight per unit volume of reagent or to
contact time. A 3- to 15-fold increase in Cd extracted was produced by dec
reasing sample weight from 10 g to 1 g in 50 mi of reagent. This change in
extractable-Cd was more pronounced with increasing pH of the soil, ranging
from 5.2 to 8.1 amongst the control samples. Leach period was less signific
ant in determining results but longer time (1-3 h) generally produced lower
extractable-Cd, suggesting readsorption. Lack of stability of Cd in this r
eagent was further demonstrated by spiking experiments where Cd was added a
t the beginning of the leach. Recoveries of Cd at 50 and 200 ppb were below
20% for soils of pH 6.1 and 6.9. Such severe adsorption of Cd was not enco
untered with another unbuffered reagent, 1 M NH4Cl, operating at a similar
initial pH of 5. Cadmium levels extracted from soils by NH4Cl and 0.1 M Na4
P2O7 were comparable and could be used to predict uptake in durum wheat on
the Canadian Prairies, whereas data by the 1 M NH4NO3 leach were generally
near the detection limit of 0.1 ppb (ng g(-1)) Cd. Readsorption of Cd and l
ack of equilibrium in the 1 M NH4NO3 extraction could lead to underestimati
on of plant-available Cd in neutral and alkaline soils. (C) 1998 Elsevier S
cience B.V. All rights reserved.