M. Hesselsoe et al., Development of nitrification hot-spots around degrading red clover (Trifolium pratense) leaves in soil, BIOL FERT S, 33(3), 2001, pp. 238-245
Litterbags with clover leaves in soil were buried in the field to study the
influence of degrading clover leaves on the development of elevated nitrif
ication activity (hot-spots) in space and time. Potential NH3 oxidation act
ivity indicating the population size of ammonia-oxidizing bacteria was meas
ured in soil samples taken in a zone a few millimetres thick around the lea
ves and in bulk soil. On 3 sampling days during leaf degradation, the poten
tial NH4+ oxidation was significantly higher in leaf-associated soil than i
n bulk soil, the largest difference (factor of 2) occurring 24 days after b
urial. At all sampling occasions, NH4+ oxidation rates followed a normal di
stribution, except for a lognormal distribution in the leaf-associated soil
sampled 24 days after burial when some very active samples (hot-spots) app
eared. In a similar laboratory experiment we examined the effects of soil w
ater on the development of nitrification hot-spots. We observed that the de
velopment of hot-spots did not take place in soil incubated at 60% of water
-holding capacity (WHC), whereas they developed faster when the soil was in
cubated at approximately 100% WHC. It was concluded that soil water in comb
ination with easily degradable organic N were essential parameters for the
development of nitrification hot-spots in this soil.