A transient ATPase was produced when a grassland soil was incubated wi
th glucose (5000 mu g glucose C g(-1) soil) and inorganic N. The activ
ity of this enzyme reached a maximum after about 2 days, declining to
ambient levels by 10 days. Its formation was strongly repressed by the
addition of inorganic phosphate during the incubation with glucose an
d N. This ATPase was surprisingly resistant to denaturation in the tri
chloracetic acid-based reagent we use to extract ATP from soil, althou
gh it had almost completely disappeared 30 s into extraction. In deter
mining ATP in soil with the TCA-based extractant, a spike of ATP is ad
ded to correct for losses of ATP during extraction. These losses can b
e by hydrolysis (enzymatic or chemical) during extraction, by adsorpti
on on the soil colloids and by quenching during measurement of ATP by
the luciferin-luciferase reaction. An ATP spike added at the beginning
of the extraction of a soil recently amended with glucose was much mo
re completely broken down than a spike added 30 s into the extraction.
Presumably the glucose-induced ATPase was active at the beginning of
extraction but almost completely denatured by 30 s. In contrast, the e
xtraction of ATP from the soil microbial biomass did not appear to be
influenced by the ATPase, presumably because this ATP was released dur
ing extraction and was therefore not all present at the start, unlike
spike ATP. Most measurements of soil ATP using TCA-based extractants w
ill not be influenced by this ATPase because it is only active in soil
s that have recently received substrate. However, even in such soils,
valid ATP measurements can be obtained by taking simple precautions -
adding the spike after 30 s or cooling the soil before extraction. Cop
yright (C) 1996 Elsevier Science Ltd