J. Diels et al., Temporal variations in plant delta C-13 values and implications for using the C-13 technique in long-term soil organic matter studies, SOIL BIOL B, 33(9), 2001, pp. 1245-1251
The C-13 natural labeling technique in combination with modeling could pote
ntially be used to analyze SOM changes in long-term experiments involving c
omplex cropping systems such as aeroforestry systems. It requires informati
on on quantity and C-13 abundance of all plant materials entering the soil
throughout the experiment. The occurrence of significant year-to-year chang
es of 6 13C values of the plant inputs may complicate the technique, as it
would require a systematic isotopic analysis of all plant inputs over the e
ntire life span of the experiment. By analyzing crop and tree samples from
different sampling times in a long-term agroforestry experiment under a sub
-humid tropical climate we established that year-to-year variations in plan
t delta C-13 values were of the order of only 0.4-0.6%, i.e. only 3-4% of t
he maximum tracer signal difference between C-3 and C-4 plants (similar to
15 parts per thousand,) Hence plant sampling and isotopic analysis can be l
imited to 2-3 years or even a single representative year in terms of weathe
r. Important and consistent within-year variations were, however, observed
for legume tree prunings (up to 2.4 parts per thousand) and weeds (up to 7
parts per thousand), pointing to the need for frequent sampling within a si
ngle year if such seasonal variation is suspected. Observed delta C-13 valu
es for the weed vegetation revealed a clear shift in weed composition in te
rms of C-3 and C-4 weeds within the season and across treatments, as was co
nfirmed by a visual weed species identification in the field. (C) 2001 Else
vier Science Ltd. All rights reserved.