S. Saggar et al., PARTITIONING AND TRANSLOCATION OF PHOTOSYNTHETICALLY FIXED C-14 IN GRAZED HILL PASTURES, Biology and fertility of soils, 25(2), 1997, pp. 152-158
Information on carbon (C) flows and transformations in the rhizosphere
is vital for understanding soil organic matter dynamics and modelling
its turnover. We followed the translocation of photosynthetically fix
ed C in three hill pastures that varied in their phosphorus (P) fertil
ity, using a C-14-CO2 pulse-labelling chamber technique. Pasture shoot
, root and soil samples were taken after 4 h, 7 days and 35 days chase
periods to examine the fluxes of C-14 in the pasture plant-root-soil
system. Shoot growth over 35 days amounted to 114, 179 and 182 gm(-2)
at the low (LF), medium (MF) and high (HF) fertility pasture sites, re
spectively. The standing root biomass extracted from the soil did not
differ significantly between sampling periods at any one level of fert
ility, but was significantly different across the three levels of fert
ility (1367, 1763 and 2406 g m(-2) at the LE MF and HF pastures, respe
ctively). The above- and below-ground partitioning of C-14 was found t
o vary with the length of the chase period and fertility. Although mos
t C-14 (74%, 65% and 57% in the LE MF and HF pastures, respectively) w
as in the shoot biomass after 4 h, significant translocation to roots
(23-39%) was also detected. By day 35, about 10% more C-14 was partiti
oned below-ground in the LF pasture compared with the HF pasture. This
is consistent with the hypothesis that, at limiting fertility, pastur
e plants allocate proportionally more resource below-ground for the ac
quisition of nutrients. In the LF site, with an annual assimilated C o
f 7064 kg ha(-1), 2600 kg was respired, 1861 kg remained above-ground
in the shoot and 2451 kg was translocated to roots. In the HF pasture,
of the 17313 kg ha(-1) C assimilated, 7168 kg was respired, 5298 rema
ined in the shoot and 4432 kg was translocated to the roots. This stud
y provides, for the first time, data on the fluxes and quantities of C
partitioned in a grazed pasture. Such data are critical for modelling
C turnover and for constructing C budgets for grazed pasture ecosyste
ms.