Carbon allocation to roots,rhizodeposits and soil after pulse labelling: a comparison of white clover (<Emphasis Type="Italic">Trifolium repens</Emphasis> L.) and perennial ryegrass (<Emphasis Type="Italic">Lolium perenne</Emphasis> L.)

Organically managed farm areas in Denmark are expanding and typically contain clover-grass leys that are known to stimulate accumulation of organic matter in arable soils. We compared the C allocation to roots and soil from clover and grass, and determined for how long assimilated C remained mobile in these plant-soil systems. Pots with perennial ryegrass, white clover or a mixture of both were pulse-labelled with ¹⁴CO₂, and harvested for analyses after 4, 11, 20, and 30 days. ¹⁴C losses by shoot respiration stopped within 4 days and after this incubation time the input of assimilated ¹⁴C to below-ground compartments was greater in grass (52%) than in clover (36%). During the next 4 weeks, ¹⁴C allocation below ground increased in grass (up to 75% at day 30), but remained constant in clover (37% at day 30). In the grass/clover mixture, the below-ground fraction increased to 50% at day 30. In clover, ¹⁴C was incorporated sooner into stable plant and soil pools and less was released in rhizodeposition than in grass. This was confirmed by the ¹⁴C in the soil microbial biomass that decreased fastest in the clover treatment. Root-derived C compounds of clover probably decomposed faster than those from grass. The larger size and specific activity of the soil microbial biomass in the mixed treatment suggested a stimulating effect of the two plant species on substrate utilisation by the microbial community. This study showed that a 2- to 3-week distribution period is needed before sampling for quantitative estimates of C allocation.