Soil organic matter distribution as influenced by enchytraeid and earthworm activity

Loam and sandy soils, and the earthworm casts produced with C-14-labelled p lant material in both soils, were incubated in airtight glass vessels with and without enchytraeids to evaluate the effects of soil fauna on the distr ibution and fragmentation of organic matter: After 1, 3, and 6 weeks, the a mount of C mineralised was determined in soils and earthworm casts, and the soil was fractionated into particulate organic matter (POM), the most acti ve pool of soil organic matter, after complete physical dispersion in water The percentage weight of fine :Fractions (0-50 mum) was 67.4% in he Loam s oil. Sand (coarse, i.e. :150-2,000 mum and fine 56-150 mum) represented 87. 2% of total weight in sandy soil, while the percentages of C (PC) were 23.2 % in coarse POM (2,000-150 mum) and 11.9% in fine POM (150-50 mum). These p ercentages were higher than those in loam soil, i.e. 3.4% (coarse POM) and 5.4% (fine: POM). The PC in coarse POM (9.50%) and fine POM (16.4%) remaine d higher in casts from sandy soil than in casts from loam soil (4.7% in coa rse and 14.3% in fine: POM). The highest percentages of C-14-labelled leave s were found in fine fractions, 55.9% in casts from loam soil and 48.8% in casts from sandy soil. The C mineralisation of the added plant material was higher in casts from the sandy soil. (20.3%) than from the loam soil (13.5 %). Enchytraeids enhanced C mineralisation in the balk sandy soil, but did not affect the mineralisation of added plant. material in either soil. The main enchytraeid effect was enhancement of the humification process in the bulk sandy soil, the casts from this soil, and the bulk loam soil.