| Popis: |
Soil pore structure exerts a profound influence on distribution of moisture, O 2 and micro-organisms, thereby potentially controlling organic matter (OM) decomposition in soils. Although pore space is the habitat for soil micro-organisms and the actual location of soil biochemical processes, to date, very few studies looked into this relation mainly because of practical constraints. New experimental designs need to be developed which allow specific investigations of the relation between soil pore network structure, the microbial community and OM decomposition. We therefore subjected a sandy loam soil to a number of artificial manipulations namely i) compaction, ii) artificial change in particle size distribution, iii) addition of different substrates and iv) change in soil pH to manipulate soil pore structure and the decomposer community for use in lab incubation set-ups. Moisture retention data showed that compaction and artificial change in particle size distribution decreased volumes of large (9–300 μm) and small ( |
Full Text from ScienceDirect