ANAEROBIC DECOMPOSITION AND DENITRIFICATION DURING PLANT DECOMPOSITION IN AN ORGANIC SOIL

Citation
La. Schipper et al., ANAEROBIC DECOMPOSITION AND DENITRIFICATION DURING PLANT DECOMPOSITION IN AN ORGANIC SOIL, Journal of environmental quality, 23(5), 1994, pp. 923-928
Citations number
24
Categorie Soggetti
Environmental Sciences
ISSN journal
00472425
Volume
23
Issue
5
Year of publication
1994
Pages
923 - 928
Database
ISI
SICI code
0047-2425(1994)23:5<923:ADADDP>2.0.ZU;2-B
Abstract
Nitrate concentrations in groundwater have been shown to be reduced du ring passage through riparian soils and a possible mechanism for this reduction is bacterial denitrification. For denitrification to occur t here must be sufficient available C as an energy source. We examined t he competition for organic substrate between microbial processes durin g the anaerobic decomposition of plant matter in a laboratory study. F resh and senescent pine needles (Pinus radiata D. Don) and watercress leaves (Rorippa nasturtium-aquaticum L.Hayek) were added to an organic riparian soil, incubated anaerobically for 90 d and production of CO2 and CH4 measured. At 9-d intervals NO3 and acetylene were added to a replicate and production of CO2, CH4, and N2O was followed. In the abs ence of NO3, watercress produced the most CO2 and CH4 (21% of added C) , followed by fresh pine needles (10%), and senescent pine needles (6% ). First-order rate constants calculated for gaseous C production were 0.033 d-1, 0.0088 d-1, and 0.0071 d-1 for watercress, fresh, and sene scent pine needles, respectively. As plant tissue become increasingly decomposed via fermentation, less N2O and CO2 was produced following N O3 addition, presumably because the remaining plant matter was more re sistant to further degradation. Denitrification and CO2 production in the watercress and fresh pine needle treatments were up to 5 times hig her than that measured in the senescent pine needle treatment. As the same amount of C was added to all treatments, these results suggested that the lability of added C was of greater importance than the quanti ty of C added in regulating microbial response. The response of denitr ifying bacteria to the addition of NO3 was rapid, even after 99 d of i ncubation in the absence of either NO3 or oxygen as an electron accept or. This suggested that denitrifying bacteria could survive and compet e for C in riparian soils where NO3 concentrations fluctuate.