Biologically active soil organic matter fractions in sustainable cropping systems

Citation
Tc. Willson et al., Biologically active soil organic matter fractions in sustainable cropping systems, APPL SOIL E, 16(1), 2001, pp. 63-76
Citations number
56
Categorie Soggetti
Agriculture/Agronomy
Journal title
APPLIED SOIL ECOLOGY
ISSN journal
09291393 → ACNP
Volume
16
Issue
1
Year of publication
2001
Pages
63 - 76
Database
ISI
SICI code
0929-1393(200101)16:1<63:BASOMF>2.0.ZU;2-B
Abstract
We sampled corn (Zea mays L.), soybean (Glycine max L.), and wheat (Triticu m aestivum L.) rotations, corn monocultures, and plant successional experim ents in Southwest MI over a 2-year period to study the effects of alternati ve management practices on microbial biomass and particulate organic matter (POM) C and N in the top 20 or 25 cm of soil. Microbial biomass was measur ed using the chloroform fumigation, incubation method. POM was defined as t he organic C and N content of primary soil particles in the 53-2000 mum siz e class. Microbial C decreased during a drought in 1994, and was greater in treatments receiving compost rather than inorganic fertilizer in 1995, but was only weakly correlated with N mineralization in aerobic laboratory inc ubations. Microbial biomass accounted for an average of 2.6% of soil C and 4.9% of soil N in all treatments sampled in 1995. Microbial C:N ratio was l ower in July and November (6.0) than in April and September (7.3), and lowe r in successional treatments without tillage (5.2) than in agronomic treatm ents (6.7). Changes in microbial N were large enough to affect short term N availability, but tended to be transitory. POM increased after compost add itions, and was greater in successional plots without tillage than in tille d treatments, but did not increase immediately after the incorporation of p lant residues. POM accounted for 19.7% of C and 14.8% of N in 1995. Its C:N ratio was 20.8 in a never tilled successional treatment and 16.0 in all ot her soils. The C:N ratio was 17.0 on average in the 250-2000 mum size fract ion, compared to 15.5 in the 53-250 mum fraction. There was a strong correl ation between POM and N mineralization in 70- and 150-day aerobic incubatio ns, but there was greater N mineralization per unit POM in April and Novemb er than in September or October in both years of the study. These results s uggest that POM could be used to estimate N mineralization if combined with information about recently deposited plant residues. (C) 2001 Published by Elsevier Science B.V.