My Account: Log In | Join | Renew
Search
Author
Title
Vol.
Issue
Year
1st Page

Abstract

 

This article in SSSAJ

  1. Vol. 63 No. 5, p. 1385-1396
     
    Received: Aug 21, 1998
    Published: Sept, 1999


    * Corresponding author(s): rochettep@em.agr.ca
 View
 Download
 Alerts
 Permissions
 Share

doi:10.2136/sssaj1999.6351385x

Maize Residue Decomposition Measurement Using Soil Surface Carbon Dioxide Fluxes and Natural Abundance of Carbon-13

  1. Philippe Rochette *a,
  2. Denis A. Angersa and
  3. Lawrence B. Flanagana
  1.  aDep. of Biological Sciences, Univ. of Lethbridge, 4401 University Dr., Lethbridge, AB, Canada, T1K 3M4

Abstract

The decomposition rate of crop residues in soils directly impacts organic matter content and nutrient cycling. We hypothesized that natural abundance 13C analyses could be used with soil CO2 flux measurements to quantify the short-term decomposition rates of maize (Zea mays L.) residues under undisturbed field conditions. For this purpose, maize was grown in a sandy loam (Umbric Dystrochrept) that developed under C3 vegetation. Residues were returned to the field at the end of the growing season. During the following snowfree period (May to November), the maize residue decomposition rate was calculated for plots that were either under no-till or moldboard plowed, using the C isotope ratio (13C/12C) of the soil CO2, the C isotope ratio of the plant and soil substrates, and the soil respiration rate. The incorporation of residue-derived C into the soil microbial biomass was also evaluated. Maize residue decomposition increased the C isotope ratio of the soil CO2 by 2 to 7‰ relative to unamended control plots. Decomposition rates peaked in June (2–3 g C m−2 d−1) and were low at both the beginning and end of the growing season (<0.5 g C m−2 d−1). For a given soil temperature, the decomposition was more active early than late in the season because of decreased substrate availability as decomposition proceeded. The decomposition rate of maize-derived C correlated with the fraction of the microbial biomass derived from maize residues. This active pool represented 9% of microbial biomass and showed a high level of specific activity. The total maize residue-C losses during the study corresponded with 35% of the added residue C under no-till plots and 40% with moldboard plowing. Natural abundance 13C analyses may be successfully used with respiration measurements to quantify crop residue decomposition rates under undisturbed field conditions.

  Please view the pdf by using the Full Text (PDF) link under 'View' to the left.

Copyright © 1999. Soil Science SocietySoil Science Society of America