ISRR 2018

Do Maize Roots and Shoots Have Different Short-Term Degradability under Field Conditions? A Field Study of 13C Natural Abundance Resolved CO2 Emissions

Hui Xu 1,2 Bart Vandecasteele 2 Steven Sleutel 1
1Department of Environment, Ghent University, Belgium
2Plant Sciences Unit, Flanders Institute for Agricultural, Fisheries and Food Research, Belgium

Field experiments suggested root-derived C contributed more than shoot-derived C in build-up and long-term preservation of SOC, but this was not confirmed in lab-based incubations. The question then emerges as to whether this contradiction is due to the absence of a comparable physical disturbance as introduced in incubation experiments. In this study, a shoot and root exclusion approach and natural-13C labeling technique were applied to confirm and time the differential degradation of maize (zea mays) shoots and roots under field conditions.

A field trial with five treatments and 3 replicates started in fall 2016 in Melle, Belgium on a light-sandy loam textured soil. We compared maize fields where roots were removed as T0, where roots were chopped and incorporated back to the soil as Tmr, or where roots stayed in situ as Tris with C3 crop fields with maize root (TC3r) and shoot (TC3s) incorporation. Soil respiration was estimated based on both LI-8100 automated soil CO2 flux and chamber-based trace gas flux measurements. The maize fraction in soil respiration was calculated from δ13C value of CO2 and monthly decomposed maize-C was estimated by maize-CO2 flux and temperature. The results showed that TC3s displayed a higher CO2 flux than other treatments and most of both maize roots and shoots were decomposed after 12 months.

Higher maize-CO2 emission of TC3s could be caused by more maize-C being incorporated in the soil. In fall 2017, the experiment was repeated. Beside the five treatments, an extra treatment with the same amount of shoot-C as root-C in TC3r was incorporated in the C3 crop field (TC3s’) was included to evaluate the quantity effect of C input. CO2 flux and its δ13C of each treatment was monitored by cavity ring down spectroscopy (CRDS). Currently, soil CO2 flux measurements in the second year are still on-going thus more information will be presented at the ISRR-10 conference.









Powered by Eventact EMS