Spatial heterogeneity of soil respiration and related properties at the plant scale

Geostatistical techniques were used to quantify the scale and degree of soi l heterogeneity in 2 m(2) plots around 9-year-old poplar trees and within a wheat field. Samples were taken during two years, on an unaligned grid, fo r analysis of soil respiration, C and N content, available P, gravimetric m oisture, pH, nitrification potential, and root biomass. Kriged maps of soil respiration, moisture, and C content showed strong spatial structure assoc iated with poplar trees but not with wheat rows. All soil properties showed higher autocorrelation in June than in April. Isopleth patchiness for all variates was less in June. This was associated with lower respiration rates due to lower litter decomposition. From the degree and scale of heterogene ity seen in this study, we conclude that the main causes of soil heterogene ity at this scale (2 m(2)) are likely to be found at micro scales controlle d in part by plant root and plant residue patterns. These must be understoo d in the evaluation of ecosystem processes.