01799naa a2200301 a 450000100080000000500110000800800410001910000150006024500890007526000090016452010200017365000110119365000130120465000210121765000120123865000160125065000070126665000330127365000250130665300060133165300310133765300060136870000170137470000130139170000210140470000160142577300560144115972452000-12-14       2000    bl ---       0--  u    #d1 aSTOYAN, H.  aSpatial heterogeneity of soil respiration and related properties at the plant scale.  c2000  aGeostatistical techniques were used to quantify the scale and degree of soil heterogeneity in 2 m2 plots around 9-year-old poplar trees and within a wheat field. Samples were taken during two years, on an unaligned grid, for analysis of soil respiration, C and N content, available P, gravimetric moisture, pH, nitrification potential, and root biomass. Kriged maps of soil respiration, moisture, and C content showed strong spatial structure associated 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 heterogeneity seen in this study, we conclude that the main causes of soil heterogeneity at this scale (2 m2) are likely to be found at micro scales controlled in part by plant root and plant residue patterns. These must be understood in the evaluation of ecosystem processes.  acarbon  anitrogen  asoil respiration  aCarbono  aNitrogênio  aPh  aPropriedade Físico-Química  aRespiração do Solo  aC  aChemicophysical properties  aN1 aDE-POLLI, H.1 aBOHM, S.1 aROBERTSON, G. P.1 aPAUL, E. A.  tPlant and Soil, Dordrechtgv.222, p. 203-214, 2000.