Soil respiration in an apple orchard

Abstract

To investigate why the largest CO 2 concentration occurred before sunrise at 0.6 m below an apple tree canopy, seasonal and diurnal fluctuations in soil and grass respiration were recorded in an apple orchard near Bonn, Germany between May 1994 and April 1995 with a portable, battery-driven infrared gas analyser and a soil respiration chamber. Respiration from soil on raised nursery beds with fresh organic matter was compared with herbicide treated, flat soil in tree rows and the grass between the rows to study the contribution of soil and grass respiration to the CO 2 balance of a fruit orchard. The following results were found. 1. 1. Soil and grass respiration ranged from 0.18 to 24 μmol CO 2 m 2− s −1. 2. 2. On cold winter days, with soil temperatures below 0°C, soil and grass respiration during the day remained below 0.6 μmol CO 2 m −2 s −1 and had the smallest diurnal variation. 3. 3. The largest diurnal variations were in late spring with diurnal temperature differences of 15°C, resulting in respiratory values between 3 in the morning and 5–8 μmol CO 2 m −2 s −1 in the afternoon. 4. 4. Soil and grass respiration (up to 40 kg CO 2 ha −1 hr −1) exceeded the CO 2 exchange of the apple trees per unit surface area, contributed significantly to the CO 2 flux in a fruit orchard, and were a pertinent source of CO 2 for tree photosynthesis. 5. 5. The temperature coefficient, Q 10, ranged from 4 below 0°C, to 2.3 above 0°C, 1.7 above 10°C and 1.3 above 20°C.