Soil–plant–atmosphere ammonia exchange associated with calluna vulgaris and deschampsia flexuosa

Abstract

Ammonia fluxes and compensation points at atmospheric NH 3 concentrations corresponding to those occurring under natural growth conditions (0–26 nmol NH 3 mol air -1) were measured for canopies of two species native to heathland in N.W. Europe, viz. Calluna vulgaris (L.) Hull and Deschampsia flexuosa (L.) Trin. The NH 3 compensation point in 2 yr-old C. vulgaris plants, in which current year’s shoots had just started growing, was below the detection limit (0.1 nmol mol -1 at 8°C). Fifty days later, when current year’s shoots were elongating and flowers developed, the NH 3 compensation point was approximately 6±2.0 nmol mol -1 at 22°C (0.8±0.3 nmol mol -1 at 8°C). The plants in which the shoot tips had just started growing were characterized by a low N concentration in the shoot dry matter (5.8 mg N g -1 shoot dry weight) and a low photosynthetic CO 2 assimilation compared to the flowering plants in which the average dry matter N concentration in old shoots and woody stems was 7.4 and in new shoots 9.5 mg N g -1 shoot dry weight. Plant-atmosphere NH 3 fluxes in C. vulgaris responded approximately linearly to changes in the atmospheric NH 3 concentration. The maximum net absorption rate at 26 nmol NH 3 mol -1 air was 12 nmol NH 3 m -2 ground surface s -1 (equivalent to 13.3 pmol NH 3 g -1 shoot dry matter s -1). Ammonia absorption in Deschampsia flexuosa plants increased approximately linearly with increasing NH 3 concentrations up to 20 nmol mol -1. The maximum NH 3 absorption was 8.5 nmol m -2 ground surface s -1 (30.4 pmol g -1 shoot dry weight s -1). The NH 3 compensation point at 24°C was 3.0±1.1, and at 31°C 7.5±0.6 nmol mol air -1. These values correspond to a NH 3 compensation point of 0.45±0.15 at 8°C. The soil used for cultivation of C. vulgaris (peat soil with pH 6.9) initially adsorbed NH 3 at a rate which exceeded the absorption by the plant canopy. During a 24 d period following the harvest of the plants soil NH 3 adsorption declined and the soil NH 3 compensation point increased from below the detection limit to 8.0±1.8 nmol NH 3 mol air -1 (22°C). No detectable NH 3 exchange took place between the D. flexuosa soil (sandy soil with pH 6.8) and the atmosphere.