Differential effects of reduced versus oxidized N in speciesrich grasslands and heathlands Roland Bobbink Landscape Ecology, Utrecht University & B-WARE Research Centre, Nijmegen OUTLINE OF PRESENTATION • Introduction - impacts of N deposition - reduced versus oxidized N - species-rich grassland & heaths • Effect studies - correlative field studies - waterculture & pot experiments - mesocosm experiments - field addition studies (very rare) • Concluding remarks Overview impacts of N deposition • direct toxicity of gases & aerosols; • accumulation of nitrogen, resulting in changes in productivity and species composition in the long term; • soil-mediated effects of acidification • increased sensitivity to stresses and disturbances (drought, frost, pathogens, herbivores) • THUS: Very complex, many interactions, different timescales Plant species richness and N All vegetation deposition (Sn/Sc) types Species richness ratio 1.00 0.80 0.60 0.40 0.20 0.00 0 5 10 15 Exceedance (g N m -2) (n=44; mostly grasslands & heaths; P<0.01) (Bobbink 2004) Overview impacts of reduced N • membrane dysfunction & cell solute leakage; • dysfunction of cell pH regulation (internal cell acidification); • nutritional imbalance (increased N%; lower cation % by reduced uptake and increased shoot leaching; accumulation N-rich amino-acids); ▬►reduction in plant growth (roots!!) & survival Species-rich grassland (pH 4.5 – 6.5) Species-rich heaths (pH 4.5 - 6.0) Correlative field studies on plant species and soil conditions • 300 vegetation samples with full soil chemistry • acidic grasslands and heaths in the Netherlands (sandy parts); • Almost 90 areas (nature reserves!!) • To avoid pseudo-replication: never more than 2 randomly selected samples per area; • Kleijn et al. (submitted) Ammonium/Nitrate ratio Growth site characteristics of common (blue) and rare (red) species of heaths and acidic grasslands 150 100 50 0 3.9 4.4 4.9 5.4 5.9 pH Kleijn et al (submitted) Water culture & pot experiments pH =4 (De Graaf et al. 1998) Interaction of pH and ammonium Green = shoot Brown = root Van den Berg et al. 2005 (Soil pH 4.3) Dorland 2004 Survival of Succisa with increasing ammonium (Dorland et al. 2003) pH soil 4.3 Mesocosm experiments • Plant – plant interactions included; • Plant – (natural) soil interactions; • Also more “long-term” processes in plants and soil incorporated; • Best experimental alternative for field addition in high N regions. Influence of ammonium:nitrate ratio (2 experiments; 3 grasses; 6 endangered species) Biomass of grasses (Deschampsia & Danthonia) after 2 yrs biomass (g/m2) 200 150 100 50 0 N load 10 10 (4:0) (3:1) Soil pH ca. 6.8 10 10 40 40 (1:1) (1:3) (4:0) (3:1) Ammonium:Nitrate ratio 40 40 (1:1) (1:3) Tomassen et al 1999 Cover of endangered forbs (as % of total) after 2 yrs addition of ammonium or nitrate % rare forbs 75 50 25 0 N load 10 10 10 10 40 40 40 40 (4:0) (3:1) (1:1) (1:3) (4:0) (3:1) (1:1) (1:3) Soil pH ca. 6.8 Ammonium:Nitrate ratio Tomassen et al 1999 Mechanism: full nitrification in grassland or heath soil; Æ hardly any ammonium in soil! (Dorland et al. Potential net NO 3- production (μ mol g-1 dry soil) 2004) 70 a 60 pH 5.5 pH 4.3 50 40 b c cd 30 20 10 0 0-5 cm Control 6-10 cm Control 0-5 cm Acidified 6-10 cm Acidified Influence of ammonium:nitrate ratio (second experiment; 3 grasses; 6 endangered species) pH 4.3; Start 09-01 / end 03-04 Mortality of typical species (Van den Berg et al submitted) Low ammonium / nitrate ratio High ammonium / nitrate ratio Van den Berg et al submitted And now: field addition experiments with both reduced and oxidized N PROBLEM: no DATA at all in grassland or heaths!!!! Rich fen: Addition study of reduced or oxidized N (small scale / large scale exp) Species-rich vegetation, especially brown mosses!! Small-scale addition experiment 4 yrs -2 -1 Bryophyte biomass after 4 years of N addition (5 g N m yr ) Scragh Bog, central Ireland -2 living standing crop (g m ) 300 a 250 200 a a* a ab* 150 b 100 50 * differ significantly at the 10 % level (Paulissen et al in prep) NH4-N NO3-N control Sphagnum NH4-N NO3-N control Scorpidium 0 Small-scale addition experiment 4 yrs Tissue asparagine concentration 350 B µmol g -1 dwt 300 250 AB 200 Scorpidium 150 Sphagnum 100 50 A 0 control nitrate ammonium (Paulissen et al in prep) Cover of Phanerogams (afer 4 yrs) (5 g N m-2 jr-1) 100 b 80 ab a 60 40 20 0 Control Alpha = 0.10 NO3-N NH4-N N content rich fen Ireland (3 yrs) New 5-10 yr experiment dominant sedge brown mosses 25 mg N / g DW 20 15 10 5 0 control 35NH4 70NH4 35NO3 70NO3 Conclusions: • Toxic impacts of reduced N much larger than those (if any) of oxidized N; • Most sensitive systems (and their endangered plants) have intermediate soil pH (4.5 – 6.5); • Most sensitive plants for reduced N: bryophytes & lichens (full shoot uptake!); • Effects of reduced N mediated by (potential) nitrification rate. • (Long-term) field additions with both reduced and oxidized N highly needed !! (ESF-BEGIN) • Development of critical loads for reduced N and oxidized N separately.
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