Work Package 2: Impacts, Recovery and Processes Task 7: Whim Moss Nitrogen Manipulation Experiment and Open-Top-Chamber Flux Work Dr Lucy J Sheppard, Dr Ian D Leith, Dr Alan Crossley, Matt Jones Centre for Ecology and Hydrology, Edinburgh 51 52 Whim Moss: N Manipulation of a blanket bog ecosystem Dr Lucy J Sheppard, Dr Ian D Leith, Dr Alan Crossley, Matt Jones 1 Summary 1.1 Whim Moss • Effects of ammonia gas (NH3) on N sensitive plant species are more damaging than those of NH4+ or NO3- ions in precipitation. It is probable that intermittent high concentrations, concealed by measurements of long-term average (monthly) NH3 concentrations, are responsible. • Effects of enhanced NH3 concentrations are species specific, implying a need to screen potentially sensitive species to identify the number of NH3 exposure hours they can withstand at different concentrations and also to determine if threshold concentrations exist. • NH3 sensitive species: The lichen, Cladonia portentosa, was the most sensitive to high NH3 concentration. NH3 flux chamber studies also indicated high deposition rates to this species, reflecting the large potential uptake surface. Calluna and Sphagnum have also shown reduced cover and damage in the field, especially when the water table was low. Interactions between N and stress greatly increase the potential for damage. Favoured species: Crossleaved heath, Erica tetralix is expanding its cover. Erica appears to control NH3 uptake better than Calluna. Insensitive species: The dead leaves of cotton grass, (Eriophorum) may absorb some of the NH3, providing protection for the new leaves. So far, we have not observed invasion by nitrophilous grasses, as reported in studies on the dry heaths. • N concentrations in Sphagnum capitula (heads) showed a memory effect of previous N exposure. Damaged Sphagnum appears not to be able to accumulate N, as membrane integrity appears to be impaired by exposure to NH3 concentrations > 40 µg m-3. Capitulum N concentrations at Whim Moss, with a low N exposure history, were still almost 100% higher under the NH3 treatment than those reported by Lamers et al. (2000) for a European survey. • The N exposure history was apparent from the N content of the youngest pleurocarpous moss shoots, ie. each year of N treatment raised the N content, implying re-translocation of N. N concentrations in these mosses could provide useful indicators of past N pollution climates, once they have been calibrated. • The N content of ericoid foliage (Calluna or Erica) is less well coupled to N deposition than moss foliage, especially that of the pleurocarpous moss Hypnum jutlandicum. In this moss, N concentrations increased in proportion to the N deposition received over time in both wet and dry treatments. • No differential effects of oxidised versus reduced N were observed in the wet plots, except in the pleurocarpous mosses which took up more NH4+, despite accumulated inputs of ~170 kg N ha-1 over and above ambient N. This could 53 reflect the more realistic application frequency, the washing effect of natural precipitation and the relatively low concentrations of the applied ions, ≤ 4 mol m-3, which represents 2-3 times cloud water and 10-15 times rainfall concentrations at a high (600 m) altitude site in Eastern Scotland. However, the measured increases in foliar N imply the likelihood of detrimental change in the future. 1.2 RECOVERY in open-top chamber experiments following N cessation • No regrowth was observed from existing Calluna plants affected by N deposition > 16 kg N ha-1 y-1, because of the accelerated ageing effect. However, there was some evidence of new Calluna propagules at higher N inputs. • Previous NH3-N exposure appeared to impair reproduction or the viability of Calluna seedlings since almost none were observed. Low doses, up to 32 kg N ha-1 y-1, of wet deposited NH4-N did not affect propagation, enabling the potential for some recovery of Calluna cover. • Moss colonisation, following the cessation of N treatment, was generally independent of previous N treatment, except where the treatment had influenced the extent of the ‘open’ areas or where there had been colonisation by more aggressive competitors for light. • The acrocarpous moss, Dicranum scoparium, a ‘new’ species appears to be an aggressive and strong coloniser and insensitive to previous N deposition history. • A history of high NH3-N deposition encouraged invasion by nitrophilous grasses. 1.3 Flux chamber studies • Canopy resistance to NH3 deposition depends on the species of bog plant, but several species behave in a similar way. Resistance changes with respect to NH3 concentration, leading to potential over or under estimation of N deposition if simple models are used. • In the mosses Sphagnum and Hypnum (without stomata), canopy resistance does not increase with increasing NH3, so these species form a strong sink for NH3, making them potentially vulnerable to direct toxicity. These results corroborate the findings from the Whim Moss field N manipulation study. • Canopy resistances change diurnally in species with stomata. During the day, resistance to NH3 deposition decreases, because stomata are open enabling more NH3 to be absorbed. 54 • Surface wetness has important implications for NH3 deposition. Wet surfaces have a lower canopy resistance to NH3, which can result in increased N deposition. Bog ecosystems should therefore provide a strong NH3 sink and may be more vulnerable than drier ecosystems to NH3 damage. Acid bog ecosystems will also absorb more NH3 because it is an alkaline gas. 2. Policy Relevance The work, undertaken at Whim Moss and in the open-top chambers (OTCs), addresses 5 issues connected with source attribution and damage or recovery: Separation of the different N forms allows: 1. Identification of N sensitive species and traits that can be monitored to conform with the European Habitats Directives. 2. Validation of critical loads (CL) for bogs and evaluation of the role of concentration (Critical Levels). 3. Evaluation of the potential of N impacts on wetlands (eutrophication or acidification) to affect climate change via effects on C and N sequestration and greenhouse gas emissions (CO2, N2O, CH4). 4. Provision of a demonstration of N impacts on a blanket bog, under near natural exposure conditions, and at a site that has a low N history of ambient inputs to identify species at risk and validate the UNECE agreed CL taking into account modifiers i.e. P&K availability and environmental conditions. 5. Examination of the potential for recovery, recolonisation and invasion of bog species in peat monoliths, previously exposed to 5 years of N inputs, in OTCs. 6. Provision of equations to estimate N deposition from NH3 concentration data to individual species and mixtures of bog vegetation and identification of the role of environmental influences on NH3 – N deposition processes based on canopy resistance theory. 2.1 Background Whim Moss (280 m asl) represents the transition between a lowland raised ombrotrophic bog and an upland blanket mire (Calluna vulgaris – Eriophorum vaginatum blanket mire, NVC M19a). The major European resource of these mires with their enormous conservation value is based in the U.K., where < 6% exists in pristine condition (Thompson et al. 1995). There were no field studies, prior to Whim, to evaluate the impacts of N under near natural conditions, where treatment is coupled to wind direction and speed, temperature and rainfall, taking place throughout the year when meteorological conditions permit. Whim is also unique in that the wet N treatment doses span the UK deposition range at 8, 24 and 56 kg N ha-1 yr-1, over and above the background 810 kg N ha-1 yr-1 ambient inputs. The ionic concentrations are below 4 mol m-3 for 95% of the time and most importantly the N deposition history of the site is low so the system should not have started to acclimate. The treatment solutions NaNO3 or NH4Cl, applied in rainfall, increase the average annual precipitation by 10%. The large plots, 13 m2 can accommodate a range of sampling strategies, are widely separated to minimize cross contamination and well replicated, 4 plots per wet treatment. The NH3 fumigation transect simulates emissions downwind of a 100,000 55 bird poultry unit (PPCR 2000), with NH3 concentrations being monitored along the 60 m transect. Recovery from N deposition is being assessed in the OTC’s (Emmett et al. 2004) where 7 bog species (Calluna vulgaris, Molinia caerulea, Deschampsia flexuosa, Eriphorum vaginatum, Potentilla erecta, Narthecium ossifragum and Polytrichum commune planted in 3 m2 acid peat monoliths had been previously treated with NH4Cl or NH3. For 5 years (1999-2003), from April to October, NH4Cl was applied thrice weekly at 4, 12, 20, 32, 68 and 132 kg N ha-1 yr-1 or gaseous NH3 continuously at ambient (1.5), 6, 20, 45 and 90 µg m-3. Treatment stopped in October 2002 and since then the chambers have been exposed to ambient rainfall and gases. The Calluna was cut back to ground level in January 2004. Resistances to NH3 deposition to bog species are being quantified using a purpose built flux chamber for gas phase NH3, so that comparisons can be drawn with wet N deposition. Approximately 2.5 m2 of bog vegetation mixtures or monocultures have been exposed to varying NH3 concentrations to provide improved estimates of surface resistances. 3 Project Update Whim Moss: Initially the emphasis of the project was to establish a site where impacts of reactive N on a blanket bog ecosystem under near natural conditions could be demonstrated to stakeholders. A range of potentially N sensitive species including the lichen Cladonia portentosa, pleurocarpous mosses Hypnum jutlandicum and Pleurozium schreberi along with Sphagnum capillifolium, grasses including Eriophorum spp, and ericoids (Erica tetralix, Calluna vulgaris, Vaccinium oxycoccus, V. myrtillus and Empetrum nigrum) have been monitored. A comprehensive set of pre-treatment foliar N, P and Mg values were collected together with plot pH. Meteorological parameters, including water-table depth, rainfall, temperature, net and solar radiation are measured continuously together with ambient and treatment N inputs (Sheppard et al. 2004; Leith et al. 2004). Photographic records have been kept of changes to healthy and damaged species. Monthly biochemical and physiological changes were monitored over the second and third treatment seasons in the key species C. vulgaris and S. capillifolium (Carfrae 2005). The site was also used to test the specificity of different biomarkers (Leith et al. 2005). Under this project changes in species cover based on permanent quadrats (3 x 0.25m2) per wet plot and 3 per position along the ammonia transect have been assessed, biannually for the wet plots and annually for the transect, 160 in total. The N status of 4 moss or lichen species and Calluna has been measured and this summer the extent to which the added N has moved down the vegetation/peat profile will be examined. Measurements are underway to validate the N saturation concept (Aber et al. 1989) for blanket bogs. Lamers et al. (2000) predicts that once the N status of the Sphagnum exceeds 1.2%, its natural filtering effect will fail and N will start to leak from the system. We have already exceeded these values near the NH3 source, so we will be following N concentrations in interstitial water in and below Sphagnum clumps using mini-Rhizon soil solution samplers together with trace gas efflux measurements. In addition we will look at the processing of N below-ground by 56 assessing enchytraeid worm mass and their predators, microbial activity and N mineralization potential. OTC Recovery: In April 2005, before the start of the second growing season with no additional N treatment, the open-top chamber monoliths (Emmett et al. 2004) were assessed for species cover and recruitment. Ammonia flux Analysis Studies are continuing, and the significances of environmental variables, diurnal cycle, temperature and surface wetness for NH3-N deposition have been evaluated. 4 Collaboration Data for extension of the MAGIC model. The scale of the Whim Moss experiment and the heterogeneity of such sites with respect to topography and repeating mosaics of vegetation preclude the sampling of all treatment plots for chemical data. Likewise the different layers of vegetation, litter and necromass mean that any sampling for modelling purposes must be targeted after preliminary investigations. Such preliminary studies are underway to identify where to sample, i.e. depth from the surface etc. Standing biomass has been assessed and key properties of the peat (pH, loss on ignition (LOI), CN, available P, exchangeable cations) are being measured. In addition soil water is being collected monthly, 7cm into the peat, for 12 months to characterize the peat soil for acidity, dissolved organic carbon, NO3-, NH4+, K+, Ca2+, Mg2+ and phosphate. These data will be supplied to Chris Evans (WP3). 5 Key Findings 5.1 Nitrate versus ammonium (wet) Species cover: After 2 years of treatment increases or decreases in cover in the different plots were generally small (5-10% maximum), especially when the effects on the control were taken into account (i.e. the effect of the growing conditions at the site). A preliminary analysis suggests only one moss, Hypnum jutlandicum differentiated between reduced and oxidized N, declining under reduced and expanding under oxidised N (Table 1). Table 1 Effects of reduced versus oxidized N on change in cover (after 2 treatment years) and foliar N concentrations, negative effects are shown in bold. Values in the same rows with different letters are significantly different p =0.05. * The data have not been adjusted for effects of environmental conditions as judged from the changes in the cover of the control plots. % cover change* Foliar N* Oxidised Reduced Oxidised Reduced Calluna vulgaris +9 +10 1.26 1.32 Erica tetralix +3 +4 1.17 1.17 Eriophorum vaginatum -2 -2 Cladonia portentosa 0.93 0.99 -4 -3 Hypnum jutlandicum +7 1.47a 1.69b -3 Pleurozium schreberi -7 -4 Sphagnum capillifolium +1 1.48 1.51 -2 57 N status of current year foliage: Hypnum again discriminated between oxidised and reduced, with higher N concentrations under reduced N. Given that oxidised N appeared to stimulate growth, the lower N values in Hypnum receiving NaNO3 may be explained by growth dilution. Visible injury: was only observed on the lichen, Cladonia portentosa in response to N dose/concentration, not N form. Damage has not increased with accumulating N dose. Frost hardiness: Effects of reduced versus oxidised N were dependent on dose and time of year, generalisations are not therefore possible. Conclusion: After 3 years at the maximum N input, 64 kg N ha-1 yr-1, it would appear effects of N form are species dependent and far less important than the effects N dose/concentration. So far only the ubiquitous moss, Hypnum jutlandicum has been negatively affected by reduced N, decreasing its cover and accumulating more N. Sphagnum and Cladonia have not shown detrimental effects of reduced N though, many studies, especially ones that are laboratory based in hydroponics, have found reduced N is more toxic than oxidised N. 5.2 Wet N dose and Critical Loads Species cover: With the exception of the highest N treatment which slightly reduced the cover of both the pleurocarpous mosses, Hypnum and Pleurozium schreberi, no significant changes in species cover due to dose were detected for ericoids, grasses, lichens or Sphagnum after 2 years at 16, 32 or 64 kg N ha-1 yr-1 inputs. Table 2 Concentrations of N (% dwt) in control plots and the percentage enhancement in response to the wet N dose in 2003 (after 60% treatment had been applied and 2005 (after 2 years and ~ 70% of the 3rd years treatment). Apical growing tips or the capitulum were sampled in March. (Values followed by a letter are significantly different (p=0.05) from the control, and differences between treatments are indicated by different letters. # Control 16 32 64 N % dwt % difference % difference % difference 1.36 <1 -2 1 Calluna 2003 1.16 9 6 17a 2005 0.72 11 14 42a Cladonia 2003 0.93 5 22a 27a Sphagnum 2003 1.10 12a 45b 64c 2005 Hypnum 2003 1.10 12 19a 33a 1.32 3 23b 40c 2005 # note large inter-annual differences up to 20% even though sampling occurred at the same time of year. N status of the youngest foliage: Despite having received less than half of the annual target N dose at the time of sampling, significant effects on foliar N concentrations were recorded in the first year (Table 2) for Cladonia, Sphagnum and Hypnum but not Calluna. The largest changes were measured in Cladonia (> 40% enhancement at 64 kg N). By 2005, Sphagnum, Hypnum and Cladonia were showing significant enhancement also in the 32 kg N treatment. The N concentrations in young Calluna 58 shoots were by contrast much less sensitive. N concentrations in Sphagnum above 1.2% exceed the level proposed by Lamers et al. (2000) to indicate N saturation. However, there is no evidence, so far, to suggest that Sphagnum is being adversely affected by these high N doses. Rather, it is possible that when the N deposition is spread throughout the year, when NH4+ and NO3- concentrations are relatively low (≤ 4 mol m-3) and background N inputs are low, Sphagnum is more N tolerant than suggested by the Dutch model (Lamers et al. 2000). P & K additions markedly affected foliar N concentrations in the ericoids, with much smaller effects on the mosses, which were more responsive to N alone. N responses between the ericoids were quite different. In the absence of P & K foliar N in Calluna barely increased with NO3-, with a slightly bigger NH4+ response, whereas in Erica foliar N went down. P & K supplied with N however, increased N in both species, but especially in Erica. 5.3 Dry N dose and Critical Levels Effects along the NH3 transect have been very pronounced. The mat forming lichen Cladonia portentosa was very sensitive to the high average NH3 concentrations, 80100 µg NH3 m-3 measured 2-8 m from the NH3 source (Sheppard et al. 2003). Visible injury and eventual death have now (April 2005) been recorded up to 44 m from the source, indicating the rapid spread of damage with exposure duration (average >9 µg NH3 m-3). Although the accumulated doses in the wet N plots now match some of those along the NH3 transect, where the Cladonia have died, no such death or even worsening damage has been seen in these wet N plots. Therefore, it appears that the fatal damage reflects critical levels of NH3 under the type of NH3 scenarios described by Van der Eerden (1991). Other vulnerable species include Calluna and Sphagnum capillifolium (Fig. 1). The cover of Erica tetralix, by contrast, has increased. Sphagnum capillifolium varies in colour reflecting different amounts of carotenoids. The very red variant, with more carotenoids, was less sensitive to NH3. Hypnum jutlandicum was also sensitive to NH3, but only when conditions were hot and dry. The warm wet summer of 2003 brought about its recovery although, as found in the wet NH4-N treatments, cover declined within 12 m of the NH3 source (Fig.1). Uptake of NH3-N by Hypnum, indicated by % N dwt, was correlated (R2 = 0.85) with the mean annual NH3 exposure concentration, with uptake increasing exponentially at higher concentrations. The relationship was less good for Sphagnum and results suggest potential loss of N, caused by membrane damage at higher NH3 concentrations, likewise for Cladonia. Foliar K concentrations were much lower near the source, supporting the likelihood of detrimental effects of NH3 on membrane integrity. N interactions with stress: The differential sensitivities of Calluna and Erica to NH3-N were investigated with respect to cold (Calluna) and desiccation stress (both). NH3 exposure reduced frost tolerance in Calluna, however, the level of tolerance achieved even in NH3 treated shoots was adequate for normal winter protection. NH3 exposed Calluna, was more susceptible to winter desiccation than Erica. Drying curves indicated Calluna closed its stomata at lower water contents than Erica making it more vulnerable to drying out and potentially taking up more NH3. Fungal (Botrytis) damage was also observed in Calluna, but not in Erica, with damage strongly dependent on the level of NH3-N exposure and being absent from the wet 59 plots. Analyses of foliar N status, N and chlorophyll content all indicate that N uptake is greater in Calluna, which may reflect the effect of NH3 on stomatal control in Calluna. Thus the expansion of Erica under conditions of high NH3 seems likely to reflect its lower uptake of NH3 and potentially better stomatal control. Plants with lower N contents are less susceptible to pests and pathogens. Table 4 N dose kg N ha-1 yr-1 required to raise foliar N content by 0.1% (1mg g-1 dwt), calculated by regression of foliar N versus treatment N dose. Values in bold indicate that the slope of the linear response was statistically significant (p < 0.05). Probability values for estimated responses are shown for all relationships below. Treatment NaNO3 NH4Cl NH3 P values NaNO3 NH4Cl NH3 One year Three years One year Three years One year Three years Sphagnum capillifolium 9.2 13.5 10.9 11.2 13.0 13.1 Hypnum jutlandicum 9.5 7.3 10.5 8.4 15.8 17.0 1 3 1 3 1 3 0.32 0.035* 0.12 0.15 0.22 0.16 0.10* 0.26 0.08* 0.04* 0.04* 0.11 Cladonia portentosa 8.7 8.1 6.7 8.4 10.6 9.1 0.93 0.25 0.04* 0.13 0.80 0.32 Analysis of the relationships between N deposition and foliar N concentrations (Table 3) suggests that N uptake from NH3 is generally less than from wet applied NH4+ or NO3- . This observation contrasts with those from the former OTC study and flags a problem when trying to extrapolate from controlled pollutant exposures to the field. The OTC study involved continuous exposure to constant NH3 concentrations. At Whim Moss, as in situations downwind of agricultural sources, exposure to NH3 occurs at most 14 % of the time, and usually ≈ 5%. NH3 concentrations during exposure are very much higher than average time integrated measurements. The calculated NH3 deposition, even using concentration – dependent surface resistances, does not allow for the possibility of emission of NH3 immediately after exposure to high concentration periods (Sutton 1993) and therefore may overestimate net N deposition in situations with intermittent exposures to high NH3 concentrations. 60 120 pre treat year 1 year 2 120 NH3 µg m-3 pre treat 25 20 0 0 NH 3 µg m-3 m -3 80 % co ver NH3 µg % co ver 40 5 100 20 60 10 NH3 µg m-3 25 80 Killed in years 2 and 3 so absent up to 44 m 15 year 2 Green Calluna vulgaris Live Cladonia portentosa 20 year 1 30 100 60 15 40 10 64 m 32 m 16 m 12 m 8m 6m 4m 2m 20 5 0 1m 0 64 m 32 m 16 m distance from ammonia source 12 m 8m 6m 4m 2m 1m distance from ammonia source 120 120 year 1 35 year 2 NH3 µg m-3 Dead Hypnum jutlandicum year 2 NH3 µg m-3 100 Green Erica tetralix -3 ver 3 NH3 40 60 8 NH 60 15 80 10 -3 80 % co ver Pre-treatment no dead Hypnum 20 % co year 1 12 30 25 pre treat 14 100 6 40 4 10 20 5 0 0 0 64 m 32 m 16 m 12 m 8m 6m 4m 2m 20 2 1m 0 64 m 32 m 16 m distance from ammonia source 120 pre treat 35 year 1 year 2 12 m 8m 6m 4m 2m 1m distance from ammonia source 30 120 NH3 µg m-3 pre treat Sphagnum capillifolium 100 25 80 20 60 100 -3 80 60 40 10 40 20 5 20 0 0 NH 3 15 NH 3 15 NH3 µg m-3 % co ver -3 % cov er 20 year 2 Green Eriophorum vaginatum 30 25 year 1 10 5 0 64 m 32 m 16 m 12 m 8m 6m 4m 2m 1m 0 64 m 32 m 16 m 12 m 8m 6m 4m 2m 1m distance from ammonia source distance from ammonia source Figure 1 Cover values (%) for live Cladonia, dead Hypnum, live Sphagnum, dead Calluna, live Erica and Eriophorum at different distances from the ammonia release pipe pre-treatment and after one or two years of treatment. The red dashed line indicates the mean annual NH3 concentration (µg m-3) at the different distances. 5.4 Recovery in OTCs Calluna had already gone from the 90 µg m-3 NH3 treatment, within the treatment period, (Fig. 2). Polytrichum commune too, had disappeared from all treatments early in 1999. The 2005 survey showed it has reappeared, but only in the control treatment. All the other species:D. flexuosa, E. vaginatum, Molinia caerulea, Narthecium ossifragum, Polytrichum commune and Potentilla erecta were present throughout the study period (1999-2003) and except for Calluna are currently to be found in all treatments. Calluna, the dominant species throughout the study period, has regrown in treatments receiving < 32 kg N ha-1 yr-1 or exposed to < 6 µg NH3 m-3 dry N treatments but has failed to re-establish at higher N inputs (Fig. 2d). The Calluna plants in the higher N treatments were structurally older, their stems woodier and with a denser canopy, features of accelerated senescence. Accelerated ageing probably explains the inability of the woodier stems to sprout new shoots, a common consequence of high N. Eriophorum also recovered poorly when wet and dry N inputs exceeded 16 kg N ha-1 yr-1. There was a dramatic increase in the moss, Dicranum scoparium a ‘new’ species, on the exposed peat, especially above 16 kg N ha-1 yr-1 wet, but not dry treatments. Molinia caerulea % cover increased, almost linearly, in response to N dose, wet or dry, with the opening up of the canopy (Fig. 3). 61 Deschampsia likewise appears to be benefiting from the ‘openness’ but only in the dry N treatments. These dramatic differences in cover, contrasting between Calluna, grasses and Dicranum colonization in the control and highest N chambers are illustrated in Figure 3a, c & d. A total of 16 new species were recorded in the wet and dry N treatments (Table 4). Sedges preferred the higher dry N treatments while the mosses favoured the lower dry N treatments and were more sporadic in the wet N deposition treatments. Table 4 ‘New’ species recorded in the wet and dry N deposition treatments. Coloured square indicates species presence. Colonising species Wet N deposition (kg N ha-1 y-1) 8 32 64 128 Grasses, Sedges & Rushes Agrostis tenuis Carex nigra Eriophorum angustifolium Holcus lanatus Luzula multiflora Mosses Aulacomnium palustre Dicranum scoparium Hylocomium splendens Hypnum jutlandicum Pleurozium schreberi Rytidiadelphus squarrous Spagnum capillifolium Sphagnum papillosum Vascular plants Epilobium palustre Erica tetralix Sagina procumbens Vaccinium myrtillus . 62 Dry N deposition (µg m-3) Control 6 21 45 90 a) Control plot April 2005 b) Pre-harvest dry N treatment (90 ug NH3 m-3) Sept. 2003 c) Dry N treatment (90 ug NH3 m-3) April 2005 d) Wet N dep. treatment (132 kg N ha-1 yr-1) April 2005 Figure 2. Photographs of N treatment plots in the N deposition study prior to harvest in 2003 ( b) and after two years non N treatment. Young Calluna vulgaris Dicranum scoparium Eriophorum vaginatum Molinia caerulea 50 Young Calluna vulgaris 60 % cover (May 2005) % Cover (May 2005) 40 70 30 20 10 Dicranum scoparium Eriophorum vaginatum 50 Molinia caerulea 40 30 20 10 0 0 0 0 20 40 60 80 100 120 140 -1 160 20 40 60 80 100 120 140 -1 160 -1 Previous dry N deposition treatments (kg N ha y ) -1 Previous wet N deposition treatments (kg N ha y ) Figure 3. % cover for 4 species in the wet and dry N treatments after 2 years recovery in the absence of additional N 63 5.5 Refining Cuticular Resistance to NH3 A single cuticular resistance value was found to be inadequate to explain deposition to different bog species because of differences in characteristics such as surface area, presence of stomata, and surface wetness properties. 6 References Aber J.D., Nadelhoffer K.J., Steudler P., Melillo J.M. 1989. Nitrogen saturation in northern forest ecosystems. Bioscience 39: 378-386. Carfrae J.A. 2005. The influence of reactive nitrogen on the ecophysiology of ombrotrophic bryophytes and Calluna. PhD Thesis, Dundee University. Lamers L.P.M., Bobbink R. and Roelofs J.G.M. 2000. Natural nitrogen filter fails in polluted raised bogs. Global Change Biology 6, 583-586. Leith I.D., Sheppard L.D., Fowler D., Cape J.N., Jones M., Crossley A., Hargreaves K.J., Tang Y. S., Theobald M. and Sutton M.R. 2004. Quantifying Dry NH3 deposition to an ombrotrophic bog from an automated NH3 field release system. Water, Air and Soil Pollution: Focus 4: 207-218. PPCR. 2000. New permit application form for pig and poultry installations. Sheppard L. J., Crossley A., Leith I.D., Hargreaves K.J., Carfrae J.A., van Dijk N., Cape J.N., Sleep D., Fowler D., and Raven J.A. 2004. An automated wet deposition system to compare the effects of reduced and oxidised N on ombrotrophic bog species: practical considerations. Water, Air and Soil Pollution: Focus 4: 197-205. Sheppard, L.J., Leith, I.D. and Crossley, A. 2004. Responses of Cladonia portentosa growing on an ombrotrophic bog, Whim Moss, to a range of atmospheric ammonia concentrations. Lichens in a changing environment. Eds Lamberley P. and Wolsey P. English Nature Research Report 525, 84-89. Van der Eerden L.J.M, Dueck T.A., Berdowski J.J.M., Greven H., van Dobbe H.F. 1991. Influence of NH3 and (NH4 )2SO2 on heathland vegetation. Acta Botania Neerlandica 40, 281-297. Sutton M.A., Pitcairn C.E.R., Fowler D. 1993. The exchange of ammonia between the atmosphere and plant communities In: Begon M., Fitter A.H. (Eds.), Advances in Ecological Research, 24. Academic Press, London, New York, 301-393. 64
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