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Journal of Biogeosciences and Forestry published by SISEF
ISSN: 1971-7458
iForest - Biogeosciences and Forestry
vol. 4, pp. 49-60 (Apr 2011)
Copyright © 2011 by the Italian Society of Silviculture and Forest Ecology
doi: 10.3832/ifor0565-004

Collection: IUFRO RG 7.01 2010 - Antalya (Turkey)
“Adaptation of Forest Ecosystems to Air Pollution and Climate Change”
Guest Editors: Elena Paoletti, Yusuf Serengil

Research Articles

Long-term monitoring of air pollution effects on selected forest ecosystems in the Bucegi-Piatra Craiului and Retezat Mountains, southern Carpathians (Romania)

O. Badea (1)Corresponding author, S. Neagu (1-8), A. Bytnerowicz (7), D. Silaghi (1), I. Barbu (1), C. Iacoban (1), F. Popescu (1), M. Andrei (6), E. Preda (6), C. Iacob (1), I. Dumitru (2), H. Iuncu (3), C. Vezeanu (4), V. Huber (5)


In Central Europe, since the late 1980s, levels of industrial pollutants have been considerably declining, but photochemical pollution, especially ozone (O3) and other phytotoxic agents (SO2, NO2, NH3), registered an important increase with damaging effects upon forests. At the same time the climate factors exert a permanent influence, temporal and spatial fluctuant, but determinant upon forest ecosystem status at global, regional and local scale. Simultaneous with photochemical pollution, increasing climate changes stimulated long-term trans- and inter- disciplinary researches on effects of this phenomenon upon forest ecosystems. At large scale level, various long term research/monitoring networks were developed, and the activities focused on specific aspects (e.g., monitoring of climatic and physical-chemical air parameters, taking into account only the pressure, state and impact, not including social and economical component). Socio-economic development depends on appropriate management of natural resources based on ecological processes manifested by productive and supportive capacity. In order to meet these actual requirements, an interdisciplinary consortium focused on the relationship between ecology and social and economical systems was developed, leading to the foundation of Long Term Social and Ecological Research - LTER Europe, of which Romania is an integrated part. Long term social and ecological research areas represents local or regional social and ecological complex, consisting of natural ecosystems, created, controlled or dominated by humans, specially designed and administered locally and/or regionally. These areas provide both the framework for multi- and transdisciplinary research programs and the space where the operational infrastructure, the policies and the adaptive management plans for ensuring social and economic sustainability can be projected, developed, tested and implemented.

The Carpathians are one of Europe’s largest mountain ranges, a unique natural treasure of great beauty and ecological value, and home of several major rivers. They are an important ecological, economic, cultural and living environment in the very heart of Europe, and form the patrimony of many people and countries. This region is an important reservoir for biodiversity, a sanctuary for many unique habitats and Europe’s last refuge of well known large mammals ([13]). The transition to the market economy, increasing possibilities of sustainable development based on the rich natural, environmental, cultural and human resources of the region are in a delicate balance with preserving its natural and cultural heritage for the future generations ([17]). Retezat National Park (Retezat NP), Bucegi Natural Park (Bucegi NP) and Piatra Craiului National Park (Piatra Craiului NP) represent social and ecological complex, are sites of the Long Term Social and Ecological Research [LT(S)ER-Europe], and are of a major national and European importance in specific researches concerning the status, productive capacity and support characterization of social and ecological systems in the context of climate change and air pollution effects.

The general objective of these research and monitoring activities in the Romanian Carpathians Mts is to characterize the air pollution and its potential effects upon forest ecosystems status and biodiversity in two LTER sites (Retezat and Bucegi - Piatra Craiului), in close connection with climate changes. The specific objectives of this paper are: i) to characterize the spatial and temporal distribution of selected air pollutants (O3, NO2 and NH3); ii) to determine precipitation and throughfall acidity and chemical composition in selected forest sites; iii) to evaluate forest health status and biodiversity of forest vegetation; iv) to asses trees and forest stands growth in relation to crown condition.

Study location 

Bucegi - Piatra Craiului and Retezat Mts are located in the Romanian southern Carpathians. Bucegi NP (32.500 ha), Piatra-Craiului NP (13.800 ha) and Retezat NP (38.047 ha) are located in these mountains. In 2003, these areas were nominated as two ILTER Sites and in 2008 as LTER - Europe sites (Bucegi - Piatra Craiului and Retezat, respectively). The diversity and vast richness of Bucegi - Piatra Craiului and Retezat Massifs vegetation, with many endemic species and rich fauna which includes endangered species and unique plant communities like chamois, bear, lynx and wolf ([10]) were the main reasons for the natural and national park status for Bucegi - Piatra Craiului and Retezat Mts, respectively.

Two monitoring networks consisting in 11 (Retezat Mts) and 22 (Bucegi - Piatra Craiului) permanent plots (LTERp) were established in 2000 (Retezat) and 2006-2009 (Bucegi - Piatra Craiului). These plots were located within Bucegi - Piatra Craiului parks and both within and outside Retezat NP boundaries, in forest zone at elevation ranging from 800 to 1800 m (Fig. 1, Fig. 2, Tab. 1, Tab. 2). They were selected by considering the criteria of species composition, age distribution, and potential exposure to trans-boundary pollution. Monitoring plots were located in representative forest ecosystems, well exposed to incoming air masses allowing good measurements of air pollution status and its effects on forest ecosystems ([11]).

Fig. 1 - Permanent plots network in Retezat LTER Site.
Fig. 2 - Permanent plots network in Bucegi - Piatra Craiului LTER Site.
Tab. 1 - Research activities in Retezat LTER Site.
Tab. 2 - Research activities in Bucegi - Piatra Craiului LTER site.


The plot area is 0.7 hectares (Fig. 3). It contains five permanent circular subplots of 500 m2 apiece, in which tree health status, dendrometric characteristics (species, DBH, height, Kraft class, quality, etc.), vegetation and biodiversity were regularly recorded. A number of destructive sampling methods (increment cores, leaves and soil samples) and several measurements of atmospheric deposition and soil solution were completed, but only in the buffer zone. Trees health (crown defoliation) was assessed annually during the study periods (between mid of July to the end of August), although with several gaps in the data series due to different causes. In every evaluation, all the dominant trees (predominant, dominant and codominant) were evaluated in accordance with the UN/ECE & ICP-Forests ([16]). Dendrometric measurements have been made in the year 2000 (Retezat NP), in 2006 (Bucegi NP) and in 2009 (Piatra Craiului NP), according to the methodological manual that was specially developed for long term ecological research ([4]). Biodiversity of trees and herbaceous vegetation was assessed using Braun-Blanquet. Increment cores were taken from 25 to 30 trees located in the buffer zone of each LTERp (Fig. 3), both from trees within defoliation classes 0-1 and 2-4. In cases of mixed stands (Norway spruce, silver fir and European beech), 10-15 increment cores have been taken from each of the main species. The annual volume growth and volume growth losses (due to the action of stress factors) have been determined based on the stands inventory and radial increment data. Information processing was done according to the methodological manual ([4]).

Fig. 3 - Design of long term ecological research plot (LTERp).

Close to the long-term research plot, at the point of local maximum altitude and maximum exposure to air wind direction (E-V) special locations (trees) for exposure of passive filters (2 replicates) for O3, NO2 and NH3 were established ([11]). These measurements were made monthly, during vegetation seasons, and the chemical analysis of the passive filters was carried out in the first years at USDA-Forest Service laboratory, in Riverside, and since 2009 in ICAS laboratory.

Wet and dry deposition (under canopy and in open field) was sampled on a total of 12 plots, of which 6 in Bucegi-Piatra Craiului and 6 in Retezat. In each plot, eight collectors were placed in the buffer zone, on each side of its centers, and on the same level curve ([8]). Monthly, the samples of atmospheric deposition and soil solution were collected and analyzed in the laboratory of ICAS. In addition, sampling methodology and chemical analysis methods were adopted and applied according to the methodological manual ([4]). SPSS software was used for processing the experimental data.

Results and discussions 

Air quality

On Retezat and Bucegi-Piatra Craiului LTER sites, the ozone concentrations were measured during the growing season (15 June -15 October) using passive samplers. In most of the Retezat NP’s research plots, the ambient ozone concentration followed an irregular distribution. At the beginning of summer (15 June - 15 July), the highest seasonal average values were registered (Fig. 4). A second peak, but smaller than the first one, was recorded between mid August and mid September. Exceptions were registered in four sites (OGA, Gura Zlata, Rausor and Judele) where the second peak was recorded at the end of the exposure period (15 September-15 October). Also, an increase of ozone concentration correlated with altitude was noticed both in terms of exposure period and growing season levels (Fig. 5).

Fig. 4 - Spatial and temporal distribution of ozone concentration in 2009 growing season (Retezat NP).
Fig. 5 - Variation of ozone concentration in relation to exposure period and altitude during the 2009 growing season (Retezat NP).

Compared with the results registered in 2000-2002 period ([10]), in 2009 ozone concentrations on altitudinal strata were lower, but slightly higher than in 2002 (Fig. 6). The correlation between this multiannual ozone distributions and altitude was not statistically significant (p > 0.05). The correlation coefficient values (r) vary between 0.469, p > 0.05 (in 2009) and 0.601, p > 0.05 (in 2002). Also, one-way ANOVA shows that location had a significant influence on ozone concentrations (F = 31.25, p = 0.01), while exposure period had no significant influence (F = 0.860, p = 0.470).

Fig. 6 - Distribution of ozone concentration by altitude during the period 2000-2002 and 2009 (Retezat NP). Pearson correlation coefficient between ozone concentration and altitude ranged from r = 0.469, p > 0.05 (in 2009) to r = 0.601, p > 0.05 (in 2002) - no significant correlation.

The ammonia concentrations (NH3) showed the lowest values at the beginning of summer, when they were < 1 μg m-3 (exception - Gura Zlata); maximum values were recorded in midsummer (15 July - 15 August). Towards the end of the season (September - October), and sometimes during it, the majority of ammonia concentrations were around 2 μg m-3, and seldom between 1-2 μg m-3 (Fig. 7).

Fig. 7 - Monthly averages of the ambient NH3 concentrations in 2009 (Retezat NP). One-way ANOVA showed no significant influence of location (p = 0.697) and significant influence of time (p = 1.5E-5).

One-way ANOVA shows that exposure period significantly influenced the ammonia concentrations (F = 11.379, p ≤ 0.05) Location had no significant influence (F = 0.724, p ≥ 0.05 - Fig. 7). The significant influence of exposure period on ammonia concentration confirms the intensity of touristic activities along Retezat NP in different vegetation season periods.

Relative to the 2000-2001 period, in 2009 the mean NH3 concentrations was significantly reduced from 5.92 μg m-3 (2001) to 1.97 μg m-3 (2009). This can be explained by the decreasing human and industrial activities in the area, and by high altitude pollution.

During the year 2009, Bucegi-Piatra Craiului LTER site had a decreasing distribution of ozone concentration, from 46 ppb at the beginning of the summer season (15 June - 15 July) to 29.9 ppb by the end of the growing season (15 September -15 October - Fig. 8 AB).

Fig. 8 - Spatial and temporal distribution of ozone concentration in 2009 growing season in Bucegi NP (left) and in Piatra Craiului NP (right).

In the Piatra Craiului NP the maximum ozone concentration was recorded in mid August until September (35.9 ppb) compared to Bucegi NP when the maximum value (46 ppb) was registered at the beginning of the summer season (15 June-15 July - Fig. 9). In general, for the entire season and for the entire LTER site the average value was 36.3 ppb. The seasonal mean values for each location were between 21.4 ppb (Brusturet) and 39.3 ppb (Coltii Ghimbavului) in Piatra Craiului Mts and between 22.5 ppb (Observator Urs) and 54.6 ppb (Cariera Lespezi) in Bucegi Mts. The average value for the entire season was 32.7 ppb in Piatra Craiului National Park, compared to 39.9 ppb in the Bucegi NP (Fig. 8A and B). It is worth noticing that the variation coefficients of ozone concentration were significantly lower in Piatra Craiului than in Bucegi Mts (s% = 17.4% compared to 23.2%, respectively).

Fig. 9 - Temporal distribution of ozone concentrations in Bucegi NP, Piatra Craiului NP and Bucegi-Piatra Craiului LTER Site. No data were collected in Piatra Craiului Mountains in the 15/06-15/07 period.

In 2009, similar to Retezat LTER site, in Bucegi - Piatra Craiului an increase of ambient ozone concentrations with altitude was noticed (Fig. 10A). The same situation was encountered in Bucegi Mountains during the period 2006-2009 (Fig. 10B).

Fig. 10 - Distribution of ozone concentration by altitude in 2009 - Bucegi - Piatra Craiului LTER Site (A) and during the period 2006-2009 - Bucegi NP (B). Pearson correlation coefficient between ozone concentration and altitude in Bucegi NP is between r = 0.821, p < 0.01 (in 2007) and r = 0.880, p < 0.01 (in 2006 - significant correlation at p = 0.01).

One way ANOVA shows a significant influence of location and exposure periods on ozone concentrations (F = 16.950, p = 0.01 and F = 13.981, p = 0.01, respectively). Overall, during this period (2006 to 2009) the spatial and temporal variation of ozone in the Bucegi Mts was relatively low (s% = 20.6%), denoting increased stability.

Compared with the previous period (2006-2008), in 2009 the seasonal average of ambient ozone concentrations in Bucegi Mts was the lowest at most locations (except Podu cu Flori - Fig. 11). The maximum annual average was registered in 2007, when the temperatures during the growing season were very high (over 35° C), followed by a small decrease in the following years, 2008 and 2009.

Fig. 11 - Distribution of ozone concentration by location during the period 2006-2009 (Bucegi NP).

At these two LTER sites, representing the Southern Romanian Carpathians, the ozone values were in accordance with ranges of annual seasonal means measured in previous periods (1997 to 1999) for the Romanian Carpathians ([10]).

The average ammonia (NH3) concentrations in 2009 were low for most locations in Bucegi Mts (Fig. 12). However, elevated levels were occasionally registered in Poiana Stanii (especially between 15 August and 15 September - 2.64 µg m-3). This spike in NH3 was probably caused by some local emissions from touristic activities, agricultural operations or biological fertilization. One-way ANOVA showed a significant influence of location (F = 4.196, p ≤ 0.01) and no significant influence of time (F = 0.378, p > 0.05) on NH3 concentrations.

Fig. 12 - Fluxes of ions (deposition and soil solution) during the growing season 2009 in Piatra Craiului N P, plot Magura (Fagus sylvatica).

Generally, in 2009 seasonal mean concentrations of NH3 in Piatra Craiului Mts were higher than in Bucegi Mts (2.38 µg m-3 vs 1.36 µg m-3). The averages over the whole LTER site (Bucegi-Piatra Craiului) were below 2.0 µg m-3 (1.8 µg m-3).

During the period 2006-2009, the annual means of NH3 in Bucegi Mts were the lowest in 2007 (1.00 µg m-3). At location level, these values were between 0.66 µg m-3 and 2.46 µg m-3 (in 2006) and between 0.59 µg m-3 and 1.78 µg m-3 (in 2007). Nevertheless, the concentrations were much lower than in Retezat mountains during the period 2000 to 2002 ([10]) and in 2009.

Both in Retezat and Bucegi-Piatra Craiului Mts all of NH3 concentrations were below phytotoxic levels ([9]). In the long term they may contribute to increasing nitrogen deposition ([10]).

Atmospheric deposition

In 2009 growing season, S-SO4 inputs in the open field (bulk deposition) vary from 2 to about 8 kg ha-1. The highest values were measured in Bucegi NP (Poiana Stanii and Podu cu Flori LTERp - Fig. 13, Fig. 14), and the lowest values were found in Piatra Craiului National Park, at Salvamont Bran and Valea Podurilor (Fig. 15).

Fig. 13 - Fluxes of ions (deposition and soil solution) during the growing season 2009 in Bucegi NP, plot Poiana Stanii (Fagus sylvatica).
Fig. 14 - Fluxes of ions (deposition and soil solution) during the growing season 2009 in Bucegi NP, plot Podu cu Flori (Picea abies).
Fig. 15 - Fluxes of ions (deposition) during the growing season 2009 in Piatra Craiului NP, plot Valea Podurilor (Fagus sylvatica and Picea abies mixed stand).

Throughfall input of sulphate varied in relation to bulk deposition, with values from 3 to 6 kg ha-1. In the areas located far from roads and populated places, the fluxes under the canopy were lower than in the open field (Valea Podurilor and Magura, and in Gura Zlata and Judele (Fig. 15, Fig. 16, Fig. 17 and Fig. 18).

Fig. 16 - Fluxes of ions (deposition and soil solution) during the growing season 2009 in Piatra Craiului N P, plot Magura (Fagus sylvatica).
Fig. 17 - Fluxes of ions (deposition and soil solution) during the growing season 2009 in Retezat NP, site Gura Zlata (Fagus sylvatica).
Fig. 18 - Fluxes of ions (deposition) during the growing season 2009 in Retezat NP, site Judele (Picea abies).

As SO4 -2 shows low interaction with plant canopies ([6]), the SO4 enrichment in throughfall shows an accumulation of dry depositions between two rain events ([14]). Low enrichment factors (ratio between fluxes under the canopy and in the open field) indicate that studied areas are less polluted. In 2009 the S-SO4 input increased two times relative to 2000-2002 ([3]).

Nitrogen input was very low and ranged from 0.2 kg ha-1 (Podu cu Flori, Valea Podurilor, Magura, and Gura Zlata) to 3.5 kg ha-1 (Poiana Stanii, located on the slope exposed to the Prahova Valley with high density of traffic). There was a similar pattern between deposition of NO3 and NH4; the range of N-NH4 being much higher than N-NO3 deposition. At different soil depths N-NO3 increased in Campusel and was nearly constant in Magura or decreased in Poiana Stanii; N-NH4 increased in soil and reached a maximum of 4-10 kg ha-1 in Poiana Stanii and Gura Zlata. Throughfall was dominated by N-NH4 mainly on plots located at high altitudes. Bulk precipitation of N-NH4 varied from 0.5 kg ha-1 to 2 - 4 kg ha-1 (Fig. 13, Fig. 15, Fig. 18 and Fig. 19). This input was enhanced by to 2-8 times at Podu cu Flori location by the addition of dry deposition of NH4 like particles or aerosols.

Fig. 19 - Fluxes of ions (deposition) during the growing season 2009 in Retezat NP, site Campusel (Fagus sylvatica and Abies alba mixed stand)

In some sites, throughfall content of NO3 and NH4 was lower than in bulk deposition (Poiana Stanii, Campusel, and Magura) possibly due to direct canopy uptake of NO3 or NH4 ([7]). Sites receiving very low levels of nitrogen in bulk precipitation registered insignificant amounts in throughfall, too ([12]).

Base cations (K+, Mg+2 and Ca+2) fluxes in the growing season showed high amount of K leached from the canopy in all plots; Mg+2 showed low amounts not only in the atmospheric deposition but also in the gravitational water in soils. Ca+2 input was estimated at 5-7 kg ha-1. The throughfall Ca+2 fluxes were not very much modified as compared with those registered in the open field, probably due to reactions with acidic ions. In soil solution, the Ca+2 content was quite high, mainly in the plots located on the soils formed on limestone at Campusel (18-20 kg ha-1). On soil originated from granite parent material (Gura Zlata), the amount of Ca+2 in the gravitational water on the profile decreased from 3 to 2 kg ha-1 in the first 20 cm and increased at 7 kg ha-1 at 40 cm.

In the Bucegi - Piatra Craiului LTER site the monitoring of atmospheric depositions in the period 2006-2008 allows comparisons with the growing season 2009. The input of S-SO4 in open field was variable from 1.1 kg ha-1 (Podu cu Flori) to 3.7 kg ha-1 (Salvamont Bran) and 3.1 kg ha-1 (Poiana Stanii). No visible trend of the main ions was detected, because of the high variability due to variable weather conditions and rainfall regimes.

In comparison with the results obtained at the beginning of the monitoring program in Retezat NP ([3]) the amounts of sulphur in 2009 were similar to those determined in 2000 at Judele and nearly double (4-6 kg ha-1) in Judele, Gura Zlata and Campusel.

Concerning Cl, N-NO3 and N-NH4, no significant changes were observed. Also, the input of the basic cations K, Mg, Ca was higher in 2009 than in 2000.

Using bulk depositions, throughfall and soil water collected in the growing season in these two LTER sites, it was possible to show the influence of the canopy on the mineral ions fluxes.

Forest condition

In 2009, 2385 and 876 trees were assessed in Bucegi - Piatra Craiului LTER-site (20 permanent plots) and Retezat (10 permanent plots), respectively. Several significant differences regarding the damaged trees population (defoliation classes 2-4, crown defoliation > 25%) were registered both among plots and between the two LTER sites (Tab. 3 and Tab. 4). As a result, for all species, the share of damaged trees (defoliation classes 2-4) was much lower in Retezat (12.1%) than in Bucegi - Piatra Craiului (22.5%). The damage intensity was higher in Bucegi NP (28.0%) than in Piatra Craiului NP (17.5% - Tab. 4). Individually, the health status of European beech (Fagus sylvatica) was almost the same in Retezat (8.0%) and in Bucegi - Piatra Craiului (9.8%), but Norway spruce (Picea abies) was healthier in Retezat than in Bucegi - Piatra Craiului (12.9% and 27.7%, respectively - Tab. 5).

Tab. 3 - Trees crown defoliation share for all plots in 2009 (Retezat LTER site).
Tab. 4 - Trees crown defoliation share for all plots in 2009 (Bucegi-Piatra Craiului LTER site).
Tab. 5 - Trees crown defoliation share for the main species in 2009 (Retezat and Bucegi-Piatra Craiului LTER sites). (*): in Retezat LTER site the number of trees assessed was very small (33). The values are not representative.

In Retezat Mts, compared with results in the 2000-2002 period, the crown condition for all species had considerably improved from 16.1% in 2002 to 12.1% in 2009 (Fig. 20). In addition, Norway spruce and European beech showed a better crown condition in 2009 as compared with 2002, with the share of damaged trees (defoliation classes 2-4) decreasing from 17.9% in 2002 to 12.9% in 2009 and from 11.8% in 2002 to 8.0% in 2009.

Fig. 20 - Proportion of damaged trees (group of defoliation classes 2-4) for all species during the period 2000-2002 and 2009 - Retezat NP.

Nevertheless, in 2009, some plots (Campusel Neagu, Rotunda and Baleia Stana) registered over 20% of damaged trees (Tab. 3). This can be explained by canopy cover reducing, ageing factor and extreme environment conditions.

The increased share of damaged trees is explained by: degradation processes of low density and high age (more than 120 years) forest stands: extreme conditions of soil (with surfaced rocks fragments), with average to low productivity; and presence of secondary deciduous species with a very poor crown condition. Even resinous species and Norway spruce especially showed a high rate of damaged trees, because many trees were assessed at the lower limit (crown defoliation 30 - 35%) of defoliation class 2 (moderately affected damaged class). These trees showed very active migration intensity in healthy group classes (defoliation ≤ 25% - [2]). The other stands with a small share of damaged trees were mostly in the early development stages and have a superior stability and vitality.

In Bucegi Mts, compared to the previous period (2006-2008), the share of damaged trees for all species slowly decreased from 33.9% in 2008 to 28.0% in 2009 (Fig. 21). Norway spruce and Silver fir followed the same trend from 31.8% in 2008 to 30.1% in 2009 and from 31.8% in 2008 to 27.7% in 2009, respectively. This improvement, both at individual level and for all species can be explained by the influence of elevated precipitation in previous spring and autumn seasons (2008) and during the growing season 2009. Furthermore, as compared to previous years, in the 2009 vegetation season, the excessive hot weather had a low frequency and occurred for very short periods of time. The influence upon crown condition of trees was not significant.

Fig. 21 - Proportion of damaged trees (group of defoliation classes 2-4) for all species during the period 2006-2009 - Bucegi NP.

Also, in 2009, many trees reported in previous years with a defoliation ratio at the lower limit of moderate class (crown defoliation of 30-35% - class 2) intensively migrated in the healthy trees group class (defoliation ≤ 25%), for European beech especially ([1]).

Based on these considerations, the crown condition of forests improved in the Bucegi NP in 2009.

The ambient ozone (described as seasonal mean concentrations among locations) had no significant influence on forest health status (percent of trees with crown defoliation above 25%) in Retezat and Bucegi Mts (Fig. 22 and Fig. 23). In addition, in Bucegi mountains forests, ozone concentration had no effect on annual volume growth losses (due to action of different stress factors) (Fig. 24). In fact, ozone concentrations in Romanian Carpathians were rather low and below the levels considered to be toxic for Norway spruce and European beech, especially in Retezat ([10]) and Bucegi-Piatra Craiului Mts.

Fig. 22 - The influence of ozone concentrations on percentage of damaged trees (defoliation classes 2 - 4 - Retezat LTER Site). R2 for linear relationship was 0.002 indicating no significant effects of ambient ozone on defoliation.
Fig. 23 - The influence of ozone concentrations on percentage of damaged trees (defoliation classes 2 - 4 - Bucegi-Piatra Craiului LTER Site). R2 for linear relationship was 0.125 indicating no significant effects of ambient ozone on defoliation.
Fig. 24 - The influence of ozone concentration on growth losses (Bucegi NP). R2 for linear relationship was 0.047 indicating no significant effects of ambient ozone on growth losses.

The dynamics of annual average ring width was analyzed both for healthy trees (defoliation classes 0-1) and damaged trees (defoliation classes 2-3) during the entire life of selected trees. The results were relevant for most of the forest stands studied in these two LTER Sites, showing downward increment tendency of damaged trees compared with healthy trees ([10]). This comparative dynamics of annual mean radial increment shows the reference moments for the beginning of declining process of trees which at present are damaged, as an effect of some negative events in the past, like excessive drought, air pollution, pathogens and pests actions, human activities, etc. (Fig. 25 and Fig. 26).

Fig. 25 - Dynamics of annual mean radial increment of Picea abies per defoliation group classes (0-1 and 2-3) in Podul cu Flori permanent plot (Bucegi NP).
Fig. 26 - Dynamics of annual mean radial increment of Fagus sylvatica per defoliation classes (0-1 and 2-3) in Dichiu permanent plot (Bucegi NP).


Retezat and Bucegi-Piatra Craiului Mts are characterized by rich and varied vegetation, protected under special regulations in order to preserve rare and endemic species. Both sites are dominated by forests and alpine meadows, harmoniously embedded in the steep and rocky terrain and home of several glacial lakes and water courses. Across the entire area over 1100 plant species have been identified, of which many are endemic ([15], [5]).

The research on forest vegetation across each LTER site was carried out based on a list of species organized by layers (A-trees, B-shrubs, C-herbaceous plants, D-mosses). The coverage ratio was assessed for each layer using the Braun-Blanquet method, allowing the identification of 6 representative plant communities, in each research site (Tab. 6 and Tab. 7).

Tab. 6 - Vegetation community types in Bucegi NP. (*): in Piatra Craiului National Park there is not yet a complete dataset on biodiversity, since the first assessment was carried out in aestival period of the year 2009.
Tab. 7 - Vegetation community types in Retezat NP.

European beech (Fagus sylvatica) and Norway spruce (Picea abies) are the main tree species in the studied sites, along with silver fir (Abies alba), which seldom is found. Maple (Acer pseudoplatanus), Scots pine (Pinus sylvestris), birch (Betula pendula) and rowan (Sorbus aucuparia) are secondary species.

The identified plant communities are relatively diverse, ranging from pure stands of Norway spruce or European beech to mixed stands of European beech and Norway spruce or silver fir and European beech, and having in their composition other resinous species (larch, pine) and broadleaf species (mountain maple, birch, mountain ash, etc.). The number of plant species varies between 37 and 57 in Bucegi (Tab. 6) and between 11 and 36 in Retezat (Tab. 7). At least in the Retezat LTER site, by comparing the biodiversity parameters assessed in the years 2000 and 2009, there is no confirmation regarding rapid environmental modifications, and furthermore no significant reduction of biodiversity.

In most of the pure or mixed European beech stands (European beech and Norway spruce, European beech and silver fir) there is evidence of superior richness of species compared to the Norway spruce pure stands. In a similar manner, dendrometric parameters of trees fluctuate in relation to stand structure and site type, demonstrating higher diversity in European beech and mixed stands than in Norway spruce pure stands (Tab. 8 and Tab. 9).

Tab. 8 - Dendrometric diversity of trees for representative stand types in Retezat NP.
Tab. 9 - Dendrometric diversity of trees for representative stand types in Bucegi NP.

Diameter diversity, diameter-height relation and age structure patterns reveal spatial variability and the value of ecological potential. Spatial variability is linked with environmental influences, especially with effects of disturbance, including pollution and climate change stressors, biotic interactions and substrate fertility. As a limited conclusion to the extent of the research plots, all the vegetation biodiversity components of the forest ecosystems are specific for the stand type’s structures and climatic conditions, and concerning the air pollution stressor, it seems there are no significant consequences on ecosystems’ biodiversity component.


  1. In general, the air quality in the Retezat and Bucegi - Piatra-Craiului Mts was relative good during the study period.
  2. The ambient ozone concentrations were situated under critical limits. There was no significant influence of ozone levels on tree crown condition and annual volume growth losses assessed on trees with high crown defoliation (damaged trees). The spatial and temporal O3 distribution in the area was stable. Generally location had a significant influence on ozone concentrations whereas the effect of the exposure period during the growing season was evident only in some cases.
  3. Depositions estimated in the soil solution (collected by lysimetric plates) were generally higher than in the open field because of the accumulation of the ions in the soil layers. Along the soil profile the fluxes of the main pollutant ions decreased, while others (e.g., Ca+2) were highly influenced by the soil substrate and soil type. The study validated the use of a long-term integrated monitoring program for the evaluation of the impact of pollutants on forests and assessed the role of the forests in buffering the acidity of the rain.
  4. Forest health status (crown condition) was better in Retezat than in Bucegi or Bucegi - Piatra Craiului region, where air pollution and anthropogenic influence have had a major effect in the close past. These forest ecosystems can be considered as moderately affected. Abies alba and Picea abies were more affected than Fagus sylvatica, which was the healthiest species at national level.
  5. Variation of annual mean radial increment per defoliation group class (0-1 and 2-3) offered very good information on major negative events in the past, like very strong drought, air pollution, windfalls, human activities and inappropriate forest management.
  6. There was no evidence of rapid environmental modifications, and furthermore no significant reduction of biodiversity. In addition, all the vegetation biodiversity components of the forest ecosystems were specific to the types of stand structures and local climate conditions, and concerning the air pollution stressor, it seems there were no quantifiable consequences on ecosystems’ diversity.


The long-term monitoring researches in Retezat and Bucegi - Piatra-Craiului LTER Sites were financed by USDA - Forest Service International Programs (2000-2002) then by the Excellence Program of the Romanian Authority for Research (2005-2008). Researches were conducted under a close and fruitful collaboration between ICAS, USDA - Forest Service, “Transilvania” University, University of Bucharest and National Forest Administration (Romsilva). Since 2009, these long-term monitoring researches continue with the support of Romanian Authority for Research under the GEDEOFOR Program and the LIFE+ Program (EnvEurope project), cofinanced by the European Commission and Romsilva. The scientific activities and main results on long term monitoring research in Retezat and Bucegi-Piatra Craiului LTER sites were presented at the 24th IUFRO Conference for Specialists in Air Pollution and Climate Change Effects on Forest Ecosystems “Adaptation of Forest Ecosystems to Air Pollution and Climate Change” in Antalya and the manuscript was written within the COST Action FP0903 Climate Change and Forest Mitigation and Adaptation in a Polluted Environment.


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