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In 2004, soil properties and the species composition of vascular plants and lichens were studied at five sites in a former zinc and lead mining region (Olkusz region, southern Poland). The sampled sites, four reclaimed by planting trees differed in age (5, 15, 30, 35 years old), and one spontaneously vegetated (100 years old). The sites were similar in soil structure and chemical composition. These were skeletal soils poor in N and P, and rich in Ca, Mg, Zn, Pb and Cd. The 100-year vegetation which has developed there spontaneously is represented by grasslands formed mostly by species of open, dry, warm, calcareous and metalliferous habitats, with a numerous group of lichens. On sites with planted trees, the herb layer plants appeared as the result of spontaneous colonization. In the herb layer of younger sites there were species typical of spontaneously developed grassland. Older sites harbored fewer grassland species but also included shade-tolerant meadow species. Expansion of trees caused the disappearance of species characteristic of metalliferous waste habitats. Though tree planting accelerates the formation of plant cover in post-mining areas, it is not conducive to the maintenance of the specific composition of local plant species. Spontaneous development of local vegetation seems an appropriate way to rehabilitate at least part of post-mining areas with regard to the maintenance of the vegetation typical for the metalliferous soils. Islands of such vegetation increase the biodiversity of degraded areas.
The Niepołomice Forest, a large forest complex typical of Central European lowlands, is located near an urban-industrial agglomeration in southern Poland. During the past 20 years, SO₂ emissions from industry decreased from 75,000 t yr⁻¹ to 6000 t yr⁻¹. Concentration of SO₂ in the air, and pH, SO₄⁻² concentration in bulk precipitation were measured during the last 11 years and compared with data from the 1970s. The spatial distribution of concentrations and deposition of S were calculated on the basis of 30 bulk precipitation samples in 1999-2000. Mean annual concentration of SO₂ in the air was 8.25 μg m⁻³ in 2000, that is 2.5 times lower than during the period 1967-1978. At the beginning of the 1990s the concentration of SO₂ exceeded the critical level for plants during 3% of the days over the year, and at the end of the 1990s only on single days. In 1999 and 2000 the yearly mean concentration of S-SO₄⁻² in bulk precipitation in the Niepołomice Forest was 1.11 mg l⁻¹, ranging between 0.99 and 1.27 mg l⁻¹ in the forest complex. The yearly mean sulphur deposition (S-SO₄⁻²) was 8.1 kg ha⁻¹, varying from 7.3 to 8.9 kg ha⁻¹. The present concentrations and deposition of S-SO₄ were a quarter those of 1974-1978. The spatial distribution of S deposition pointed to the influx of S compounds to the Niepołomice Forest with air masses from the west. The yearly mean pH of atmospheric precipitation was 4.64 (1999-2000), and was steady within the forest complex. In the Niepołomice Forest, atmospheric precipitation was more acid recently than in the 1970s.
Grassland communities of areas with high levels of zinc and lead in the Olkusz region (southern Poland) were studied. They developed spontaneously on mine waste deposited at the beginning of the 20th century. Twenty phytosociological releves in two areas are presented, along with pH and the zinc and lead concentrations in the upper soil layer. The soils were shallow, pH-neutral or slightly alkaline, and with very high heavy metal content (Zn 3.3–10.4%, Pb 0.32–1.66%). The grasslands were generally short and rather dense, and floristically similar to the Armerietum halleri Libbert 1930 association described by many authors from metalliferous areas of Germany; they differed from German ones by the presence of Biscutella laevigata and by the constant and often abundant occurrence of some vascular plants and lichen species (e.g., Rumex thyrsifl orus, Cardaminopsis arenosa, Diploschistes muscorum, Verrucaria muralis). Difficulties in comparing phytosociological materials from various areas are discussed. The paper points to the need to conserve grassland islands in the monotonous, seriously degraded landscape of the area.
Two plant species growing on calamine spoils (vicinity of Olkusz, S. Poland) were examined for their ability to accumulate metals. The plants in these pilot studies were Biscutella laevigata L., a rare plant that occurs in lowlands on zinc-lead mine spoils only in the vicinity of Olkusz, and Plantago lanceolata L. which is a common species in Poland. Concentrations of alkaline metals (Ca, K, Mg) and heavy metals (Cd, Fe, Mn, Pb, Zn) in soil and plants (shoots, roots) from two locations of calamine spoils 100 and 30 years old and control areas were determined. Soils from the mine spoils were alkaline (pH >7.4), with large concentrations of Ca and Mg. Concentrations of Cd, Pb and Zn in soil were up to 224 mg kg-1 3100 mg kg-1 and 78,000 mg kg-1, respectively. The amounts of exchangeable metals (1 M NH4NO3) were up to 9.51 mg kg-1 Cd, < mg kg-1 Pb, and 24.5 mg kg-1 Zn. Concentrations of heavy metals in plants from the calamine spoils and their distribution within plants depended on the species. B. laevigata accumulated heavy metals in roots (Cd) or shoots (Fe, Mn, Zn). P. lanceolata accumulated heavy metals mainly in roots. Maximum concentrations in roots and shoots of B. laevigata were 14.3 mg kg-1 Cd, 111 mg kg-1 Pb and 410 mg kg-1 Zn. P. lanceolata contained up to 65.6 mg kg-1 Cd, 157 mg kg-1 Pb and 2540 mg kg-1 Zn. Our data suggest that both species tend to exclude Cd, and P. lanceolata also Zn, present in large concentrations in the soil.
The post-mining (Zn, Pb) open pit under study (local name “Krążek”) is situated in the Silesian Upland (50°17’N, 19°27’E) in an area abounding in zinc-lead ores. The open pit, 7.5 ha in area and 30 m deep, was designated for reclamation. Reclamation work started in 1999 and consisted in filling the excavation with foreign (nonlocal) material, and planting pine and oak. It was completed in 2002. Studies of the vegetation colonizing the open pit were carried out in 20 permanent plots (25 m²) representing two types of imported soil substrate (sandy, clayey) in the years 2003–2005. They were based on 60 phytosociological relevés made according to Braun-Blanquet’s methods. In the studied open pit, 178 vascular plant species, spontaneously colonizing the newly created substrate, were found. Only 43 species were present in every year of the study. Most frequent were sporadic species (130), occurring in less than 20% of the relevés. The plants of the reclaimed area represented different ecological groups. Species associated with human-transformed sites (e.g. Solidago canadensis, Tussilago farfara) were the most numerous, but their number decreased with time during the study. Species connected with seminatural (meadow) sites (e.g. Achillea millefolium, Daucus carota) and natural (xerothermic and sandy grassland) sites (e.g. Hypericum perforatum, Poa compressa, Corynephorus canescens) were less frequent, but their number increased with time during the study. Six groups of species connected with the soil substrate type (sand – Rumex acetosella, Cardaminopsis arenosa; clay – Ranunculus repens, Medicago lupulina) and the colonization period (2003 – Atriplex patula, Polygonum lapathifolium, Polygonum hydropiper; 2004–2005 – Calamagrostis epigejos, Leontodon hispidus) were distinguished. Species composition changed over the study period. In the clayey plots these changes were more apparent than in the sandy ones. The numbers of species were lower, the diversity indexes slightly lower and the evenness indexes slightly higher in 2003 than in later years (2004–2005). The initial stages of colonization of the open pit were characterized by the presence of mostly nonlocal ruderal species (Melandrium album, Matricaria maritima, Atriplex patula) which originated from the bank of diaspores in the soil brought to the open pit and from seeds introduced during the reclamation work. Local plants contributed little to the colonization process. Ecological restoration methods in areas degraded by mining activity are discussed; the use of local soil material containing the local bank of diasporas and soil microorganism associations is recommended.
The response of Armeria maritima to heavy metals was examined in plants from two populations, one from metalliferous and the other from non-metalliferous soil. Concentrations of metals (Cd, Zn, Pb) were determined in organs of plants growing on 100-year-old calamine spoil (S Poland) and in a "clean" area (central Poland), and in the first generations of those plants grown in hydroponic culture with addition of metals. Large differences between root and green leaf concentrations of metals were found, indicating restriction of transport of metals from roots to aboveground parts in A. maritima, and an exclusion strategy. Even under full availability of metals (hydroponic culture), adult plants effectively limited the flow of metals to their aboveground parts. In A. maritima from calamine populations, part of the metals transported to aboveground plant organs were directed to the oldest leaves. Plants from the "clean" population growing in a non-metalliferous area did not accumulate heavy metals in ageing leaves. It seems that the ability to accumulate metals in withering leaves characterizes plants growing under strong environmental pressure from metal contamination, in which one may expect intensification of metal detoxification processes.
This study investigates the air deposition of heavy metals (past and recent) in Poland using a common bioindicator – moss Pleurozium schreberi. In 2010 moss samples were collected from 320 sites evenly distributed throughout the country; 297 sites coincided with those in which the 1995 survey was carried out. In green parts of mosses, the concentrations of Cd, Cu, Fe, Pb, and Zn were determined. The 2010 data were compared with those from 1995. The moss concentration of most of the studied metals decreased significantly (P<0.05) between the surveyed years: from 0.45 to 0.30 mg Cd·kg-1, from 7.6 to 6.0 mg Cu·kg-1, from 362 to 344 mg Fe·kg-1, and from 18.8 to 4.9 mg Pb·kg-1, taking into account median values. This temporal trend was dependent on region (for some provinces decreases were insignificant). The concentration of Zn did not alter in time; median values of this variable were 42.8 and 47.5 mg·kg-1 in 1995 and 2010, respectively. The spatial patterns of the heavy metal concentrations in mosses were similar in both surveys; southern parts of Poland, industrialized and densely populated, were contaminated more than the rest of the country.
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