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1

Metale ciężkie w środowisku glebowym olkuskiego rejonu eksploatacji rud Zn-Pb

100%
Cabala J.
Prace Naukowe Uniwersytetu Śląskiego w Katowicach
|
2009
|
nr 2729
2

Three morphotypes of chrysophycean stomatocysts from Poland

100%
Cabala J.
Polish Botanical Journal
|
2003
|
tom 48
|
nr 1
3
Artykuł dostępny w postaci pełnego tekstu - kliknij by otworzyć plik
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Chrysophycean stomatocysts from Morskie Oko and Zabie Oko Lakes in the Tatra National Park, Poland

100%
Cabala J.
Acta Societatis Botanicorum Poloniae
|
2005
|
tom 74
|
nr 4
Sixteen chrysophycean stomatocysts are reported from the lakes Morskie Oko and Żabie Oko in the Tatra National Park, Poland. Of these, six morphotypes are new to Poland, and two morphotypes plus one forma are new to science. These stomatocysts are illustrated with SEM micrographs and described according to International Statospore Working Group (ISWG) guidelines. The comparison of stomatocyst community between Morskie Oko and Żabie Oko lakes is given.
4

Chrysophyceae stomatocysts from Budzyn peat bog [Krakow-Czestochowa Upland, Poland]

100%
Cabala J.
Polish Botanical Journal
|
2002
|
tom 47
|
nr 1
5

Active mode of tectonic deformation of Silesian-Cracovian Zn-Pb ore mine area

100%
Cabala J.
Prace Naukowe Uniwersytetu Śląskiego w Katowicach
|
1996
|
nr 1602
6
Artykuł dostępny w postaci pełnego tekstu - kliknij by otworzyć plik
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Some interesting colourless euglenophytes found in Southern Poland

100%
Cabala J.
Acta Societatis Botanicorum Poloniae
|
2003
|
tom 72
|
nr 3
This study present 9 species of colourless euglenoid flagellates found in a small peat bog in Budzyń, a village north-west of Cracow, which belongs to the Małopolska Upland (Southern Poland). This threatened peat bog is covered with rubble brought from neighbouring Cracow. Only ca 30% of its area is relatively little influenced by human activity. Many of the present species are rarely and infrequently reported from nature. Three species, including Rhabdomonas incurva Fresenius, Entosiphon obliąuum Klebs, E. ovatum Stokes, and one variety Menoidium pellucidum Perty var. gracile (Playfair) Popova have been recorded for the first time from Poland. Three species Astasia dangeardii Lemmermann var. dangeardii, Rhabdomonas costata (Korsikov) Pringsheim and Entosiphon sulcatum (Dujardin) Stein var. sulcatum Stein are new for the flora of Cracow-Częstochowa Upland. The remaining taxa: Menoidium pellucidum Perty var. pellucidum and M. tortuosum (Stokes) Senn var. tortuosum are very rarely recorded from Poland. For each species illustrations, taxonomic information and biogeographical data are given.
7

Charakterystyka slasko-krakowskich zloz cynku i olowiu oraz perspektywy eksploatacji tych rud

63%
Cabala J., Konstantynowicz E.
Prace Naukowe Uniwersytetu Śląskiego w Katowicach
|
1999
|
nr 1809
76-98
8

On the occurrence of Sistotrema confluens [Stereales] in Poland

63%
Piatek M., Cabala J.
Acta Mycologica
|
2002
|
tom 37
|
nr 1-2
9
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Flagelloscypha minutissima [Basidiomycetes], a new for Poland minute cyphellaceous fungus

63%
Piatek M., Cabala J.
Acta Societatis Botanicorum Poloniae
|
2004
|
tom 73
|
nr 4
The first records of Flagelloscypha minutissima (Burt) Donk are reported from Poland, being easternmost on the European continent. A brief description and illustration of the species based on Polish specimens are given and its ecology, distribution, and taxonomy are surveyed.
10

Cyanophyta and algae as an important component of biological crust from the Pustynia Bledowska Desert [Poland]

63%
Cabala J., Rahmonov O.
Polish Botanical Journal
|
2004
|
tom 49
|
nr 1
11

Mineralogical alterations of Zn-Pb flotation wastes of Mississippi Valley-Type ores (southern Poland) and their impact on contamination of rainwater runoff

51%
Bauerek A., Cabala J., Smieja-Krol B.
Polish Journal of Environmental Studies
|
2009
|
tom 18
|
nr 5
Research was carried out on the slopes of a tailings pond built from carbonate wastes, rich in metal flotation wastes of Mississipi Valley-Type Zn-Pb ores in the Silesia-Kraków ore district (southern Poland). These wastes, resulting from Zn-Pb ore processing, may have a detrimental impact on the environment. This study presents results of chemical (ICP, IC, AAS) and mineralogical (XRD, SEM-EDS) characterizations of material from the superficial waste layer, water runoff and relocated suspension. They indicate the occurrence of several secondary mineral phases (Fe oxide, Zn and Pb carbonate, and sulfate-containing metals), resulting from the weathering processes of primary Fe, Zn, and Pb sulfides. Results of XRD and SEM examinations point to the increase of sulfate mineral content in the top layer of wastes compared to the wastes in depth. Rainwater runoff (RWR) on the slopes of tailings is characterised by the prevalence of calcium and sulfate, as well as the presence of metals such as Zn, Fe, Mn, Sr and Cd. Metals and sulfates migration in RWR is one of the ways of contaminants’ spreading around Zn-Pb processing mine tailings.
12

Geochemical and geophysical study of historical Zn-Pb ore processing waste dump areas [southern Poland]

51%
Cabala J., Zogala B., Dubiel R.
Polish Journal of Environmental Studies
|
2008
|
tom 17
|
nr 5
693-700
This paper presents the results of mineralogical, geochemical and geophysical studies of Zn-Pb processing waste dump stored at the turn of the 19th and 20th centuries. The mineral composition of wastes was identified using the XRD method, the contents of Zn, Pb, Fe, Mn, Cd, and Tl were determined using the AAS method, whereas the characteristic features of metalliferous grains were examined using the ESEM method. High geochemical mobility of these metals reduces plant succession and brings about the pollution of the former Zn-Pb ores mine areas. High contents of Zn-Pb-Fe sulfides and unstable, hydrated Pb, Fe, Pb-Fe sulfates result in distinctly raised levels of heavy metals (Zn 121,501 mg kg⁻¹, Pb 208,869 mg kg⁻¹, Cd 477 mg kg⁻¹). Various waste types and surrounding Triassic or Quaternary deposits differ significantly in mineral composition, and consequently in physical properties such as electrical conductivity of top soil horizons. This enabled using geoelectric methods for the purpose of this study, and contouring mine wastes in the polluted areas. The field geophysical survey was carried out with a high-resolution conductivity meter (Geonics EM31-MK2).
13

Heavy metals (Zn, Pb, Cd, Tl) rich phases on roots of early-succession plants growing on the wastes from historical Zn-Pb mining and processing (Southern Poland)

51%
Rozek D., Cabala J., Rahmonov O.
Acta Biologica Cracoviensia. Series Botanica. Supplement
|
2014
|
tom 56
|
nr 2
14

Zagrozone stanowisko Cyperus flavescens [Cyperaceae] pod Krakowem

51%
Cabala J., Paul W., Piatek M.
Fragmenta Floristica et Geobotanica Polonica
|
2004
|
tom 11
|
nr 2
410-412
15

Mineral composition in rhizosphere of plants grown in the vicinity of a Zn-Pb ore flotation tailings pond. Preliminary study

45%
Cabala J., Teper E., Teper L., Malkowski E., Rostanski A.
Acta Biologica Cracoviensia. Series Botanica
|
2004
|
tom 46
65-74
Mineral forms in rhizosphere and bulk substrate were examined for selected plant species (Cardaminopsis arenosa, Calamagrostis epigeios, Deschampsia caespitosa, Festuca ovina, Silene vulgaris, Viola tricolor) growing spontaneously in the close vicinity of a tailings pond and in a zone of eolian transmission of waste particles. Samples of substrates and plant roots were taken from sites in the Bolesław orefield near Olkusz. The substrates together with plant roots were studied by scanning electron microscopy coupled with energy dispersive spectroscopy. Apart from quartz and carbonates, the most frequent mineral phases found were crystalline and amorphous Fe oxides, as well as primary Fe, Zn and Pb sulphides (marcasite, pyrite, sphalerite, galena). Hydrated Ca, Mg and Fe sulphates (gypsum, epsomite and melanterite) and other secondary minerals (smithsonite, cerussite, otavite, and Fe, K and Mg aluminosilicates) were found at larger concentrations in the rhizosphere than in bulk soil, suggesting that plant roots can change the mineral composition of the soil.
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