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Heavy isotope analyses in soil sciences: possibilities and challenges

100%

Binczycki T. , Tyszka R. , Weber J.

Polish Journal of Environmental Studies

2014

tom 23

nr 2

In this study we summarize spectroscopic methods used in Pb isotopic analyses as well as show the role of the methods in modern soil science. The study is focused mainly on Pb isotopes due to their wide applications in soil sciences, especially in solving environmental problems. Pb and Sr isotopic composition-based methods are effective when distinguishing a two-source mixture, and comparing with the known signature of a potential pollution source. Advancing analytical methods and more data containing isotopic composition from many natural and anthropogenic sources gives them a much higher possibility of use. This text shows the wide use of spectroscopic methods and their impact on many aspects of environmental science.

Interactive effects of Ni, Cr, Co, Ca, and Mg in seeds germination test: implications for plant growth in ultramafic soils

88%

Pedziwiatr A. , Kierczak J. , Potysz A. , Tyszka R. , Slodczyk E.

nr 5

In situ growth of monazite in anchizonal to epizonal mudrocks: first record from the Variscan accretionary prism of the Kaczawa Mountains, West Sudetes, SW Poland

75%

Kryza R. , Zalasiewicz J. A. , Charnley N. , Milodowski A. E. , Kostylew J. , Tyszka R.

Geologia Sudetica

2004

tom Vol. 36

39-51

We report the first occurrence of diagenetic or low grade metamorphic monazite from the Palaeozoic mudrock successions of the Kaczawa Complex of the West Sudetes, Poland. Where observed in relation to the enclosing mudrock, this monazite comprises tiny irregular grains, less than 20 microns in diameter, intergrown with the surrounding matrix minerals. This monazite resembles previously described examples of diagenetic monazite from elsewhere in the world in mostly possessing low contents of Th and U but differs in forming much smaller grains, which show only slight zonation of rare earth elements (REEs). Some of the monazite grains studied also appear to have formed synchronously with the cleavage, perhaps a function of early deformation and fluid release in an accretionary prism environment. Relatively Th-rich cores, and an association with altered detrital biotite in some instances, suggests that at least some of the in situ monazite growth might have taken place as overgrowths on primary detrital monazite particles.

In situ growth of monazite in anchizonal to epizonal mudrocks: first record from the Variscan accretionary prism of the Kaczawa Mountains, West Sudetes, SW Poland

75%

Kryza R. , Zalasiewicz J. A. , Charnley N. , Milodowski A. E. , Kostylew J. , Tyszka R.

Geologia Sudetica

2004

tom 36

Wplyw wieloletniego stosowania sciekow komunalnych na wybrane wlasciwosci gleb pol irygacyjnych

63%

Licznar M. , Drozd J. , Licznar S. E. , Weber J. , Bekier J. , Tyszka R. , Walenczak K. , Szadorski J. , Pora E.

tom 10

nr 3[31]

129-137