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Metody wyznaczania rozkładu granulometrycznego gleb mineralnych

100%

Ryzak M. , Bartminski P. , Bieganowski A.

nr 4[175]

Hydrophysical characteristics of selected soils from arctic and temperate zones

100%

Witkowska-Walczak B. , Bartminski P. , Slawinski C.

tom 29

nr 4

Przygotowanie próbek glebowych do pomiaru składu granulometrycznego gleb metodą dyfrakcji laserowej

100%

Bartminski P. , Krusinska A. , Bieganowski A. , Ryzak M.

tom 62

nr 2

Accumulation of heavy metals (Cd, Cr, Cu, Pb, Zn) in soils and grass swards in roads of Lublin city

100%

Plak A. , Bartminski P. , Debicki R. , Bis M.

Polish Journal of Soil Science

2012

tom 45

nr 2

The aim of this study has been to determine the level of contamination of the soils and grass swards abutting the selected busiest traffic routes of Lublin City with heavy metals: Cu, Cd, Cr, Pb, Zn. 36 surface soil samples (0–20 cm) and grass swards (roots and above ground parts) were collected. The goal of the research has been to assess the impact of road traffic on the content of heavy metals and to determine indicators of migration between the soil and the plant based on the enrichment factor. The examined soils were characterized by a high content of heavy metals, on average: Cu 80.14 mg kg⁻¹, Cd 0.97 mg kg⁻¹, Cr 12.80 mg kg⁻¹, Pb 56.89 mg kg⁻¹, Zn 87.31 mg kg⁻¹. Grass swards in the immediate vicinity of the examined roads had the following average content of heavy metals: Cu 46.91 mg kg⁻¹, Cd 1.41 mg kg⁻¹, Cr 16.36 mg kg⁻¹, Pb 15.05 mg kg⁻¹, Zn 129.01 mg kg⁻¹. The accumulation of heavy metals in the experimental soils and plants was varied. The impact of the content of heavy metals designated in the soils on their concentration in the grass swards collected from the busiest traffic routes in Lublin were considered to be significant.

Visible and near-infrared spectroscopy as a tool for soil classification and soil profile description

100%

Debaene G. , Bartminski P. , Niedzwiedzki J. , Miturski T.

2017

tom 50

nr 1

This paper presents preliminary results of the use of visible and near-infrared (VIS -NIR) spectroscopy for soil classification and soil profile examination. Three experiments involving (1) three different soil types (Albic Luvisol, Gleyic Phaeozem, Brunic Arenosol), (2) three artificial micro-plots with similar texture (loamy sand, Gleyic Phaeozem) but different soil organic carbon (SOC) content and (3) a soil profile (Fluvisol) have been investigated using VIS -NIR spectroscopy. Results indicated that VIS -NIR is a promising technique for preliminary soil description and can classify soils according to soil properties (especially SOC ) and horizons. Instead of complex chemical and physical analyses involved in routine soil profile classification, VIS-NIR spectroscopy is suggested as a useful, rapid, and inexpensive tool for soil profile investigation.

Water conductivity of Arctic zone soils (Spitsbergen)

88%

Witkowska-Walczak B. , Slawinski C. , Bartminski P. , Melke J. , Cymerman J.

International Agrophysics

2014

tom 28

nr 4

The water conductivity of arctic zone soils derived in different micro-relief forms was determined. The greatest water conductivity at the 0-5 cm depth for the higher values of water potentials (> -7 kJ m-3) was shown by tundra polygons (Brunic-Turbic Cryosol, Arenic) – 904-0.09 cm day-1, whereas the lowest were exhibited by Turbic Cryosols – 95-0.05 cm day-1. Between -16 and -100 kJ m-3, the water conductivity for tundra polygons rapidly decreased to 0.0001 cm day-1, whereas their decrease for the other forms was much lower and in consequence the values were 0.007, 0.04, and 0.01 cm day-1 for the mud boils (Turbic Cryosol (Siltic, Skeletic)), cell forms (Turbic Cryosol (Siltic, Skeletic)), and sorted circles (Turbic Cryosol (Skeletic)), respectively. In the 10-15 cm layer, the shape of water conducti-vity curves for the higher values of water potentials is nearly the same as for the upper layer. Similarly, the water conductivity is the highest – 0.2 cm day-1 for tundra polygons. For the lower water potentials, the differences in water conductivity increase to the decrease of soil water potential. At the lowest potential the water conductivity is the highest for sorted circles – 0.02 cm day-1 and the lowest in tundra polygons – 0.00002 cm day-1.

Stress or help, how does the grey heron Ardea cinerea L. modify the vegetation structure of the forest foor?

88%

Hryn W. , Czarnecka J. , Kitowski I. , Bartminski P. , Zubel R.

Acta Societatis Botanicorum Poloniae

2019

tom 88

nr 2