Jolanta Kwiatkowska-Malina, Anna Bielska and Andrzej Szymon Borkowski
Usowicz B., Marczewski W., Łukowski M.I., Lipiec J., Usowicz J.B., 2011. Assessment of soil moisture from ground measurements and satellite data in ESA SMOS mission, conference materials of the 28 th Congress of the Polish Soil Science Society. Soil-Human-Environment: 5–50 (in Polish).
Usowicz B., Hajnos M., Sokołowska Z., Józefaciuk G., Bowanko G., Kossowski J., 2004. Spatial variability of physical and chemical soil properties at a scale of a field and commune. Acta Agrofizyka, Rozprawy i monografie: 103 pp. (in Polish).
Vasu D., Singh S.K., Sahu N
Organic matter takes part in all soil processes and influences the physical, chemical and biological properties of soil. The paper presents the analysis of heavy metal contents (Zn, Pb, Cd) in soil and biomass of darnel multifloral (Lolium multiflorum Lam.) cultivated at diverse conditions of soil reaction and organic matter content. A brown coal preparation (Rekulter) was applied as the source of organic matter in autumn 1999 to the studied soil, which was contaminated with cadmium, lead and zinc. The limiting influence of Rekulter on the uptake of heavy metals by darnel multifloral (two cuts of the test plant) was the highest in the case when the largest dose was applied to soil with the highest pH (about 6.0). Bioaccumulation indexes (BI) for Cd, Pb, Zn indicate the mobility and bioavailability of Cd, Pb and Zn in soils. The BI for particular heavy metals were generally low, with the lowest in the case when the largest dose of Rekulter was applied to all cuts of the test plant
The subsoil conditions of Surfers Paradise in Southeast Queensland of Australia have been examined in terms of soil stiffness by using geographic information system (GIS). Peat is a highly organic and compressible material. Surfers Paradise (as a study area) has problematic peat layer due to its high water content, high compressibility, and low shear strength. This layer has various thicknesses at different locations ranging between R.L. . 10 to R.L. -19.6 m. Buildings in Surfers Paradise are using piled foundations to avoid the high compressibility and low shear strength peat layer. Spatial Analyst extension in the GIS ArcMap10 has been utilised to develop zonation maps for different depths in the study area. Each depth has been interpolated as a surface to create Standard Penetration Test SPT-N value GIS-based zonation maps for each depth. In addition, 8 interpolation techniques have been examined to evaluate which technique gives better representation for the Standard Penetration Test (SPT) data. Inverse Distance weighing (IDW) method in Spatial Analyst extension gives better representation for the utilised data with certain parameters. Two different cross sections have been performed in the core of the study area to determine the extent and the depth of the peat layer underneath already erected buildings. Physical and engineering properties of the Surfers Paradise peat have been obtained and showed that this peat falls within the category of tropical peat.
Joanna Hydzik-Wiśniewska, Anna Wilk, Łukasz Bednarek and Sebastian OIesiak
method of marking the indicator for material requires to conductit after four days of soaking, which simulates unfavourable conditions of water saturation. Unfortunately, the CBR test method is laborious and time consuming [ 22 ].
This article analyses the geotechnical and physicaltest results with particular consideration of CBR of mixtures of crushed aggregate assessed for their application in road construction as subgrade layer. An attempt was also made to find the correlation between CBR ratio and other physical properties. All aggregate tests were performed at
Omar Mohamed, Ahmed Mansour, Sameh S. Tahoun, Ashraf M. T. Elewa and Muhammad Ali Mekkey
The current study presents a fully qualitative palynological investigation carried out on the Raha Formation encountered from three wells in the Bakr Oil Field of the Gulf of Suez, Egypt. Around 30 species of pteridophytic spores, 26 species of angiosperm pollen, 24 species of gymnosperm pollen and 27 species of dinoflagellate cysts have been recorded. However, achritarchs, microforaminiferal test linings and freshwater algae are impoverished and sparsely documented throughout the Raha Formation. Two palynozones have been identified based on some stratigraphically significant pollen and spores, arranged from youngest to oldest: (1) Palynozone I (Classopollis brasiliensis–Tricolpites sagax Assemblage Zone) of late Cenomanian age; (2) Palynozone II (Afropollis jardinus–Crybelosporites pannuceus Assemblage Zone) of early-middle Cenomanian age. The distribution and ecological affiliation of specific palynomorph species, as well as various palynofacies parameters, are interpreted. A shallow marine environment from supratidal to distal inner neritic under proximal suboxic–anoxic to dysoxic–anoxic shelf conditions is reconstructed. Palaeobiogeographically, the absence of elaters from the recovered taxa is interpreted in terms of minor floral variation. This may be attributed to climatic and/or an environment-controlled niche establishment, which possibly was shaped by the existence of a physical barrier hindering the distribution of such type of elaterate parent plants.
degraded soil by natural and planted fallows udner humic tropical conditions. Soil Science Society of America Journal 64: 222–228.
Trabaquini K., Formaggio A.R., Galvao L.S., 2015. Changes in physical properties of soils with land use time in the Brazilian savanna environment. Land Degradation & Development 26: 397–408.
Vivoni E.R., Rinehart A.J., Méndez-Barroso L.A., et al. 2008. Vegetation controls on soil moisture distribution in the Valles Caldera New Mexico, during the North American Monsoon. Ecohydrology 1: 225–238.
Vliet J., de Groot H
., 2016, Development and implementation of a testing method for the characterization of interlaminar delamination propagation in laminates under fatigue mode I loading conditions, Transactions of the Institute of Aviation, No. 2(243).
 Jaśkiewicz R., Stepniowska A., 2016, Pracitcal application of FAA methodology of composite specimens used to material tests qualifications, Transactions of the Institute of Aviation, No. 3(244).
 Sałacińska A., 2016, Review of physicaltests for composite materials characterization, Transactions of the Institute
Ad Litteram DREAM, 2009. A European project coordinated by the BIA research unit. Newsletter of the INRA Centre ofAn- gers-Nantes, July 2009.
Aghbashlo M., Kianmehr M.H., Khani S., Ghasemi M., 2009. Mathematical modelling of thin-layer drying of carrot. Int. Agrophysics 23: 1-5.
Akinoso R., Raji A.O., 20ll. Physical properties of fruit, nut and kernel of oil palm Int. Agrophysics 25(l): 85-88.
Aladjadjiyan A., 2010. Influence of stationary magnetic field on lentil seeds. Int
Adam Bogacz, Dominika Dzięcioł, Bartłomiej Glina and Leszek Gersztyn
BOGACZ A. 2000. Physical properties of organic soil in Stołowe Mountains National Park (Poland), Suo 51 , 3: 105-113.
BOGACZ A. 2005. Właściwości i stopień przeobrażenia gleb organicznych Sudetów. Zeszyty Naukowe Akademii Rolniczej we Wrocławiu, Rozprawy 512 : 1-150.
BOGACZ A., ROSZKOWICZ M. 2010. Wpływ gospodarki leśnej na właściwości gleb organicznych brzegowej części Krągłego Mokradła (Park Narodowy Gór Stołowych). Rocz. Glebozn. 45 , 2: 17
Monografie 44 .
KWIATKOWSKA J., DĘBSKA B., MACIEJEWSKA A., GONET S. 2005. Brown coal as the factor modifying the properties of soil organic matter. Rocz. Glebozn. 56 , 3/4: 31-41.
KWIATKOWSKA J., SOKOŁOWSKA Z., MACIEJEWSKA A. 2006. Selected physical and chemical properties for evaluating brown coals used for soil reclamation. Int. Agrophysics 20 (2), 121-128.
MACIEJEWSKA A., KWIATKOWSKA J. 2002. Niektóre właściwości chemiczne gleby oraz jej zdolności buforowe po zastosowaniu nawozu