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Tytuł artykułu

The Relationships of Texture and Hydrophysical Properties in Soil Profiles Under Selected Exotic Trees in the Context of Climate Change in Central Europe

Treść / Zawartość
Identyfikatory
Warianty tytułu
Języki publikacji
EN
Abstrakty
EN
Suitable soil and environmental conditions are the main prerequisites for successful growth of plants. Generally, all soil properties are substantially affected by textural composition. Therefore, the objective of the study was to test the interrelationships between particle size distribution and such physical soil properties, which usually predetermine the survival/death of plants, since they significantly affect the content and availability of water and air. Textural composition and physical soil properties were studied in profiles under monocultures of selected exotic trees in Arboretum Mlyňany, Slovakia. The results showed that medium-textured dominated in topsoils, whereas heavy-textured classes were dominant in luvic and stagnic horizons. Evaluation of entire profiles had confirmed standard, expected relationships between the individual grain fractions and soil physical properties. However, differences have occurred when the correlations between texture and physical properties in individual horizons were evaluated. Considering entire soil profiles, increased sand content significantly supported drainage of rainwater and soil aeration; silt contributed to increase the total porosity and aeration as well as available water capacity; clay contributed to the decrease in the available water capacity, total, and particularly coarse porosity and aeration, and to rise water retention, as well as the values of the wilting point. The results showed silt as key fraction providing suitable hydrophysical properties for the survival and growth of trees introduced in Arboretum. In compacted luvic and stagnic horizons, silt was significantly involved in the formation of total, and particularly coarse porosity and thereby increase soil aeration, while conversely, in loose topsoils just silt fraction significantly contributed to the reduction of coarse pores and increase of fine capillary pores and therefore water retention. In loose eluvial horizons, the silt contributed to significant increases in capillary porosity and water availability, which is essential in terms of meeting the plant needs.
Rocznik
Strony
244--252
Opis fizyczny
Bibliogr. 33 poz., rys., tab.
Twórcy
  • Department of Soil Science, Faculty of Agrobiology and Food Resources, Slovak University of Agriculture, Tr. A. Hlinku 2, 949 76 Nitra, Slovakia
  • Department of Soil Science, Faculty of Agrobiology and Food Resources, Slovak University of Agriculture, Tr. A. Hlinku 2, 949 76 Nitra, Slovakia
  • Department of Soil Environment Sciences, Warsaw University of Life Sciences, Nowoursynowska St. 159, 02-776 Warsaw, Poland
Bibliografia
  • 1. Asgarzadeh H., Mosaddeghi M.R., Mahboubi A.A., Nosrati A., Dexter A.R. 2011. Integral energy of conventional available water, least limiting water range and integral water capacity for better characterization of water availability and soil physical quality. Geoderma, 166, 34–42.
  • 2. Cifra J. 1958. Short characteristic of soil conditions in the Arboretum Mlyňany. In: Benčať, F. (Ed.), Natural conditions of Arboretum Mlyňany, Slovak Academy of Science, Bratislava, 79–96, (in Slovak).
  • 3. Čimo J., Šinka K., Novotná B., Tárník A., Aydin E., Toková L., Kišš V., Kotuš T. 2020. Change in Temperature Conditions of Slovakia to the Reference Period 1961–2010 and their Expected Changes to Time Horizons Years 2035, 2050, 2075 and 2100 under the Conditions of Changing Climate. Journal of Ecological Engineering, 21(7), 232–240.
  • 4. European Environment Agency. 2017. Climate change, impacts and vulnerability in Europe 2016, An indicator-based report. Publications Office of the European Union, Luxembourg.
  • 5. Ferus P., Hoťka, P., Košútová, D., Konôpková, J. 2020. Invasions of alien woody plant taxa across a cluster of villages neighbouring the Mlynany Arboretum (SW Slovakia). Folia Oecologica, 47(2), 121–130.
  • 6. Fulajtár E. 2006. Physical properties of soil. Soil Science and Conservation Research Institute, Bratislava, (in Slovak).
  • 7. Gera M., Damborská I., Lapin M., Melo, M. 2019. Climate changes in Slovakia: Analysis of past and present observations and scenarios of future developments. In: Barceló D., Kostianoy A.D. (Ed.). The handbook of environmental chemistry. Springer Nature Switzerland, Cham, 21–51.
  • 8. Ghanbarian-Alavijeh B., Millán, H. 2009. The relationship between surface fractal dimension and soil water content at permanent wilting point. Geoderma, 151, 224–232.
  • 9. Heiskanen J., Saksa T., Hyvöne J. 2016. Effects of mounding and soil clay content on postplanting success of Norway spruce. Forest Ecology and Management, 378, 206–213.
  • 10. Hosseini F., Mosaddeghi M.R., Hajabbasi M.A., Sabzalian M.R. 2016. Role of fungal endophyte of tall fescue (Epichloë coenophiala) on wateravailability, wilting point and integral energy in texturally-differentsoils. Agricultural Water Management, 163, 197–211.
  • 11. Hoťka P., Barta M. 2012. Inventory of living collections of the Mlyňany Arboretum SAS. Slovak Academy of Science, Bratislava, (in Slovak).
  • 12. Hrubík P., Holečková D. 2016. Analysis of the essential climatic factors in the Arboretum Mlyňany SAS in Vieska nad Žitavou for the period 2001–2015. Proc. Slovak Academy of Science, 129–136, (in Slovak).
  • 13. Hrubík P., Hoťka P. 2007. The climatic conditions characteristics of Arboretum Mlyňany SAS during period 1971–2006 (2007). Proc. Slovak Academy of Science, 28–37 (in Slovak).
  • 14. Huxley A.J., Griffiths M., Levy M., 1992. The new Royal Horticultural Society dictionary of gardening. Macmillan, London.
  • 15. Ištoňa J., Pavlenda P. 2011. Monitoring of water storage in forest soils on PMP Čifáre in the years 1999–2009. Forestry Journal, 57, 178–186.
  • 16. Kobza J., Hrivňáková K., Makovníková J., Barančíková G., Bezák P., Bezáková Z., Dodok R., Grečo V., Chlpík J., Lištjak M., Mališ J., Píš V., Schlosserová J., Slávik O., Styk J., Širáň, M. 2011. Obligatory methods of soil analyses. Soil science and conservation research institute, Bratislava (in Slovak).
  • 17. Kutílek M. 1978. Water management pedology. SNTL – state publishing of technical literature, Praha, (in Czech).
  • 18. Lal R. 1979. Physical properties and moisture retention characteristics of some Nigerian Soils. Geoderma, 21, 209–223.
  • 19. Lal R., Shukla M.K. 2004. Principles of soil physics. Marcel Dekker, New York.
  • 20. Marković M., Filipović V., Legović T., Josipović M. & Tadić V. 2015. Evaluation of different soil water potential by field capacity threshold in combination with a triggered irrigation module. Soil and Water Research, 10, 164–171.
  • 21. Mezősi G., Blanka V., Ladányi Z., Bata T., Urdea P., Frank A., Meyer B.C. 2016. Expected midand long-term changes in drought hazard for the SouthEastern Carpathian basin. Carpathian Journal of Earth and Environmental Sciences, 11(2), 355–366.
  • 22. Minasny B., McBratney A.B. 2003. Integral energy as a measure of soil-water availability. Plant and Soil, 249, 253–262.
  • 23. Ministry of Environment. 2017. Adaptation Strategy of the Slovak Republic on Adverse Impacts of Climate Change – update. Ministry of Environment of the Slovak Republic, Bratislava, (in Slovak).
  • 24. Obalum S.E., Nwite J.C., Oppong J., Igwe C.A., Wakatsuki T. 2011. Variations in selected soil physical properties with landforms and slope within an inland valley ecosystem in Ashanti region of Ghana. Soil and Water Research, 6, 73–82.
  • 25. De Paepe J.L., Bono A.A., Alvarez R. 2017. Simple estimation of available water capacity in soils of semiarid and subhumid environments. Arid Land Research and Management, 32(2), 133–148.
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  • 28. Polláková N., Šimanský V., Jonczak J. 2017. Characteristics of physical properties in soil profiles under selected introduced trees in the Nature Reserve Arboretum Mlyňany, Slovakia. Folia Oecologica, 44(2), 78–86.
  • 29. Safadoust A., Feizee P., Mahboubi A.A., Gharabaghi B., Mosaddeghi M.R., Ahrens B. 2014. Least limiting water range as affected by soil texture and cropping system. Agricultural Water Management, 136, 34–41.
  • 30. Statistica. 2008. Statistica. StatSoft, Praha.
  • 31. Wall A., Heiskanen J. 2009. Soil-water content and air-filled porosity affect height growth of Scots pine in afforested arable land in Finland. Forest Ecology and Management, 257, 1751–1756.
  • 32. Whitmore A.P., Whalley W.R. 2009. Physical effects of soil drying on roots and crop growth. Journal of Experimental Botany, 60, 2845–2857.
  • 33. Zangiabadi M., Gorji M., Shorafa M., Khorasani S.K., Saadat, S. 2017. Effects of soil pore size distribution on plant available water and least limiting water range as soil physical quality indicators. Pedosphere, 30(2), 1–10.
Typ dokumentu
Bibliografia
Identyfikator YADDA
bwmeta1.element.baztech-3a5a6b34-43f4-402b-a77b-eb074e7ef286
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