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Introduction to Precipitation Runoff Process and Soil Erosion Risk Analysis in a Specific Area of Interest to Design Control Measures

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Warianty tytułu
Języki publikacji
EN
Abstrakty
EN
The knowledge on the spatial variability and hydrological behaviour of contributing areas to specific outlet is a fundamental input for developing appropriate water resource planning and management actions that take part in various areas of human activities. The aim of this contribution is to present the possibilities to assess the precipitation-runoff process and soil erosion risk in a specific area using the theoretical approaches with the simplest requirements for meteorological and surface runoff data. Considering the connectivity and behaviour of natural processes, the analysis of precipitation-runoff process and soil erosion risk is crucial prior to the design of technical water management practices and technical erosion control measures in the landscape. The characteristics of design rain, e.g. the intensity, annual frequency and duration can be determined using practical tools or according to the analysis of the cost and damages related to specific technical measure. The intensity of design rain can be estimated according to the long-term meteorological observations and intensity-duration-frequency curves developed using region specific equations (Dub’s formula, Urcikan’s formula). For the design of water management, conservation (especially erosion) or other measures for ecological stabilization and protection of the area, it is important in particular to determine the following characteristics of surface runoff: beginning of surface runoff, design discharge from the contributing area, the depth of the surface runoff, and the volume of surface runoff. Estimating the soil erosion risk by water erosion can be done according to the slope gradient or USLE calculation and subsequent comparison of estimated value with tolerable soil loss. Regardless of the location of specific areas, we have found that the design parameters of water management and technical erosion control practices, facilities and measures, including their localization can be determined by applying and modifying the existing theoretical and practical hydrological knowledge. We also found that this design cannot be executed without an analysis of the precipitation-runoff process and the erosion risk of this territory. In relation to the climate change and changing rainfall patterns in all regions worldwide, further studies should be conducted to specify the regional characteristics of precipitation, soil and its usage.
Rocznik
Strony
44--50
Opis fizyczny
Bibliogr. 23 poz., rys., tab.
Twórcy
autor
  • Department of Biometeorology and Hydrology, Faculty of Horticulture and Landscape Engineering, Slovak University of Agriculture in Nitra, Hospodárska 7, 949 76 Nitra, Slovak Republic
  • Department of Biometeorology and Hydrology, Faculty of Horticulture and Landscape Engineering, Slovak University of Agriculture in Nitra, Hospodárska 7, 949 76 Nitra, Slovak Republic
Bibliografia
  • 1. Act No.220/2004 Coll. on protection and utilisation of agricultural land (in Slovak).
  • 2. Antal J. 1985. Soil conservation and forest amelioration II. Exercise guide. VŠP in Nitra, Nitra (in Slovak).
  • 3. Antal J., Bárek V., Čimo J., Halaj P., Halászová K., Horák J., Igaz D., Jurík Ľ., Muchová Z., Novotná B., Šinka K. 2014. Hydrology of agricultural land. SPU in Nitra, Nitra (in Slovak).
  • 4. Bara M., Kohnová S., Gaál L., Szolgay J., Hlavčová K. 2010. Estimation of IDF curves of extreme rainfall by simple scaling in Slovakia. Contributions to Geophysics and Geodesy, 39 (3), 187–206.
  • 5. Chiang S., Tsay T.K., Nix S.J. 2002. Hydrologic regionalization of watersheds I: Methodology development. Journal of Water Resources Planning and Management, 128(1), 3–11.
  • 6. Chow V. T. 1964. Handbook of applied hydrology: a compendium of water-resources technology. Mc-Graw-Hill, New York.
  • 7. Dile Y.T., Karlberg L., Srinivasan R., Rockström J. 2016. Investigation of the curve number method for surface runoff estimation in tropical regions. Journal of the American Water Resources Association, 52 (5), 1155–1169.
  • 8. Elsebaie I.H. 2012. Developing rainfall intensity–duration–frequency relationship for two regions in Saudi Arabia. Journal of King Saud University – Engineering Sciences, 24, 131–140.
  • 9. Hadadin N.A. 2005. Rainfall intensity-duration-frequency relationship in the Mujib Basin in Jordan. Journal of Applied Sciences, 5 (10), 1777–1784.
  • 10. Jambor P., Ilavská B. 1998. Methodology of erosion control tillage systems. VÚPÚ, Bratislava (in Slovak).
  • 11. Kaletová T., Németová Z. 2017. Determination of surface runoff from the modelled area. Environment, earth and ecology, 1 (1), 61–66.
  • 12. Leń P., Król Ż. 2016. Analysis of economic and environmental effects of land consolidation on the example of Hucisko village. Journal of Ecological Engineering, 17 (5), 232–239.
  • 13. Mekonnen M., Melesse A.M., Keesstra S.D. 2016. Spatial runoff estimation and mapping of potential water harvesting sites: A GIS and remote sensing perspective, Northwest Ethiopia. p. 565–584. In Landscape dynamics, soils and hydrological processes in varied climates. Cham: Springer.
  • 14. Muchová Z., Antal J. 2013. Land consolidation. SPU in Nitre, Nitra (in Slovak).
  • 15. Steenhuis T.S., Collick A.S., Easton Z.M., Leggesse E.S., Bayabil H.K., White E.D., Awulachew S.B., Adgo E., Ahmed A.A. 2009. Predicting discharge and sediment for the Abay (Blue Nile) with a simple model. Hydrological Processes, 3737, 3728–3737.
  • 16. STN 75 4501. 2000. Hydro-melioration. Erosion control of agricultural land. Fundamental terms (in Slovak).
  • 17. Šinka K., Kaletová T. 2013. Determining the characteristics of direct runoff from real rain using GIS environment. Acta Horticulturae et Regiotectuare. 16 (2), 48–52.
  • 18. Šinka K., Muchová Z., Konc Ľ. 2015. Geographical information systems in spatial planning SPU, Nitra (in Slovak).
  • 19. Tárník A., Igaz D. 2015. Determination of plant available soil water storage in agricultura land of the Nitra river catchment. Acta Horticulturae et Regiotecturae. 18 (1), 16–19.
  • 20. Tárník A., Leitmanová M. 2017. Analysis of the development of available soil water storage in the Nitra river catchment. IOP Conf. Series: Materials Science and Engineering, 1–8.
  • 21. White E.D., Easton Z.M., Fuka D.R., Collick A.S., Adgo E., McCartney M., Awulachew S.B., Selassie Y.G., Steenhuis T.S. 2011. Development and application of a physically based landscape water balance in the SWAT model. Hydrological Processes, (25) 915–925.
  • 22. Wishmeier W.H., Smith D.D. 1978. Predicting rainfall erosion losses – a guide to conservation planning. Agriculture handbook no. 537. U. S. Department of Agriculture, Hyatsville.
  • 23. Zelelew D.G. 2017. Spatial mapping and testing the applicability of the curve number method for ungauged catchments in Northern Ethiopia. International Soil and Water Conservation Research, 5, 293–301.
Uwagi
Opracowanie rekordu w ramach umowy 509/P-DUN/2018 ze środków MNiSW przeznaczonych na działalność upowszechniającą naukę (2019).
Typ dokumentu
Bibliografia
Identyfikator YADDA
bwmeta1.element.baztech-627373f1-e305-4931-b17b-f2a89a8b14e6
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