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2013 | 27 | 4 |

Tytuł artykułu

Evapotranspiration and simulation of soil water movement in small area vegetation

Treść / Zawartość

Warianty tytułu

Języki publikacji

EN

Abstrakty

EN
In Greece, crops are frequently cultivated in small isolated areas in close proximity to roads and bare soils and therefore evapotranspiration is affected by local advection. Under these circumstances, oasis effect conditions are present and evapotranspiration is higher than what is expected. In this paper, the evapotranspiration and soil water dynamics of a cotton crop cultivated in small areas under the oasis effect is studied. To this end, two isolated free-drainage lysimeters cultivated with cotton in the year 2007 were used. Soil moisture of the soil profile of both the lysimeters was monitored with two capacitance water content probes. The soil water balance method was used to estimate crop evapotranspiration and corresponding crop coefficients in one of the two lysimeters. These coefficients were 75% larger than the FAO-56 crop coefficients at the mid-season stage. The FAO-56 and the derived crop coefficients were used for the simulation of the water dynamics in the second lysimeter by the SWBACROS model. The derived crop coefficients for these conditions produced much better results than the FAO-56 crop coefficients. The results were improved when crop coefficient value equal to 2.5 was used for the mid-season stage.

Słowa kluczowe

Wydawca

-

Rocznik

Tom

27

Numer

4

Opis fizyczny

p.445-453,fig.,ref.

Twórcy

  • Department of Hydraulics, Soil Science and Agricultural Engineering, Aristotle University of Thessaloniki, 54124 Thessaloniki, Greece
autor
  • Department of Hydraulics, Soil Science and Agricultural Engineering, Aristotle University of Thessaloniki, 54124 Thessaloniki, Greece
autor
  • Land Reclamation Institute, National Agricultural Research Foundation, 57400 Sindos, Greece
autor
  • Land Reclamation Institute, National Agricultural Research Foundation, 57400 Sindos, Greece
  • Department of Hydraulics, Soil Science and Agricultural Engineering, Aristotle University of Thessaloniki, 54124 Thessaloniki, Greece

Bibliografia

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  • Allen R.G., Smith M., Perrier A., and Pereira L.S., 1994. An update for the definition of reference evapotranspiration. Int. Commission Irrigation Drainage Bulletin, 43, 1-34.
  • Babajimopoulos C., 2000. Revisiting the Douglas-Jones method for modelling unsaturated flow in a cultivated soil. Environ. Model. Software, 15, 303-312.
  • Babajimopoulos C., Budina A., and Kalfountzos D., 1995. SWBACROS: A model for estimation of the water balance of a cropped soil. Environ. Software, 10, 3, 211-220.
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  • Oke T.R., 1987. Boundary Layer Climates. Methuen Press,London, UK.
  • Paraskevas C., Georgiou P., Ilias A., Panoras A., and Babajimopoulos C., 2012. Calibration equations for two capacitance water content probes in a lysimeter field. Int. Agrophys., 26, 285-293.
  • Potchter O., Goldman D., Kadish D., and Iluz D., 2008. The oasis effect in an extremely hot and arid climate: The case of Southern Israel. J. Arid Environ., 72, 1721-1733.
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  • Sentek, 2007. Sentek Diviner 2000 User Guide Version 1.4. Australia Sentek Pty Press, Stepney, Australia.
  • Spronker-Smith R.A., Oke T.R., and Lowry W.P., 2000. Advection and the surface energy balance across an irrigated urban park. Int. J. Climatol., 20, 1033-1047.
  • Van Genuchten M.T., 1978. Calculating the unsaturated hydraulic conductivity with a new, closed-form analytical model. Research Report 78-WR-08, Water Resources Program, Department of Civil Engineering, Princeton University, Princeton, NJ, USA.
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  • Zhang Q. and Huang R., 2004. Water vapor exchange between soil and atmosphere over a Gobi surface near oasis in the summer. J. Appl. Meteorol., 43, 1917-1928.

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Bibliografia

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