Semi-empirical approach for estimating actual evapotranspiration in Greece

被引:20
作者
Poulovassilis, A
Anadranistakis, M
Liakatas, A
Alexandris, S
Kerkides, P
机构
[1] Agr Univ Athens, Dept Nat Resources & Agr Engn, GR-11855 Athens, Greece
[2] Hellen Natl Meteorol Serv, GR-16603 Athens, Greece
关键词
soil water balance; actual evapotranspiration;
D O I
10.1016/S0378-3774(01)00121-4
中图分类号
S3 [农学(农艺学)];
学科分类号
0901 ;
摘要
Reliable estimation of actual evapotranspiration rates (ET) may be achieved if extensive information on the soil-plant-atmosphere system is available. Agricultural and irrigation engineers facing the problem of rational irrigation planning, rarely have at their disposal such information. Therefore, there is a demand for simpler approaches to estimate actual evapotranspiration. In this paper, a semi-empirical approach is proposed for estimating actual water losses from crops. It is assumed that the ratio of actual to maximum evapotranspiration (ET/ETm) is an exponential function of the water content w in the root-zone, of the form: ET/ETm = exp[c(w - w(fc))/ (w - w(wp))], where c is a constant introduced to adjust the decrease of the ratio ET/ETm according to what is observed for the climatic conditions, soils and crops of Greece, wfc the water content at field capacity and w(wp) denotes the water content at wilting point. Verification of the above approach for estimating actual evapotranspiration was achieved by comparing ET-values obtained by the soil moisture profile changes and the ET-values obtained by the above equation. Meteorological, crop and soil data required were collected from experimental fields of the Agricultural University of Athens (38 degrees 23 'N, 23 degrees6 'E). The agreement of actual versus computed ET-values for three widely grown crops in Greece (cotton, wheat and maize) may be considered as satisfactory. (C) 2001 Elsevier Science B.V. All rights reserved.
引用
收藏
页码:143 / 152
页数:10
相关论文
共 12 条
[1]  
AMOOZEGAR A, 1986, AGRONOMY 1, V9
[2]   Crop water requirements model tested for crops grown in Greece [J].
Anadranistakis, M ;
Liakatas, A ;
Kerkides, P ;
Rizos, S ;
Gavanosis, J ;
Poulovassilis, A .
AGRICULTURAL WATER MANAGEMENT, 2000, 45 (03) :297-316
[3]  
BLAKE GR, 1986, AGRONOMY 1, V9
[4]   HYDROMETER METHOD IMPROVED FOR MAKING PARTICLE SIZE ANALYSES OF SOILS [J].
BOUYOUCOS, GJ .
AGRONOMY JOURNAL, 1962, 54 (05) :464-&
[5]   A SIMPLE SOIL-PLANT-ATMOSPHERE TRANSFER MODEL (SISPAT) DEVELOPMENT AND FIELD VERIFICATION [J].
BRAUD, I ;
DANTASANTONINO, AC ;
VAUCLIN, M ;
THONY, JL ;
RUELLE, P .
JOURNAL OF HYDROLOGY, 1995, 166 (3-4) :213-250
[6]   AVAILABILITY OF SOIL WATER TO PLANTS AS AFFECTED BY SOIL MOISTURE CONTENT AND METEOROLOGICAL CONDITIONS [J].
DENMEAD, OT ;
SHAW, RH .
AGRONOMY JOURNAL, 1962, 54 (05) :385-&
[7]  
Doorenbos J., 1986, FAO Irrigation and Drainage
[8]   EVAPORATION AND SURFACE-TEMPERATURE [J].
MONTEITH, JL .
QUARTERLY JOURNAL OF THE ROYAL METEOROLOGICAL SOCIETY, 1981, 107 (451) :1-27
[9]  
MONTEITH JL, 1973, PRINCIPLES ENV PHYSI
[10]  
Philip J.R., 1969, Advances in hydroscience, P215, DOI DOI 10.1016/B978-1-4831-9936-8.50010-6