Evaporation Losses and Evapotranspiration Dynamics in Overhead Sprinkler Irrigation

被引:11
|
作者
Uddin, M. J. [1 ]
Murphy, S. R. [2 ]
机构
[1] Trangie Agr Res Ctr, New South Wales Dept Primary Ind, 7878 Mitchell Hwy, Trangie, NSW 2823, Australia
[2] Tamworth Agr Inst, New South Wales Dept Primary Ind, 4 Marsden Pk Rd, Calala, NSW 2340, Australia
关键词
Canopy evaporation; Droplet evaporation; Evaporation; Evaporation losses interception capacity; Sprinkler irrigation; Transpiration; Sap flow; WATER DROPLET EVAPORATION; PLANT CANOPY MODEL; SIZE DISTRIBUTIONS; SPRAY EVAPORATION; AIR-TEMPERATURE; INTERCEPTION; TRANSPIRATION; FOREST; ENERGY; FIELD;
D O I
10.1061/(ASCE)IR.1943-4774.0001469
中图分类号
S2 [农业工程];
学科分类号
0828 ;
摘要
A comprehensive review of evaporation losses and evapotranspiration (ET) dynamics in sprinkler irrigation revealed substantial differences in the magnitudes of the different components of evaporation. Field studies reported that droplet evaporation losses ranged from 0.5%-45%, whereas theoretical studies indicated losses of less than 1%. A recent experimental study using advanced instruments and methodologies estimated that canopy evaporation is the major evaporation loss and droplet evaporation could be assumed to be negligible. Other studies showed that evaporation increased and transpiration decreased in evapotranspiration dynamics during wet canopy conditions. Sensible and latent heat fluxes in sprinkler irrigated crops act in opposite ways, but both positively contribute to the available energy and total ET.
引用
收藏
页数:9
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