Using Grapevine Water Status Measurements for Irrigation Scheduling of Table Grapes-A Review

被引:0
|
作者
Howell, C. L. [1 ]
Myburgh, P. A. [1 ]
机构
[1] ARC Infruitec Nietvoorbij, Agr Res Council, Fruit Vine & Wine Inst, Private Bag X5026, ZA-7599 Stellenbosch, South Africa
关键词
berry mass; leaf water potential; stem water potential; total diurnal water potential; vegetative growth; DIFFERENT FERTIGATION STRATEGIES; DEFICIT IRRIGATION; MEASURED EVAPOTRANSPIRATION; SEEDLESS; GROWTH; SOIL; FRACTIONS; PRESSURE; QUALITY; VINE;
D O I
10.21548/44-1-5653
中图分类号
TS2 [食品工业];
学科分类号
0832 ;
摘要
Water is becoming an increasingly scarce resource, so agriculture competes with urban and industrial needs for water. The production of table grapes with high export potential is the objective of South African producers. Vegetative growth, production, ripening aspects and quality parameters of table grapes can potentially be manipulated by means of irrigation. Consequently, it is an important management practice to help ensure economically viable table grape production. The objective for optimum irrigation scheduling should be to combine soil and plant water status measurements to calibrate grapevine water potential against reliable soil water monitoring instruments. Considering previously reported literature, poorer vegetative growth was related to lower levels of leaf water potential (1PL). Given that berry size is a crucial aspect for yield as well as quality, it was evident that low levels of water potential can restrict berry development, thereby reducing berry size. Bunch mass was lower where there were lower levels of 1PL and pre-dawn leaf water potential (1PPD). Poorer yield was generally related to lower levels of 1PL experienced throughout the season. However, lower levels of 1PL in the post-veraison period did not affect grapevine yield. The juice total soluble solids (TSS) did not respond to levels of 1PL but juice total titratable acidity (TTA) was related to lower levels of 1PL. Grape colour was affected where wet soil conditions induced higher levels of 1PL as well as where dry soil conditions induced lower levels of 1PL.
引用
收藏
页码:75 / 80
页数:6
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