Crop yield response to water - Cra
Crop yield response to water - Cra Crop yield response to water - Cra
Modify horticultural practicesPruning – More severe pruning may be effective in reducing water use since Tr is related tocanopy size and leaf area density. However, the relationships between canopy size and Trare not linear (see Figure 11) and significant pruning may be needed to change Tr. When thereduction in water supply is going to be drastic (a small fraction of tree Tr), a mature plantationcan be saved for later years by heavy pruning (sometimes called ‘dehorning’ or ‘stumping’).The objective is to remove most of the canopy, leaving only short primary scaffolds. Thiseffectively eliminates any yield for that season but it permits the tree to survive the drought.Full production may not resume for several years.Fruit thinning – Heavy fruit thinning under limited water allows the grower to produce fruit ofmarketable sizes, thus increasing crop value relative to normal thinning. This practice is commonand achieves higher grower revenue, even though yields are lower. Also, because the presenceof fruit enhances Tr, heavy thinning can reduce Tr rates somewhat in many tree species anddecrease the level of water stress in the trees, leading to an acceptable commercial size for theremaining fruit. As a general conclusion, it must be said that there is not much evidence thatthese measures are very effective, relative to others discussed in this Section, except in extreme,very low water supply situations. Further, because the reduction in transpiration associated withfruit thinning is mediated by reduced stomatal conductance, this practice might increase heatdamage where water deficit and high temperatures occur at the same time.Reduce evaporation from soil – If runoff is avoided and deep percolation is minimized, theonly option left to decrease unproductive water use is to reduce or even eliminate E loss. Infull coverage systems, irrigating as infrequently as possible would also minimize E. Evaporationlosses from drip irrigation are low but they can be reduced further if the systems are notrun daily, but every few days. The optimum interval would depend on the depth of waterrequired and on soil type, as deep percolation must also be avoided. Because the depth ofapplied water is reduced under deficit, the irrigation set (duration of irrigation) should notbe changed, but the interval between applications should be expanded (irrigation frequencylowered). Having the drip lines under the canopy will contribute to the E reduction because ofboth the shade and the mulch layer of dead leaves over the wetted soil. Buried drip networkscan theoretically eliminate E. However, some surface wetting has been reported with manyburied drip systems, even with line placement 45 cm deep. The magnitude of this problemseems to depend on soil transport properties, the installation depth, the method used forline installation, and the duration of the irrigation. Moreover, these systems are relativelyexpensive and more difficult to maintain. Thus, the installation of buried drip systems for thepurpose of reducing E is generally not justified, as the savings relative to surface drip would besmall in absolute terms. In cases where the amount of water applied is very low, the relativeimportance of E increases, and the small E savings from buried drip may pay off.Deficit irrigationOnce all the measures described above have been considered and adopted as needed, the onlyoption left to cope with water scarcity is to reduce the application of irrigation water. Deficitirrigation (DI) is defined as a regime where the irrigation water applied is less than the orchardET requirements. When the irrigation rate is below the ET rate, there will be a net extraction ofwater from the soil reservoir. Two situations may then develop. In one case, if sufficient wateris stored in the soil and transpiration is not limited by soil water, the consumptive use (ET)Yield Response to Water of Fruit Trees and Vines 289
- Page 254 and 255: Growth and developmentThe common me
- Page 256 and 257: soils (EARO, 2002). Tef has some to
- Page 258: tef 243
- Page 261 and 262: Lead AuthorsElias Fereres(Universit
- Page 264: equirements per unit land area for
- Page 268 and 269: figure 6 The water balance of an or
- Page 270 and 271: ox 2 Understanding the transpiratio
- Page 272: Orchard transpirationTree Tr is det
- Page 276 and 277: ox 4 Sample calculation of E dz , E
- Page 278 and 279: ox 5 Computing olive tree transpira
- Page 280 and 281: FIGURE 10 Crop coefficient (K c ) c
- Page 282 and 283: For training systems on a vertical
- Page 284 and 285: ox 7Consumptive and non-consumptive
- Page 286 and 287: are seeking more precision in their
- Page 288 and 289: ox 9 Examples of soil water monitor
- Page 290 and 291: ox 10 (CONTINUED)The major limitati
- Page 292 and 293: ox 12Definition of CWSI and an exam
- Page 294 and 295: The water budget methodWith this me
- Page 296 and 297: ox 15 Evolution of soil water under
- Page 298 and 299: opening and photosynthesis relative
- Page 300 and 301: that occur during the periods of fr
- Page 302 and 303: The crop, where price can vary more
- Page 306 and 307: Figure 12Patterns of seasonal appli
- Page 308 and 309: figure 14Response of an almond orch
- Page 310: Additional ReadingFollowing are a n
- Page 314 and 315: Lead AuthorSRiccardo Gucci,(Univers
- Page 316 and 317: in the first years of production (t
- Page 318: Because olives flower late, the ris
- Page 321 and 322: Table 1b Summary of recommended oli
- Page 323 and 324: Table 2 Relative yield and gross re
- Page 325 and 326: Figure 5Hypothetical seasonal cours
- Page 327: ReferencesAngelopulos, K., Dichio,
- Page 331 and 332: Early vegetative and reproductive g
- Page 333 and 334: Summer stressDuring this period of
- Page 335 and 336: almond had its highest Gl of close
- Page 337: Water Production FunctionsThe two p
- Page 340 and 341: Figure 3aCrop-water production func
- Page 342: Goldhamer, D. A. & Salinas, M. 2000
- Page 345 and 346: Figure 1 Production trends for appl
- Page 347 and 348: division, and that limitation of po
- Page 349: oth irrigation level and crop load.
- Page 352 and 353: Figure 6Seasonal reference ET o cro
Modify horticultural practicesPruning – More severe pruning may be effective in reducing <strong>water</strong> use since Tr is related <strong>to</strong>canopy size and leaf area density. However, the relationships between canopy size and Trare not linear (see Figure 11) and significant pruning may be needed <strong>to</strong> change Tr. When thereduction in <strong>water</strong> supply is going <strong>to</strong> be drastic (a small fraction of tree Tr), a mature plantationcan be saved for later years by heavy pruning (sometimes called ‘dehorning’ or ‘stumping’).The objective is <strong>to</strong> remove most of the canopy, leaving only short primary scaffolds. Thiseffectively eliminates any <strong>yield</strong> for that season but it permits the tree <strong>to</strong> survive the drought.Full production may not resume for several years.Fruit thinning – Heavy fruit thinning under limited <strong>water</strong> allows the grower <strong>to</strong> produce fruit ofmarketable sizes, thus increasing crop value relative <strong>to</strong> normal thinning. This practice is commonand achieves higher grower revenue, even though <strong>yield</strong>s are lower. Also, because the presenceof fruit enhances Tr, heavy thinning can reduce Tr rates somewhat in many tree species anddecrease the level of <strong>water</strong> stress in the trees, leading <strong>to</strong> an acceptable commercial size for theremaining fruit. As a general conclusion, it must be said that there is not much evidence thatthese measures are very effective, relative <strong>to</strong> others discussed in this Section, except in extreme,very low <strong>water</strong> supply situations. Further, because the reduction in transpiration associated withfruit thinning is mediated by reduced s<strong>to</strong>matal conductance, this practice might increase heatdamage where <strong>water</strong> deficit and high temperatures occur at the same time.Reduce evaporation from soil – If runoff is avoided and deep percolation is minimized, theonly option left <strong>to</strong> decrease unproductive <strong>water</strong> use is <strong>to</strong> reduce or even eliminate E loss. Infull coverage systems, irrigating as infrequently as possible would also minimize E. Evaporationlosses from drip irrigation are low but they can be reduced further if the systems are notrun daily, but every few days. The optimum interval would depend on the depth of <strong>water</strong>required and on soil type, as deep percolation must also be avoided. Because the depth ofapplied <strong>water</strong> is reduced under deficit, the irrigation set (duration of irrigation) should notbe changed, but the interval between applications should be expanded (irrigation frequencylowered). Having the drip lines under the canopy will contribute <strong>to</strong> the E reduction because ofboth the shade and the mulch layer of dead leaves over the wetted soil. Buried drip networkscan theoretically eliminate E. However, some surface wetting has been reported with manyburied drip systems, even with line placement 45 cm deep. The magnitude of this problemseems <strong>to</strong> depend on soil transport properties, the installation depth, the method used forline installation, and the duration of the irrigation. Moreover, these systems are relativelyexpensive and more difficult <strong>to</strong> maintain. Thus, the installation of buried drip systems for thepurpose of reducing E is generally not justified, as the savings relative <strong>to</strong> surface drip would besmall in absolute terms. In cases where the amount of <strong>water</strong> applied is very low, the relativeimportance of E increases, and the small E savings from buried drip may pay off.Deficit irrigationOnce all the measures described above have been considered and adopted as needed, the onlyoption left <strong>to</strong> cope with <strong>water</strong> scarcity is <strong>to</strong> reduce the application of irrigation <strong>water</strong>. Deficitirrigation (DI) is defined as a regime where the irrigation <strong>water</strong> applied is less than the orchardET requirements. When the irrigation rate is below the ET rate, there will be a net extraction of<strong>water</strong> from the soil reservoir. Two situations may then develop. In one case, if sufficient <strong>water</strong>is s<strong>to</strong>red in the soil and transpiration is not limited by soil <strong>water</strong>, the consumptive use (ET)Yield Response <strong>to</strong> Water of Fruit Trees and Vines 289