Increasing crop productivity when water is scarce—from breeding to field management
Introduction
The ideas of drought resistance and drought tolerance are giving way in the agricultural world to the idea of water productivity (“more crop per drop”). This change is a great advance because the latter can be quantified, with units of amount of crop yield per volume of water supplied or used, say, kg m−3 or kg ha−1 mm−1. Because it can be quantified it enables improvements to be charted, thereby encouraging faster progress.
Nevertheless, the idea of drought remains in widespread use—certainly in the mass media, and also among crop scientists. It comes with connotations of hardship, or, in poor agricultural communities, malnutrition or even famine. It is an idea that inevitably enters any discussion of the impact of the scarcity of water on food production. It is important therefore to be clear about what it means, for it means different things to different people depending on their time scale of interest (Table 1); debates can easily be at cross purposes.
Many explorations of water deficits by plant physiologists, biochemists and molecular biologists are rather more concerned with survival than production, as noted in Table 1. While it is true that a crop plant that does not survive severe water deficits will not produce any yield, the converse is rarely true. Thus the challenge provided by changing focus from “drought tolerance” to “water productivity” clarifies the targets of research, especially those carried out at time scales of hours to days. Some processes occurring at these time scales can strongly affect water-limited yields; others have little relevance, as I shall discuss later.
“Water productivity” can also mean different things to different people (see, for example, Kijne et al., 2003, Pereira et al., 2002). To an economist it might mean the monetary value of outputs divided by that of the necessary inputs. To a geographer or irrigation engineer, it might mean the value of crops produced in a catchment in relation to the water supply of that catchment. But the quintessence of the idea is that it is quantifiable. In this paper, I will concentrate primarily on improving water productivity on farm (with units of amount of crop yield per amount of water supplied or used), though with occasional reference to other aspects.
Section snippets
Water as a limiting resource
This heading implies two questions:
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First, how can we tell, in specific instances, if it is water that is mainly limiting crop yield?
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Second, when water is the main limitation, how can we most effectively improve the yields that we currently obtain?
An answer to the first question is not always clear cut, for in farmers’ fields there are typically multiple environmental influences on yield. But comparing actual yield with an expected one can nevertheless be revealing, and any large discrepancy is
How to gauge if water is the predominant limitation to yield?
There is a lot of available information on winter-cereal crop yields in relation to rainfed water supply in southern Australia, a climatically mediterranean environment. Fig. 1, adapted from Angus and van Herwaarden (2001), compares simulated yields of well-managed rain-fed wheat with mean annual reported yields in the shire of Wagga Wagga in Australia, in relation to growing-season rainfall. The solid diagonal line depicts a transpiration efficiency of 20 kg ha−1 mm−1, an upper limit that is
Avenues for improving water-limited yield of rainfed crops
While it is clear that water productivity will be low in crops beset by diseases, pests, or weeds, there are also more subtle aspects of crop management or the behaviour of various cultivars that can have large effects on productivity. Hatfield et al. (2001) have reviewed many aspects of soil and stubble management that influence the water balance of the soil by affecting infiltration and water storage in the soil, and evaporative losses from the soil surface. These combined effects can
Capturing more of the water supply: reducing losses from soil evaporation, deep drainage and runoff
A rainfed crop's water supply comprises available water in the soil at the time of sowing plus rainfall during the growing season. The main losses are by direct evaporation from the soil surface and vertical drainage of water beyond the reach of the roots. Run-off from the soil surface may be substantial during heavy rain, but much of that run-off may become run-on in lower parts of a field, with little net loss from the field as a whole (Batchelor et al., 2002) unless infiltration rate is poor
Improving the exchange of water for CO2 by leaves
The transpiration efficiency of leaves, i.e. the amount of carbon fixed per unit of water transpired, depends on both evaporative demand by the environment and the CO2 concentration within the leaves (Tanner and Sinclair, 1983, Condon et al., 2002). For a given evaporative demand and stomatal conductance, the lower is the concentration of CO2 within a leaf the larger is the transpiration efficiency and the less is the discrimination against the heavy stable isotope of carbon, 13C, during
Converting biomass into grain
The timing of flowering is the most important trait that plant breeders select for when targeting water-limited environments. For example, winter-growing crops that flower too early may not have built enough biomass to set and fill a large number of seeds, and may also be prone to frost damage at flowering. Those that flower too late, while they may have set a large number of grains per unit area and thereby have a large yield potential, may fail to fill their grain adequately because they have
Getting the most out of irrigation
As water for irrigated agriculture becomes scarcer, it is likely that it will increasingly be used supplementally—that is, full irrigation will be replaced by deficit irrigations targeted to periods without rain that coincide with especially sensitive stages of a crop's life. Pereira et al. (2002) review the possibilities as well as outlining general good irrigation practice. Ideally, supplemental irrigation means using limited irrigation water so that it gives the greatest marginal return over
Farming systems and agricultural landscapes
Water productivity depends not only on how a crop is managed during its life, but also on how it is fitted in to the management of a farm as a whole, both spatially and through time. Further, the management of water use by crops may generate offsite effects that lead to dryland salinity or eutrophication or other pollution of discharge areas. The role of tillage has been changing and is likely to keep on changing as the advantages of direct-drilling techniques become more widely appreciated,
Opportunities for molecular plant breeding to improve water productivity
The foregoing discussion describes how breeding and agronomy are closely intertwined in improving water productivity of rainfed crops. While plant breeders have many agronomically important traits under control, for example flowering time and height, others, especially ones relating to the performance of roots, have been difficult to handle. Marker-assisted selection (MAS) is becoming increasingly useful. There are about 50 markers listed on the Plantstress website (//www.plantstress.com/biotech/index.asp?Flag=1
The way ahead?
Improvements in water productivity will most likely come, approximately equally, from better agronomy and better cultivars, with improvements in one stimulating improvements in the other. That is what has happened in the past, and there is no strong reason to expect that the pattern will change. Developing expectations about what water-limited yield might reasonably be, given the growing season's weather and other conditions, has proved to be an important stimulus to the way farmers’ think
Acknowledgments
I thank John Angus, John Boyer, Scott Chapman, Tony Fischer, John Kirkegaard, Greg Rebetzke, Richard Richards, and Wolfgang Spielmeyer for many helpful discussions while preparing this paper.
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