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35 -1 <br />30 j 25 <br />20 <br />I <br />s � <br />0 <br />Average wl1F. =0.16 Mg 1 a 4 cm' <br />r =0.651 <br />• <br />•o <br />% .p. • <br />* <br />_• . #• • •. <br />•g4 t • <br />I • <br />25 50 75 100 125 <br />ET (an) <br />150 <br />• <br />• M • <br />• . <br />175 200 <br />Fig. 1. Season long alfalfa biomass yield and evapotranspiration <br />(ET) from studies with variable irrigation in the Great Plains <br />and Intermountain West of the United States. Each study (not <br />each point) was weighted equally to create the regression line. <br />The slope of the line represents a regional average water -use <br />efficiency (WUE) of 0.16 Mg ha 1 cm-1. <br />irrigation treatments, and 39 cm for dryland treatments (Table <br />1). Average annual biomass yield was 16.6 Mg ha under <br />full irrigation, 11.1 Mg ha under a variety of deficit irriga- <br />don treatments, and 6.0 Mg ha under dryland conditions. <br />Although the irrigation treatments are pooled over a wide <br />range of climatic conditions, the comparison illustrates the <br />magnitude of water use by irrigated alfalfa, the potential water <br />savings from converting full irrigation alfalfa to deficit irriga- <br />tion or dryland, and the extent of biomass yield reduction that <br />would accompany the reduced irrigation levels. <br />A regional average WUE for alfalfa was estimated from the <br />slope of a water production function created by aggregating the <br />results of the reviewed studies. To illustrate the spatial and tem- <br />poral variability in the water production function, results from <br />individual study years were used (Fig. 1) rather than multi -year <br />treatment averages (Table 1). Alfalfa biomass yield responds in <br />a positive, linear relationship to increasing ET, with an aver- <br />age WUE of 0.16 Mg ha cni 1 . This. WUE is consistent with <br />values reported for this region by others (Hanson and Putnam, <br />2000). There is wide variation in reported WUE, with total <br />seasonal WUE values ranging from 0.08 to 0.23 Mg ha cm <br />(Table 1 and Fig. 1). To normalize ET and biomass yield for <br />different climatic and environmental conditions, a relative water <br />production function with multi -year average data was created <br />(Fig. 2.). Relative biomass yield declines at a greater rate than rela- <br />tive ET (slope = 1.28), indicating that WUE will decrease with <br />decreasing ET under either deficit irrigation or dryland condi- <br />tions. The relative water production function (Fig. 2) can be used <br />with localized estimates of maximum yield and ET to predict <br />alfalfa production under planned reductions in irrigation. <br />Several individual studies confirm decreasing WUE with defi- <br />cit irrigation over a wide range of environmental conditions. Retta <br />and Hanks (1980) used line source irrigation in an alfalfa study <br />in Utah and found that WUE ranged from 0.19 Mg ha cm <br />under deficit irrigation to 0.21 Mg ha. cm- for full irriga- <br />tion (Table 1). Sammis (1981) found that WUE ranged from <br />0.09 Mg ha cm in the driest conditions to 0.15 Mg ha cm <br />in the wettest conditions under lint source irrigation in New <br />Mexico (Table 1). Another New Mexico study under line <br />source irrigation ( Smeal et al., 1991) supports these findings; <br />WUE ranged from 0.07 Mg ha cm- in the driest conditions <br />to 0.14 Mg ha cm in the wettest conditions (Fig. 3). A similar <br />observation ofdeclining WUE with ET was observed in a more <br />humid environment in Minnesota, where average WUE values <br />were 0.23, 0.23, 0.21, and 0.12 Mg ha cm for high, medium <br />high, medium low, and rainfed irrigation treatments (Carter <br />and Sheaffer, 1983). Thus, over a wide range of environmental <br />conditions, there is a consistent trend of decreased WUE with <br />decreasing ET under deficit irrigation. <br />Seasonal Differences in Water -Use Efficiency <br />Water -use efficiency varies with harvest interval due to dif- <br />ferences in environmental conditions and plant carbohydrate <br />partitioning. Smeal et al. (1991) compared biomass yield and <br />transpiration over harvest interval. Greatest WUE was measured <br />during the first harvest of each season, and the remaining har- <br />vests had lesser WUE (Table 2). A study conducted by Under - <br />sander (1987) in Texas also found that the greatest WUE was <br />observed for the first harvest (Table 2), and the trend is echoed in <br />the results of both Daigger et al. (1970) and Wright (1988). <br />Variation in solar irradiance helps explain seasonal differences <br />in WUE. Smeal et al. (1991) compared biomass yield per unit of <br />transpiration with level of solar irradiance over time. The results of <br />this experiment showed that biomass yield increased with increas- <br />ing average daily solar irradiance (S during the growingperiod <br />from alow of 16.1 MJ m d -1 to a maximum of 28.0 MJ m d-1. <br />Values of S greater than 28 MJ m2 d-1 resulted in biomass yields <br />that decreased slowly or plateaued. Based on a plant growth simu- <br />lation model, the increase in biomass yield per unit of transpiration <br />was explained by increasing S due to increased light penetration <br />into the canopy rather than an increase in heat energy (Holt et aL, <br />1975). Both conditions, high light and relatively low temperatures <br />only occur in the spring, whereas, light levels are limiting in the <br />fall. Thus, harvest intervals corresponding to the greatest WUE <br />occur when solar irradiance is high enough to induce high levels of <br />photosynthesis and temperatures are low enough to keep evapora- <br />tion at a minimum, such as the first harvest in the spring (Delaney <br />et al., 1974; Leavitt et al., 1979). <br />The seasonal variation in WUE also relates to carbohydrate <br />reserve flux in the alfalfa plant. Biomass development early in the <br />season depends on carbohydrate reserves accumulated during the <br />fall of the previous season and results in the highest WUE of the <br />season (Smith, 1962; Robinson and Massengale, 1968). After the <br />first harvest, carbohydrates for growth and restoration of root <br />reserves come from photosynthesis in new leaves, and transpira- <br />tion is correlated with leaf surface area (MacAdam and Barta, <br />2007). As day - length shortens and temperatures decline in the <br />late summer and early fall, greater amounts of photosynthate are <br />partitioned into root reserves, resulting in lower levels of aboveg- <br />round biomass, yield, and WUE (Hanson et al., 1988). <br />These observations suggest an approach to saving water from <br />irrigated alfalfa may be to concentrate irrigation during periods <br />of the growing season that have the greatest WUE, such as the <br />first harvest interval, followed by deficit or no irrigation during <br />periods of the growing season with the least WUE, such as mid- <br />summer harvest intervals. This approach, referred to as irriga- <br />tion termination or partial season irrigation, has the potential <br />to improve WUE relative to a controlled deficit irrigation that <br />• is applied uniformly through the growing season. None of the <br />studies reported in Table 1 managed irrigation in this manner, <br />46 Agronomy Journal • Volume 103, Issue 1 • 2011 <br />