Water Use in Row Crops Crop water use, or evapotranspiration, represents soil water evaporation and the water used by a crop for growth and cooling purposes. Factors that can influence crop water use include: prevailing weather conditions, regional climate, soil water availability, crop species, and crop growth stage. Better planning and management decisions can be made by understanding evapotranspiration. Evapotranspiration Crop root systems come into contact with water from precipitation or irrigation that enters the soil. Evapotranspiration (ET) is the water removed by soil evaporation and plant transpiration. Transpiration is the movement of water from the soil into plant roots, through plant stems and leaves, and back out into the atmosphere. Evaporation is the water evaporated or lost from wet soil and plant surfaces. Significant evaporation can only take place when the top 1 to 2 inches of soil is wet or the plant canopy is wet. Once the soil surface is dry, evaporation decreases sharply. Therefore, significant evaporation occurs after rainfall or irrigation. The difference between ET and water that is stored in the plant root zone determines irrigation requirements, so ET estimates can be used to help determine proper irrigation scheduling. Factors That Influence Evapotranspiration Weather conditions, water availability in the soil, crop species, and growth stage can all influence crop water use. Weather/Climate: The ability of the atmosphere to evaporate water is the driving force for soil evaporation and crop transpiration. Weather factors that have a major impact include: solar radiation, temperature, relative humidity, and wind. These all increase the amount of water the plant must transpire to keep cool and produce biomass. Seasonal crop water use may vary across geographies as shown in Table 1. Crop Growth Stage: Crop ET also depends on the crop growth stage (Tables 2). ET is related to crop surface area, so small plants transpire less than large ones. In general, row crops like corn and soybean reach maximum ET just prior to the reproductive growth stage. For example, a corn plant will require the most water during the 4 to 5 weeks surrounding silking. During this time, a corn plant can use over 0.3 inches of water per day. Any moisture stress around the time of silking may cause the pollen to shed from the tassel before silking occurs, resulting in poor or no pollination. Table 1. Seasonal crop water use across geographies.* South Midwest East West Crop (inches/year) Corn 10 23-28 20-307 20-241 20-226 Soybean 20-2510 20-254 ~255 18-209 *Crop water use varies across geographies and these values represent a range depending on several factors including region and soil type. Table 2. Average crop water use (ET) by growth stage for 113-day maturity corn (Western region). Approximate Water use days to to maturity Growth stage maturity (inches) Corn R4 R4.7 R5 R6 Dough 34 7.5 Beginning dent 24 5.0 1/4 milk line 19 3.75 1/2 milk line (full dent) 13 2.25 3/4 milk line 7 1.0 Physiological maturity 0 0.0 End of pod elongation Beginning seed enlargement End of seed enlargement 37 29 18 9.0 6.5 3.5 Leaves begin to yellow 10 1.9 Beginning maturity 0 0.0 Soybean R4 R5 R6 R6.5 R7 *Long-term average number of days since planting required to progress from the previous growth stage to the next. For example, to go from the blister kernel stage to the beginning dent stage requires approximately 15 days (day 89 to day 104). Days to each growth stage were determined using the Hybrid-Maize Corn Growth Model for the period 1982-2005 at Clay Center, NE. Table modified from Kranz, W.L. et al. 2008. Irrigation management for corn NebGuide G1850. University of Nebraska-Lincoln Extension. Water Use in Row Crops Relative Maturity: Seasonal ET can be affected by crop relative maturity. For example, at the same location, a corn product with 120 day maturity will use more water than an 85 day maturity product. While longer season products use more water, they may also have a higher yield potential if heat units and adequate water are available. Population: Recommended populations for dryland production are less than those for irrigated production. Populations are lowered below 18,000 plants per acre to reduce the transpiration component of ET by the crop and to better match precipitation and stored soil moisture in dryland.2 On ground with higher plant populations, research would suggest populations above 18,000 plants per acre will transpire similar amounts of water regardless of the population. Crop roots should be checked during the growing season to determine if soil compaction is an issue. Subsoiling may help increase water use in droughty, shallow soils by breaking up hardpans that have formed.3 Fall subsoiling may help with infiltration and storage of winter moisture. Water Content: As soil dries, it becomes more difficult for plants to extract water. At field capacity, plants use water at the maximum rate. Plants use less water as the water content of the soil drops close to the permanent wilting point. When crops do not receive enough water to meet their ET demands, grain yield potential can be reduced. Water Stress Crops respond to water stress differently depending on the growth stage. Many grain crops respond to water stress during the vegetative growth stages with reduced yield and delayed reproductive or grain fill growth stages. For water use in corn, the critical growth stages are from tassel until grain is fully formed. For soybeans, the critical growth stage begins at full pod (R4) and continues until seed set. Shortages in water supply during these growth stages may cause a reduction in yield potential. Figure 1. Evapotranspiration is the combination of the water removed from the soil through evaporation and plant transpiration. Summary Crop water use is dependent upon a variety of factors. Agronomic practices such as no-till can increase the water holding capacity and help improve water needs. Research and advancements in plant breeding can help growers improve yield potential under water stress by developing corn and soybean products with water use efficiency characteristics and provide plant population recommendations for different field situations. Sources 1 Wright, J. 2002. Irrigation scheduling checkbook method. University of Minnesota. http://www.extension.umn.edu/agriculture/water/irrigation-scheduling-checkbook-method/ #amount. 2 Is a population change warranted in irrigated corn due to water constraints? 2013. University of Nebraska—Lincoln. Crop Watch. http://cropwatch.unl.edu/. 3 Tacker, P. and Vories, E. Irrigation. Arkansas Soybean Handbook. M197. University of Arkansas. 4 Thomas, J.G. and Blaine, A. Soybean irrigation. Pub. 2185. Mississippi State University Cooperative Extension. 5 Irrigation. Corn Agronomy. 2015. University of Wisconsin Extension. http://corn.agronomy.wisc.edu/Management/L026.aspx. 6 Barker, D. et. al. Ohio Agronomy Guide. 14th edition. Bulletin 472. The Ohio State. 7 Espinoza, L. and Ross, J. Corn Production Handbook. MP 437. University of Arkansas Extension. 8 Martin, C., Burr, C., and Olson, B. 2015. Irrigation handbook for the great plains. 9 Irrigation. Ag 101. 2012 Environmental Protection Agency Ag Center. http://www.epa.gov/oecaagct/ag101/ cropirrigation.html. 10 Klocke, N.L., Hubbard, K., Kranz, W.L., and Watts, D.G.1990. G90-992 Evapotranspiration (ET) or crop water use. University of Nebraska-Lincoln Extension. Paper 1197. http://digitalcommons.unl.edu. Web sources verified 7/28/15.140504060312 Excess Water Excess moisture can negatively impact crop growth and yield potential, as well as increase nitrogen leaching and runoff. Waterlogged soils can be due to poor irrigation management, above-normal rainfall, and/or poor drainage conditions. Overirrigation can result in reduced root oxygen, increased toxicity build-up, increased negative microbial growth and root disease, and a reduction in root mass due to lower soil temperature. For additional agronomic information, please contact your local seed representative. Developed in partnership with Technology, Development, & Agronomy by Monsanto. Individual results may vary, and performance may vary from location to location and from year to year. This result may not be an indicator of results you may obtain as local growing, soil and weather conditions may vary. Growers should evaluate data from multiple locations and years whenever possible. 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