Abstract

This study examined evapotranspiration (ET) from no-till, rainfed maize and soybean during three growing seasons (May-Sep) of normal rainfall years (2009, 2010, 2011) and a drought year (2012) in Michigan, USA, based on daily soil water uptake measured by time-domain reflectometry at multiple depths through the root zone. During normal rainfall years, growing-season ET was similar between continuous maize (mean ± standard deviation: 471 ± 47 mm) and maize in rotation (469 ± 51 mm). During the drought year, ET decreased by only 3% for continuous maize but by 20% for maize in rotation. During the normal rainfall years, ET for soybean (453 ± 34 mm) was statistically indistinguishable from ET for maize, and was lower during the drought year (333 mm). Water use efficiency (WUE), calculated from harvest yield (grain + corn stover) and ET, was 25.3 ± 4.2 kg ha−1 mm-1 for continuous maize and 27.3 ± 3.1 kg ha−1 mm−1 for maize in rotation during the normal rainfall years, whereas WUEs for both continuous maize and maize in rotation were much lower in the 2012 drought year (14.0 and 15.5 kg ha−1 mm−1, respectively), coincident with lower production. Soybean had a much lower WUE than maize during the three normal years (6.95 ± 0.96 kg ha−1 mm−1) and the drought year (4.57 kg ha−1 mm−1), also explained by lower yield. Both maize and soybean tended to use all available water in the soil profile; there was no consistent difference in ET between these crops, while yield varied markedly from year to year.

Highlights

  • The return of water to the atmosphere through evapotranspiration (ET) controls terrestrial water and energy balances (USGS, 1990; Williams et al, 2012)

  • We investigated the ET of continuous maize and maize and soybean grown in rotations during the growing season (May-Sep) in years of normal rainfall (2009, 2010 and 2011) and a severe drought year (2012)

  • Air temperature during the growing season (May-September, inclusive) in the years of normal rainfall (2009–2011) averaged 19.0 °C, which was close to the long-term growing season average (1988−2013: 18.7 °C); mean air temperature was warmer by 1.0 °C in the drought year (2012)

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Summary

Introduction

The return of water to the atmosphere through evapotranspiration (ET) controls terrestrial water and energy balances (USGS, 1990; Williams et al, 2012). Water loss by transpiration dominates annual ET (Hanson, 1991), and in temperate climates like the Midwest US, the majority of annual ET occurs during the growing season (e.g., Abraha et al, 2015). The Corn Belt of the Midwest United States is the world’s most expansive region of maize and soybean production with over 70 million ha of land currently under maize or soybean cultivation (USDA, 2015a). Evapotranspiration returns approximately two-thirds of precipitation to the atmosphere in this temperate climate (USGS, 1990). The ET water loss from this vast agricultural landscape strongly influences regional climate, and the surplus precipitation that is not lost to ET determines surface-groundwater exchanges, groundwater availability, and river flows

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