In Michigan, converting large tracts of the Midwest’s marginal farming land to perennial biofuel crops carries with it some key unknowns, including how it could affect the balance of water between rainfall, evaporation and movement of soil water to groundwater.
In humid climates such as the U.S. Midwest, evaporation returns more than half of the annual precipitation to the atmosphere, with the remainder available to recharge groundwater and maintain stream flow and lake levels.
A recent study from the Great Lakes Bioenergy Research Center and published in Environmental Research Letters looks at how efficiently “second generation” biofuel crops – perennial, non-food crops such as switchgrass or native grasses – use rainwater and how these crops affect overall water balance.
The study, led by Michigan State University professor of ecosystem ecology and GLBRC scientist Stephen Hamilton, is the first multi-year effort to compare the water use of conventional corn crops to the perennial cropping systems of switchgrass, miscanthus, native grasses, restored prairies and hybrid poplar trees.
“When we established the different cropping systems in 2008,” Hamilton said, “we installed soil-water sensors at various depths through the root zone. We’ve been continuously monitoring the soil water content ever since.”
Hamilton uses the soil-water sensors to measure the rate of evapotranspiration occurring within each cropping system. Evapotranspiration refers to the sum total of water lost while the plant is growing, either from transpiration, which is evaporation through the plant stem itself, or from water evaporated off of the plant’s leaves or the ground. By measuring the amount of precipitation that has fallen against actual soil water content, it’s possible to quantify the water lost to evapotranspiration while each crop is growing.
Hamilton’s team reports that the perennial system’s evapotranspiration did not differ greatly from corn – a finding that contrasts sharply with earlier studies that found particularly high perennial water use in areas with high water tables. Hamilton’s study, however, took place in Michigan’s temperate humid climate and on the kind of well-drained soil characteristic of marginal farming land.
“The message here,” Hamilton said, “is that in many settings, perennials may not use more water. For well-drained soils in the upper Midwest at least, and probably for eastern North America in general, these results most likely apply, and water balance would not be adversely affected.”