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首页> 外文期刊>Journal of irrigation and drainage engineering >Effects of Subsurface Drainage on Evapotranspiration for Corn and Soybean Crops in Southeastern North Dakota
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Effects of Subsurface Drainage on Evapotranspiration for Corn and Soybean Crops in Southeastern North Dakota

机译:北达科他州东南部地下排水对玉米和大豆作物蒸散的影响

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摘要

A field experiment was conducted during the 2009 and 2010 growing seasons to determine the effect of subsurface drainage (SSD) on evapotranspiration (ET) and crop coefficients (K_c) for a farm field in the Red River Valley of North Dakota. The total area of the field was 44 ha, half of which had subsurface drainage installed in the fall of 2002 at an approximate depth of 1.1 m and a spacing of 18.3 m. Corn (Zea mays) was planted in 2009 and soybean (Glycine max) in 2010. Evapotranspiration rates were measured in both the SSD and surface drained [or undrained (UD)] by using the eddy covariance (EC) method. The changes in water table and soil moisture content were monitored continuously in both fields. The K_c for corn and soybean was developed by using the ET measured by the EC system, and the reference ET was estimated by using the American Society of Civil Engineers Environmental and Water Resources Institute alfalfa reference method. As expected, the use of SSD affected the ET in a seasonal pattern and the ET was crop dependent. Seasonally, higher ET was observed during spring and fall in the UD field attributable to shallower water table and higher soil moisture content. In the summer, a higher ET was found in the SSD field. The higher ET in the UD field in spring and fall, which was 109 and 191 mm in 2009 and 2010, compared with 105 and 176 mm in 2009 and 2010 in the SSD field, did not offset the higher ET in the SSD field in the summer, which was 310 and 351 mm in 2009 and 2010, compared with 249 and 324 mm in 2009 and 2010 in the UD field. For July and August, the ET in the SSD field was 31% greater in 2009 for corn and 14% greater in 2010 for soybean than that in the UD crop fields. For the entire growing season, the ET in the SSD field was 16% higher in 2009 and 7% higher in 2010 compared with the UD field. During the peak growing season (July), the K_c was greater in the SSD field, with peak values of 0.70 for corn and 0.76 for soybean, but in the UD field, the peak K_c values were only 0.54 for corn and 0.65 for soybean.
机译:在2009年和2010年生长季节进行了田间试验,以确定北达科他州红河谷农田的地下排水(SSD)对蒸散(ET)和作物系数(K_c)的影响。该油田的总面积为44公顷,其中一半在2002年秋季安装了地下排水系统,排水深度约为1.1 m,间距为18.3 m。玉米(Zea mays)于2009年种植,大豆(Glycine max)于2010年种植。通过使用涡度协方差(EC)方法测量了SSD和表面排水[或不排水(UD)]中的蒸散速率。在这两个领域中,都连续监测了地下水位和土壤水分的变化。玉米和大豆的K_c是使用EC系统测得的ET开发的,参考ET是使用美国土木工程师协会环境与水资源研究所的苜蓿参考方法估算的。不出所料,SSD的使用以季节性方式影响了ET,并且ET依赖于作物。季节性地,UD田春季和秋季观测到较高的ET,这归因于地下水位较浅和土壤水分含量较高。夏季,SSD领域发现了更高的ET。春季和秋季UD领域的ET较高,2009和2010年分别为109和191 mm,而SSD领域的2009和2010年分别为105和176 mm,并不能抵消SSD领域的ET较高。夏季,2009年和2010年分别为310和351毫米,而UD领域的2009和2010年分别为249和324毫米。在7月和8月,与UD作物田相比,2009年玉米SSD田的ET增长了31%,2010年大豆大豆的ET增长了14%。在整个生长季节中,与UD领域相比,SSD领域的ET在2009年增长了16%,在2010年增长了7%。在高峰生长季节(7月),SSD田的K_c较大,玉米的峰值为0.70,大豆的为0.76,而在UD田地,玉米的K_c峰值仅为玉米的0.54,大豆的0.65。

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