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Spatial-temporal analysis of soil water storage and deep drainage under irrigated potatoes in the Central Sands of Wisconsin, USA

机译:美国威斯康星州中央砂土土壤蓄水和灌溉土豆灌区的空间 - 时间分析

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Knowledge of soil water storage and deep drainage is important for improving irrigation efficiency, maximizing crop water use, and understanding groundwater table fluctuation. This is particularly important in sandy soils that depend on irrigation to produce high crop yields. In sandy soils under potato in the Wisconsin Central Sand Plains, soil water storage using tension probes was measured in three irrigation zones over the 2014 and 2015 growing seasons. Soil water storage was estimated across a 78 ha field using apparent electrical conductivity maps. Deep drainage was estimated using the Richards equation and Hydrus-1D software. It was found that the average soil water storage ranged from 74 to 110 mm in the top 0.45 m in three irrigation zones in 2014, and from 70 to 95 mm in 2015. Rainfall and irrigation was 387 and 269 mm in 2014, and 328 and 281 mm in 2015. Estimated deep drainage was uniform in three irrigation zones, and ranged from 222 to 244 mm in 2014, and from 167 to 180 mm in 2015. A negative correlation was found between soil water storage and potato yields possibly due to over-irrigation. The methods used in this study can be applied to improve irrigation and water use efficiency.
机译:了解土壤储水和深排水对于提高灌溉效率,最大化作物用水,并了解地下水表波动,这是重要的。这在含有灌溉的沙质土壤中尤为重要,以产生高作物产量。在威斯康星州中央砂平原的马铃薯下的沙质土壤中,在2014年和2015年生长季节的三个灌溉区测量了使用张力探头的土壤储水。使用表观电导率图估计土壤储水量在78公顷的场上估计。利用理查兹方程和氢气-1D软件估计深排水。有人发现,2014年三次灌溉区的平均土壤蓄水量在0.45米的顶部0.45米处的74至110毫米,2014年降雨量和灌溉为387和269毫米,328 2015年281毫米。估计的深深排水在三个灌溉区中均匀,2014年的222%至244毫米,2015年的167至180毫米。土壤储水和马铃薯产量可能会产生负相关性可能是由于造成的-灌溉。本研究中使用的方法可以应用于改善灌溉和用水效率。

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