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Recharge and Groundwater Use in the North China Plain for Six Irrigated Crops for an Eleven Year Period

机译:华北平原六个灌溉作物十一年的补给和地下水利用

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摘要

Water tables are dropping by approximately one meter annually throughout the North China Plain mainly due to water withdrawals for irrigating winter wheat year after year. In order to examine whether the drawdown can be reduced we calculate the net water use for an 11 year field experiment from 2003 to 2013 where six irrigated crops (winter wheat, summer maize, cotton, peanuts, sweet potato, ryegrass) were grown in different crop rotations in the North China Plain. As part of this experiment moisture contents were measured each at 20 cm intervals in the top 1.8 m. Recharge and net water use were calculated based on these moisture measurement. Results showed that winter wheat and ryegrass had the least recharge with an average of 27 mm/year and 39 mm/year, respectively; cotton had the most recharge with an average of 211 mm/year) followed by peanuts with 118 mm/year, sweet potato with 76 mm/year, and summer maize with 44 mm/year. Recharge depended on the amount of irrigation water pumped from the aquifer and was therefore a poor indicator of future groundwater decline. Instead net water use (recharge minus irrigation) was found to be a good indicator for the decline of the water table. The smallest amount of net (ground water) used was cotton with an average of 14 mm/year, followed by peanut with 32 mm/year, summer maize with 71 mm/year, sweet potato with 74 mm/year. Winter wheat and ryegrass had the greatest net water use with the average of 198 mm/year and 111 mm/year, respectively. Our calculations showed that any single crop would use less water than the prevalent winter wheat summer maize rotation. This growing one crop instead of two will reduce the decline of groundwater and in some rain rich years increase the ground water level, but will result in less income for the farmers.
机译:在整个华北平原,地下水位每年下降约一米,这主要是由于年复一年灌溉冬小麦的水量减少。为了检验是否可以减少用水量,我们计算了2003年至2013年为期11年的田间试验的净用水量,在该试验中,六种灌溉作物(冬小麦,夏季玉米,棉花,花生,红薯,黑麦草)分别种植了华北平原的作物轮作。作为该实验的一部分,在顶部1.8 m以20 cm的间隔分别测量水分含量。根据这些水分测量值计算补给量和净用水量。结果表明,冬小麦和黑麦草的补给量最少,分别为27毫米/年和39毫米/年。棉花补给最多,平均为211毫米/年),其次是花生,为118毫米/年,地瓜为76毫米/年,夏季玉米为44毫米/年。补给取决于从含水层中抽出的灌溉水的量,因此不足以指示未来地下水的下降。取而代之的是,发现净用水量(补给量减去灌溉量)是地下水位下降的良好指标。所用的最低净水量(地下水)是棉花,平均水平为14毫米/年,其次是花生,平均水平为32毫米/年,夏季玉米为71毫米/年,甘薯为74毫米/年。冬小麦和黑麦草的净用水量最大,分别为198毫米/年和111毫米/年。我们的计算结果表明,任何一种农作物的耗水量都比冬小麦夏玉米轮作的普遍水平低。种植一种而不是两种的作物将减少地下水的减少,并且在一些降雨丰富的年份会增加地下水位,但将导致农民的收入减少。

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