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首页> 外文期刊>Agricultural and Forest Meteorology >Energy/water budgets and productivity of the typical croplands irrigated with groundwater and surface water in the North China Plain.
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Energy/water budgets and productivity of the typical croplands irrigated with groundwater and surface water in the North China Plain.

机译:华北平原以地下水和地表水灌溉的典型农田的能量/水预算和生产力。

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Although irrigation has markedly increased agricultural productivity in the North China Plain, it has reduced groundwater levels by up to 0.8 m yr-1 and dried up the Yellow River for extended times since the 1970s. The objective of this study was to compare water, energy, and carbon fluxes in regions irrigated with groundwater and surface water (Yellow River) using almost four years of eddy covariance data from agricultural stations in Luancheng (water table depth: ~42 m) and Weishan (near Yellow River, water table depth: 1-3 m). Irrigation is mostly restricted to winter wheat as summer maize grows during the rainy season. Mean annual ET was 693 mm yr-1 for Luancheng site, which is higher than Weishan site (648 mm, ignore partial years). About ~390-480 mm of ET occurred during the wheat season (from early October to next early June, about 247 days), 230-300 mm in the maize season (from early June to late September, about 107 days). Annual crop yields were ~6864 kg/ha in the two regions. Annual water use efficiencies ranged from 4 to 6 g CO2 kg-1 H2O. Water use efficiencies were higher for maize than for wheat. Annual cropland carbon budget (CCB) was 230-280 g C m-2 yr-1 at the two sites and suggested a weak carbon sink. Irrigation compensated for seasonal and inter-annual variability in precipitation. Shifting the cropping pattern from wheat-maize double crops to a single crop of maize could significantly reduce water withdrawal and lead to a more sustainable use of water resource in this region.
机译:尽管灌溉显着提高了华北平原的农业生产力,但自1970年代以来,灌溉已使地下水位降低了多达0.8 m yr -1 ,并使黄河干dried了很长时间。这项研究的目的是使用栾城县农业站近四年的涡流协方差数据(地下水位深度:〜42 m)比较地下水和地表水灌溉区域(黄河)中的水,能量和碳通量。微山(黄河附近,地下水位深度:1-3 m)。由于夏季玉米在雨季生长,灌溉主要限于冬小麦。栾城遗址年平均ET为693 mm yr -1 ,高于巍山遗址(648 mm,忽略部分年份)。在小麦季节(从10月初至下一个六月初,约247天)发生约390-480 mm的ET,在玉米季节(从6月初至9月下旬,约107天)发生ET的约390-480 mm。这两个地区的年农作物产量约为6864千克/公顷。每年的用水效率在4到6 g CO 2 kg -1 H 2 O之间。玉米的水分利用效率高于小麦。这两个地点的年度农田碳收支(CCB)为230-280 g C m -2 yr -1 ,表明碳汇较弱。灌溉补偿了降水的季节性和年际变化。将种植方式从小麦-玉米双作转变为玉米单作可以显着减少该地区的取水量,并导致该地区水资源的可持续利用。

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