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首页> 外文期刊>Agricultural Water Management >Impact of climate change on the water requirement of summer maize in the Huang-Huai-Hai farming region.
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Impact of climate change on the water requirement of summer maize in the Huang-Huai-Hai farming region.

机译:黄淮海农区气候变化对夏玉米需水量的影响。

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Crop water requirement and the temporal and spatial changes of this important characteristic provide key information for irrigation scheduling, water resource planning, and future decision-making. In the Huang-Huai-Hai (HHH) farming region in north China, both crop evapotranspiration ( ETc ) and evapotranspiration of the applied water ( ETaw ) in the growing season of summer maize during 1960-2009 were calculated using the SIMETAW (simulation of evapotranspiration of applied water) model and the daily weather data. Inverse distance weighted interpolation (IDW) was used to interpret spatial distribution of ETc and ETaw . Results showed that: (1) During 1960-2009 in the HHH farming region, ETc of summer maize during the growing season showed a significant downward trend; the average ETc decreased from 335.6 mm/decade in the period 1960-1969 to 311.4 mm/decade in the period 2000-2009. The variation of ETaw of summer maize during the growing season did not drop significantly due to yearly fluctuation of the effective rainfall ( Re ) in the growing season, and the improvement of irrigation efficiency and cultivation management measures. Although the descent of ETc might mitigate the agricultural water stress in this area to some extent, the variation of ETaw still depended on the effective rainfall. (2) The average ETc values per decade presented higher in the eastern and lower in the western regions; inter-regional differences were observed for ETaw , and the highest ETaw value of about 109.6 mm was found in the western regions of the Shandong and Hebei Provinces. Adjusting irrigation system and adopting the different irrigation systems in different region should be taken into consideration to guarantee the maize yield in this area. (3) During 1960-2009, a significant overall increase in temperature, a significant decrease in wind speed, humidity, and solar radiation, and a slight decrease in precipitation were observed. The solar radiation decrease contributed most to the summer maize ETc decrease, while relative humidity and precipitation were negatively correlated with ETc .
机译:作物需水量和这一重要特征的时空变化为灌溉计划,水资源规划和未来决策提供了关键信息。在中国北方的黄淮海(HHH)耕作区,利用SIMETAW计算了1960-2009年夏季玉米生长季节的作物蒸散量(ETc)和施水的蒸散量(ETaw)。应用水的蒸散量)模型和每日天气数据。逆距离加权插值(IDW)用于解释ETc和ETaw的空间分布。结果表明:(1)HHH农区1960- 2009年,夏玉米生长季的ETc呈明显下降趋势;平均ETc从1960-1969年的335.6毫米/十年减少到2000-2009年的311.4毫米/十年。由于生长季节有效降雨(Re)的逐年波动以及灌溉效率和耕作管理措施的改善,夏季玉米的ETaw变化在生长季节没有明显下降。尽管ETc的下降可能在某种程度上减轻了该地区的农业缺水压力,但ETaw的变化仍然取决于有效降雨。 (2)东部地区每十年的平均ETc值较高,而西部地区则较低。观察到ETaw的区域间差异,在山东和河北省西部发现ETaw值最高,约为109.6 mm。应考虑调整灌溉系统,在不同地区采用不同的灌溉系统,以保证该地区的玉米产量。 (3)在1960-2009年期间,观测到总体温度显着上升,风速,湿度和太阳辐射显着下降,而降水略有下降。太阳辐射的减少是夏季玉米ETc降低的最大原因,而相对湿度和降水量与ETc负相关。

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