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河西走廊春玉米需水量和灌溉需水量时空变化研究OA

Spatiotemporal variations in water requirement and irrigation water requirement of spring maize in Hexi Corridor

中文摘要英文摘要

[目的]研究气候变化背景下河西走廊春玉米灌溉需水分布规律.[方法]基于河西走廊 17 个气象站1971-2024 年逐日气象数据和 3个农业气象观测站 1991-2024 年春玉米生育期观测资料,研究春玉米有效降水量(Pe)、需水量(ET)和灌溉需水量(Ir)的时空分布规律.[结果]①1971-2024 年,河西走廊春玉米生育期有效降水量(Pe)变化趋势不明显,平均值为 111.6 mm,呈自西北向东南增加趋势;②春玉米生育期需水量(ET)平均值为 682.7 mm,呈自西北向东南递减的趋势,1971-1992 年呈不断下降趋势,主要与平均风速显著减小相关(P<0.01),1993-2024年呈逐渐增加的趋势,与气温升高、平均风速增大显著正相关(P<0.01);③1971-2024年春玉米灌溉需水量(Ir)平均值为 570.0 mm,呈先减少后逐渐增加的趋势,呈自西北向东南递减的趋势,Ir 与平均气温、最高气温、平均风速显著正相关(P<0.01),与有效降水量显著负相关(P<0.01);④春玉米生育期的灌溉需水指数(IDI)均值为 0.83,空间分布与灌溉需水量分布相似,西部灌溉需水量高于中部和东部.[结论]在西北暖湿化背景下,河西走廊春玉米需水量演变趋势与平均风速、气温变化显著相关,灌溉需水量与气温、平均风速、日照时间正相关,与有效降水量显著负相关,气候变暖导致春玉米灌溉需水量增加,使得水资源供需矛盾更加突出.

[Objective]The Hexi Corridor is an arid agricultural region in Northwest China,with spring maize being the dominant crop and the largest water consumer.Affected by ongoing climate warming,meteorological conditions in the region have changed substantially over recent decades,exerting feedback effects on crop water consumption and influencing sustainable agricultural development.This paper analyses the spatiotemporal variations in water requirement and irrigation water requirement of spring maize under the influence of climate warming in this region.[Method]The analysis was based on daily meteorological data collected from 1971 to 2024 from 17 meteorological stations across the region,and spring maize growth traits observed from 1991 to 2024 from three field agrometeorological stations.The single crop coefficient method and ArcGIS spatial analysis technology were used to analyse the spatiotemporal variations in effective precipitation(Pe),crop water requirement(ET),and irrigation water requirement(Ir)of the crop.[Result]①Temporally,there was no significant variation in Pe during the spring maize growing season,with a regional average of 111.6 mm.Spatially,Pe increased from the northwest to the southeast.②The regional average ET was 682.7 mm.Temporally,ET decreased from 1971 to 1992 followed by a continuous increase from 1993 to 2024.Spatially,it decreased gradually from the northwest to the southeast.③The average Ir was 570.0 mm;it had increased at a rate of 10.4 mm per decade.Spatially,Ir decreased from the northwest to the southeast.④The irrigation demand index of the crop was high during its entire growth period.[Conclusion]As Northwest China undergoes warming and wetting,the temporal variation in spring maize ET is significantly correlated with mean wind speed and air temperature.Ir is positively correlated with air temperature,mean wind speed,and sunshine duration,and negatively correlated with effective precipitation.Climate warming has resulted in an increase in irrigation water demand of spring maize,further aggravating the imbalance between agricultural water supply and demand in the region.

贾建英;马玉龙;张雅馨;方锋;王鹤龄;赵鸿;周忠文;王莺;殷雪莲;王帆;黄鹏程

兰州区域气候中心,兰州 730020兰州区域气候中心,兰州 730020兰州区域气候中心,兰州 730020兰州区域气候中心,兰州 730020中国气象局 兰州干旱气象研究所,中国气象局干旱气候变化与减灾重点实验室,甘肃省干旱气候变化与减灾重点实验室,兰州 730020中国气象局 兰州干旱气象研究所,中国气象局干旱气候变化与减灾重点实验室,甘肃省干旱气候变化与减灾重点实验室,兰州 730020庆阳市气象局,甘肃 庆阳 745000中国气象局 兰州干旱气象研究所,中国气象局干旱气候变化与减灾重点实验室,甘肃省干旱气候变化与减灾重点实验室,兰州 730020张掖市气象局,甘肃 张掖 734000兰州区域气候中心,兰州 730020兰州区域气候中心,兰州 730020

农业科技

气候变化春玉米河西走廊有效降水量需水量

climate changespring maizeHexi Corridoreffective precipitationwater requirement

《灌溉排水学报》 2026 (7)

10-18,9

中国气象局创新发展专项(CXFZ2024J056)甘肃省科技计划项目(25ZDFA011,25ZYJA035,24YFFA052,25JRRA1113,21JR7RA708,24JRRA1181)甘肃省气象局创新团队(GSQXCXTD-2026-01)

10.13522/j.cnki.ggps.2025341

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