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甘肃河西地区膜下滴灌条件下春玉米田水盐特征分析
引用本文:杨宏伟,杨正华,侯淑梅,王增丽,张富仓.甘肃河西地区膜下滴灌条件下春玉米田水盐特征分析[J].干旱地区农业研究,2017,35(2):213-219.
作者姓名:杨宏伟  杨正华  侯淑梅  王增丽  张富仓
作者单位:1. 甘肃省水利厅石羊河流域管理局,甘肃武威,733000;2. 武威七中,甘肃武威,733000;3. 武威市中心灌溉试验站,甘肃武威,733000;4. 西北农林科技大学旱区农业水土工程教育部重点实验室,陕西杨凌,712100
基金项目:甘肃省水利技术推广项目
摘    要:通过对甘肃河西地区膜下滴灌春玉米种植条件下土壤水分、盐分的观测,分析了膜下滴灌春玉米生育期土壤水分、盐分动态变化及其产量和水分利用效率。结果表明:不同生育期,同一土层深度,土壤水分含量高低分布与土壤盐分含量高低分布相反,均表现出土壤不同深度盐分含量高的区域相应水分含量低,滴灌带之间土壤盐分积累较滴头之间显著;灌水定额480 m~3·hm~(-2)处理,灌溉水分在土层纵向运移显著,深层渗漏明显,灌水定额420 m~3·hm~(-2)处理,灌溉水在土壤不同深度横向层面运移显著,有利于作物吸收利用;膜下滴灌能够在滴水过程中明显降低土壤表层0~40 cm盐分含量,土壤下层40~100 cm为盐分聚集区域;灌水定额420 m~3·hm~(-2)处理,春玉米产量构成和水分利用效率较高。从作物生长水盐环境及高效节水的角度出发,灌水定额420 m~3·hm~(-2)处理的效益最优。

关 键 词:膜下滴灌  春玉米田  灌水定额  水盐运移  产量

Analysis of soil water and salt characteristics in farmland of spring maize under mulched drip irrigation in Hexi Region of Gansu Province
YANG Hong-wei,YANG Zheng-hu,HOU Shu-mei,WANG Zeng-li,ZHANG Fu-cang.Analysis of soil water and salt characteristics in farmland of spring maize under mulched drip irrigation in Hexi Region of Gansu Province[J].Agricultural Research in the Arid Areas,2017,35(2):213-219.
Authors:YANG Hong-wei  YANG Zheng-hu  HOU Shu-mei  WANG Zeng-li  ZHANG Fu-cang
Institution:Basin Management Bureau of Shiyang River, The Water Resources Department of Gansu Province, Wuwei, Gansu 733000, China,Basin Management Bureau of Shiyang River, The Water Resources Department of Gansu Province, Wuwei, Gansu 733000, China,Seventh Middle School of Wuwei, Wuwei, Gansu 733000, China,Central Irrigation Experiment Station of Wuwei, Wuwei, Gansu 733000, China and Key Laboratory of Agricultural Soil and Water Engineering in Arid and Semiarid Areas, Ministry of Education, Northwest A&F University, Yangling, Shaanxi 712100, China
Abstract:Through the observation of soil water and salt in the farmland of spring maize under mulched drip irrigation in Hexi Region of Gansu Province,the characteristics of soil moisture and salt dynamic change,and the yield and water use efficiency of maize were analyzed.The results showed that the distribution of soil moisture content in different soil profiles at different growth stages was opposite to that of salt content,i.e.,in the soil profiles where there was a high salt content,there was a low moisture content.The salt accumulation at the imerval of drip pipes was significantly higher than that at the interval of emitters.Under the irrigation quota of 480 m3· hm-2,the irrigated water moved significantly along vertical direction and the deep leakage was remarkable;under the irrigation quota of 420 m3· hm-2,the irrigated water moved significantly along horizontal direction in different depth,being beneficial to the absorption and utilization of crop.Mulched drip irrigation could significantly reduce soil salt content in 0 ~ 40 cm profile,while the profile of 40 ~100 cm was the accumulating zone of salt during drip process.Under the irrigation quota of 420 m3· hm-2,the yield and water use efficiency of spring maize were relatively high.Therefore,from the viewpoim of water and salt environment as well as efficient water-saving,the benefit of the irrigation quota of 420 m3 ·hm-2 was the best.
Keywords:mulched drip irrigation  spring maize farmland  irrigation quota  water and salt movement  yield
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