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应用生态学报 ›› 1997, Vol. 8 ›› Issue (2): 139-142.

• 研究论文 • 上一篇    下一篇

黄土塬区旱作玉米生产潜力的实验研究

刘文兆, 魏翔, 李玉山   

  1. 中国科学院水利部水土保持研究所, 杨陵 712100
  • 收稿日期:1996-01-03 修回日期:1996-09-10 出版日期:1997-03-25 发布日期:1997-03-25
  • 基金资助:

    国家自然科学基金(59509001)

Potential productivity of dryland spring corn on Loess tableland

Liu Wenzhao, Wei Xiang, Li Yushan   

  1. Institute of Soil and Water Conservation, Academia Sinica and Ministry of Water Resources, Yangling 712100
  • Received:1996-01-03 Revised:1996-09-10 Online:1997-03-25 Published:1997-03-25

摘要: 在黄土高原南部长武旱塬所做的田间试验结果表明,玉米的水分效应函数为:Pw=1.00-5.293(1-k)2把式中k取为农田干湿指数(旱作玉米全生育期内高肥水平下耗水量与需水量的比值),则Pw即为旱作玉米生产潜力指数.试验中k值的表现区间为0.78至1.10,k值的理论上界与局部农田潜在蒸散有关.1985~1988年,旱作玉米的Pw的平均值为0.87.旱作玉米生产潜力的远期值与近期值变化趋势相似,前者4年平均值为11247kg·hm-2,后者为7696kg·hm-2.由于试区近年来物质能量向农田的不断强化投入以及对作物品种的改良,试区大田实际产量连年来向潜力值逼近.

关键词: 旱作生产潜力, 玉米, 黄土高原, PROSAIL模型, 植被等值线, 缨帽三角, 叶面积指数, WorldView 3

Abstract: According to the field experiments on Changwu tableland of southern Loess Plateau,the function of corn yield response to water could be described as: Pw=1.00-5.293(1-k)2 ,where Pw is the potential productivity index of dryland corn, and k is the water stress index, a ratio of water consumption to water requirement during the entire growth period of dryland corn under high soil fertility conditions.The k value varies from 0.78 to 1.10,and its theoretical upper limit is related to the local potential evapotranspiration.The average Pw was 0.87 from 1985 to 1988.Its long term value has a similar fluctuating trend with the short term one over the four years.The former was 11247 kg·hm-2,and the latter was 7696 kg·hm-2.The actual yields in the field experimental region during recent years approach to the short term value,due to the high input of fertilizers and the improvement of crop varieties.

Key words: Potential productivity of dryland crop, Corn, Loess Plateau, PROSAIL model, leaf area index, vegetation isoline, tasseled cap triangle, WorldView 3