摘要
据奇台县多年气象数据和农业生产资料,应用方差分析外推法、农业生态区域法等方法,分析了温度和降水的变化特征、光温水生产潜力与粮食实际单产的关系。结果表明:温度和降水的整体变化过程可分为冷、干时段(1970-1981)、过渡时段(1982-1999)和暖、湿时段(2000-2006)。预计今后平均温度(2007-2014年)5.84℃和平均降水量(2007-2013年)207.61mm,较上一周期将分别增加0.14℃和10.35mm。光温水生产潜力模型精度较高(精度达94%),据此预测2007-2014年的粮食平均产量将达6338.25kg/hm2。光温水生产潜力变化可划分为三个阶段:低增长阶段(1970-1981年)、加速增长阶段(1982-1999年)和平稳阶段(2000-2006年)。其中,第三阶段的光温水生产潜力为第一阶段1.88倍。在干旱区,水分有效利用率是提高粮食生产潜力最主要的因素。
Based on the data of climate and agricultural production from 1970 to 2006 in Qitai County,the research analyzed the variation between temperature and rainfall,the relation of light-temperature-water potential productivity and grain yield by variance analysis,AEZ and so on.The results of research show that:the whole tendency of temperature and rainfall was divided into three phases:cold and dry(from 1970 to 1981),transition(from 1982 to 1999),warm and wet(from 2000 to 2006).The temperature(2007-2014,5.84℃)and precipitation(2007-2013,207.61mm) will be increased to 0.14℃,10.35mm.The light-temperature-water potential productivity model with high precision and accuracy rate of 94%,the grain yield is 6338.25kg/ha from 2007 to 2014.The tendency of light-temperature-water potential productivity and grain yield was divided into three stages:low-increased(1970-1981),accelerate-growed(1982-1999) and steady(2000-2006).The third stage of grain yield and light-temperature-water potential productivity for the first phase were 2.09 times,1.88 times.In addition to,the first two phases of grain yield was lower than 315.83kg/hm^2 with light-temperature-water potential productivity.But the third stage was opposite,the former was more than 82.04kg/hm2 for the latter.
出处
《干旱区资源与环境》
CSSCI
CSCD
北大核心
2011年第2期29-33,共5页
Journal of Arid Land Resources and Environment
基金
国家自然科学基金(40771194)
北京市属高等学校人才强教计划项目(PHR200906125)资助