摘要
利用西峰农业气象试验站1989-1990和1990-1991年度旱作麦田土壤水分观测资料,采用零通量面法计算农田蒸散。结果表明,在旱农地区存在稳定少变的零通量面位置;农田蒸散随时间的变化一般多呈双峰型,但其谷值均在8月8日。
Using Observational data of soil moisture of dry wheat field in Xifeng agromete-orological station in 1989-1990 and 1990-1991,by means of the method of Zero flux sur-face that calculates farmland evapotranspiration. The resuLts show that positions of Zero fluxsurface tended to stabilize. Farmland evapotranspiration often appears by bimodal distribu-tion. But its valley value appears on August eighth.
出处
《干旱气象》
1995年第3期21-24,共4页
Journal of Arid Meteorology
关键词
旱田
零通量面
蒸散变化
Zero flux surface of dry farmland Evapotranspiration change