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小时与日尺度PM公式的参照作物腾发量及其水稻单作物系数值差异
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  • 英文篇名:Difference in reference crop evapotranspiration calculated by PM equation and the corresponding single crop coefficient of rice between hourly scale and daily scale
  • 作者:王可纯 ; 蔡少杰 ; 卫琦 ; 吕玉平 ; 廖林仙 ; 徐俊增
  • 英文作者:WANG Kechun;CAI Shaojie;WEI Qi;L Yuping;LIAO Linxian;XU Junzeng;Key Laboratory of Efficient Irrigation-Drainage and Agricultural Soil-Water Environment in Southern China,Hohai University;State Key Laboratory of Hydrology-Water Resources and Hydraulic Engineering,Hohai University;
  • 关键词:ASCE ; PM公式 ; FAO56 ; PM公式 ; 不同时间尺度 ; 参考作物腾发量 ; 作物系数 ; 水稻
  • 英文关键词:ASCE penman-monteith formula;;FAO56 penman-monteith formula;;different temporal scales;;reference crop evapotranspiration;;crop coefficients;;rice
  • 中文刊名:XBSZ
  • 英文刊名:Journal of Water Resources and Water Engineering
  • 机构:河海大学南方地区高效灌排与农业水土环境教育部重点实验室;河海大学水文水资源与水利工程科学国家重点实验室;
  • 出版日期:2019-02-15
  • 出版单位:水资源与水工程学报
  • 年:2019
  • 期:v.30;No.143
  • 基金:江苏水利科技项目(2015089)
  • 语种:中文;
  • 页:XBSZ201901037
  • 页数:7
  • CN:01
  • ISSN:61-1413/TV
  • 分类号:250-256
摘要
以昆山试验站2012-2013年自动气象站观测的小时气象资料为依据,分别采用ASCE PM公式和FAO56PM公式计算小时ET_0,在对比两种小时ET_0计算结果基础上,通过逐小时累积求和得到日ET_0值(分别记作ET_(0-dhA)和ET_(0-dhF)),进而与日尺度参照作物腾发量ET_0(记作ET_(0-d))进行对比,在明确ET_(0-d),ET_(0-dhA)和ET_(0-dhF)差异的基础上,分析了基于不同ET_0确定的水稻单作物系数差异(分别记为K_(c-d)、K_(c-dhA)与K_(c-dhF))。结果表明:在水稻不同生育阶段内,小时ET_0值大致呈抛物线型日变化,在中午时ET_0达到最大,午夜则最低; 2种PM公式计算得到的小时ET_0值存在微小差异,差异范围在-0. 02~0. 5 mm/h内,白天ASCE PM公式计算值偏大,夜间则无明显规律。在日尺度上,ET_(0-d),ET_(0-dhA)和ET_(0-dhF)三者之间具有良好的线性关系,大小关系表现为:ET_(0-dhA)> ET_(0-d)> ET_(0-dhF)。总体上,由实测日腾发量ET_a求得的节水灌溉水稻单作物系数大于按照FAO推荐方法确定的作物系数值,且采用不同日ET_0计算结果得到的水稻K_c值之间的大小关系为:K_(c-dhA)        Based on the hourly meteorological data collected by an automatic meteorological station in Kunshan Experimental Station during 2012-2013,hourly ET_0 were calculated by ASCE PM and FAO56 PM formulas equations separately to show the difference in hourly ET_0 calculated by two different equations. Then the hourly ET_0 were summed up to obtain the daily ET_0 ( termed as ET_(0-dhA) and ET_(0-dhF)) and compared to the daily ET_0 calculated by PM equation at daily scale( ET_(0-d)). Differences among ET_(0-d),ET_(0-dhA) and ET_(0-dhF) were discussed,as well as the difference among the single crop coefficient of rice based on daily ET_0 determined by different procedures. The results showed that hourly ET_0 varied in parabolic shape,with the maximum observed at noon and minimum at midnight. Hourly ET_0 were slightly different between two methods,with the difference fell in range of -0. 02 ~ 0. 5 mm/h. Hourly ET_0 by ASCE PM were found slightly higher than by FAO56 PM in daytime. Daily ET_0 were highly correlated to each other,and ranked in sequence of ET_(0-dhA)> ET_(0-d)> ET_(0-dhF). Local calibrated single crop coefficient K_c of rice were higher than the value determined following the procedure by FAO,and ranked in sequence of K_(c-dhA)< K_(c-d)< K_(c-dhF),with the difference among them less than 5%.
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