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作物生长条件下的阿维里扬诺夫潜水蒸发公式改进
引用本文:罗玉峰,毛怡雷,彭世彰,郑 强,王卫光,缴锡云,冯跃华.作物生长条件下的阿维里扬诺夫潜水蒸发公式改进[J].农业工程学报,2013,29(4):102-109.
作者姓名:罗玉峰  毛怡雷  彭世彰  郑 强  王卫光  缴锡云  冯跃华
作者单位:1. 河海大学水文水资源与水利工程科学国家重点实验室,南京 2100982. 河海大学水利水电学院,南京 210098;1. 河海大学水文水资源与水利工程科学国家重点实验室,南京 2100982. 河海大学水利水电学院,南京 210098;1. 河海大学水文水资源与水利工程科学国家重点实验室,南京 210098;2. 河海大学水利水电学院,南京 210098;1. 河海大学水文水资源与水利工程科学国家重点实验室,南京 210098;1. 河海大学水文水资源与水利工程科学国家重点实验室,南京 210098;3. 河南省豫东水利工程管理局惠北水利科学试验站,开封 475101
基金项目:国家自然科学基金项目(50809021,51179048);水文水资源与水利工程科学国家重点实验室自主研究项目(2010585412);"十二五"国家科技支撑计划课题(2011BAD25B07)
摘    要:为提高作物生长条件下潜水蒸发强度计算精度,引入作物影响系数概念,提出2种阿维里扬诺夫潜水蒸发改进公式。采用河南惠北水利科学试验站2005-2007年的逐日潜水蒸发量与水面蒸发量试验数据和最小二乘法率定改进公式中各参数值,并用平均绝对误差、均方根误差和相关系数等3个统计指标对改进公式的计算精度进行评价,利用2007-2008年的试验数据对改进公式进行了验证。结果表明,提出的改进公式一的经验指数、潜水蒸发极限埋深以及各生育阶段的作物影响系数等参数值较为合理;验证期平均绝对误差0.30~0.59mm/d,均方根误差0.57~0.87mm/d,相关系数0.58~0.72,各统计指标值基本优于前人的研究,提高了潜水蒸发计算精度。

关 键 词:蒸发  模型  土壤  阿维里扬诺夫公式  作物系数
收稿时间:2012/7/10 0:00:00
修稿时间:2013/1/20 0:00:00

Modified Aver'yanov's phreatic evaporation equations under crop growing
Luo Yufeng,Mao Yilei,Peng Shizhang,Zheng Qiang,Wang Weiguang,Jiao Xiyun and Feng Yuehua.Modified Aver''yanov''s phreatic evaporation equations under crop growing[J].Transactions of the Chinese Society of Agricultural Engineering,2013,29(4):102-109.
Authors:Luo Yufeng  Mao Yilei  Peng Shizhang  Zheng Qiang  Wang Weiguang  Jiao Xiyun and Feng Yuehua
Institution:1.State Key Laboratory of Hydrology-Water Resources and Hydraulic Engineering,Hohai University,Nanjing 210098,China;2.College of Water Conservancy and Hydropower Engineering,Hohai University,Nanjing 210098,China;3.Huibei Water Science Experiment Station,East Henan Water Projects Management Bureau,Kaifeng 475100,China)
Abstract:Phreatic evaporation is an important component of the water balance in irrigated areas, and accurate estimates of phreatic evaporation are useful in regional water resources assessments and irrigation water management. Aver'yanov's equation with high accuracy is one of the most widely used empirical equations for estimating phreatic evaporation. To improve the calculation accuracy of phreatic evaporation under the crop growth conditions, the concept of crop influencing coefficient was introduced in this paper and two modified Aver'yanov equations were proposed based on the fact that the ratio of phreatic evaporation from crop-covered and bare soils regularly increases when the crop grows. The modified Aver'yanov Equation I used the crop coefficient estimating crop water requirements, reflecting the influences of crop growth on the phreatic evaporation. The crop has less impact on phreatic evaporation in the initial stage, and the impact gradually enhances the phreatic evaporation in the middle stage with phreatic evaporation maintaining at a relatively high level. At last, the effect of crop on phreatic evaporation drops down due to the maturity of the crop. In the second equation, the modified Aver'yanov Equation II, the effect of crop growth on the change of extinction depth was taken further into consideration. Lysimeter experiments were conducted at the Huibei Water Science Experiment Station during 2005-2007 in Henan Province, and the daily weather data and infiltration, runoff, evaporation data were collected, and then phreatic evaporation was calculated. Three statistical indicators, mean absolute error, root mean square error and correlation coefficient, were adopted to evaluate the performance of the modified equations. Experimental data were used to verify the values of parameters of the modified equations in crop growing season for 2007-2008. The results showed that the values of the empirical index, extinction depth and crop influencing coefficients of the modified Aver'yanov Equation I were within the reasonable range. For the verification period, the mean absolute error was 0.30-0.59 mm·d-1, the root mean square error was 0.57~0.87 mm·d-1, and the correlation coefficient was 0.58-0.72. The values of statistical indicators indicated that the modified Aver'yanov Equation I performed better than the equation reported in a previous study and Aver'yanov Equation II. The modified Aver'yanov Equation I has a rational structure and explicit physical meaning and this equation could be recommended calculating phreatic evaporation.
Keywords:evaporation  models  soils  aver'yanov's equation  crop coefficient
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