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路 璐, 王振龙, 杜富慧, 胡永胜, 张晓萌.淮北平原基于水文气象多因子的土壤水分动态预测水资源与水工程学报[J].,2019,30(4):237-243
淮北平原基于水文气象多因子的土壤水分动态预测
Dynamic prediction of soil moisture based on hydrometeorological multi-factors in Huaibei Plain
  
DOI:10.11705/j.issn.1672-643X.2019.04.37
中文关键词:  冬小麦  土壤水分  水文气象因子  灰色关联度  多元线性回归  土壤水分动态
英文关键词:winter wheat  soil moisture  hydrometeorological factors  grey correlation degree  multiple linear regression  soil moisture dynamic
基金项目:国家重点研发计划课题(2017YFC0404504)
作者单位
路 璐1, 王振龙2, 杜富慧1, 胡永胜2, 张晓萌1 (1.河北工程大学 水利水电学院 河北 邯郸 056021 2.安徽省(水利部淮委)水利科学研究院 安徽 蚌埠 233000) 
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中文摘要:
      为研究土壤水分动态变化,利用五道沟水文实验站1989-2015年水文气象和大田土壤水实测资料,采用灰色关联度和线性回归分析,建立了冬小麦各生长阶段不同土层土壤水分预测模型。结果表明:不同土层土壤水分与气象因子的关联度一致;不同生长阶段土壤水分与气温和地下水埋深关联度最强,分别达0.92和0.95;分蘖-越冬期,土壤水分与地下水埋深和日照时数关联度最强,其他生长阶段,土壤水分与气温和地下水埋深关联度最强。通过水文气象因子模拟土壤水分拟合度较高,R2达0.94。不同生长阶段不同土层,土壤水分计算模型均具有良好的预测能力,R2达0.80。成果为实施作物不同生长阶段的灌溉计划提供科学依据。
英文摘要:
      To study the dynamic changes of soil moisture, the gray correlation and multiple linear regression analysis were used based on hydrological meteorological and soil water measurements data from 1989 to 2015 at Wudaogou Hydrological Experiment Station, and Hydrological and meteorological factors and soil moisture prediction models in different soil layers at each growth stage of winter wheat were established. The results indicated that the correlation degree between soil moisture and meteorological factors in different soil layers at the same growth stage was the same. The correlation degree between soil moisture and temperature and groundwater depth was the strongest, with correlation coefficient 0.92 and 0.95, respectively. During the tillering-overwintering period, the correlations between soil moisture and groundwater depth, sunshine hours was the strongest, while the correlation degree between soil moisture and temperature, groundwater depth was the strongest in other growth stages. The fitting of soil moisture by hydrometeorological factors was relatively high (R2=0.94). The soil moisture calculation models have different prediction ability in different soil layers at different growth stages (R2= 0.80).This study provides a basis for the implementation of irrigation plans at different stages of crop growth.
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