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海河流域不同下垫面土壤水分动态模拟研究
  • ISSN号:1001-8166
  • 期刊名称:地球科学进展
  • 时间:0
  • 页码:778-787
  • 分类:P332[天文地球—水文科学;水利工程—水文学及水资源;天文地球—地球物理学] S152.7[农业科学—土壤学;农业科学—农业基础科学]
  • 作者机构:[1]北京师范大学遥感科学国家重点实验室,地理学与遥感科学学院,北京100875
  • 相关基金:国家自然科学基金项目“基于探地雷达面反射法的土壤水分观测实验研究”(编号:41071225)和“地表水热通量的时空尺度扩展研究”(编号:40971194);中央高校基本科研业务费专项;中德合作项目“基于遥感和数据同化方法的海河流域水文通量预测研究--SP2:不同尺度蒸散量和土壤水分的观测研究”(编号:30911130504)资助.
  • 相关项目:地表水热通量的时空尺度扩展研究
中文摘要:

针对海河流域不同的下垫面类型,选取密云(果园林地)、大兴(城郊农田)、馆陶(平原农田)3个观测站,建立垂直方向上以含水率臼为因变量、含根系吸水项的非饱和土壤水分运动数值计算模型。该模型以一维Richards方程为基础(以下简称RE模型),采用实测的降水和蒸散数据作为模型的上边界条件,运用全隐式有限差分法,分别对不同生长期内的土壤水分进行数值模拟,得到时间序列的土壤水分廓线,并分别采用成熟软件HYDRUS-1D的模拟结果和各观测站实测土壤水分对RE模型进行交叉验证和直接验证。结果表明RE模型能够很好地模拟海河流域不同下垫面土壤水分动态变化过程,3个站模拟结果与实测土壤水分数据的均方根误差(RMSE)分别为0.03127,0.0359和0.0409cm3/cm3。与HYDRUS-1D软件模拟结果(其与观测值的RMSE分别为0.03759,0.0647和0.0467cm3/cm3)相比,RE模型模拟的土壤水分具有更高的精度,也显示出RE模型的可靠性。探讨3个站土壤水分的时空变异规律及其影响因子并以大兴站为例,通过优化RE模型参数,探讨犁底层对土壤水分模拟结果的影响,进一步改善RE模型的模拟精度。

英文摘要:

A vertical soil moisture (θ)-based unsaturated soil hydrodynamic numerical model was developed and used to simulate soil moisture movement at Miyun (orchard woodland), Daxing (Suburban farmland), Guan- tao (plain farmland) sites, which represent different underlying surface types in the Hai River Basin. The model based on one dimensional Richards' equation (hereinafter referred to as the RE model) and the top boundary was input ground-measured rainfall and evapotranspiration data. Soil moisture during different growth stages was numeri- cally simulated based on the fully implicit Finite Differential Method to obtain time series of soil moisture profile. Soil moisture simulated by mature HYDRUS-1D software and observed at the sites was used for cross-validation and direct verification on the RE model simulation results, respectively. The result showed that the RE model was able to simulate the soil water dynamic changes of different underlying surfaces in Hai River Basin, with root mean square error (RMSE) compared to the observed soil moisture at three sites being 0. 0313, 0. 0359 and 0. 0409 cm3/cm3, respectively. Compared to the simulation results of HYDRUS-1D software (whose RMSE were 0. 0376, 0. 0647 and 0. 0467 cm3/cm3 , respectively) , the soil water simulated by RE model had higher precision which also showed the RE model reliability. The spatial and temporal variation of soil moisture and its impact factors were dis- cussed. For the case of Daxing site,we analyzed the impact of plow on soil moisture modeling by optimizing the RE model parameters, under which consideration improved the simulation accuracy of the RE model was improved.

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期刊信息
  • 《地球科学进展》
  • 北大核心期刊(2011版)
  • 主管单位:中国科学院
  • 主办单位:中国科学院资源环境科学与技术局 国家自然科学基金委员会地球科学部 中国科学院资源环境科学信息中心
  • 主编:傅伯杰
  • 地址:兰州市天水中路8号
  • 邮编:730000
  • 邮箱:adearth@lzb.ac.cn
  • 电话:0931-8762293
  • 国际标准刊号:ISSN:1001-8166
  • 国内统一刊号:ISSN:62-1091/P
  • 邮发代号:54-86
  • 获奖情况:
  • 国家“双效”期刊,甘肃社优秀期刊,中国数字化优秀期刊
  • 国内外数据库收录:
  • 美国化学文摘(网络版),日本日本科学技术振兴机构数据库,中国中国科技核心期刊,中国北大核心期刊(2004版),中国北大核心期刊(2008版),中国北大核心期刊(2011版),中国北大核心期刊(2014版)
  • 被引量:36043