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Comparisons of a numerical model and a water balance model to quantify soil water balance in root zone of winter wheat

机译:数值模型与水平衡模型的比较量化冬小麦根区土壤水平

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To obtain soil water balance components in root zone of winter wheat, a numerical model and a waterbalance model were established and compared in this study based on existing research results and Field experimental data of winter wheat seasons from 2007 to 2009 in Shijing Irrigation Scheme in Hebei province, China. The results are as follows :( 1) Mean Sum of Residuals Fraction (MSRF) and Root Mean Square Fraction (RMSF) between actual experimental and stimulated values of soil moisture of two models are both within 15%, but the accuracy of the waterbalance model is slightly higher because of the automated parameter optimization function provided by Vensim software which is used to build the waterbalance model, (2) two models present close simulated results in cumulative water balance components. Simulated dynamic process lines of actual soil evaporation, crop transpiration and 2m-soil water storage are very close as well, yet the water-balance model gives an upward flux due to capillary rise consideration, (3) compared with the numerical model, the water-balance model has hysteresis effect in simulated seepage process, and the peak of seepage process is slightly lower, which is caused by the roughness in spatial and temporal discretization. (4) less soil parameters are involved in the waterbalance model.
机译:为了获得冬小麦根区中的土壤水平衡分量,在河北2007年至2009年的冬小麦季节的现有研究成果和现场实验数据,在这项研究中建立了数值模型和疏树模型,并在河北省石井灌溉计划中的冬小麦季节的实地试验数据省,中国。结果如下:( 1)剩余物体分数(MSRF)的平均总和和两种模型的土壤水分的实际实验和刺激值之间的均方方分数(RMSF)均在15%以内,但疏水阀模型的准确性由于Vensim软件提供的自动参数优化功能略高,用于构建Waterbalance模型,(2)两种模型在累积水平衡组件中存在关闭模拟结果。模拟动态工艺生产线的实际土壤蒸发,作物蒸腾和2M土壤水储存非常接近,但由于毛细血管上升考虑,(3)与数值模型,水相比,水平模型给出了向上的助焊剂 - 平衡模型在模拟渗流过程中具有滞后效果,渗流过程的峰值略低,这是由空间和时间离散化的粗糙度引起的。 (4)Waterbance模型较少的土壤参数涉及。

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