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The effect of parameter uncertainty on DRAINMOD predictions for hydrology, yield and water quality.

机译:参数不确定性对DRAINMOD预测的水文,产量和水质的影响。

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摘要

Reducing the nutrient levels in sensitive coastal waters has become a national priority. Agriculture has been targeted as a significant contributor to the nutrient problem. Controlled drainage has been recognized as one way to reduce nitrate losses from agricultural fields requiring subsurface drainage. The computer model DRAINMOD can be used to determine the effect of drainage design on the rate of subsurface drainage, crop yield and water quality. An uncertainty analysis was conducted to quantitatively assess the variability in model results caused by parameter uncertainty. The methodology included a sensitivity analysis, First Order Approximation and Monte Carlo Simulation. The objective functions evaluated were average annual subsurface drainage, SEW30, relative yield, NO3-N loss via subsurface drainage, NO3-N loss via surface runoff, and NO3-N transformation by denitrification for conventional and controlled drainage. Base values for the parameters were taken from an experimental site in Plymouth, North Carolina. The predominant soil type at the site was a poorly drained Portsmouth sandy loam. Results of the analysis showed that the majority of the uncertainty in the hydrology/yield objective functions was caused by the uncertainty in the horizontal saturated hydraulic conductivity and the maximum surface storage. The majority of the uncertainty in the water quality objective functions was caused by the denitrification rate constant. Despite the uncertainty in the model objective functions a clear difference between controlled drainage and conventional drainage was found for all of the objective functions. Monte Carlo Simulations for conventional and controlled drainage showed significant (alpha = 0,05) reductions of NO3-N (29%) at the field edge.
机译:减少敏感沿海水域的营养水平已成为国家优先事项。农业已成为营养问题的重要贡献者。控制排水是减少需要地下排水的农田中硝酸盐损失的一种方法。计算机模型DRAINMOD可用于确定排水设计对地下排水速率,作物产量和水质的影响。进行了不确定性分析,以定量评估由参数不确定性引起的模型结果的可变性。该方法包括敏感性分析,一阶近似和蒙特卡洛模拟。评估的目标函数是:年平均地下排水量,SEW30,相对产量,地下排水造成的NO3-N损失,地面径流引起的NO3-N损失以及常规和控制排水的反硝化NO3-N转化。参数的基值取自北卡罗来纳州普利茅斯的一个实验点。该地点的主要土壤类型是排水不良的朴茨茅斯沙壤土。分析结果表明,水文/屈服目标函数的大部分不确定性是由水平饱和导水率和最大表层存储的不确定性引起的。水质目标函数的大部分不确定性是由反硝化速率常数引起的。尽管模型目标函数存在不确定性,但所有目标函数在受控排水和常规排水之间都存在明显差异。常规排水和受控排水的蒙特卡洛模拟显示,在田间边缘,NO3-N的减少量很大(α= 0.05)(29%)。

著录项

  • 作者

    Haan, Patricia Kay.;

  • 作者单位

    North Carolina State University.;

  • 授予单位 North Carolina State University.;
  • 学科 Engineering Agricultural.;Hydrology.;Agriculture Soil Science.
  • 学位 Ph.D.
  • 年度 2000
  • 页码 152 p.
  • 总页数 152
  • 原文格式 PDF
  • 正文语种 eng
  • 中图分类
  • 关键词

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