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Modeling runoff and soil water balance under mechanized conservation tillage in dry land of north China

机译:北方旱地机械化耕作下的径流和土壤水平

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PERFECT (Productivity Erosion and Runoff Functions to Evaluate Conservation Techniques), which has been widely used in Australia, is designed to predict runoff, erosion and crop yield under various management pratices including residue, tillage, sequences of plantings, harvesting and stubble managements in dryland cropping areas. The objectives of this study were to modify and calibrate PERFECT to simulate the impacts of tillage, residue and traffic on runoff and soil water balance under conservation tillage of small- to medium-sized machinery, and to assist identifying appropriate conservation practices for sustained crop production in dry land areas of Northern China. The procedure of runoff prediction using USDA Curve Numbers was modified by incorporating the effects of field slope and rainfall intensity. Runoff was calculated daily as a function of rainfall, soil water, residue cover, slope, surface roughness resulted from tillage, and rainfall energy. A simplified Priestley-Taylor equation was employed in the model to calculate potential evapotranspiration, and the effect of residue cover on evapotranspiration was also considered in the model. Input data for the simulation model included daily weather, runoff, soil hydraulic properties, plant available water capacity, cropping systems, and traffic and tillage management. Data were collected from field experiments on Loess Plateau of Northern China. Preliminary results of model calibration and validation showed that the R~2 between predicted and observed runoff was 0.86~0.90 and R~2 between predicted and observed available soil moisture was 0.82~0.94.
机译:PERFECT(生产力侵蚀和径流的功能,以评估保护技术),它已广泛应用于澳大利亚,目的是为了预测下各种管理pratices包括残渣,耕作,种植的序列,收获和旱地茬管理层径流,土壤侵蚀和作物产量裁剪区域。本研究的目标是修改和校准完美,以模拟耕作,残留和交通在小于中小型机械的保护耕作下对径流和土壤水平的影响,并协助识别持续作物生产的适当保护措施在中国北方的旱地地区。通过结合现场斜坡和降雨强度的影响来修改使用USDA曲线数进行径流预测程序。每天计算径流作为降雨,土壤水,残留盖,坡度,表面粗糙度,从耕作引起的表面粗糙度以及降雨能量。在模型中使用简化的普利斯特利 - 泰勒方程来计算潜在的蒸散,并且在模型中也考虑了残留物覆盖物对蒸散物的影响。仿真模型的输入数据包括每日天气,径流,土壤液压性能,植物可用水力容量,种植系统和交通和耕作管理。从中国北方黄土高原的现场实验中收集了数据。模型校准和验证的初步结果表明,预测和观察到的径流之间的R〜2为0.86〜0.90,预测和观察到的土壤水分之间的R〜2为0.82〜0.94。

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