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Simulation of Water and Nitrate Transport in Soil Using HYDRUS-1D Model in Furrow Irrigation of Sugarcane

机译:利用HYDRUS-1D模型进行甘蔗沟灌的土壤水氮运移模拟。

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Simulation of water and solute transport in soil is very useful for optimum management of water and fertilizer use. In this study, the HYDRUS-1D model was used to simulate water and nitrate transport in furrow irrigation of sugarcane. For this putpose, a large-scale experiment was performed as a split plot design based on the randomized complete blocks with 3 replications in a 25-hectare piece of land in the Dehkhoda Sugarcane Agro-Industry Company from March 2012 to October 2013. The main factor was split application of fertilizer at three levels: two, three and four splits. The sub-main factor was fertilizer amount, applied at three levels (i.e. 350, 280 and 210 kg urea corresponding to 100%, 80% and 60% fertilizer requirements, respectively). Soil hydraulic parameters were estimated through inverse modeling using moisture data collected during more than 4 months of the sugarcane growing season. Solute transport parameters were then estimated using the hydraulic parameters and nitrate concentration data. In this study, statistical criteria including R2, RMSE, ME and SSQ were used to compare the observed and simulated values of moisture content and nitrate concentration. The results indicated that R2 for simulated moisture content and nitrate concentration in four splits and 60% fertilizer requirement treatment (i.e. calibrated treatment) were 62.7 and 91.2 percent, respectively. Cumulative infiltration depths were about 46 and 58 mm for calibration and validation treatments, respectively. For these treatments, the cumulative evapotranspiration rates were 50 and 60 mm, respectively. Soil moisture content in the surface layer varied from 21 to 45 and 21 to 42 percent, for calibration and validation treatments, respectively while the changes in the deep layer moisture content were 33 to 38 percent, for both treatments.
机译:模拟土壤中水和溶质的运移对于优化水和肥料的使用非常有用。在这项研究中,HYDRUS-1D模型用于模拟甘蔗沟灌中的水和硝酸盐迁移。为此,从2012年3月至2013年10月,在Dehkhoda Sugarcane Agro-Industry Company的25公顷土地上,基于随机完整块并进行了3次重复试验,以分割图设计的形式进行了大规模实验。影响因素是在三个水平上分别施肥:两个,三个和四个分裂。次要因素是施肥量,分三个等级施用(即分别对应于100%,80%和60%肥料需求的350、280和210 kg尿素)。通过使用甘蔗生长季节超过4个月期间收集的水分数据,通过反演模型估算土壤水力参数。然后使用水力参数和硝酸盐浓度数据估算溶质运移参数。在这项研究中,使用包括R2,RMSE,ME和SSQ在内的统计标准来比较水分含量和硝酸盐浓度的观察值和模拟值。结果表明,在4个分割段和60%需肥处理(即校准处理)中,模拟水分含量和硝酸盐浓度的R2分别为62.7%和91.2%。校准和验证处理的累积渗透深度分别约为46和58 mm。对于这些处理,累积蒸散速率分别为50和60 mm。对于校准和验证处理,表层土壤水分含量分别为21%至45%和21%至42%,而两种处理方法的深层水分含量变化均为33%至38%。

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