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Analysis of 2,4-D residues in soil profile using HYDRUS-1D model

机译:使用HYDRUS-1D模型分析土壤剖面中的2,4-D残留

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Despite the benefits of herbicides, their persistence in soil can harm other plants in next rotations and contaminate ground water. The main purpose of this research is to simulate 2,4-dichlorophenoxyaceticacid(2,4-D) movement in silty clay loam soil using HYDRUS-1D model in a corn root zone. The maximum contaminant level goal, MCLG, of 2,4-D in water resources is 10 ppb. The 3.5 kg a.i ha-1 of 2,4-D was applied to the experimental field under two irrigation treatments including normal and deficit irrigation. The presence of 2,4-D along with soil water content was measured in soil profile at different depths during the growing season at 8, 13, 23, 30, 37 and 57 days after application. Both measured and simulated data showed that 2,4-D concentrations reduced from top to bottom of soil profile, maximum 40 cm in both irrigation treatments. The 2,4-D residues in normal and deficit irrigation were used for calibration and validation of HYDRUS-1D model, respectively. In general, total measured and simulated 2,4-D concentration in normal irrigation treatment were 68.94 and 64.96 mg kg-1and in deficit irrigation treatment were 74.3 and 74.0 mg kg-1, respectively. Statistical parameters including NRMSE, CRM and d were used for comparison of measured and simulated data. These parameters were 0.267, 0.77 and 0.846 for normal irrigation and 0.189, -0.02 and 0.937 for deficit regime, respectively. Therefore, the results showed a good agreement between measured values of herbicide residue and the values simulated using HYDRUS 1D model. The numerical simulations for deficit irrigation regime were more precise than normal irrigation because of less microbial activity due to less soil moisture. The numerical models could not simulate microbial activity with acceptable accuracy.
机译:尽管除草剂有很多好处,但它们在土壤中的持久性在下一轮耕作中可能损害其他植物并污染地下水。本研究的主要目的是使用HYDRUS-1D模型在玉米根区模拟2,4-二氯苯氧基乙酸(2,4-D)在粉质粘土壤土中的运动。水资源中2,4-D的最大污染物水平目标MCLG为10 ppb。将3.5 kg a.i ha-1的2,4-D在包括普通灌溉和亏水灌溉在内的两种灌溉处理下施用于实验田。在施用后第8、13、23、30、37和57天的生长季节中,在不同深度的土壤剖面中测量了2,4-D与土壤水分的存在。实测数据和模拟数据均显示,从土壤剖面的顶部到底部,2,4-D浓度均降低,两种灌溉处理均达到最大40 cm。正常灌溉和亏缺灌溉中的2,4-D残留分别用于HYDRUS-1D模型的校准和验证。通常,正常灌溉处理中的总测量和模拟2,4-D浓度分别为68.94和64.96 mg kg-1,而在亏水灌溉处理中分别为74.3和74.0 mg kg-1。包括NRMSE,CRM和d在内的统计参数用于比较测量数据和模拟数据。对于正常灌溉,这些参数分别为0.267、0.77和0.846,对于缺水状况,这些参数分别为0.189,-0.02和0.937。因此,结果表明除草剂残留的测量值与使用HYDRUS 1D模型模拟的值之间有很好的一致性。亏缺灌溉制度的数值模拟比常规灌溉更为精确,因为土壤水分较少,微生物活动较少。数值模型不能以可接受的精度模拟微生物活动。

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