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Crop rotations in Argentina: Analysis of water balance and yield using crop models

机译:阿根廷的作物轮作:使用作物模型分析水量平衡和产量

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摘要

Cropping schemes have developed in east-central Argentina for rainfed soybean (Glycine max Merr.) production that invariably employ no-tillage management. Often these schemes include growing soybean in a sequence of crops including wheat (Triticum aestivum L.) and maize (Zea mays L.). The full impact of various rotation schemes on soil water balance through a sequence of seasons has not been explored, although the value of these rotations has been studied experimentally. The objective of this work was to investigate through simulations, potential differences in temporal soil water status among rotations over five years. In this study, mechanistic models of soybean (Soy), maize (Maz), and wheat (Wht) were linked over a five-years period at Marcos JucLrez, Argentina to simulate soil water status, crop growth, and yield of four no-till rotations (Soy/Soy, Soy/Wht, Soy/Maz, and Soy/Maz/Wht). Published data on sowing dates and initial soil water contents in the first year from a no-till rotation experiment were used as inputs to the model. After the first year, soil water status output from the model was used to initiate the next crop simulation in the sequence. The results of these simulations indicated a positive impact on soil water balance resulting from crop residue on the soil surface under no-till management. Continuous soybean and the two-year soybean/maize rotation did not efficiently use the available water from rainfall. Residue from maize was simulated to be especially effective in suppressing soil evaporation. Thus, the Soy/Maz simulation results indicated that this rotation resulted in enhanced soil water retention, increased deep water percolation, and increased soybean yields compared with continuous soybean crops. The simulated results matched well with experimental observations. The three-crop rotation of Soy/Maz/Wht did not increase simulated soybean yields, but the additional water retained as a result of decreased soil evaporation resulting from the maize residue allowed the addition of a wheat crop in this two-year rotation. Simulated soybean yields were poorly correlated with both the amount of soil water at sowing and the rainfall during the cropping period. These results highlight the importance of temporal distribution of rainfall on final yield. These models proved a valuable tool for assessing the consequences of various rotation schemes now being employed in Argentina on temporal soil water status, and ultimately crop yield.
机译:在阿根廷中东部地区已经制定了雨育大豆(Glycine max Merr。)生产的种植计划,这些种植总是采用免耕管理。这些计划通常包括在一系列作物中种植大豆,包括小麦(Triticum aestivum L.)和玉米(Zea mays L.)。尽管已通过实验研究了这些轮换的价值,但尚未探讨各种轮换方案在整个季节中对土壤水平衡的全部影响。这项工作的目的是通过模拟研究五年内轮换之间土壤水分状况的潜在差异。在这项研究中,大豆(Soy),玉米(Maz)和小麦(Wht)的机理模型在阿根廷Marcos JucLrez的五年期间相互关联,以模拟土壤水分状况,作物生长和四种非玉米的产量。直到轮换(大豆/大豆,大豆/ WHT,大豆/马兹和大豆/马兹/ Wht)。免耕轮作试验第一年的播种日期和初始土壤含水量的公开数据用作模型的输入。第一年之后,使用该模型输出的土壤水分状态来启动序列中的下一个作物模拟。这些模拟的结果表明,在免耕管理下,土壤表面的农作物残留对土壤水分平衡有积极影响。连续的大豆和两年的大豆/玉米轮换没有有效利用降雨中的可用水。模拟了玉米中的残留物,对抑制土壤蒸发特别有效。因此,Soy / Maz模拟结果表明,与连续的大豆作物相比,这种轮作可提高土壤保水率,增加深水渗透并增加大豆产量。仿真结果与实验结果吻合良好。大豆/玉米/ Wht的三茬轮作不会增加模拟大豆的产量,但是由于玉米残留导致土壤蒸发减少而保留的额外水分使这两年的轮作增加了小麦作物。模拟的大豆单产与播种时的土壤水量和种植期间的降雨均不相关。这些结果突出了降雨时间分布对最终产量的重要性。这些模型被证明是评估阿根廷目前采用的各种轮换方案对暂时土壤水分状况以及最终作物产量的影响的有价值的工具。

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