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Farming system context drives the value of deep wheat roots in semi-arid environments

机译:耕作制度环境驱动半干旱环境中深小麦根的价值

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摘要

The capture of subsoil water by wheat roots can make a valuable contribution to grain yield on deep soils. More extensive root systems can capture more water, but leave the soil in a drier state, potentially limiting water availability to subsequent crops. To evaluate the importance of these legacy effects, a long-term simulation analysis at eight sites in the semi-arid environment of Australia compared the yield of standard wheat cultivars with cultivars that were (i) modified to have root systems which extract more water at depth and/or (ii) sown earlier to increase the duration of the vegetative period and hence rooting depth. We compared simulations with and without annual resetting of soil water to investigate the legacy effects of drier subsoils related to modified root systems. Simulated mean yield benefits from modified root systems declined from 0.1–0.6 t ha−1 when annually reset, to 0–0.2 t ha−1 in the continuous simulation due to a legacy of drier soils (mean 0–32mm) at subsequent crop sowing. For continuous simulations, predicted yield benefits of >0.2 t ha−1 from more extensive root systems were rare (3–10% of years) at sites with shallow soils (<1.0 m), but occurred in 14–44% of years at sites with deeper soils (1.6–2.5 m). Earlier sowing had a larger impact than modified root systems on water uptake (14–31 vs 2–17mm) and mean yield increase (up to 0.7 vs 0–0.2 t ha−1) and the benefits occurred on deep and shallow soils and in more years (9–79 vs 3–44%). Increasing the proportion of crops in the sequence which dry the subsoil extensively has implications for the farming system productivity, and the crop sequence must be managed tactically to optimize overall system benefits.
机译:小麦根吸收地下土壤水可以为深层土壤的谷物产量做出重要贡献。更大范围的根系可以捕获更多的水,但会使土壤保持更干燥的状态,这可能会限制随后的作物获得水。为了评估这些遗留效应的重要性,在澳大利亚半干旱环境中的八个地点进行了长期模拟分析,将标准小麦品种的产量与经过(i)改良后具有根系的品种进行了对比,深度和/或(ii)播种较早,以增加营养期的持续时间,从而增加生根深度。我们比较了有和没有每年重置土壤水的模拟,以研究与改良根系相关的较干土壤的遗留效应。改良根系模拟的平均产量收益从每年重置时的0.1–0.6 t ha -1 下降到连续模拟中的0–0.2 t ha -1 ,这是由于在随后的作物播种中,土壤较干(平均0–32mm)。对于连续模拟,在较浅的土壤(<1.0 m)处,从更广泛的根系获得的预计增产收益> 0.2 t ha −1 很少(占年的3–10%),但在在土壤较深的地方(1.6-2.5 m),有14-44%的年。与改良的根系相比,较早播种对水分吸收(14–31 vs 2–17mm)和平均单产增加(高达0.7 vs 0–0.2 t ha -1 )的影响更大,并且产生了收益在较深和较浅的土壤上以及更长的时间(9–79对3–44%)。大量增加使地下土壤干燥的顺序中的农作物比例对耕作系统的生产率有影响,因此必须从策略上管理农作物的顺序以优化整个系统的效益。

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