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改变根系结构如何有助于解决土壤中磷酸盐(P)水平降低的问题,从而更好地获取植物 P。

How changing root system architecture can help tackle a reduction in soil phosphate (P) levels for better plant P acquisition.

机构信息

Institute for Complex Systems Simulation, University of Southampton, Southampton, SO17 1BJ; Mathematical Sciences, Faculty of Social and Human Sciences, University of Southampton, Southampton, SO17 1BJ; Centre of Operational Research, Management Sciences and Information Systems, University of Southampton, Southampton, SO17 1BJ; IFLS Crop Systems Engineering, University of Southampton, Southampton, SO17 1BJ.

出版信息

Plant Cell Environ. 2015 Jan;38(1):118-28. doi: 10.1111/pce.12376. Epub 2014 Jun 24.

Abstract

The readily available global rock phosphate (P) reserves may run out within the next 50-130 years, causing soils to have a reduced P concentration which will affect plant P uptake. Using a combination of mathematical modelling and experimental data, we investigated potential plant-based options for optimizing crop P uptake in reduced soil P environments. By varying the P concentration within a well-mixed agricultural soil, for high and low P (35.5-12.5 mg L(-1) respectively using Olsen's P index), we investigated branching distributions within a wheat root system that maximize P uptake. Changing the root branching distribution from linear (evenly spaced branches) to strongly exponential (a greater number of branches at the top of the soil) improves P uptake by 142% for low-P soils when root mass is kept constant between simulations. This causes the roots to emerge earlier and mimics topsoil foraging. Manipulating root branching patterns, to maximize P uptake, is not enough on its own to overcome the drop in soil P from high to low P. Further mechanisms have to be considered to fully understand the impact of P reduction on plant development.

摘要

全球现有的易获取的磷矿(P)储备可能会在未来 50-130 年内耗尽,导致土壤中 P 浓度降低,从而影响植物对 P 的吸收。我们通过结合数学建模和实验数据,研究了在土壤 P 减少的环境中优化作物 P 吸收的潜在植物方案。通过在充分混合的农业土壤中改变 P 浓度,对于高 P(Olsen's P 指数为 35.5-12.5mg·L-1)和低 P(分别为 35.5-12.5mg·L-1),我们研究了在小麦根系中最大化 P 吸收的分枝分布。当模拟中保持根系质量不变时,将根系分枝分布从线性(均匀间隔的分支)改变为强指数(土壤顶部有更多的分支),可将低 P 土壤中的 P 吸收提高 142%。这使得根系更早出现,并模拟了表土觅食。仅通过操纵根系分枝模式来最大化 P 吸收,不足以克服高 P 到低 P 土壤中 P 含量的下降。需要进一步考虑其他机制,以充分了解 P 减少对植物发育的影响。

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