Modelling variety dependant least limiting water range: assessing the limits to root elongation in field soil.

模拟品种相关的最小限制水范围：评估田间土壤中根系伸长的限制。

• 批准号: 1805417
• 金额: --
• 依托单位: University of Nottingham
• 依托单位国家: 英国
• 项目类别: Studentship
• 财政年份: 2016
• 资助国家: 英国
• 起止时间: 2016 至 无数据
• 项目状态: 已结题
• 来源: https://gtr.ukri.org/projects?ref=studentship-1805417
• 关键词: Modelling; variety; dependant; least; limiting

Compaction is listed as one of the major issues affecting many UK soils and can limit crop yields. Compaction affects the integral network of soil particles and pores that comprise field soil, reducing the pore space and affecting the water holding capacity and the hydraulic properties of soil. The soil texture and moisture content can also influence the hardness of the soil. Root elongation is restricted if the soil is too hard for the roots to penetrate, lacks oxygen or is under water deficit conditions. The response of an average plant / root to these variable properties can be captured graphically as the least limiting water range (LLWR, See Figure: the range of water in a specific soil that does not significantly limit plant growth, calculated using standard growth limiting factors of soil strength (SS), wilting point (WP) and oxygen deficiency (OD). )This calculation takes into account average limits of soil strength, oxygen deficiency and water deficit. However crop varieties differ particularly in their root elongation responses to differences in water deficit and soil strength. These differences are underpinned by variances in root traits and how these relate to the pore structure, water availability and soil strength (e.g. Border cells assist in elongation in compacted soil). There is therefore an integral link between plant trait effectiveness in assisting in plant performance and the soil structure. The aim of this project is to develop a model based on the LLWR visual approach that allows the effect of root: soil interactions on individual varieties to be taken into account based on the rooting traits. The model will assist in assessing whether differences in variety responses to soil tillage are linked to underlying variances in the limiting water ranges for the specific varieties and their response to complex soils.

压实被列为影响许多英国土壤的主要问题之一，并可能限制作物产量。压实影响了土壤颗粒和孔隙组成的完整网络，减少了孔隙空间，影响了土壤的持水能力和水力特性。土壤质地和含水量也会影响土壤的硬度。如果土壤太硬，根无法穿透，缺乏氧气或处于缺水条件下，则根伸长受到限制。平均植物/根对这些可变特性的响应可以图形化地捕获为最小限制水分范围（LLWR，参见图：在特定土壤中不显著限制植物生长的水分范围，使用土壤强度（SS）、萎蔫点（WP）和缺氧（OD）的标准生长限制因子计算。这种计算考虑了土壤强度、缺氧和缺水的平均极限。然而，作物品种对水分亏缺和土壤强度差异的根伸长反应尤其不同。这些差异是由根性状的差异以及这些性状与孔隙结构、水分供应和土壤强度的关系（例如，边缘细胞有助于压实土壤的伸长）所支撑的。因此，在植物性状的有效性，以协助植物性能和土壤结构之间有一个不可分割的联系。该项目的目的是开发一个基于LLWR可视化方法的模型，该模型允许根：土壤相互作用对单个品种的影响基于生根性状被考虑在内。该模型将有助于评估不同品种对土壤耕作的反应差异是否与特定品种的限制水分范围及其对复杂土壤的反应的潜在差异有关。