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Plant root tortuosity: an indicator of root path formation in soil with different composition and density

机译:植物根曲折度:指示不同组成和密度的土壤中根路径形成的指标

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摘要

>Background and Aims Root soil penetration and path optimization are fundamental for root development in soil. We describe the influence of soil strength on root elongation rate and diameter, response to gravity, and root-structure tortuosity, estimated by average curvature of primary maize roots.>Methods Soils with different densities (1·5, 1·6, 1·7 g cm−3), particle sizes (sandy loam; coarse sand mixed with sandy loam) and layering (monolayer, bilayer) were used. In total, five treatments were performed: Mix_low with mixed sand low density (three pots, 12 plants), Mix_medium - mixed sand medium density (three pots, 12 plants), Mix_high - mixed sand high density (three pots, ten plants), Loam_low sandy loam soil low density (four pots, 16 plants), and Bilayer with top layer of sandy loam and bottom layer mixed sand both of low density (four pots, 16 plants). We used non-invasive three-dimensional magnetic resonance imaging to quantify effects of these treatments.>Key Results Roots grew more slowly [root growth rate (mm h–1); decreased 50 %] with increased diameters [root diameter (mm); increased 15 %] in denser soils (1·7 vs. 1·5 g cm–3). Root response to gravity decreased 23 % with increased soil compaction, and tortuosity increased 10 % in mixed sand. Response to gravity increased 39 % and tortuosity decreased 3 % in sandy loam. After crossing a bilayered–soil interface, roots grew more slowly, similar to roots grown in soil with a bulk density of 1·64 g cm–3, whereas the actual experimental density was 1·48±0·02 g cm–3. Elongation rate and tortuosity were higher in Mix_low than in Loam_low.>Conclusions The present study increases our existing knowledge of the influence of physical soil properties on root growth and presents new assays for studying root growth dynamics in non-transparent media. We found that root tortuosity is indicative of root path selection, because it could result from both mechanical deflection and active root growth in response to touch stimulation and mechanical impedance.
机译:>背景和目标:根系土壤渗透和路径优化是土壤根系发育的基础。我们用原始玉米根的平均曲率描述了土壤强度对根系伸长率和直径,对重力的响应以及根系弯曲的影响。>方法不同密度的土壤(1·5,使用1·6、1·7μgcm −3 ),粒径(砂壤土;粗砂和砂壤土混合)和分层(单层,双层)。总共进行了五种处理:Mix_low-低密度混合砂(三盆,十二株),Mix_medium-中等密度混合砂(三盆,十二株),Mix_high-高密度混合砂(三盆,十株), Loam_low沙质壤土的土壤密度低(4个盆栽,有16种植物),双层沙质壤土的顶层和底层混合了低密度的沙子(4个盆栽,有16种植物)。我们使用无创三维磁共振成像来量化这些治疗的效果。>主要结果,根的生长较慢[根生长速率(mm h –1 );直径[根部直径(mm)增大,减小50%];在较稠密的土壤中增加了15%](1·7与1·5μgcm –3 )。随着土壤压实度的增加,根系对重力的响应降低了23%,而在混合砂土中,弯曲度提高了10%。砂壤土对重力的反应增加了39%,曲折度降低了3%。穿过双层-土壤界面后,根的生长更加缓慢,类似于在土壤中以1·64μgcm –3 的堆积密度生长的根,而实际实验密度为1·48±0 ·02 g cm –3 。 >结论:本研究增加了我们对物理土壤性质对根系生长影响的现有知识,并提出了用于研究非透明根系生长动力学的新方法媒体。我们发现根的曲折度表明了根路径的选择,因为它可能是由于机械变形和响应触摸刺激和机械阻抗而引起的主动根生长的结果。

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