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土壤湿度决定了生长在喀斯特土壤中的多年生草本植物L. 的水平和垂直根系延伸。

Soil Moisture Determines Horizontal and Vertical Root Extension in the Perennial Grass L. Growing in Karst Soil.

作者信息

Zhang Jing, Wang Jiamin, Chen Jinyi, Song Haiyan, Li Suhui, Zhao Yajie, Tao Jianping, Liu Jinchun

机构信息

Key Laboratory of Eco-environments in Three Gorges Reservoir Region (Ministry of Education), Chongqing Key Laboratory of Plant Ecology and Resources Research in Three Gorges Reservoir Region, School of Life Sciences, Southwest University, Chongqing, China.

出版信息

Front Plant Sci. 2019 May 15;10:629. doi: 10.3389/fpls.2019.00629. eCollection 2019.

Abstract

Karst regions are characterized by heterogeneous soil habitats, with shallow wide soil (SW) on hilly slopes and deep narrow soil (DN) in rocky trenches. To make full use of limited water and nutrients, plants have therefore developed a number of root extension strategies. This study investigated the effect of soil moisture on horizontal root extension in SW and vertical root extension in DN by assessing root growth responses, biomass allocation, and root distribution. A full two-way factorial blocked design of soil dimensions by water availability was followed. The perennial grass L. was grown in SW and DN under high (W100%), moderate (W50%), and low (W30%) water availability, respectively. The main results were as follows: (1) The total biomass of was not influenced either by soil habitat or by water application. Root length, root surface area, root biomass and root to shoot ratio all decreased with decreasing water application in SW, but not in DN soil. (2) With decreasing water application, the cumulative percentage of root length, root surface area and root biomass in 4 rings from the center out to 12 cm of SW soil showed a trend of W50% > W30% > W100% in SW, however, the cumulative percentage of root biomass in 4 layers from the surface to a depth of 36 cm was not significantly different between different water treatments in DN. (3) Under all three water treatments, specific root length showed an increase but root length density showed a decreasing trend from the center outward in SW soil or from the surface to bottom in DN soil. Overall, these results suggest that in SW habitat, soil moisture determines horizontal expansion of the roots in , although the overall expansion ability was limited in severe drought. However, due to the relatively strong water retention ability, soil moisture changes were less obvious in DN, resulting in no significant vertical extension of the root system. The root response of helps our understanding of how herbaceous plants can adjust their belowground morphology to support their growth in harsh karst soil environments.

摘要

岩溶地区的土壤生境具有异质性,山坡上有浅薄宽广的土壤(SW),岩石沟壑中有深厚狭窄的土壤(DN)。因此,为了充分利用有限的水分和养分,植物发展出了多种根系延伸策略。本研究通过评估根系生长响应、生物量分配和根系分布,研究了土壤水分对SW土壤中根系水平延伸和DN土壤中根系垂直延伸的影响。采用了土壤维度与水分有效性的完全双因素区组设计。多年生草本植物L.分别在高(W100%)、中(W50%)和低(W30%)水分有效性条件下的SW和DN土壤中生长。主要结果如下:(1)L.的总生物量不受土壤生境或水分施用的影响。在SW土壤中,根长、根表面积、根生物量和根冠比均随水分施用量的减少而降低,但在DN土壤中则不然。(2)随着水分施用量的减少,SW土壤中从中心向外至12 cm的4个环带内根长、根表面积和根生物量的累积百分比呈现W50%>W30%>W100%的趋势,然而,DN土壤中从地表至36 cm深度的4个土层内根生物量的累积百分比在不同水分处理之间无显著差异。(3)在所有三种水分处理下,比根长在SW土壤中从中心向外或在DN土壤中从地表至底部均呈现增加趋势,但根长密度呈现降低趋势。总体而言,这些结果表明,在SW生境中,土壤水分决定了L.根系的水平扩展,尽管在严重干旱条件下总体扩展能力有限。然而,由于DN土壤相对较强的保水能力,土壤水分变化不太明显,导致根系无明显垂直延伸。L.的根系响应有助于我们理解草本植物如何调整其地下形态以支持其在恶劣的岩溶土壤环境中生长。

https://cdn.ncbi.nlm.nih.gov/pmc/blobs/0c1c/6529846/92ddbe3e3df8/fpls-10-00629-g001.jpg

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