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Hydraulic redistribution by two semi-arid shrub species: Implications for Sahelian agro-ecosystems

机译:两种半干旱灌木树种的水力再分配:对萨赫勒农业生态系统的影响

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摘要

Hydraulic redistribution is the process of passive water movement from deeper moist soil to shallower dry soil layers using plant roots as conduits. Results from this study indicate that this phenomenon exists among two shrub species (Guiera senegalensis and Piliostigma reticulatwn) that co-exist with annual food crops in Sahelian agro-ecosystems. Real-time measurements were conducted for soil water content, soil water potential and microclimate variables notably; air temperature, relative humidity, wind speed, precipitation and solar irradiance. Additionally, sap flow measurements were conducted in shrub roots using the thermal dissipation technique on intact and coppiced shrubs. Monthly predawn leaf water potential was measured using a portable pressure chamber. Soil water potential (Ψs) at the 20 cm depth declined significantly during the dry season with diel changes in Ψ_s of -0.6 to -1.1 MPa. These variations were attributed to passive water release from shrub roots resulting in overnight rewetting of drier upper soil layers. Sap flow measurements on tap and lateral shrub roots indicated daily reversals in the direction of flow. During the peak of the dry season, both positive (toward shrub) and negative (toward soil) flows were observed in lateral shrub roots with sap flow in the lateral roots frequently negative at night and rapidly becoming positive soon after sunrise. The negative sap flow at night in superficial lateral roots and the periodic positive flow in the descending tap roots were indicative of hydraulic redistribution. Hydraulic redistribution may be an important mechanism for drought stress avoidance while maintaining plant physiological functions in both shrubs and neighboring annuals in water-limited environments.
机译:水力再分配是利用植物根系作为管道,使水分从较深的潮湿土壤转移到较浅的干燥土壤层的被动水运动过程。这项研究的结果表明,这种现象在萨赫勒地区农业生态系统中与一年生粮食作物共存的两种灌木物种(塞内加尔圭亚那和Piliostigma reticulatwn)中都存在。实时测量土壤水分,土壤水势和微气候变量。气温,相对湿度,风速,降水和太阳辐照度。此外,对树木的根部进行树液流量测量,方法是使用散热技术对完整的灌木丛和灌木丛进行灌木丛。使用便携式压力室测量黎明前每月的水势。在干旱季节,20 cm深度的土壤水势(Ψs)显着下降,di变化在-0.6至-1.1 MPa之间。这些变化归因于灌木根部的被动水释放,导致干燥的上层土壤层隔夜重新润湿。对自来水和侧生灌木根的树液流量测量表明,水流方向每天都在逆转。在干旱季节的高峰期,在侧灌根中均观察到正向(灌丛)和负向(正向土壤)的流动,侧根中的汁液流在夜间常常为负,并在日出后不久迅速变为正。夜间在表层侧根中的负汁液流和在下降的自根中的周期性正液流指示了水力的重新分配。水力重新分配可能是避免干旱胁迫的重要机制,同时在水有限的环境中在灌木和邻年植物中保持植物的生理功能。

著录项

  • 来源
    《Journal of arid environments》 |2012年第8期|p.69-77|共9页
  • 作者单位

    International Water Management Institute, PMB CT 112 Accra, Ghana;

    Department of Crop and Soil Science, Oregon State University, ALS Building 3017, Corvallis, OR 97331 USA;

    Institut Senigalais de Recherches Agricoles (ISRA)/CERAAS, B.P 3320 Thies-Escale, Senegal;

    Western Ecology Division, US EPA/NHEERL, 200 SW 35th St, Corvallis, OR 97333, USA;

    USDA Forest Service, PNW Research Station, 3200 SW Jefferson Way, Corvallis.OR 97331, USA;

    Institut Senigalais de Recherches Agricoles (ISRA)/CERAAS, B.P 3320 Thies-Escale, Senegal;

    Institut Senigalais de Recherches Agricoles (ISRA)/CERAAS, B.P 3320 Thies-Escale, Senegal;

    The World Bank, 1818 H Street, NW Washington, DC 20433, USA;

    School of Environment and Natural Resources, Ohio State University, Columbus, OH 43210, USA;

    Oregon State University, Water Resources Engineering, Department of Bioengineering, Cilmore Hall, Km. 116, Corvallis, OR 97331, USA;

    Oregon State University, Water Resources Engineering, Department of Bioengineering, Cilmore Hall, Km. 116, Corvallis, OR 97331, USA;

  • 收录信息 美国《科学引文索引》(SCI);
  • 原文格式 PDF
  • 正文语种 eng
  • 中图分类
  • 关键词

    agro-ecosystems; annual food crops; hydraulic redistribution; sahel; shrubs;

    机译:农业生态系统;一年生粮食作物;水力再分配;萨赫勒灌木丛;

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