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Seasonal patterns in depth of water uptake under contrasting annual and perennial systems in the Corn Belt Region of the Midwestern U.S.

机译:在美国中西部玉米带地区不同的年度和多年生系统下,水深吸收的季节性模式

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In agricultural landscapes, variation and ecological plasticity in depth of water uptake by annual and perennial plants is an important means by which vegetation controls hydrological balance. However, little is known about how annual and perennial plants growing in agriculturally dominated landscapes in temperate humid regions vary in their water uptake dynamics. The primary objective of this study was to quantify the depth of water uptake by dominant plant species and functional groups growing in contrasting annual and perennial systems in an agricultural landscape in Central Iowa. We used stable oxygen isotope techniques to determine isotopic signatures of soil water and plant tissue to infer depth of water uptake at five sampling times over the course of an entire growing season. Our results suggest that herbaceous species (Zea mays L., Glycine max L. Merr., Carex sp., Andropogon gerardii Vitman.) utilized water predominantly from the upper 20 cm of the soil profile and exhibited a relatively low range of ecological plasticity for depth of water uptake. In contrast, the woody shrub (Symphoricarpos orbiculatus Moench.) and tree (Quercus alba L.) progressively increased their depth of water uptake during the growing season as water became less available, and showed a high degree of responsiveness of water uptake depth to changes in precipitation patterns. Co-existing shrubs and trees in the woodland and savanna sites extracted water from different depths in the soil profile, indicating complementarity in water uptake patterns. We suggest that deep water uptake by perennial plants growing in landscapes dominated by rowcrop agriculture can enhance hydrologic functioning. However, because the high degree of ecological plasticity allows some deep-rooted species to extract water from surface horizons when it is available, positive effects of deep water uptake may vary depending on species’ growth patterns and water uptake dynamics. Knowledge about individual species’ and plant communities’ depth of water uptake patterns in relation to local climate conditions and landscape positions can provide valuable information for strategically incorporating perennial plants into agricultural landscapes to enhance hydrologic regulation.
机译:在农业景观中,一年生和多年生植物对水的吸收深度的变化和生态可塑性是植被控制水文平衡的重要手段。然而,对于在温带潮湿地区农业占主导地位的景观中生长的一年生和多年生植物的吸水动态如何变化知之甚少。这项研究的主要目的是量化与爱荷华州中部农业景观中不同的年度和多年生系统形成对比的优势植物物种和功能群吸收的水分深度。我们使用稳定的氧同位素技术确定土壤水和植物组织的同位素特征,以推断整个生长季节过程中五个采样时间的吸水深度。我们的研究结果表明,草本物种(Zea mays L.,Glycine max L. Merr。,Carex sp。,Andropogon gerardii Vitman。)主要利用土壤剖面上部20 cm的水,并表现出相对较低的生态可塑性范围吸水深度。相反,在生长季节,木本灌木(Symphoricarpos orbiculatus Moench。)和乔木(Quercus alba L.)会逐渐增加其对水的吸收深度,因为水的供应量越来越少,并且对水的变化具有高度的响应能力。在降水模式中。林地和热带稀树草原地区同时存在的灌木和树木从土壤剖面的不同深度提取水,表明吸水模式具有互补性。我们建议,在以大田作物为主的景观中生长的多年生植物对深水的吸收可以增强水文功能。但是,由于高度的生态可塑性,使得一些根深蒂固的物种(如果有)可以从地表水平抽取水,因此深水吸收的积极影响可能会因物种的生长方式和水分吸收动态而异。有关单个物种和植物群落与当地气候条件和景观位置有关的水吸收模式深度的知识,可以为战略地将多年生植物纳入农业景观以增强水文调节提供有价值的信息。

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