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In situ measurements of soil and plant water isotopes: a review of approaches, practical considerations and a vision for the future

机译:原位测量土壤和植物水同位素:对未来的方法,实践考虑和愿景的审查

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The number of ecohydrological studies involving water stable isotope measurements has been increasing steadily due to technological (e.g., field-deployable laser spectroscopy and cheaper instruments) and methodological (i.e., tracer approaches or improvements in root water uptake models) advances in recent years. This enables researchers from a broad scientific background to incorporate water-isotope-based methods into their studies. Several isotope effects are currently not fully understood but might be essential when investigating root water uptake depths of vegetation and separating isotope processes in the soil–vegetation–atmosphere continuum. Different viewpoints exist on (i)?extraction methods for soil and plant water and methodological artifacts potentially introduced by them, (ii)?the pools of water (mobile vs. immobile) measured with those methods, and (iii)?spatial variability and temporal dynamics of the water isotope composition of different compartments in terrestrial ecosystems. In situ methods have been proposed as an innovative and necessary way to address these issues and are required in order to disentangle isotope effects and take them into account when studying root water uptake depths of plants and for studying soil–plant–atmosphere interaction based on water stable isotopes. Herein, we review the current status of in situ measurements of water stable isotopes in soils and plants, point out current issues and highlight the potential for future research. Moreover, we put a strong focus and incorporate practical aspects into this review in order to provide a guideline for researchers with limited previous experience with in?situ methods. We also include a section on opportunities for incorporating data obtained with described in?situ methods into existing isotope-enabled ecohydrological models and provide examples illustrating potential benefits of doing so. Finally, we propose an integrated methodology for measuring both soil and plant water isotopes in?situ when carrying out studies at the soil–vegetation–atmosphere continuum. Several authors have shown that reliable data can be generated in the field using in?situ methods for measuring the soil water isotope composition. For transpiration, reliable methods also exist but are not common in ecohydrological field studies due to the required effort. Little attention has been paid to in?situ xylem water isotope measurements. Research needs to focus on improving and further developing those methods. There is a need for a consistent and combined (soils and plants) methodology for ecohydrological studies. Such systems should be designed and adapted to the environment to be studied. We further conclude that many studies currently might not rely on in?situ methods extensively because of the technical difficulty and existing methodological uncertainties. Future research needs to aim on developing a simplified approach that provides a reasonable trade-off between practicability and precision and accuracy.
机译:近年来,由于技术(例如,现场 - 可部署的激光光谱和更便宜的仪器)和方法论(即,根水摄取模型中的示踪方法或改进),涉及水稳定同位素测量的生态学研究的数量已经稳步增加。这使得研究人员能够从广泛的科学背景中将基于水同位素的方法纳入他们的研究。目前尚未完全理解几种同位素效应,但在调查植被的根水摄取深度和分离土壤 - 植被 - 大气中的同位素过程时可能是必要的。存在不同的观点(i)?诸如其潜在的土壤和植物水的提取方法,(ii)?用这些方法测量的水(移动与不动)和(iii)的水池(III)?空间变异性和陆地生态系统中不同隔室水同位素组成的时间动态。已经提出了解决这些问题的创新性和必要方法,并且是为了解散同位素效应,并考虑到植物的根水吸收深度以及研究基于水的土壤 - 植物 - 大气相互作用,以考虑到同位素效应并考虑到它们稳定的同位素。在此,我们审查了土壤和植物中水稳定同位素的原位测量的现状,指出了当前的问题,并突出了未来研究的潜力。此外,我们提出了强烈的焦点并将实际方面纳入了本综述,以便为研究人员提供有限的先前经验的研究指导意见。我们还包括一部分有关将在现有同位素的生态水上模型中描述的α原位方法中获得的数据的机会的一部分,并提供了这样做的潜在益处的例子。最后,我们提出了一种用于测量土壤和植物水同位素的综合方法,当在植被的土壤 - 植被 - 气氛连续内进行研究时,原位。有几位作者表明,可以使用载物在该领域中产生可靠的数据来测量土壤水同位素组合物的方法。对于蒸腾,由于所需的努力,可靠的方法也存在但在生态学田间研究中并不常见。很少注意进入?原位Xylem水同位素测量。研究需要专注于改善和进一步发展这些方法。需要一种始终如一的和组合(土壤和植物)的生态学研究方法。这些系统应设计和适应待研究的环境。我们进一步得出结论,由于技术难度和现有的方法的不确定性,许多研究目前可能不依赖于?原位方法。未来的研究需要旨在开发一种简化的方法,可在实用性和精度和准确性之间提供合理的权衡。

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