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基于稳定同位素的半干旱黄土高原三种植物水分吸收模式的季节性变化。

Seasonal variation in water uptake patterns of three plant species based on stable isotopes in the semi-arid Loess Plateau.

机构信息

State Key Laboratory of Urban and Regional Ecology, Research Center for Eco-Environmental Sciences, Chinese Academy of Sciences, Beijing 100085, China; University of Chinese Academy of Sciences, Beijing 100049, China.

State Key Laboratory of Urban and Regional Ecology, Research Center for Eco-Environmental Sciences, Chinese Academy of Sciences, Beijing 100085, China.

出版信息

Sci Total Environ. 2017 Dec 31;609:27-37. doi: 10.1016/j.scitotenv.2017.07.133. Epub 2017 Jul 19.

Abstract

Water is a limiting factor and significant driving force for ecosystem processes in arid and semi-arid areas. Knowledge of plant water uptake pattern is indispensable for understanding soil-plant interactions and species coexistence. The 'Grain for Green' project that started in 1999 in the Loess Plateau of China has led to large scale vegetation change. However, little is known about the water uptake patterns of the main plant species that inhabit in this region. In this study, the seasonal variations in water uptake patterns of three representative plant species, Stipa bungeana, Artemisia gmelinii and Vitex negundo, that are widely distributed in the semi-arid area of the Loess Plateau, were identified by using dual stable isotopes of δH and δO in plant and soil water coupled with a Bayesian mixing model MixSIAR. The soil water at the 0-120cm depth contributed 79.54±6.05% and 79.94±8.81% of the total water uptake of S. bungeana and A. gmelinii, respectively, in the growing season. The 0-40cm soil contributed the most water in July (74.20±15.20%), and the largest proportion of water (33.10±15.20%) was derived from 120-300cm soils in August for A. gmelinii. However, V. negundo obtained water predominantly from surface soil horizons (0-40cm) and then switched to deep soil layers (120-300cm) as the season progressed. This suggested that V. negundo has a greater degree of ecological plasticity as it could explore water sources from deeper soils as the water stress increased. This capacity can mainly be attributed to its functionally dimorphic root system. V. negundo may have a competitive advantage when encountering short-term drought. The ecological plasticity of plant water use needs to be considered in plant species selection and ecological management and restoration of the arid and semi-arid ecosystems in the Loess Plateau.

摘要

水是干旱半干旱地区生态系统过程的限制因素和重要驱动力。了解植物水分吸收模式对于理解土壤-植物相互作用和物种共存至关重要。1999 年在中国黄土高原启动的“退耕还林”工程导致了大规模的植被变化。然而,对于栖息在该地区的主要植物物种的水分吸收模式知之甚少。在这项研究中,使用δH 和 δO 的双稳定同位素以及贝叶斯混合模型 MixSIAR,对广泛分布于黄土高原半干旱地区的三种代表性植物物种(芨芨草、沙蒿和黄荆)的水分吸收模式的季节性变化进行了鉴定。在生长季,0-120cm 深度的土壤水分别为芨芨草和沙蒿总水分吸收的 79.54±6.05%和 79.94±8.81%。7 月(74.20±15.20%)0-40cm 土壤提供的水量最多,8 月(33.10±15.20%)120-300cm 土壤提供的水量最大。然而,黄荆主要从表层土壤(0-40cm)获取水分,然后随着季节的进展转向深层土壤(120-300cm)。这表明,黄荆具有更大的生态可塑性,因为随着水分胁迫的增加,它可以从更深的土壤中探索水源。这种能力主要归因于其功能二态根系。当遇到短期干旱时,黄荆可能具有竞争优势。在黄土高原干旱半干旱生态系统的植物物种选择和生态管理与恢复中,需要考虑植物水分利用的生态可塑性。

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