Temporal patterns in root water uptake and intrinsic water-use efficiency of overstory and understory tree species in a subtropical humid pine forest

IF 5.6 1区 农林科学 Q1 AGRONOMY
Lu Li , Wei Ren , Lide Tian
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引用次数: 0

Abstract

Root water uptake and leaf-level intrinsic water-use efficiency (WUEi) and their temporal variations are important determinates of plant water balance and carbon fixation, yet these processes in humid forest trees are much less explored. We investigated the monthly variations in xylem and soil water isotopes (δ18O, δ2H), leaf carbon isotope (δ13C), soil, xylem and leaf water contents as well as the seasonal variations in leaf oxygen isotope (δ18O) and N contents for the dominant overstory species (Pinus massoniana) and a neighboring common understory species (Camellia japonica) in a subtropical humid pine forest within April 2021-June 2022. Water stable isotopes revealed that the two species exhibited similar water uptake patterns over time and both shifted water uptake toward deeper and shallow soil layers during the wet and relatively dry seasons, respectively. Evident soil water partitioning only occurred during a spring drought when only C. japonica shifted water uptake toward deeper soil layers, indicating high interspecific competition for shallow water. For P. massoniana, the reliance on shallow water positively correlated with WUEi (leaf δ13C) through negatively affecting leaf relative (to xylem) water content and stomatal conductance (proxied by leaf 18O enrichment above source water). In contrast, C. japonica exhibited non-sensitive WUEi response to temporal changes in water uptake depth, and its low leaf N contents indicate severe N limitation on photosynthesis and WUEi. Our results highlight the tight coupling between water uptake depth and WUEi for the overstory species, but not for the understory species likely associated with the stronger water and particularly N limitation it was experiencing. Our analysis of temporal changes in water uptake depth and WUEi (leaf δ13C) provides a useful framework to evaluate belowground constraints on resource acquisition and leaf-level water use strategies for plants in humid forests.
亚热带湿润松林上下层树种根系水分吸收和内在水分利用效率的时间格局
根系水分吸收和叶片水平内在水分利用效率(WUEi)及其时间变化是植物水分平衡和碳固定的重要决定因素,但这些过程在潮湿森林树木中的研究很少。研究了2021年4月~ 2022年6月亚热带湿润松林优势林种马尾松(Pinus massoniana)和邻近常见林种山茶(Camellia japonica)木质部和土壤水分同位素(δ18O、δ2H)、叶片碳同位素(δ13C)、土壤、木质部和叶片水分含量的月变化,以及叶片氧同位素(δ18O)和N含量的季节变化。水稳定同位素表明,随着时间的推移,这两个物种的水分吸收模式相似,在湿润季节和相对干旱季节,它们的水分吸收分别向深层和浅层土壤转移。明显的土壤水分分配只发生在春季干旱时,只有粳稻将水分吸收向较深的土层转移,表明对浅水的高度种间竞争。马尾松对浅水的依赖与叶片δ13C正相关,通过负向影响叶片相对(木质部)含水量和气孔导度(以源水以上叶片18O富集程度为代表)。而粳稻对水分吸收深度的时间变化不敏感,叶片氮含量低表明氮素对光合作用和氮素的限制严重。我们的研究结果强调了林下物种的吸水深度与WUEi之间的紧密耦合,但林下物种可能与更强的水特别是氮限制有关。我们对水分吸收深度和叶片δ13C的时间变化的分析为评估湿润森林植物资源获取和叶片水分利用策略的地下约束提供了一个有用的框架。
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来源期刊
CiteScore
10.30
自引率
9.70%
发文量
415
审稿时长
69 days
期刊介绍: Agricultural and Forest Meteorology is an international journal for the publication of original articles and reviews on the inter-relationship between meteorology, agriculture, forestry, and natural ecosystems. Emphasis is on basic and applied scientific research relevant to practical problems in the field of plant and soil sciences, ecology and biogeochemistry as affected by weather as well as climate variability and change. Theoretical models should be tested against experimental data. Articles must appeal to an international audience. Special issues devoted to single topics are also published. Typical topics include canopy micrometeorology (e.g. canopy radiation transfer, turbulence near the ground, evapotranspiration, energy balance, fluxes of trace gases), micrometeorological instrumentation (e.g., sensors for trace gases, flux measurement instruments, radiation measurement techniques), aerobiology (e.g. the dispersion of pollen, spores, insects and pesticides), biometeorology (e.g. the effect of weather and climate on plant distribution, crop yield, water-use efficiency, and plant phenology), forest-fire/weather interactions, and feedbacks from vegetation to weather and the climate system.
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