The seasonal origins and ages of water provisioning streams and trees in a tropical montane cloud forest

IF 5.7 1区 地球科学 Q1 GEOSCIENCES, MULTIDISCIPLINARY Hydrology and Earth System Sciences Pub Date : 2023-11-21 DOI:10.5194/hess-27-4173-2023
Emily I. Burt, Gregory R. Goldsmith, Roxanne M. Cruz-de Hoyos, Adan J. Ccahuana Quispe, A. J. West
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Abstract

Abstract. Determining the sources of water provisioning streams, soils, and vegetation can provide important insights into the water that sustains critical ecosystem functions now and how those functions may be expected to respond given projected changes in the global hydrologic cycle. We developed multi-year time series of water isotope ratios (δ18O and δ2H) based on twice-monthly collections of precipitation, lysimeter, and tree branch xylem waters from a seasonally dry tropical montane cloud forest in the southeastern Andes mountains of Peru. We then used this information to determine indices of the seasonal origins, the young water fractions (Fyw), and the new water fractions (Fnew) of soil, stream, and tree water. There was no evidence for intra-annual variation in the seasonal origins of stream water and lysimeter water from 1 m depth, both of which were predominantly comprised of wet-season precipitation even during the dry seasons. However, branch xylem waters demonstrated an intra-annual shift in seasonal origin: xylem waters were comprised of wet-season precipitation during the wet season and dry-season precipitation during the dry season. The young water fractions of lysimeter (< 15 %) and stream (5 %) waters were lower than the young water fraction (37 %) in branch xylem waters. The new water fraction (an indicator of water ≤ 2 weeks old in this study) was estimated to be 12 % for branch xylem waters, while there was no significant evidence for new water in stream or lysimeter waters from 1 m depth. Our results indicate that the source of water for trees in this system varied seasonally, such that recent precipitation may be more immediately taken up by shallow tree roots. In comparison, the source of water for soils and streams did not vary seasonally, such that precipitation may mix and reside in soils and take longer to transit into the stream. Our insights into the seasonal origins and ages of water in soils, streams, and vegetation in this humid tropical montane cloud forest add to understanding of the mechanisms that govern the partitioning of water moving through different ecosystems.
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热带山地云雾林中水源供给溪流和树木的季节性起源和年龄
摘要。确定溪流、土壤和植被的水源可以提供重要的信息,让我们了解目前维持关键生态系统功能的水源,以及在全球水文循环预计发生变化的情况下,这些功能预计会如何反应。我们根据对秘鲁东南部安第斯山脉季节性干旱热带山地云林的降水、溶液计和树枝木质部水的每月两次采集,建立了水同位素比率(δ18O 和 δ2H)的多年时间序列。然后,我们利用这些信息确定了土壤水、溪流水和树木水的季节起源指数、新水分馏指数(Fyw)和新水分馏指数(Fnew)。没有证据表明1米深的溪水和溶样池水的季节起源存在年内变化,即使在干旱季节,这两种水也主要由雨季降水组成。然而,木质部分支水体的季节来源在年内会发生变化:木质部水体在雨季由雨季降水组成,而在旱季则由旱季降水组成。裂隙水(< 15%)和溪水(5%)的新水部分低于木质部分支水体的新水部分(37%)。据估计,木质部分支水体的新水部分(在本研究中指水龄小于 2 周的水体)为 12%,而在 1 米深的溪流或赖氨酸层水体中没有明显的新水证据。我们的研究结果表明,该系统中树木的水源随季节而变化,因此最近的降水可能更快地被浅层树根吸收。相比之下,土壤和溪流的水源没有季节性变化,因此降水可能会混合并滞留在土壤中,需要更长的时间才能进入溪流。我们对这片潮湿的热带山地云雾林中土壤、溪流和植被中水的季节性来源和年龄的深入研究,有助于我们了解水在不同生态系统中流动的分区机制。
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来源期刊
Hydrology and Earth System Sciences
Hydrology and Earth System Sciences 地学-地球科学综合
CiteScore
10.10
自引率
7.90%
发文量
273
审稿时长
15 months
期刊介绍: Hydrology and Earth System Sciences (HESS) is a not-for-profit international two-stage open-access journal for the publication of original research in hydrology. HESS encourages and supports fundamental and applied research that advances the understanding of hydrological systems, their role in providing water for ecosystems and society, and the role of the water cycle in the functioning of the Earth system. A multi-disciplinary approach is encouraged that broadens the hydrological perspective and the advancement of hydrological science through integration with other cognate sciences and cross-fertilization across disciplinary boundaries.
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