Increased tree water use with the development of a dense understory layer in a North American hardwood forest

IF 2.5 3区 环境科学与生态学 Q2 ECOLOGY Ecohydrology Pub Date : 2024-04-01 DOI:10.1002/eco.2648
Arielle Rasoanaivo, Claudele Ghotsa Mekontchou, Pascal Rochon, Philippe Nolet, Audrey Maheu
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Abstract

The formation of a single species, recalcitrant understory vegetation layer can limit tree regeneration and, in the long term, modify the composition of forests. Few studies have investigated how recalcitrant vegetation influences competition for water resources although the formation of a dense understory is likely to modify the forest water balance. In eastern North American hardwood forests, the development of a dense understory layer of American beech (Fagus grandifolia) has been observed in stands dominated by sugar maple (Acer saccharum), a phenomenon that shares many characteristics associated with recalcitrant vegetation. Given that water availability is generally negatively correlated with stand density, we hypothesized that the formation of a dense understory beech layer increased competition for water resources, thus leading to reduced water use by sugar maple trees in beech-dominated stands. Using thermal dissipation sensors, we measured sap flux density (Fd) of two sugar maple trees at three beech-dominated sites and three control sites. During the growing season, Fd of sugar maple trees was significantly larger at beech-dominated sites compared to control sites, indicating a greater rate of water use by sugar maples in stands with a dense understory beech layer. We provide two hypotheses to explain our results at the tree scale: (i) reduced cover by forest floor vegetation could limit transpiration by this layer, thus allowing increased water availability to supply transpiration by overstory trees, or (ii) increased tree transpiration rate could be a mechanism to satisfy nutrient requirements in beech-dominated stands often associated with lower soil fertility.

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北美阔叶林林下致密层的形成增加了树木的用水量
形成单一物种、难以生长的林下植被层会限制树木再生,从长远来看,还会改变森林的组成。虽然浓密林下植被的形成很可能会改变森林的水分平衡,但很少有研究调查反季节植被如何影响对水资源的争夺。在北美东部的硬木森林中,人们观察到在以糖槭为主的林分中形成了茂密的山毛榉林下层,这种现象具有许多与反季节植被相关的特征。鉴于水分供应量通常与林分密度呈负相关,我们假设林下茂密山毛榉层的形成会加剧对水资源的竞争,从而导致以山毛榉为主的林分中糖枫树的用水量减少。我们使用热耗散传感器测量了三个以山毛榉为主的地点和三个对照地点两棵糖槭树的树液通量密度(Fd)。在生长季节,以山毛榉为主的地点糖枫树的液流密度明显大于对照地点,这表明在林下山毛榉层茂密的林分中,糖枫树的用水量更大。我们提出了两个假设来解释我们在树木尺度上的结果:(i) 林地植被覆盖率降低可能会限制林下植被层的蒸腾作用,从而使更多的水供应上层树木的蒸腾作用;或者 (ii) 在以山毛榉为主的林分中,树木蒸腾作用的增加可能是满足养分需求的一种机制,通常与土壤肥力较低有关。
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来源期刊
Ecohydrology
Ecohydrology 环境科学-生态学
CiteScore
5.10
自引率
7.70%
发文量
116
审稿时长
24 months
期刊介绍: Ecohydrology is an international journal publishing original scientific and review papers that aim to improve understanding of processes at the interface between ecology and hydrology and associated applications related to environmental management. Ecohydrology seeks to increase interdisciplinary insights by placing particular emphasis on interactions and associated feedbacks in both space and time between ecological systems and the hydrological cycle. Research contributions are solicited from disciplines focusing on the physical, ecological, biological, biogeochemical, geomorphological, drainage basin, mathematical and methodological aspects of ecohydrology. Research in both terrestrial and aquatic systems is of interest provided it explicitly links ecological systems and the hydrologic cycle; research such as aquatic ecological, channel engineering, or ecological or hydrological modelling is less appropriate for the journal unless it specifically addresses the criteria above. Manuscripts describing individual case studies are of interest in cases where broader insights are discussed beyond site- and species-specific results.
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