Liu Feiyao, Zhang Lijuan, You Quangang, Xue Xian, Liu Guohua, Feng Chang
College of Geography and Tourism, Hengyang Normal University, Hengyang, China.
College of Foreign Languages, Hengyang Normal University, Hengyang, China.
Front Plant Sci. 2025 Jul 23;16:1563166. doi: 10.3389/fpls.2025.1563166. eCollection 2025.
Plant transpiration is a fundamental process for maintaining the water cycle, regulating temperature and facilitating nutrient uptake, while also playing a critical role in climate regulation and ecosystem services. However, a significant knowledge gap remains in the understanding of how plant transpiration responds to changes in precipitation patterns within dryland ecosystems. In the present study, the stem sap flow of the phreatophyte xerophytic shrub , meteorological factors, soil moisture content, and bare soil evaporation were examined to assess the effects of two different rainfall categories (category I: lower mean rainfall amount and duration; category II: higher mean rainfall amount and duration) on stem sap flow dynamics. Our results reveal that the rainfall reduced the stem sap flow by 46.5% and 29.5% compared to the previous days across rainfall category I and II, respectively. The daily and diurnal variation of stem sap flow during the three days following rainfall showed non-significant variation compared to pre-rainfall, regardless of rainfall category. The soil moisture content at depth of 0-40 cm (SMC) exhibits a pronounced increase to rainfall events, irrespective of rainfall category, although these events did not significantly increase the soil available moisture content within this depth. Concurrently, the weighing micro-lysimeters utilized in this study revealed that approximately 91.5% of the total precipitation during the experimental period evaporated into the atmosphere. In addition, the daily stem sap flow on the rainfall day and the following three days post rainfall was strongly positively correlated with photosynthetically active radiation, air temperature, and vapor pressure deficit within the two rainfall categories rather than with SMC. Together, our findings indicate that the effects of rainfall variability on stem sap flow of are primarily driven by meteorological factors, independent of the rainfall category. The results of this study provide a valuable insight for assessing species-specific water-use strategies and implementing effective reforestation practices in the future.
植物蒸腾作用是维持水循环、调节温度和促进养分吸收的基本过程,同时在气候调节和生态系统服务中也发挥着关键作用。然而,在理解旱地生态系统中植物蒸腾作用如何响应降水模式变化方面,仍存在重大知识空白。在本研究中,对潜水植物旱生灌木的树干液流、气象因素、土壤含水量和裸土蒸发进行了研究,以评估两种不同降雨类别(类别I:较低的平均降雨量和持续时间;类别II:较高的平均降雨量和持续时间)对树干液流动态的影响。我们的结果表明,与前几天相比,降雨使类别I和类别II的树干液流分别减少了46.5%和29.5%。无论降雨类别如何,降雨后三天内树干液流的日变化和昼夜变化与降雨前相比均无显著差异。0-40厘米深度的土壤含水量(SMC)对降雨事件表现出明显增加,无论降雨类别如何,尽管这些降雨事件并未显著增加该深度内的土壤有效含水量。同时,本研究中使用的称重式微型蒸渗仪显示,实验期间约91.5%的总降水量蒸发到大气中。此外,在两种降雨类别中,降雨日及降雨后三天的每日树干液流与光合有效辐射、气温和水汽压差呈强正相关,而非与SMC相关。总之,我们的研究结果表明,降雨变异性对[具体植物名称]树干液流的影响主要由气象因素驱动,与降雨类别无关。本研究结果为评估物种特异性水分利用策略和未来实施有效的造林实践提供了有价值的见解。