Wan Yanbo, Peng Lei, Anwaier Abudureyimu, Shi Haobo, Li Dinghao, Ma Yu, Shi Qingdong
College of Ecology and Environment, Xinjiang University, Urumqi, China.
Key Laboratory of Oasis Ecology, Xinjiang University, Urumqi, China.
Front Plant Sci. 2024 Feb 9;15:1330426. doi: 10.3389/fpls.2024.1330426. eCollection 2024.
Accurate estimation of desert vegetation transpiration is key to regulating desert water resources of desert ecosystems. Sap flow density (SFD) can indirectly reflect a tree's transpiration consumption, and it has been affected by climate warming and groundwater depths in desert ecosystems. Sap flow responses to meteorological conditions and groundwater depths are further affected by tree of different sizes. However, how meteorological factors and groundwater depths affects tree sap flow among tree sizes remains poorly understand. In this study, a 50 × 50 m stand was selected as a sample plot in the hinterland of the Taklamakan Desert, and the SFD of of different sizes was measured continuously using the thermal diffusion technique from May to October of 2021 and 2022. The results showed that SFD of large was consistently higher than that of small in 2021 and 2022. and the SFD of was significantly and positively correlated with solar radiation (Rad) and vapor pressure deficit (VPD), and the correlation was higher than that of the air temperature (Ta) and relative humidity (RH), and also showed a strong non-linear relationship. Analysis of the hour-by-hour relationship between SFD and VPD and Rad showed a strong hysteresis. Throughout the growing season, there was no significant relationship between SFD of and groundwater depth, VPD and Rad were still the main controlling factors of SFD in different groundwater depths. However, during the period of relative groundwater deficit, the effect of groundwater depth on the SFD of increased, and the small was more sensitive, indicating that the small was more susceptible to groundwater changes. This study emphasized that Rad and VPD were the main drivers of SFD during the growing season, as well as differences in the response of different sizes of to groundwater changes. The results of the study provide a scientific basis for future modeling of transpiration consumption in forests in desert oases, as well as the regulation and allocation of water resources.
准确估算荒漠植被蒸腾作用是调节荒漠生态系统水资源的关键。液流密度(SFD)能够间接反映树木的蒸腾消耗,并且在荒漠生态系统中已受到气候变暖和地下水位的影响。不同大小树木的液流对气象条件和地下水位的响应会进一步受到影响。然而,气象因素和地下水位如何影响不同大小树木的液流仍知之甚少。在本研究中,在塔克拉玛干沙漠腹地选取了一块50×50米的林分作为样地,并于2021年5月至10月以及2022年5月至10月使用热扩散技术连续测量了不同大小树木的液流密度。结果表明,在2021年和2022年,大树的液流密度始终高于小树,并且树木的液流密度与太阳辐射(Rad)和水汽压差(VPD)显著正相关,且这种相关性高于气温(Ta)和相对湿度(RH),还呈现出很强的非线性关系。对树木液流密度与水汽压差和太阳辐射的逐小时关系分析显示出很强的滞后现象。在整个生长季,树木液流密度与地下水位之间没有显著关系,水汽压差和太阳辐射仍是不同地下水位条件下树木液流密度的主要控制因素。然而在相对地下水亏缺期,地下水位对树木液流密度的影响增大,且小树更敏感,这表明小树更容易受到地下水变化的影响。本研究强调太阳辐射和水汽压差是生长季树木液流密度的主要驱动因素,以及不同大小树木对地下水变化响应的差异。研究结果为未来荒漠绿洲树木林蒸腾消耗建模以及水资源的调控与分配提供了科学依据。