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林业科学 ›› 2025, Vol. 61 ›› Issue (9): 59-69.doi: 10.11707/j.1001-7488.LYKX20250159

• 研究论文 • 上一篇    

北京山区侧柏人工林液流密度对极端土壤干旱的响应

康敏敏1,2,李平平2,万艳芳2,*(),段文标1(),于澎涛2,王彦辉2,张小全3,李未来3,高原3   

  1. 1. 东北林业大学林学院 哈尔滨 150040
    2. 中国林业科学研究院森林生态环境与自然保护研究所 国家林业和草原局森林生态环境重点实验室 北京 100091
    3. 大自然保护协会 北京 100026
  • 收稿日期:2025-03-21 出版日期:2025-09-25 发布日期:2025-10-10
  • 通讯作者: 万艳芳 E-mail:wanyf@caf.ac.cn;dwbiao88@163.com
  • 基金资助:
    国家重点研发计划项目(2022YFF0801804,2022YFF0801803);四川省绿化基金会(2023031P)。

Response of Sap Flow Density to Extreme Soil Drought in Platycladus orientalis Plantation in Mountainous Area of Beijing

Minmin Kang1,2,Pingping Li2,Yanfang Wan2,*(),Wenbiao Duan1(),Pengtao Yu2,Yanhui Wang2,Xiaoquan Zhang3,Weilai Li3,Yuan Gao3   

  1. 1. College of Forestry, Northeast Forestry University Harbin 150040
    2. Ecology and Nature Conservation Institute,Chinese Academy Forestry Key Laboratory of Forestry Ecology and Environment of National Forestry and Grassland Administration Beijing 100091
    3. The Nature Conservancy Bejing 100026
  • Received:2025-03-21 Online:2025-09-25 Published:2025-10-10
  • Contact: Yanfang Wan E-mail:wanyf@caf.ac.cn;dwbiao88@163.com

摘要:

目的: 准确量化北京山区侧柏人工林的树干液流密度对极端土壤干旱的响应,明确其应对极端干旱胁迫的水分利用策略,为气候变化背景下北京山区林水协调综合管理提供科学依据。方法: 2024年生长季(5—10月),在北京市密云区五座楼林场选取侧柏(当地主要造林树种)人工林,设置1块20 m×20 m固定样地。采用热扩散液流探针连续监测树干液流密度变化,并同步观测气象因子和0~40 cm土层土壤湿度(用土壤相对可利用水分REW表示),分析树干液流密度的变化特征及其对环境因子的响应。结果: 1) 2024年生长季出现连续73天的极端土壤干旱(干旱期5月1日—7月12日),期间REW极低,平均仅为0.11,并伴随着持续高温和强太阳辐射。干旱降低了侧柏的树干液流密度,其在干旱期内一直维持在低水平,平均值仅为0.004 4 mL·cm?2min?1,显著低于生长季内非干旱期的平均值(0.020 2 mL·cm?2min?1)(P<0.01)。2) 干旱胁迫使干旱期内晴天、阴天和雨天等天气类型的液流密度差异减小且不显著(P>0.05)。干旱期内的日间降雨使液流密度短暂回升,导致雨天的平均液流密度(0.004 9 mL·cm?2min?1)略高于晴天和阴天,分别高4.3%和16.7%。3) 干旱改变了液流密度的日变化模式和昼夜占比。非干旱期晴天和阴天的液流密度呈“单峰型”日变化模式,且日间液流密度占比达95%以上,而干旱期晴天和阴天的液流密度日变化呈“波谷型”,且日间液流密度占比大幅降低到44%和51%。干旱期的日间降雨会改变液流密度日变化特征,表现为随日间降雨量增加而增大,有可能日变化模式也恢复为“单峰型”,且日间液流密度占比也逐渐增加。4) 侧柏树干液流密度在干旱期主要受气象因子(太阳辐射强度、饱和水汽压差、降水量)影响,而在非干旱期主要受气象因子和土壤湿度的共同影响。结论: 在极端土壤干旱胁迫下,侧柏会显著降低其液流密度,并改变液流密度日变化特征。在干旱期白天基本未测定到侧柏的树干液流,夜间反而测定到用于补充树体储水的液流。这表明侧柏具有较强的抗旱性,通过白天关闭气孔降低液流密度以减少蒸腾耗水、夜间维持较高液流密度以补充树体储水的方式来改变液流日变化模式和昼夜比例,从而形成较高的干旱胁迫环境适应性。因此,对于极易遭受土壤干旱胁迫的旱区阳坡瘠薄立地,应优先选择栽植耐旱性强的侧柏,并通过密度管理等措施降低林木蒸腾和蒸散耗水,维持基本的林水平衡。本研究阐明了侧柏适应严重土壤干旱胁迫的用水策略,为制定适应气候变化的林水协调综合管理方案提供了理论依据。

关键词: 侧柏, 极端土壤干旱, 土壤湿度, 树干液流密度, 日变化模式

Abstract:

Objective: To accurately quantify the response of the sap flow density of Platycladus orientalis plantations in the mountainous areas of Beijing to extreme soil drought, and to clarify its water use strategy in response to extreme drought stress, so as to provide a scientific basis for the coordinated and comprehensive management of forest and water in mountainous areas of Beijing under the background of climate change. Method: During the growing season of 2024 (May - October), the plantation of P. orientalis, the main local afforestation tree species, was selected in Wuzuolou Forest Farm in Miyun District, Beijing, and fixed a sample plot of 20 m×20 m was set up. The change characteristics of P. orientalis sap flow density in the growing season was continuously monitored by a thermal diffusion sap flow probe, and meteorological factors and soil moisture in 0?40 cm soil layer (expressed as relatively extractable soil water REW) were simultaneously observed, and the change characteristics of sap flow density and the response to environmental factors were analyzed. Result: 1) In the 2024 growing season, there was a continuous 73-days (May 1 to July 12) extreme soil drought, the REW was extremely low at 0.11 during the 73-days, accompanied by continuous high temperature and strong solar radiation intensity. Drought reduced the sap flow density of P. orientalis, maintaining a low level throughout the drought period, with an average value of 0.004 4 mL·cm?2min?1, which is significantly lower than the average sap flow density during non-drought periods in the growing season (0.020 2 mL·cm?2min?1) (P<0.01). 2) Drought stress diminished and no longer significantly affected the differences in sap flow density among weather types such as sunny, cloudy, and rainy days during the drought period (P > 0.05). Daytime rainfall during the drought period caused a temporary increase in sap flow density, resulting in a slightly higher average sap flow density on rainy days (0.0049 mL·cm?2min?1) compared to sunny and cloudy days, which were 4.3% and 16.7% higher, respectively. 3) Drought altereed the diurnal variation pattern and day-night ratio of sap flow density. During non-drought periods, the diurnal variation pattern of sap flow density on sunny and cloudy days follows a “unimodal” pattern, with the diurnal sap flow density accounting for over 95% of the total. However, during drought periods, the diurnal variation of sap flow density on sunny and cloudy days exhibits a “trough” pattern, and the diurnal sap flow density proportion significantly decreases to 44% and 51%, respectively. Daytime rainfall during drought periods can alter the diurnal variation characteristics of sap flow density, showing an increase with the increase in daytime rainfall. The diurnal variation pattern may also revert to a “unimodal” pattern, and the daytime sap flow density ratio gradually increases. 4) The sap flow density of P. orientalis was mainly affected by the meteorological factors (solar radiation intensity, vapor pressure deficit, precipitation) during the drought period. In non-drought periods, the sap flow density was affected by a combination of soil moisture and meteorological factors. Conclusion: Under extreme soil drought stress, P. orientalis significantly reduced its sap flow density and changed the diurnal variation characteristics of sap flow density. During the drought period, the sap flow of P. orientalis was basically not measured during the daytime, but the sap flow used to supplement the water storage of the tree was measured at night. The results showed that P. orientalis had strong drought resistance, and the diurnal variation mode and day-night ratio of sap flow density were changed by closing the stomata during the day to reduce the sap flow density to reduce transpiration water consumption and maintaining a high sap flow density at night to supplement the water storage of the tree, so as to form a higher adaptability to the drought stress environment. Therefore, for arid sunny slopes with thin soils that are highly susceptible to drought stress, planting drought-tolerant P. orientalis should be prioritized. Stand-density regulation and other silvicultural measures should be implemented to reduce canopy transpiration and stand evapotranspiration, thereby sustaining a fundamental forest water balance. This study elucidates the water-use strategies employed by P. orientalis under severe soil-drought stress, thereby providing a theoretical basis for developing climate-adaptive, forest-water-coordinated management schemes.

Key words: Platycladus orientalis, extreme soil drought, soil moisture, sap flow density, diurnal variation pattern

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