Transpiration Characteristics and Its Response to Influence Factors of

SHANG Youxian; MAN Xiuling; XU Zhipeng

doi:10.13870/j.cnki.stbcxb.2023.02.036

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Transpiration Characteristics and Its Response to Influence Factors of

更新时间：2025-03-12

- Transpiration Characteristics and Its Response to Influence Factors of
- Vol. 37, Issue 2, Pages: 310-319(2023)
- 作者机构：
  
  东北林业大学林学院,哈尔滨,150040
- 作者简介：
- 基金信息：
- DOI：10.13870/j.cnki.stbcxb.2023.02.036
  CLC： S718.55
- Published：2023
- 稿件说明：
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SHANG Youxian, MAN Xiuling, XU Zhipeng. Transpiration Characteristics and Its Response to Influence Factors of[J]. 2023, 37(2): 310-319.
DOI：

SHANG Youxian, MAN Xiuling, XU Zhipeng. Transpiration Characteristics and Its Response to Influence Factors of[J]. 2023, 37(2): 310-319. DOI： 10.13870/j.cnki.stbcxb.2023.02.036.

摘要

探究多年冻土区白桦次生林蒸腾特征对影响因子的响应

为准确评估该地区森林生态系统水文效应提供科学参考。运用热扩散式探针法

从2021年5—9月对多年冻土区的白桦树干液流进行监测

并同步观测影响因子变化情况。结果表明:整个观测期

白桦次生林蒸腾表现出明显的小时、日、月变化。(1)白桦次生林小时蒸腾特征表现为优势木＞中等木＞被压木

蒸腾动态在晴天呈单峰曲线

在雨天呈双峰曲线。日尺度上

白桦次生林蒸腾平均值为1.47 mm/d

且最大值出现在7月。在整个观测期

林分蒸腾表现出明显的月变化

即7月＞6月＞8月＞9月＞5月

分别为65.08

62.43

54.27

22.92

19.84 mm;(2)林分累计蒸腾量共计224.54 mm

占同期降雨量的32.41%

其中优势木为林分蒸腾的主要贡献者

占林分总蒸腾量的62.64%;(3)在小时尺度上

林分蒸腾量主要受大气温度和饱和水汽压差所影响;日尺度上

林分蒸腾与潜在蒸散、空气温度、太阳辐射、饱和水汽压差、叶面积指数以及土壤温度极显著正相关(p＜0.01);与空气相对湿度极显著负相关(p＜0.01);与土壤含水量关系不显著(p＞0.05)

潜在蒸散、叶面积指数、饱和水汽压差以及空气温度是驱动林分日蒸腾的主要影响因子;月尺度上

空气温度对林分蒸腾的影响最大

其对林分蒸腾的解释度高达93.90%。

Abstract

To investigate the response of transpiration characteristics of Betula platyphylla secondary forest to influencing factors in permafrost area

and to provide scientific reference for accurate assessment of the hydrological effects of forest ecosystems in this region.The sap flow of Betula platyphylla was measured using thermal dissipation probes from May to September 2021 in permafrost area

and the influence factors were observed simultaneously.The results showed that the stand transpiration of Betula platyphylla secondary forest showed obvious hourly

daily and monthly changes during the study period.(1) The hourly transpiration characteristics of Betula platyphylla secondary forest was exhibited that dominant trees > intermediate trees > suppressed trees.Furthermore

diurnal variations of daily transpiration performed a single peak curve pattern in sunny days

while the bimodal curve was observed in rainy days.Meanwhile

the daily mean stand transpiration of Betula platyphylla secondary forest was 1.47 mm/d

with the maximum value appeared in July.A significant monthly variation of transpiration was found during the whole observation period and ranked as follows:July > June > August > September > May

which was 65.08

62.43

54.27

22.92 and 19.84 mm

respectively.(2) The cumulative transpiration of the stand was 224.54 mm

accounting for 32.41% of the total precipitation over the same period

and the transpiration of the dominant trees was the main contributors to the stand transpiration

accounting for 62.64% of the stand transpiration.(3) At the hourly scale

transpiration was mainly affected by air temperature and vapor pressure deficit.At the daily scale

transpiration was positively correlation with potential evapotranspiration

air temperature

solar radiation

vapor pressure deficit

leaf area index and soil temperature (p<0.01)

which was significant negative correlation with air relative humidity (p<0.01) and no significant correlation with soil water content (p>0.05)

and potential evapotranspiration

leaf area index

vapor pressure deficit and air temperature were the main factors driving the daily stand transpiration.At the monthly scale

air temperature had the greatest impact on stand transpiration

which explained 93.90% of stand transpiration.

关键词

Keywords

references

Wang L, Liu Z B, Guo J B, et al. Estimate canopy transpiration in larch plantations via the interactions among reference evapotranspiration, leaf area index, and soil moisture[J].Forest Ecology and Management,2021,481:e118749.

于松平,刘泽彬,郭建斌,等.六盘山华北落叶松林分蒸腾特征及其影响因素[J].南京林业大学学报(自然科学版),2021,45(1):131-140.

贾国栋,陈立欣,李瀚之,等.北方土石山区典型树种耗水特征及环境影响因子[J].生态学报,2018,38(10):3441-3452.

黄雅茹,马迎宾,辛智鸣,等.柽柳不同季节树干液流特征及其与土壤含水量及土壤温度的关系[J].西北林学院学报,2021,36(5):1-10.

曹恭祥,王云霓,郭中,等.六盘山南侧华北落叶松人工林蒸腾对土壤水分和潜在蒸散的响应[J].应用生态学报,2020,31(10):3376-3384.

Tie Q, Hu H C, Tian F Q. Environmental and physiological controls on sap flow in a subhumid mountainous catchment in North China[J].Agricultural and Forest Meteorology,2017,240:46-57.

Liu Z B, Wang Y H, Tian A. Modeling the response of daily evapotranspiration and its components of a larch plantation to the variation of weather, soil moisture, and canopy leaf area index[J].Journal of Geophysical Research: Atmospheres,2018,123(14):7354-7374.

Zhou Y, Hartemink A E, Shi Z, et al. Land use and climate change effects on soil organic carbon in North and Northeast China[J].Science of the Total Environment,2019,647:1230-1238.

刘家霖,满秀玲,胡悦.兴安落叶松天然林不同分化等级林木树干液流对综合环境因子的响应[J].林业科学研究,2016,29(5):726-734.

马菁,郭建斌,刘泽彬,等.六盘山华北落叶松林分蒸腾日内变化及其对环境因子的响应[J].北京林业大学学报,2020,42(5):1-11.

王媛.大兴安岭南段白桦蒸腾特征研究[D].呼和浩特:内蒙古农业大学,2020.

Yang S J, Zhang Y J, Goldstein G, et al. Determinants of water circulation in a woody bamboo species: Afternoon use and night-time recharge of culm water storage[J].Tree Physiology,2015,35(9):964-974.

Xu Z P, Man X L, Duan L L, et al. Improved subsurface soil moisture prediction from surface soil moisture through the integration of the (de) coupling effect[J].Journal of Hydrology,2022,608:e127634.

万艳芳,于澎涛,刘贤德,等.祁连山青海云杉树干液流密度的优势度差异[J].生态学报,2017,37(9):3106-3114.

李洁,任启文,孙杰肖.张家口崇礼区3种优势树种蒸腾特征研究[J].西北林学院学报,2018,33(6):40-46.

吕静.大兴安岭南段白桦昼夜蒸腾特征及其影响因素分析[D].呼和浩特:内蒙古农业大学,2021.

Wan Y F, Yu P T, Wang Y H, et al. The variation in water consumption by transpiration of Qinghai spruce among canopy layers in the Qilian Mountains, Northwestern China[J].Forests,2020,11(8):e845.

王莉.青海大通高寒区典型林地耗水特征研究[D].北京:北京林业大学,2020.

杜梦鸽,王善举,樊军,等.祁连山青海云杉低液流特征及其影响因素[J].应用生态学报,2022,33(4):931-938.

张荣,毕华兴,王宁,等.不同时间尺度下刺槐蒸腾耗水与环境因子关系[J].水土保持学报,2022,36(5):204-211.

Xu Z P, Man X L, Cai T J, et al. How potential evapotranspiration regulates the response of canopy transpiration to soil moisture and leaf area index of the Boreal Larch Forest in China[J].Forests,2022,13(4):e571.

Han C, Chen N, Zhang C K, et al. Sap flow and responses to meteorological about the

Larix principis-rupprechtii

plantation in Gansu Xinlong mountain, northwestern China[J].Forest Ecology and Management,2019,451:e117519.

孙旭,杨文慧,焦磊,等.不同时间尺度北京蟒山油松树干液流对环境因子的响应研究[J].生态学报,2022,42(10):4113-4123.

罗超,查同刚,朱梦洵,等.浅层地下水对华北地区河岸杨树林树干液流的影响[J].应用生态学报,2016,27(5):1401-1407.

Wang H, Tetzlaff D, Dick J J, et al. Assessing the environmental controls on Scots pine transpiration and the implications for water partitioning in a boreal headwater catchment[J].Agricultural and Forest Meteorology,2017,240:58-66.

陈彪,陈立欣,刘清泉,等.半干旱地区城市环境下樟子松蒸腾特征及其对环境因子的响应[J].生态学报,2015,35(15):5076-5084.

冯永建,马长明,王彦辉,等.华北落叶松人工林蒸腾特征及其与土壤水势的关系[J].中国水土保持科学,2010,8(1):93-98.

王亚蕊,王彦辉,于澎涛,等.华北落叶松人工林蒸散及产流对叶面积指数变化的响应[J].生态学报,2016,36(21):6928-6938.

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