Responses of sap flow characteristics under different Chinese fir provenances to meteorological factors under different soil moisture conditions
XU Tingyu1,2,3, NIU Xiang1,2,3, WANG Bing1,2,3, SONG Qingfeng1,2,3, WANG Nan1,2,3, SUN Jianjun4, LIU Ru4
1. Ecology and Nature Conservation Institute, Chinese Academy of Forestry, 100091, Beijing, China; 2. Key Laboratory of Forest Ecology and Environment, National Forestry and Grassland Administration, 100091, Beijing, China; 3. Dagangshan National Key Field Observation and Research Station for Forest Ecosystem, 336606, Fenyi, Jiangxi, China; 4. Experimental Center of Subtropical Forestry, Chinese Academy of Forestry, 336600, Xinyu, Jiangxi, China
Abstract:[Background] Chinese fir is a common afforestation tree species in southern China. Under the background of climate change, droughts frequently occur. Studying the water transfer process of forest trees under special weather conditions can provide a basis for predicting the characteristics of transpiration water consumption in future scenarios.[Methods] We used the Granier thermal diffusion sap flow probe (TDP) to observe the sap flow of Chinese fir from March to July, and the soil moisture dynamics were measured by the AZS-100TDR, the meteorological factors such as the solar radiation, air temperature, relative air humidity, and rainfall were simultaneously observed. The saturation index curve was used to respectively fit the sap flow density, solar radiation and air vapor pressure deficit to analyze the influence of the sap flow characteristics of different provenances of Chinese fir in Dagangshan on the meteorological factors and the response of soil moisture dynamics. [Results] 1) The diurnal changes of sap flow of different Chinese fir provenances showed obvious changes in day and night with solar radiation and air vapor pressure deficit, and the difference was significant (P<0.01). Among them, the sap flow density of the provenance from Jiangxi Tonggu was the highest. The peak sap flow density during the period of sufficient soil moisture (RSP) was higher than that during the period of soil moisture deficit (RDP). The provenance from Xiushui, Jiangxi had the smallest change in sap flow density under the two moisture conditions with the lowest sap flow density, which is suitable to plant in poor moisture conditions. 2) The fitting equations of sap flow density of different provenances to meteorological factors in the two periods showed that the rate of increase of sap flow density in the RSP period was higher than that in the RDP period. The main factor affecting sap flow during the RSP was vapor pressure deficit, and solar radiation in RDP. [Conclusions] Soil moisture conditions, meteorological factors, and provenance origin will all affect the sap flow density of fir tree trunks, and different provenances have different sensitivities to different factors. This study reveals the drought resistance characteristics of different provenances and the response mechanism to drought, aiming to provide a scientific basis for the sustainable management of fir plantations and the effective management of forest water resources in different regions of southern China.
许庭毓, 牛香, 王兵, 宋庆丰, 王南, 孙建军, 刘儒. 不同土壤水分条件下杉木种源树干液流特征对气象因子的响应[J]. 中国水土保持科学, 2023, 21(5): 99-105.
XU Tingyu, NIU Xiang, WANG Bing, SONG Qingfeng, WANG Nan, SUN Jianjun, LIU Ru. Responses of sap flow characteristics under different Chinese fir provenances to meteorological factors under different soil moisture conditions. SSWC, 2023, 21(5): 99-105.
王文杰,孙伟,邱岭,等.不同时间尺度下兴安落叶松树干液流密度与环境因子的关系[J].林业科学, 2012, 48(1):77. WANG Wenjie, SUN Wei, QIU Ling, et al. Relations between stem sap flow density of Larix gmelinii and environmental factors under different temporal scale[J]. Scientia Silvae Sinicae, 2012, 48(1):77.
[2]
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. SUN Xu, YANG Wenhui, JIAO Lei, et al. Relationships between sapflux density of Pinus tabuliformis trees and environmental factors at different temporal scales in Mangshan National Forest Park in Beijing, China[J]. Acta Ecologica Sinica, 2022,42(10):4113.
[3]
樊敏,马履一,王瑞辉. 刺槐春夏季树干液流变化规律[J]. 林业科学, 2008, 44(1):41. FAN Min, MA Lüyi WANG Ruihui. Variation of stem sap flow of Robinia pseudoacacia in spring and summer[J]. Scientia Silvae Sinicae, 2008, 44(1):41.
[4]
ORTUNO M F, CONEJERP W, MORENO F, et al. Could trunk diameter sensors be used in woody crops for irrigation scheduling? A review of current knowledge and future perspectives[J]. Agricultural Water Management, 2010, 97(1):1.
[5]
秦颢萍,刘泽彬,郭建斌,等. 环境和冠层结构对华北落叶松林树干液流的影响[J]. 应用生态学报, 2021, 32(5):1681. QIN Haoping, LIU Zebin, GUO Jianbin, et al. Effects of environment and canopy structure on stem sap flow in a Larix principis-rupprechtii plantation[J]. Chinese Journal of Applied Ecology, 2021, 32(5):1681.
[6]
王云霓,曹恭祥,王彦辉,等.六盘山南侧华北落叶松人工林冠层蒸腾及其影响因子的坡位差异[J].应用生态学报,2018, 29(5):1503. WANG Yunni, CAO Gongxiang, WANG Yanhui, et al. Canopy transpiration of Larix principis-rupprechtii plantation and its impact factors in different slope locations at the south side of Liupan Mountains,China[J]. Chinese Journal of Applied Ecology, 2018, 29(5):1503.
[7]
BINDI M,BELLESI S,ORLANDINI S,et al. Influence of water deficit stress on leaf area development and transpiration of Sangiovese graprvines grown in pots[J].American Journal of Enology and Viticulture, 2005, 56(1):68.
[8]
FISHER R A, WILLIAMS M, DA COSTA A L, et al. The response of an Eastern Amazonian rain forest to drought stress:results and modelling analyses from a throughfall exclusion experiment[J].Global Change Biology, 2007, 13(11):2361.
[9]
吕金林, 何秋月, 闫美杰, 等. 黄土丘陵区辽东栎树干液流特征对边材面积和土壤水分的响应[J]. 应用生态学报, 2018, 29(3):725. LÜ Jinlin, HE Qiuyue, YAN Meijie, et al. Sap flow characteristics of Quercus liaotungensis in response to sapwood area and soil moisture in the loess hilly region,China[J]. Chinese Journal of Applied Ecology, 2018, 29(3):725.
[10]
王媛, 魏江生, 周梅, 等. 大兴安岭南段白桦树干液流对土壤水分的响应[J].水土保持研究,2020,27(4):128. WANG Yuan, WEI Jiangsheng, ZHOU Mei, et al. Response of sap flow of Betula platyphylla to soil moisture in southern Greater Xing'an Mountains[J]. Research of Soil and Water Conservation, 2020,27(4):128.
[11]
OREN R, PATAKI D E.Transpiration in response to variation in microclimate and soil moisture in southeastern deciduous forests[J].Oecologia, 2001, 127:549.
[12]
LAGERGREN F, LINDROTH A. Transpiration response to soil moisture in pine and spruce trees in Sweden[J]. Agricultural & Forest Meteorology, 2002, 112(2):67.
[13]
涂洁, 胡良, 刘琪璟, 等.江西千烟洲杉木生长季树干液流特征及影响因子[J].浙江农林大学学报, 2015, 32(2):257. TU Jie, HU Liang, LIU Qijing, et al. Sap flow characteristics during the growing season for Cunninghamia lanceolata in red soil areas of Jiangxi province[J]. Journal of Zhejiang A&F University, 2015, 32(2):257.
[14]
赵仲辉, 康文星, 田大伦, 等.湖南会同杉木液流变化及其与环境因子的关系[J].林业科学, 2009, 45(7):127. ZHAO Zhonghui, KANG Wenxing, TIAN Dalun, et al. Sap flow rate and its relationship with environmental factors of Chinese fir plantation in Huitong, Hunan province[J]. Scientia Silvae Sinica, 2009, 45(7):127.
[15]
刘鑫, 张金池, 汪春林, 等.长三角地区典型树种杉木液流速率变化特征[J].南京林业大学学报(自然科学版), 2014, 38(2):86. LIU Xin, ZHANG Jinchi, WANG Chunlin, et al. The variation characteristics of sap flow of Chinese fir in the Yangtze River Delta[J]. Journal of Nanjing Forestry University (Natural Sciences Edition), 2014, 38(2):86.
[16]
LIU Ziqiang, LIU Qianqian, WEI Zijun, et al. Partitioning tree water usage into storage and transpiration in a mixed forest[J]. Forest Ecosystem,2021,8:72.
[17]
GRANIER A,HUC R,BARIGAH S T.Transpiration of natural rain forest and its dependence on climate factors[J].Agricultural and Forest Meteorology, 1996, 78(1):19.
[18]
CAMPBELL G S,NORMAN J M.An introduction to environmental biophysics[M].New York,USA:Springer, 1998:22.
[19]
KAKUBARI Y,HOSOKAWA K. Estimation of stand transpiration of a beech forest based on an eco-physiologica computer simulation model and superporometer[J].Journal of the Japanese Forestry Society,1992,74:263.
[20]
张建国,久米朋宣,杜盛,等.黄土高原半干旱区辽东栎的树干液流动态[J].林业科学,2011, 47(4):63. ZHANG Jianguo, KUME Tomonori, DU Sheng, et al. Sap flow dynamics of dominant trees of Quercus liaotungensis forest in the semiarid Loess Plateau region[J]. Scientia Silvae Sinica,2011, 47(4):63.
[21]
MARTINEZ V J, MANGIRON M, OGAYA R, et al. Sap flow of three co-occurring Mediterranean woody species under varying atmospheric and soil water conditions[J]. Tree Physiology, 2003,23(11):747.
[22]
GRANIER A,LOUSTAU D,BREDA N. A generic model of forest canopy conductance dependent on climate,soil water availability and leaf area index[J]. Annals of Forest Science,2000,57:755.
[23]
吴旭,陈云明,唐亚坤.黄土丘陵区刺槐和侧柏人工林树干液流特征及其对降水的响应[J].植物生态学报,2015, 39(12):1176. WU Xu, CHEN Yunming, TANG Yakun. Sap flow characteristics and its responses to precipitation in Robinia pseudoacacia and Platycladus orientalis plantations[J]. Chinese Journal of Plant Ecology, 2015, 39(12):1176.
[24]
ZHANG Zhenzhen, ZHAO Ping, MCCARTHY H R, et al. Hydraulic balance of a Eucalyptus urophlla plantation in response to periodic drought in low subtropical China[J]. Frontiers in Plant Science, 2016, 7:1346.
[25]
张瑞婷,杨金艳,阮宏华.树干液流对环境变化响应研究的整合分析[J].南京林业大学学报(自然科学版, 2022,46(5):113. ZHANG Ruiting, YANG Jinyan, RUAN Honghua. Meta-analysis of responses of sap flow to environmental factor change[J]. Journal of Nanjing Forestry University (Natural Sciences Edition), 2022,46(5):113.
[26]
BENYON R G, NOLAN R H, HAWTHORN S N D, et al. Stand-level variation in evapotranspiration in non-water-limited eucalypt forests[J]. Journal of Hydrology, 2017, 551:233.
[27]
WHITLEY R, ZEPPEL M, ARMSTRONG N, et al. A modified Jarvis-Stewart model for predicting stand-scale transpiration of an Australian native forest[J]. Plant & Soil, 2008, 305(1/2):35.