Impacts of environmental and canopy conditions on the nighttime sap flow of larch plantations in the Liupan Mountains, China

被引:2
|
作者
Yu, Songping [1 ,2 ]
Guo, Jianbin [1 ]
Liu, Zebin [2 ]
Wang, Yanhui [2 ]
Xu, Lihong [2 ]
Yu, Pengtao [2 ]
He, Liang [1 ]
机构
[1] Beijing Forestry Univ, Sch Soil & Water Conservat, Beijing 100083, Peoples R China
[2] Chinese Acad Forestry, Key Lab Forest Ecol & Environm Natl Forestry & Gra, Ecol & Nat Conservat Inst, Beijing 100091, Peoples R China
基金
中国国家自然科学基金;
关键词
Nighttime sap flow; Reference evapotranspiration; Leaf area index; Soil moisture; Multi-factor impact; NOCTURNAL WATER-LOSS; STOMATAL CONDUCTANCE; SOIL-WATER; POPULUS-EUPHRATICA; LOESS PLATEAU; WOODY-PLANTS; TRANSPIRATION; TREE; DROUGHT; FOREST;
D O I
10.1007/s11676-023-01619-0
中图分类号
S7 [林业];
学科分类号
0829 ; 0907 ;
摘要
Nighttime sap flow (Q(n)) is an important physiological activity under which trees manage drought stress. An in-depth understanding of the characteristics of Q(n) and its response to environmental and canopy conditions are of significance for arid area forest and water management. This study measured daily sap flow (Q(s)) of a Larix principis-rupprechtii plantation in the Liupan Mountains, northwest China during the 2017-2019 growing seasons, and separated Q(s) into daytime sap flow (Q(d)) and Q(n). Meteorological conditions (reference evapotranspiration, ETref), canopy structure (leaf area index, LAI), and soil moisture (relative soil water content, RSWC) were considered as the main biophysical factors affecting Q(n). The structural equation model and upper boundary line method determined the effects of compound and single factors on Q(n). The daily mean Q(n) values during the growing seasons in 2017, 2018, and 2019 were 0.024, 0.026, and 0.030 mm d(-1), accounting for 6.2, 11.2, and 10.1% of Q(s), respectively. Q(n) at different canopy development phases (leaf expanding, LG; leaf expanded, LD; and defoliation, DF) over three years was LD > LG > DF. Q(n) increased with increasing ETref, whereas the ratio of Q(n) to Q(s) decreased. Q(n) did not show regular variation in the three-year growing seasons under different soil moisture conditions. ETref and LAI mainly controlled Q(n) by affecting Q(d), whereas RSWC had no significant effect on Q(n). Q(n) had a positive and linear relationship with LAI and a quadratic relationship with ETref. Both explained 40% of variation in Q(n). Meteorological and canopy conditions are important factors affecting Q(n) on the semi-humid study site. The application of the Q(n) model coupled with the impact of ETref and LAI furthers understanding of the impacts of climate and forest structure change on Q(n).
引用
收藏
页码:1927 / 1940
页数:14
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