Stand transpiration characteristics of Larix principis-rupprechtii plantation and their influencing factors in Liupan Mountain

doi:10.12302/j.issn.1000-2006.202001025

JOURNAL OF NANJING FORESTRY UNIVERSITY ›› 2021, Vol. 45 ›› Issue (1): 131-140.doi: 10.12302/j.issn.1000-2006.202001025

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Stand transpiration characteristics of Larix principis-rupprechtii plantation and their influencing factors in Liupan Mountain

YU Songping¹^,²(), LIU Zebin², GUO Jianbin¹^,^*(), WANG Yanhui², YU Pengtao², WANG Lei¹

1. College of Soil & Water Conservation,Beijing Forestry University, Beijing 100083, China
2. Institute of Forest Ecology, Environment and Protection, Chinese Academy of Forestry, Key Laboratory of Forestry Ecology and Environment of National Forestry and Grassland Administration, Beijing 100091, China

Received:2020-01-09 Accepted:2020-05-13 Online:2021-01-30 Published:2021-02-01
Contact: GUO Jianbin E-mail:m18342800419@163.com;jianbinguo@bjfu.edu.cn

Abstract

Abstract:

【Objective】Stand transpiration, a key process in the soil-plant-atmosphere continuum, is an important water output item in the forest ecosystem, accounting for more than 50% of the total forest evapotranspiration. Therefore, exploring the stand transpiration response to environmental factors can provide a theoretical basis and data support for the scientific guidance of afforestation and integrated management of forest and water.【Method】At the Ningxia Liupan Mountain positioning station of the National Forestry and Grassland Administration, the sap flow of a Larix principis-rupprechtii plantation during the growing season (May-September) of 2016 was observed in the semi-humid area of Liupan Mountain and scaled-up for an estimation of stand transpiration. Meanwhile, the atmospheric factors outside the forest and the soil water content under the forest were simultaneously observed and the response of stand transpiration to atmospheric factors and root-zone (0-60 cm soil layer) soil water content was analyzed.【Result】 ① During the study period, the daily stand transpiration ranged from 0.005 to 1.866 mm/d, with a mean of 1.042 mm/d. The daily stand transpiration in different months was: June (1.325 mm/d) >May (1.099 mm/d) >July (1.077 mm/d) >August (1.009 mm/d) >September (0.717 mm/d). ② According to the correlation coefficient matrix of atmospheric factors and daily stand transpiration, the main atmospheric factors affecting daily stand transpiration were solar radiation intensity (R_n), saturated water vapor pressure deficit (D_VPD) and relative air humidity (H_RH). The order of correlation was: R_n (0.784) >D_VPD (0.754) >H_RH (-0.704). ③ The atmospheric factors could be reduced to three comprehensive indicators based on the factor analysis were climate fluctuation factor (44.9%), transpiration driving factor (35.2%) and air mobility factor (15.7%). The relevant analysis showed that transpiration driving factors (R_n, D_VPD and H_RH) and stand transpiration were significantly correlated. Also, the fitting effect of transpiration driving factors and stand transpiration (R² = 0.688) was better than the fitting effect of potential evapotranspiration and daily stand transpiration T_PET (R² = 0.649). ④ The contribution rate of R_n and D_VPD to the daily stand transpiration could reach 93%, of which 54.2% came from R_n,and 38.8% came from D_VPD. ⑤ The diurnal variation of decoupling coefficient and stand transpiration showed that the time of R_n controlling transpiration occurred from sunrise to the highest net radiation (at 11:00 am), while the time of D_VPD controlling transpiration occurred in the afternoon and at night. ⑥ Under humid soil conditions [root-zone relative extract water (W_REW)>0.38], the daily stand transpiration was significantly positively correlated with W_REW in the 40-60 cm soil layers (P<0.01), but there was no significant correlation or significant negative correlation with W_REW in other soil layers. Under soil drought conditions (root-zone W_REW≤0.38), the daily stand transpiration was significantly positively correlated with W_REW of ≥20-40 cm and ≥40-60 cm soil layers (P<0.01), and was not significantly negatively correlated with W_REW of 0-10 cm and ≥10-20 cm soil layers.【Conclusion】The main atmospheric factors affecting stand transpiration were R_n and D_VPD, and in the intra-day scale, the period dominating transpiration was different between the two factors. The transpiration driving factor was better than T_PET in reflecting the comprehensive effect of atmospheric factors on stand transpiration. Under humid soil conditions, the water source for transpiration in Larix principis-rupprechtii was mainly from the ≥40-60 cm soil profile layers, while under soil drought conditions, the water source of transpiration was mainly from the ≥20-60 cm soil profile layers.

Key words: stand transpiration, atmospheric factor, transpiration driving factor, soil relative extract water, response characteristics

CLC Number:

S715

YU Songping, LIU Zebin, GUO Jianbin, WANG Yanhui, YU Pengtao, WANG Lei. Stand transpiration characteristics of Larix principis-rupprechtii plantation and their influencing factors in Liupan Mountain[J]. JOURNAL OF NANJING FORESTRY UNIVERSITY, 2021, 45(1): 131-140.

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变量 variable	W	R_n	T_a	H_RH	D_VPD	T_a,min	T_a,max	T
W	1
R_n	0.287^**	1
T_a	0.029	-0.025	1
H_RH	-0.536^**	-0.720^**	0.014	1
D_VPD	0.402^**	0.730^**	0.410^**	-0.841^**	1
T_a,min	0.021	-0.058	0.999^**	0.043	0.380^**	1
T_a,max	0.042	0.017	0.999^**	-0.023	0.446^**	0.996^**	1
T	0.219^**	0.784^**	0.144	-0.704^**	0.754^**	0.118	0.177^*	1

综合因子 comprehensive factor	方差 variance	方差贡献率/% variance proportion	累计方差贡献/% variance cum
Fac-1	3.139	44.85	44.85
Fac-2	2.446	35.23	80.08
Fac-3	1.098	15.68	95.75

综合因子 comprehensive factor	Fac-1			Fac-2			Fac-3
综合因子 comprehensive factor	T_a	T_a,min	T_a,max	R_n	D_VPD	H_RH	W
Fac-1	0.999	0.999	0.996	-0.072	0.380	0.050	0.010
Fac-2	0.041	0.007	0.084	0.930	0.876	-0.873	0.252
Fac-3	0.007	0.007	0.008	0.004	0.203	-0.373	0.958
偏回归系数 partial regression coefficient	2.736	-0.521	-1.218	0.485	0.347	-0.063	—
综合贡献率 comprehensive contribution rate	0.611	0.116	0.273	0.542	0.388	0.070	1

W_REW梯度 W_REW gradient	土层深度/cm soil depths				样本容量 size
W_REW梯度 W_REW gradient	0~10	≥10~20	≥20~40	≥40~60	样本容量 size
土壤干旱 soil drought (W_REW≤0.38)	-0.473^**	-0.264^*	0.387^**	0.596^**	61
土壤湿润 soil humid (W_REW>0.38)	-0.224^*	-0.164	0.160	0.305^**	84

Stand transpiration characteristics of Larix principis-rupprechtii plantation and their influencing factors in Liupan Mountain

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