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Comprehensive Response of Daily Transpiration from Armeniaca sibirica Plantations to Meteorological and Soil Moisture/Temperature Conditions on the Semi-Arid Loess Plateau, China

文献类型： 外文期刊

作者： Han, Xinsheng 1 ; Liu, Guangquan 1 ; Xu, Hao 2 ; Dong, Liguo 2 ; Wang, Xiao 3 ;

作者机构： 1.China Inst Water Resources & Hydropower Res, State Key Lab Simulat & Regulat Water Cycle River, Beijing 100038, Peoples R China

2.Ningxia Acad Agr & Forestry Sci, Inst Forestry & Grassland Ecol, Res Ctr Ecol Restorat & Multifunct Forestry Ningxi, Ningxia Key Lab Desertificat Control & Soil & Wate, Yinchuan 750002, Peoples R China

3.Chinese Acad Forestry, Natl Forestry & Grassland Adm, Ecol & Nat Conservat Inst, Key Lab Forest Ecol & Environm, Beijing 100091, Peoples R China

关键词： tree transpiration; potential evapotranspiration; soil moisture; soil temperature; ecological economic forest; apricot; semi-arid region

期刊名称：FORESTS （ 影响因子：2.9； 五年影响因子：3.0 ）

ISSN：

年卷期： 2024 年 15 卷 2 期

页码：

收录情况： SCI

摘要： Forest transpiration plays a vital role in the regional water budget and water supply security of the semi-arid Loess Plateau of northwest China. A thorough understanding and accurate predictions of the variation in the transpiration of forests with important tree species, e.g., Armeniaca sibirica (L.) Lam., are critical for land and water management. Owing to the extreme climatic seasonality and interannual variability, detailed information on the seasonal variation in the transpiration of Armeniaca sibirica plantations and its response to climatic and soil moisture/temperature fluctuations is limited. Therefore, in this study, the sap flux density and meteorological and soil moisture/temperature conditions were continuously monitored during the growing season (May to October) in 2019-2020. The results show the four following features: (1) The mean daily transpiration of the Armeniaca sibirica plantation was 0.31 mm.day(-1); (2) the daily transpiration varied nonlinearly with increasing potential evapotranspiration (PET). Transpiration first increased rapidly until reaching the PET threshold of 4 mm.day(-1) and then slowly increased within the PET range of 4-8.5 mm.day(-1), but thereafter, it decreased slightly when PET exceeded 8.5 mm.day(-1); (3) the daily forest transpiration varied with increasing relative extractable soil water content (REW) and soil temperature (ST) following a saturated exponential function; i.e., it first increased until reaching a threshold of 0.5 of REW or 14 degrees C of ST, but thereafter tended to stabilize; (4) models for estimating the daily forest transpiration were established. According to these models, PET had the greatest limiting effect (32.17%) on forest transpiration during the observation period, while REW and ST showed lower limits at 7.03% and 3.87%, respectively. The findings of this study are useful for understanding and managing the hydrological effects of forests in the semi-arid Loess Plateau as a typical dryland with seasonal droughts.

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