Abstract

The changes in sap flow of Salix psammophila growing on a gentle slope (lower slope, P1), a middle slope (P2), and an upper slope (P3), and the response of sap flow to meteorological factors at the different slope positions were studied using the continuous and synchronized observations, the instrument were wrapped stem flowmeter EMS 62 sap-flow heat-balance-based system and the LSI-LASTEM automatic weather station. The results revealed that the soil moisture content was the highest and the growth conditions of Salix psammophila were the best at P1, followed by P2. At P3, however, although good apical dominance was observed, the proportion of dead branches was the highest. Furthermore, the daily variation patterns of sap flow on the three slopes presented as multi-peak bell-shaped curves. The daily accumulation changes in sap flow showed a trend of P1 > P3 > P2, and within the same diameter range, the sap flow at P1 was significantly different from that at P2 and P3, whereas the sap flow at P2 and P3 did not vary significantly. All the three slopes showed a significant and positive correlation with photosynthetically active radiation, atmospheric temperature, and vapor pressure difference, and a significant and negative correlation with relative humidity; however, the degrees of correlation varied slightly. The stepwise regression analysis showed that, at different slopes, different variables were selected for different branch diameters, but photosynthetically active radiation and atmospheric temperature played dominant roles on all slopes. This study reveals the sap flow pattern of Salix psammophila on different slopes and its response mechanism to meteorological factors, which was essential for understanding the restoration ability, physiological adaptability, and ecosystem stability of Salix psammophila communities.

Highlights

  • The Mu Us Desert is one of the four major sandy areas in China, with a typical fragile ecosystem of arid and semi-arid lands

  • The average crown width, total number of branches, and the LAI showed a trend of P1 > P2 > P3, which means that gentle slope conditions are conducive to the growth of Salix psammophila

  • The results of this study reported that the daily sap flow accumulation of Salix psammophila at different slope positions followed a pattern of D3 > D2 > D1 and had an overall trend of P1 > P3 > P2

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Summary

Introduction

The Mu Us Desert is one of the four major sandy areas in China, with a typical fragile ecosystem of arid and semi-arid lands. Sap flow of Salix psammophila and its principal influencing factors at different slopes in the Mu Us desert strong germination ability, tolerance to drought, wind-erosion, and sand burial, and good sand-fixing and water-conservation qualities [3,4,5], which have led to its use in sand dune stabilization and water conservation in this region. Artificial afforestation of sandy areas has led to excessive water consumption, mainly because of an overly dense plant distribution or a large water consumption by vegetation. This region has low annual precipitation, which is characterized by high interannual variations and uneven distribution; for many years, the maximum mean annual precipitation and mean annual evaporation rate here have been 300 mm and 2000 mm, respectively. A comprehensive study of transpiration in Salix psammophila plants growing in this region is of considerable importance, because it can guide rational planting of Salix psammophila, given the limited water resources, and can be used to formulate scientifically sound management measures

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