Water storage capacity of the canopy dominated by Caragana korshinskii and Hippophae rhamnoides in hilly and gully region on the Loess Plateau of Northwest China

2013 ◽  
Vol 37 (1) ◽  
pp. 45-51 ◽  
Author(s):  
Sheng-Qi JIAN ◽  
Chuan-Yan ZHAO ◽  
Shu-Min FANG ◽  
Kai YU ◽  
Wen-Ying MA
2022 ◽  
Author(s):  
Jinxia An ◽  
Guangyao Gao ◽  
Chuan Yuan ◽  
Bojie Fu

Abstract. Rainfall is known as the main water replenishment in dryland ecosystem, and rainfall partitioning by vegetation reshapes the spatial and temporal distribution patterns of rainwater entry into the soil. The dynamics of rainfall partitioning have been extensively studied at the inter-event scale, yet very few studies have explored its finer intra-event dynamics and the relating driving factors for shrubs. Here, we conducted a concurrent in-depth investigation of rainfall partitioning at inter- and intra-event scales for two typical xerophytic shrubs (Caragana korshinskii and Salix psammophila) in the Liudaogou catchment of the Loess Plateau, China. The event throughfall (TF), stemflow (SF), and interception loss (IC) and their temporal variations within the rainfall event as well as the meteorological factors and vegetation characteristics were systematically measured during the 2014–2015 rainy seasons. The C. korshinskii had significantly higher SF percentage (9.2 %) and lower IC percentage (21.4 %) compared to S. psammophila (3.8 % and 29.5 %, respectively) (p < 0.05), but their TF percentages were not significantly different (69.4 % vs. 66.7 %). At the intra-event scale, TF and SF of S. psammophila was initiated (0.1 vs. 0.3 h and 0.7 vs. 0.8 h) and peaked (1.8 vs. 2.0 h and 2.1 vs. 2.2 h) more quickly, and TF of S. psammophila lasted longer (5.2 vs. 4.8 h), delivered more intensely (4.3 vs. 3.8 mm∙h−1), whereas SF of C. korshinskii lasted longer (4.6 vs. 4.1 h), delivered more intensely (753.8 vs. 471.2 mm∙h−1). For both shrubs, rainfall amount was the most significant factor influencing inter-event rainfall partitioning, and rainfall intensity and duration controlled the intra-event TF and SF variables. The C. korshinskii with larger branch angle, more small branches and smaller canopy area, has an advantage to produce stemflow more efficiently over S. psammophila. The S. psammophila has lower canopy water storage capacity to generate and peak throughfall and stemflow earlier, and it has larger aboveground biomass and total canopy water storage of individual plant to produce higher interception loss compared to C. korshinskii. These findings contribute to the fine characterization of shrub-dominated eco-hydrological processes, and improve the accuracy of water balance estimation in dryland ecosystem.


2015 ◽  
Vol 45 (1) ◽  
pp. 15-25 ◽  
Author(s):  
Shengqi Jian ◽  
Chuanyan Zhao ◽  
Shumin Fang ◽  
Kai Yu

Understanding the water-use strategy of trees and shrubs is crucial for developing effective vegetation restoration in regions that are subjected to water scarcity. We studied the water-use strategy of Caragana korshinskii Kom. and Hippophae rhamnoides L. in the Chinese Loess Plateau to evaluate the adaption strategies of these two shrubs, which are both commonly used in the restoration programs in this region. We extrapolated the measurements of water use by individual plants to determine the area-averaged transpiration of the shrublands. There was a good agreement between transpiration estimated by the Penman–Monteith method and by the sap-flow method, which suggests that that the sap-flow method can provide reliable estimates of shrub transpiration at the stand level. Stand transpiration was mainly influenced by environmental factors such as photosynthetically active radiation, vapor pressure deficit, and soil water content. When the soil water content was sufficient, photosynthetically active radiation and vapor pressure deficit were the dominant factors; however, soil water content was the primary factor under low soil moisture levels. Stand transpiration ranged from 0.52 to 4.21 mm·day−1 with a mean of 1.42 mm·day−1 for C. korshinskii and ranged from 0.57 to 3.99 mm·day−1 with a mean of 1.94 mm·day−1 for H. rhamnoides. During the experimental period (from June to September 2013), cumulative transpirations were 173.4 and 236.6 mm for C. korshinskii and H. rhamnoides, respectively, which accounted for up to 88.2% of the rainfall registered during this period. We calculated the soil water balance and measured the water potential of stems and leaves for C. korshinskii and H. rhamnoides. Hippophae rhamnoides had a lower net soil water storage, indicating that it consumed more soil water than C. korshinskii. There were some negative water potential drops between stems and leaves for H. rhamnoides, suggesting the lack of a safety margin for H. rhamnoides. Our results indicated that C. korshinskii is more suitable for afforestation than H. rhamnoides in the Loess Plateau.


2021 ◽  
Vol 11 (1) ◽  
Author(s):  
Jie Chen ◽  
Xue-wen Lei ◽  
Han-lin Zhang ◽  
Zhi Lin ◽  
Hui Wang ◽  
...  

AbstractThe problems caused by the interaction between slopes and hydrologic environment in traffic civil engineering are very serious in the granite residual soil area of China, especially in Guangdong Province. Against the background of two heavy rainfall events occurring during a short period due to a typhoon making landfall twice or even two typhoons consecutively making landfall, laboratory model tests were carried out on the hydrological effects of the granite residual soil slope considering three vegetation types under artificial rainfall. The variation in slope surface runoff, soil moisture content and rain seepage over time was recorded during the tests. The results indicate that surface vegetation first effectively reduces the splash erosion impact of rainwater on slopes and then influences the slope hydrological effect through rainwater forms adjustment. (1) The exposed slope has weak resistance to two consecutive heavy rains, the degree of slope scouring and soil erosion damage will increase greatly during the second rainfall. (2) The multiple hindrances of the stem leaf of Zoysia japonica plays a leading role in regulating the hydrological effect of slope, the root system has little effect on the permeability and water storage capacity of slope soil, but improves the erosion resistance of it. (3) Both the stem leaf and root system of Nephrolepis cordifolia have important roles on the hydrological effect. The stem leaf can stabilize the infiltration of rainwater, and successfully inhibit the surface runoff under continuous secondary heavy rainfall. The root system significantly enhances the water storage capacity of the slope, and greatly increases the permeability of the slope soil in the second rainfall, which is totally different from that of the exposed and Zoysia japonica slopes. (4) Zoysia is a suitable vegetation species in terms of slope protection because of its comprehensive slope protection effect. Nephrolepis cordifolia should be cautiously planted as slope protection vegetation. Only on slopes with no stability issues should Nephrolepis cordifolia be considered to preserve soil and water.


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