Shan Changjuan, Liang Zongsuo, Han Ruilan, Hao Wenfang
Institute of Soil and Water Conservation, Chinese Academy of Sciences and Ministry of Water Resources, Northwest Sci-Tech Unidversity of Agriculture and Forestry, Yangling, China.
Ying Yong Sheng Tai Xue Bao. 2005 Jul;16(7):1205-12.
With locust (Robinia pseudoacacia), the main tree species in afforestation, as test material, this paper studied the characteristics of its water physiological ecology and productivity under four habitats, i. e. , sunny, shady, semi-sunny and semi-shady hillsides, in the North Shaanxi gully areas of Loess Plateau. The mean water content in 0 - 500 cm soil layer was 8.87% (shady), 8.06% (semi-shady), 7.62% (semi-sunny), and 6.96% (sunny), respectively. There was a significant discrepancy between shady, semi-shady, semi-sunny and sunnyhilisides (a 0.01), and the difference between shady, semi-shady and semi-sunny, as well as between semi-sunny and sunny hillsides was also significant (a 0.05) . Remarkable relationships were found between leaf RWC, locus WSD and soil water content (SWC) . The leaf RWC and locust water potential under sunny hillside were lower, but those under shady hillside were higher. The daily mean transpiration was in order of shady (4.07 microg x cm(-2) x s(-1)) > semi-shady (3.89 microg x cm(-2) x s(-1)) > semi-sunny (3.05 microg x cm(-2) x s(-1)) > sunny (2.70 microg x cm(-2)s(-1)) hillside. The remarkable difference of transpiration appeared at 11:00 and 13:00, and there existed a remarkable relationship between transpiration and light intensity, RH and soil water content. All of these resulted in a diversity of locust biomass under different habitats, the highest under shady hillside, and the lowest under sunny hillside, and the differences between different habitats were all significant. It could be concluded that soil water content was the main factor affecting locust growth.
以黄土高原陕北沟壑区造林主要树种刺槐为试验材料,研究了阳坡、阴坡、半阳坡和半阴坡4种立地条件下刺槐的水分生理生态特征及生产力。0~500cm土层平均含水量分别为阴坡8.87%、半阴坡8.06%、半阳坡7.62%、阳坡6.96%。阴坡、半阴坡、半阳坡和阳坡之间差异极显著(α=0.01),阴坡、半阴坡和半阳坡之间以及半阳坡和阳坡之间差异也显著(α=0.05)。叶相对含水量、刺槐水势与土壤含水量之间存在显著关系。阳坡刺槐叶相对含水量和水势较低,阴坡较高。日平均蒸腾速率大小顺序为阴坡(4.07μg·cm-2·s-1)>半阴坡(3.89μg·cm-2·s-1)>半阳坡(3.05μg·cm-2·s-1)>阳坡(2.70μg·cm-2·s-1)。蒸腾速率在11:00和13:00差异显著,且蒸腾速率与光照强度、空气相对湿度和土壤含水量之间存在显著关系。这些导致不同立地条件下刺槐生物量存在差异,阴坡最高,阳坡最低,不同立地条件之间差异显著。可以得出结论,土壤含水量是影响刺槐生长的主要因素。