Faculty of Forestry and the Forest Environment, Lakehead University, 955 Oliver Road, Thunder Bay, ON P7B 5E1, Canada.
Tree Physiol. 2009 Nov;29(11):1341-8. doi: 10.1093/treephys/tpp079. Epub 2009 Sep 28.
White birch (Betula papyrifera Marsh.) seedlings were grown under two carbon dioxide concentrations (ambient: 360 micromol mol(-1) and elevated: 720 micromol mol(-1)), three soil temperatures (5, 15 and 25 degrees C initially, increased to 7, 17 and 27 degrees C, respectively, 1 month later) and three moisture regimes (low: 30-40%; intermediate: 45-55% and high: 60-70% field water capacity) in greenhouses. In situ gas exchange and chlorophyll fluorescence were measured after 2 months of treatments. Net photosynthetic rate (A(n)) of seedlings grown under the intermediate and high moisture regimes increased from low to intermediate T(soil) and then decreased to high T(soil). There were no significant differences between the low and high T(soil), with the exception that A(n) was significantly higher under high than low T(soil) at the high moisture regime. No significant T(soil) effect on A(n) was observed at the low moisture regime. The intermediate T(soil) increased stomatal conductance (g(s)) only at intermediate and high but not at low moisture regime, whereas there were no significant differences between the low and high T(soil) treatments. Furthermore, the difference in g(s) between the intermediate and high T(soil) at high moisture regime was not statistically significant. The low moisture regime significantly reduced the internal to ambient CO2 concentration ratio at all T(soil). There were no significant individual or interactive effects of treatment on maximum carboxylation rate of Rubisco, light-saturated electron transport rate, triose phosphate utilization or potential photochemical efficiency of photosystem II. The results of this study suggest that soil moisture condition should be taken into account when predicting the responses of white birch to soil warming.
在温室中,将白桦(Betula papyrifera Marsh.)幼苗分别置于两种二氧化碳浓度(环境:360 μmol/mol 和升高:720 μmol/mol)、三种土壤温度(初始为 5、15 和 25°C,1 个月后分别升高至 7、17 和 27°C)和三种水分条件(低:30-40%;中:45-55%和高:60-70%田间持水量)下进行生长。在处理 2 个月后,对其进行原位气体交换和叶绿素荧光测量。在中、高水分条件下生长的幼苗净光合速率(A(n))从低到中土壤温度增加,然后降低到高土壤温度。在低和高土壤温度之间没有显著差异,但在高水分条件下,A(n)在高土壤温度下显著高于低土壤温度。在低水分条件下,A(n)没有显著的土壤温度效应。中土壤温度仅在中、高水分条件下增加气孔导度(g(s)),而在低水分条件下则没有显著差异。此外,高水分条件下,g(s)在中、高土壤温度之间的差异在统计学上并不显著。低水分条件显著降低了所有土壤温度下的胞间与环境 CO2 浓度比。处理对 RuBP 羧化酶最大羧化速率、光饱和电子传递速率、三磷酸甘油醛利用或光系统 II 潜在光化学效率没有显著的个体或交互作用。本研究结果表明,在预测白桦对土壤变暖的响应时,应考虑土壤水分条件。