Irvine J., Perks M. P., Magnani F., Grace J.
Institute of Ecology and Resource Management, University of Edinburgh, Darwin Building, Mayfield Road, Edinburgh EH9 3JU, U.K.
Tree Physiol. 1998 Jun;18(6):393-402. doi: 10.1093/treephys/18.6.393.
We investigated the impact of drought on the physiology of 41-year-old Scots pine (Pinus sylvestris L.) in central Scotland. Measurements were made of the seasonal course of transpiration, canopy stomatal conductance, needle water potential, xylem water content, soil-to-needle hydraulic resistance, and growth. Comparison was made between drought-treated plots and those receiving average precipitation. In response to drought, transpiration rate declined once volumetric water content (VWC) over the top 20 cm of soil reached a threshold value of 12%. Thereafter, transpiration was a near linear function of soil water content. As the soil water deficit developed, the hydraulic resistance between soil and needles increased by a factor of three as predawn needle water potential declined from -0.54 to -0.71 MPa. A small but significant increase in xylem embolism was detected in 1-year-old shoots. Stomatal control of transpiration prevented needle water potential from declining below -1.5 MPa. Basal area, and shoot and needle growth were significantly reduced in the drought treatment. In the year following the drought, canopy stomatal conductance and soil-to-needle hydraulic resistance recovered. Current-year needle extension recovered, but a significant reduction in basal area increment was evident one year after the drought. The results suggest that, in response to soil water deficit, mature Scots pine closes its stomata sufficiently to prevent the development of substantial xylem embolism. Reduced growth in the year after a severe soil water deficit is most likely to be the result of reduced assimilation in the year of the drought, rather than to any residual embolism carried over from one year to the next.
我们研究了干旱对苏格兰中部41年生欧洲赤松(Pinus sylvestris L.)生理特征的影响。对蒸腾作用的季节变化过程、冠层气孔导度、针叶水势、木质部含水量、土壤到针叶的水力阻力以及生长情况进行了测量。对干旱处理地块和平均降水量地块进行了比较。干旱时,当土壤表层20厘米处的体积含水量(VWC)达到12%的阈值时,蒸腾速率下降。此后,蒸腾作用几乎是土壤含水量的线性函数。随着土壤水分亏缺加剧,土壤与针叶间的水力阻力增加了两倍,黎明前针叶水势从-0.54兆帕降至-0.71兆帕。在1年生嫩枝中检测到木质部栓塞有小幅但显著的增加。气孔对蒸腾作用的控制使针叶水势不会降至-1.5兆帕以下。干旱处理下,断面积、嫩枝和针叶生长显著减少。干旱后的一年,冠层气孔导度和土壤到针叶的水力阻力恢复。当年针叶伸长恢复,但干旱一年后断面积增量仍显著减少。结果表明,为应对土壤水分亏缺,成熟的欧洲赤松会充分关闭气孔,以防止木质部形成大量栓塞。严重土壤水分亏缺后一年生长量减少,最可能是干旱当年同化作用降低的结果,而非前一年残留的栓塞造成的。