Gall Rolf, Landolt W, Schleppi P, Michellod V, Bucher J B
Swiss Federal Research Institute WSL, CH-8903 Birmensdorf, Switzerland.
Tree Physiol. 2002 Jun;22(9):613-23. doi: 10.1093/treephys/22.9.613.
To determine the relationship between phloem transport and changes in phloem water content, we measured temporal and spatial variations in water content and sucrose, glucose and fructose concentrations in phloem samples and phloem exudates of 70- and 30-year-old Norway spruce trees (Picea abies (L.) Karst.). Large temporal and spatial variations in phloem water content (1.4-2.6 mg mg(dw)(-1)) and phloem total sugar concentration (31-70 mg g(dw)(-1)) paralleled each other (r(2) = 0.83, P < 0.0001 for the temporal profile and r(2) = 0.96, P < 0.008 for the spatial profile), indicating that phloem water content depends on the total amount of sugar to be transferred. Changes in phloem water content were unrelated to changes in bark thickness. Maximum changes in phloem water content calculated from dendrometer readings were only 8-11% of the maximum measured changes in phloem water content, indicating that reversible changes in bark thickness did not reflect changes in internal water relations. We also studied the relationship between xylem sap velocity and changes in bark thickness in 70-year-old trees during summer 1999 and winter 1999-2000. Sap flow occurred sporadically throughout the winter, but there was no relationship between bark shrinkage or swelling and sap velocity. In winter, mean daily xylem sap velocity was significantly correlated with mean daily vapor pressure deficit and air temperature (P < 0.0001, in both cases). Changes in bark thickness corresponded with both short- and long-term changes in relative humidity, in both winter and summer. Under controlled conditions at > 0 degrees C, changes in relative humidity alone caused changes in thickness of boiled bark samples. Because living bark of Norway spruce trees contains large areas with crushed and dead sieve cell zones-up to 24% of the bark is air-filled space-we suggest that this space can compensate for volume changes in living phloem cells independently of total tissue water content. We conclude that changes in bark thickness are not indicative of changes in either phloem water capacitance or xylem sap flow.
为了确定韧皮部运输与韧皮部含水量变化之间的关系,我们测量了70年和30年生挪威云杉(Picea abies (L.) Karst.)韧皮部样本及韧皮部渗出物中含水量以及蔗糖、葡萄糖和果糖浓度的时空变化。韧皮部含水量(1.4 - 2.6 mg mg(dw)(-1))和韧皮部总糖浓度(31 - 70 mg g(dw)(-1))在时间和空间上的大幅变化相互平行(时间分布r(2) = 0.83,P < 0.0001;空间分布r(2) = 0.96,P < 0.008),这表明韧皮部含水量取决于待转运糖的总量。韧皮部含水量的变化与树皮厚度的变化无关。根据测树仪读数计算出的韧皮部含水量最大变化仅为实测最大变化的8 - 11%,这表明树皮厚度的可逆变化并未反映内部水分关系的变化。我们还研究了1999年夏季和1999 - 2000年冬季70年生树木木质部汁液流速与树皮厚度变化之间的关系。整个冬季汁液流动偶尔发生,但树皮收缩或膨胀与汁液流速之间没有关系。在冬季,平均每日木质部汁液流速与平均每日水汽压差和气温显著相关(两种情况均为P < 0.0001)。树皮厚度的变化在冬季和夏季均与短期和长期的相对湿度变化相对应。在> 0℃的受控条件下,仅相对湿度的变化就会导致煮沸树皮样本厚度的变化。由于挪威云杉的活树皮包含大面积破碎和死亡的筛胞区域——高达24%的树皮是充满空气的空间——我们认为该空间可以独立于总组织含水量来补偿活韧皮部细胞中的体积变化。我们得出结论,树皮厚度的变化并不表明韧皮部水容量或木质部汁液流动的变化。