赤皮青冈幼苗叶片解剖结构对干旱胁迫的响应

以浙江庆元、湖南洞口和湖南靖州3个种源的赤皮青冈1年生幼苗为材料,采用盆栽称量法控制土壤水分含量,设置土壤相对含水量分别为75%～80%(对照)、55%～60%(轻度干旱胁迫)、45%～50%(中度干旱胁迫)和30%～35%(重度干旱胁迫),研究不同程度干旱胁迫对赤皮青冈幼苗叶片解剖结构和蒸腾作用的影响.结果表明: 干旱胁迫下,3个种源赤皮青冈幼苗叶片的总厚度、上下表皮厚度和栅栏组织厚度均显著降低.栅栏组织厚度与海绵组织厚度比(栅海比)、气孔长度和宽度随干旱程度的增强而显著减小,而气孔密度随干旱胁迫程度的增强而显著增加.干旱处理对叶片主脉厚度无显著影响,木质部厚度的变化因种源而异.叶片结构的变化引起生理功能改变,随着胁迫程度的加强,赤皮青冈幼苗的蒸腾速率显著降低.对照和各干旱处理湖南洞口种源幼苗叶片的下表皮厚度、栅海比、气孔密度显著大于其他2个种源,蒸腾速率显著小于其他2个种源,表明湖南洞口赤皮青冈对干旱胁迫的适应性较强.     

栓皮栎地上部分构型及生物量分配

研究秦岭南坡商洛地区不同径级栓皮栎的地上部分构型、生物量及其分配和构型与生物量的关系.结果表明： 不同径级栓皮栎地上部分构型与生物量的分配存在差异.随着径级的增大,栓皮栎树高、胸径和冠幅逐渐增大;平均递减率先增大后减小;栓皮栎总体分枝率和逐步分枝率先增加后下降;不同径级栓皮栎垂直方向上的比叶面积为0.02～0.03,叶重比、叶面积指数和叶面积比的较大值在径级为Ⅰ、Ⅱ、Ⅲ时出现于树干中、上部,在径级为Ⅳ、Ⅴ、Ⅵ时出现在树干中部,径级进一步增大则在垂直方向上出现2个峰值,分别位于树干中下部和中上部.栓皮栎地上部分生物量中,树干生物量占71.8%～88.4%,枝生物量占5.8%～19.6%,叶生物量占4.2%～8.6%.随着径级的增大,树干生物量所占比例先减小后增大,而枝、叶生物量所占比例呈先增大后减小再增大的趋势.栓皮栎地上部分生物量与树高、胸径、冠幅和逐步分枝率(R_2∶1)呈显著正相关,与总体分枝率和逐步分枝率(R_3∶2)呈正相关趋势,但相关性不显著.树干生物量、地上总生物量与树干递减率呈负相关趋势,枝生物量、叶生物量与树干递减率呈正相关趋势,但相关性均不显著.     

豆腐木叶果胶含量的动态变化规律研究

测定了不同季节豆腐柴木叶中的果胶含量,并研究了不同叶位豆腐木果胶含量的变化规律.结果表明,豆腐木叶中的果胶含量在6～8月呈上升趋势,8月最高,9月开始下降.不同叶位果胶含量中,第3、5、6叶位的豆腐木叶片果胶含量较高,第5叶最高.     

Photosynthetic and morphological characters of Caragana microphylla in different slope aspects and positions

In order to find out how small scale topographical factors affect growth and physiological characters of Caragana microphylla, which is a widely distributed shrub species and has an important role in restoring degraded grassland in natural ecosystem, a natural population of C. microphylla was chosen in a typical steppe community in June, 2009. The population was 34 km to the southeast of Xilinhot City, China, and a total of 54 shrubs were selected from different slope aspects and positions. We investigated the photosynthetic and morphological characters of these shrubs and analyzed the relationship between plant traits of C. microphylla and soil nitrogen and phosphorus availability. Moreover, the relationship between plant traits of C. microphylla and herbaceous aboveground biomass was studied. (1) The maximum net photosynthetic rate (Pn_max) was significantly lower on shady slopes than that on sunny slopes and higher on upper slopes than that on lower slopes. Stomatal conductance (Gs), net photosynthetic rate/intercellular CO₂ concentration (Pn/Ci) and intercellular CO₂ concentration (Ci) under saturated irradiance showed similar trends with slope aspect and position. Likewise, the maximum photochemical efficiency of PSII (Fv/Fm), PSII potential activity (Fv/Fo) and the first-year shoot morphological characters of C. microphylla were also correlated with slope aspect and position. (2) Soil nitrogen availability showed no significant effect on photosynthetic or morphological traits of C. microphylla, however, there were several significant relationships between soil phosphorus availability and plant traits. Dry weight, shoot length, compound leaf size, and leaflet length of first-year shoots of C. microphylla were significantly negatively correlated with soil C:P ratio. Though not significant, photosynthetic parameters under saturated light and other morphological characters of first-year shoots were negatively correlated with soil C:P ratio, i.e., these traits increased with increasing soil phosphorus availability. These suggested that the difference of soil phosphorus availability played an important role in making C. microphylla having different photosynthetic and morphological characters on different slope aspects and positions. The individuals grown in relatively P-rich site had longer shoots and larger leaves and grew better. Low phosphorus content was thought to limit photosynthetic activity through several different mechanisms, including both stomatal and non-stomatal limitations, the latter being more likely in the present study. (3) Photosynthetic and morphological characters of C. microphylla were all negatively correlated with herbaceous aboveground biomass, though only Pn/Ci and length of first-year shoot were significantly correlated with it. This indicated that the difference in plant community was a factor making C. microphylla have different growth and physiological characters on different aspects and positions of slope. A number of studies showed that grazing of the herbaceous layer promoted the establishment and proliferation of woody species, and then led to grassland deterioration; but in arid and semi-arid ecosystems, some widely distributed shrub species like C. microphylla created resource islands and provide favorable microhabitat for grass species. In the present study, we found negative correlations between traits of C. microphylla and herbaceous aboveground biomass. We suggested that the removal of livestock grazing result in the decrease of the distribution C. microphylla and increase of grass coverage, and lead to the restoration of the typical steppe.     

小叶锦鸡儿灌丛群落蒸腾耗水量估算方法

为了确定沙地小叶锦鸡儿 (Caragana microphylla) 人工林的蒸腾速率, 于2006年6月运用热平衡茎流测量技术, 对科尔沁沙地一处15a生人工小叶锦鸡儿群落的分枝液流动态进行了监测。根据生物统计结果选取被测标准枝, 标准枝基径在0.4~1cm范围内。同时, 分别用基径总断面积推算法和叶片密度推算法对灌丛叶面积进行了估算。以叶面积为扩展纯量, 利用标准枝液流对灌丛群落耗水量进行尺度转换, 在转换过程中, 假设叶面积与蒸腾耗水量之间具有很强的相关性。该尺度转换方法经与大型称重式Lysimeter测值对比验证, 误差小于14.3%, 可望准确估算小叶锦鸡儿灌丛群落的蒸腾耗水量。     

长白山阔叶红松林不同深度土壤水分特征曲线

采用露点水势仪对长白山阔叶红松林不同深度（0～10 cm的壤土、20～30 cm的白浆土、50～60 cm的黄土）土壤水分特征曲线进行分析.结果表明：不同土层土壤水分特征曲线整体趋势均表现为快速下降-缓慢下降-基本平稳;用Gardner等提出的幂函数方程可较好地反映该区土壤含水量与土壤水势之间的数量关系,拟合方程的相关系数在0.9239～0.9400;不同土层土壤的持水能力大小依次为黄土>壤土>白浆土,土壤含水量随土壤水势降低而减小的速度依次为壤土>白浆土>黄土.不同土层脱湿过程的土壤水分特征曲线位于吸湿过程之下,说明土壤水分存在滞后现象,且滞后时效依次为壤土>黄土>白浆土.