边缘效应带促进红松生长的光合生理生态学研究

以一个经过12a边缘效应带处理的14年生红松幼林生态系统为研究对象,通过对3种宽度(4m,6m,8m)边缘效应带及保留带内红松幼树的光合日进程、碳素日积累量及相关生理生态学因子(光照、气孔导度、小枝木质部水势、叶片温度、叶面饱和蒸气压亏缺)的研究,探讨了造成不同效应带和保留带内红松生长差异的光合生理生态学原因。结果：4m效应带光照不足引起的碳素日积累量过低导致红松生长较差,8m效应带气孔导度过低引起的光合午休现象导致了碳素日积累量低、红松生长较差。8m效应带引起气孔导度下降的因素主要是过强光照引起叶片温度较高、叶面饱和蒸气压亏缺较大以及小枝木质部水势过低。研究认为,太宽的8m带和太窄的4m带都在一定程度上引起了光合生理生态学的不适应,导致生长水平下降,6m宽度的边缘效应带是人工促进红松生长的最佳边缘效应带。     

植物气孔气态失水与SPAC系统液态供水的相互调节作用研究进展

讨论了植物气孔气态失水与SPAC系统液态供水相互作用研究领域的一些重要现象和行为.当植物水力信号和化学信号共同作用促进气孔对叶水势的调节时,植物对叶水势的调节表现为等水行为.气孔对环境湿度变化响应的反馈机制可用来解释土壤干旱条件下气孔和光合的午休现象,以及气孔导度和水流导度之间的相关关系;而气孔对环境湿度变化响应的前馈机制,则可用来解释气孔导度对大气 叶片间水汽饱和差的滞后反应.植物最大限度地利用木质部传输水分的策略,要求气孔快速响应以避免木质部过度气穴化和短时间内将气穴逆转的相应机制.     

华北山区侧柏冠层气孔导度特征及其对环境因子的响应

冠层气孔导度(g_s)是衡量冠层-大气界面水汽通量的重要生物学常数,研究其特征及对环境因子的响应,能为开展森林冠层水汽交换过程的机理性研究提供理论依据.于2014年利用SF-L热扩散式探针测定了侧柏的树干液流密度(J_s),同步监测光合有效辐射(PAR)、饱和水汽压差(VPD)、气温(T)等环境因子,计算侧柏的冠层气孔导度特征并分析其对各环境因子的响应.结果表明: 侧柏液流密度的日变化总体呈双峰曲线,生长季高于非生长季,且胸径越大液流密度越大;冠层气孔导度日变化与单位叶面积冠层蒸腾(E_L)趋势相近,均呈双峰曲线,生长季的冠层气孔导度和蒸腾较非生长季略高.侧柏冠层气孔导度与空气温度呈抛物线关系,在10 ℃左右冠层气孔导度达到峰谷;光合有效辐射以400 μmol·m^-2·s^-1为界,小于该阈值两者呈正相关关系,大于该阈值则冠层气孔导度受其影响较小;与饱和水汽压差呈负对数函数关系,随饱和水汽压差增大而逐渐降低.较高的空气温度和光合有效辐射、较低的饱和水汽压差有利于侧柏形成较大的冠层气孔导度,进而促进冠层蒸腾.     

土壤水分变化对长白山主要树种蒙古栎幼树生长的影响

选择长白山红松阔叶林主要优势树种蒙古栎为研究对象,人工控制3种施水量研究蒙古栎幼树形态、生物量效应和光合生理特征对土壤含水量变化的响应．结果表明,不同土壤含水量变化显著影响蒙古栎叶片、枝、根的生物量及其分配格局和叶片光合气体交换特征．水分胁迫改变幼树树冠结构,抑制幼树树高、地径、叶片大小、地上和地下生物量;同时,蒙古栎幼树根冠生物量比随着土壤水分含量的减少显著提高;供水量减少对幼树净光合速率、CO2利用率和碳利用率等特征有显著的负向影响;而叶片气孔导度、蒸腾速率和水分利用率对不同土壤含水量反应较复杂,只在土壤含水量较低时,幼树气孔导度、蒸腾速率明显降低,叶片水分利用率升高,表现出蒙古栎树种是干旱可变植物,长期水分胁迫可提高树种的耐旱能力．     

基于树干液流和土壤-叶片水势梯度分析荷木干湿季整树水分利用特征

运用Granier热消散探针连续监测荷木的树干液流,于2009年的湿季(8月)和干季(11月)选择天气晴朗的3d测定叶片水势,同步连续监测林冠上方光合有效辐射、土壤含水量、气温和空气相对湿度.结果表明:干湿季下荷木树干液流存在显著差异,此外,土壤水势和液流有较好的相关性,且干季时的相关性更好;荷木的叶面积/边材面积比值平均为(0.416±0.033)m2·cm-2,并与树高呈指数函数下降关系;随着11月土壤水势下降,荷木的整树水力导度和午间叶片水势也有所下降,但不明显;对叶片水势和整树蒸腾进行回归分析,二者之间呈二次多项式关系(P＜0.01),叶片水势并非无限制下降;结果还表明,大气水汽压亏缺(D)和叶片水势呈负相关,这是否空气温度和相对湿度或共同作用影响叶片水势,需要进一步研究.     

整树水力导度协同冠层气孔导度调节森林蒸腾

冠层气孔导度决定森林的蒸腾效率,它对驱动水汽移动的水汽应力的响应受树木水力结构的影响,并随水汽压亏缺上升和水力导度下降而降低,维持水势在最低阈值之上,避免出现水力灾变,调控冠层蒸腾。由于叶形和树冠结构的特点,部分脱耦联反映了湿润地区阔叶林冠层与大气的水汽交换特征,单纯以气孔导度的变化难以完整描述水分通量的调节规律,因而,需要考虑冠层气孔导度与水力导度协同控制冠层蒸腾的潜在机理。通过整合叶片气孔气体交换、树干液流、冠层微气象和其他环境因子的野外观测值,估测不同时间尺度的森林冠层气孔导度与大气的脱耦联系数和变异范围,以基于树干液流的冠层蒸腾,结合叶片/土壤水势梯度计算的水力导度,分析水力导度影响冠层气孔导度响应水汽压亏缺的敏感性,可以揭示和阐明水力导度和冠层气孔导度联合调节森林蒸腾的机理,对准确估测全球变化背景下森林对水资源利用的潜在生态效应有明显的理论意义。     

根源ABA参与气孔调节的数学模拟

建立了包括植物体内的水分传输,并有根源ABA参与的气孔调节模型,模拟了饱和水气压差(VPD)、气温、表层土壤含水量(θ_(s1))等环境因子对叶片水势、木质部汁液中ABA浓度([ABA]_x)及气孔导度的影响。结果显示,VPD和气温的变化能够改变叶片水势及气孔导度;[ABA]_x几乎不受VPD和气温变化的影响,却决定着叶片水势及气孔导度对VPD和气温变化的响应幅度;θ_(s1)影响[ABA]_x,并由此影响气孔导度,但相比之下对叶片水势的作用并不显著。     

冬小麦叶片气孔导度模型水分响应函数的参数化

植物气孔导度模型的水分响应函数用来模拟水分胁迫对气孔导度的影响过程, 是模拟缺水环境下植物与大气间水、碳交换过程的关键算法。水分响应函数包括空气湿度响应函数和土壤湿度(或植物水势)响应函数, 该研究基于田间实验观测, 分析了冬小麦(Triticum aestivum)叶片气孔导度对不同空气饱和差和不同土壤体积含水量或叶水势的响应规律。一个土壤水分梯度的田间处理在中国科学院禹城综合试验站实施, 不同水分胁迫下的冬小麦叶片气体交换过程和气孔导度以及其他的温湿度数据被观测, 同时观测了土壤含水量和叶水势。实验数据表明, 冬小麦叶片气孔导度对空气饱和差的响应呈现双曲线规律, 变化趋势显示大约1 kPa空气饱和差是一个有用的阈值, 在小于1 kPa时, 冬小麦气孔导度对空气饱和差变化反应敏感, 而大于1 kPa后则反应缓慢; 分析土壤体积含水量与中午叶片气孔导度的关系发现, 中午叶片气孔导度随土壤含水量增加大致呈现线性增加趋势, 但在平均土壤体积含水量大于大约25%以后, 气孔导度不再明显增加, 而是维持在较高导度值上下波动; 冬小麦中午叶片水势与相应的气孔导度之间, 随着叶水势的增加, 气孔导度呈现增加趋势。根据冬小麦气孔导度对空气湿度、土壤湿度和叶水势的响应规律, 研究分别采用双曲线和幂指数形式拟合了水汽响应函数, 用三段线性方程拟合了土壤湿度响应函数和植物水势响应函数, 得到的参数可以为模型模拟冬小麦的各类水、热、碳交换过程采用。     

荷木整树蒸腾对干湿季土壤水分的水力响应

降雨在时间上的非均匀分配导致森林土壤含水量呈现明显的干、湿季变化,并可能在干季形成水分胁迫,引起植物蒸腾变化。在监测环境因子的同时,利用Granier热消散探针连续监测荷木(Schima superba)的树干液流,以液流密度值计算整树蒸腾,并结合水力导度与叶片/土壤的水势差,探讨环境因子和水力导度对荷木整树蒸腾的协同控制。结果表明,华南地区的季节性降雨形成的干、湿季并未引起荷木蒸腾在季节上的显著差异,但对产生蒸腾的水力生理产生了显著影响。荷木蒸腾在干、湿季均与主要驱动环境因子(光合有效辐射PAR和水汽压亏缺VPD)呈显著正相关。在水热充足的湿季,荷木蒸腾主要受气孔导度调节;在干季,当空气水汽压亏缺达2.132 MPa时,水力导度与气孔导度协同控制蒸腾。整树水力导度对整树蒸腾的水力补偿出现在15:00—17:00,平均补偿值为0.08 g/s。利用蒸腾的估测值与实测值之间的差值量化荷木的水力补偿效应,是对水力导度与气孔导度协同控制树木蒸腾机理的深入探索。研究结果对于掌握季节性降雨不均背景下华南地区主要造林树种需水和耗水规律,有效发挥森林保水功能具有重要意义。     

土壤水分、光照和空气湿度对木薯气孔导度的影响

为探讨土壤水分、光照等环境因子对华南8号木薯气孔导度的影响,构建气孔导度与相关环境因子的数学模型,设置7个土壤水分梯度(相对含水量20%～80%),盆栽华南8号木薯,测量净光合速率、气孔导度和空气相对湿度等参数.结果表明:空气相对湿度与气孔导度之间呈极显著正相关;光合有效辐射、土壤相对含水量与气孔导度之间呈显著正相关,但它们对气孔导度的影响程度随土壤相对含水量的变化而变化,当土壤相对含水量较低时,土壤相对含水量是影响气孔导度的主导因子,而当土壤相对含水量较高时,光合有效辐射是影响气孔导度的主导因子;土壤相对含水量、光合有效辐射、空气相对湿度与气孔导度的关系可用指数模型表达;华南8号木薯的适宜土壤相对含水量的低限临界值为52%.     

辽东山区天然更新红松幼苗种群结构与动态

本研究以辽东山区红松人工林为种源的3种不同林带(落叶松林带、针叶混交林带和阔叶混交林带)内天然更新红松幼苗为对象,运用静态生命表和生存分析方法研究天然更新红松幼苗的种群结构与动态特征.结果 表明:3种不同林带内天然更新红松幼苗的年龄结构呈"(n)"型左偏态分布,前期幼苗数量较多且死亡率较高,后期不断减少,属于衰退型种群...     

Drought-induced changes in xylem pH, ionic composition, and ABA concentration act as early signals in field-grown maize (Zea mays L.).

Early signals potentially regulating leaf growth and stomatal aperture in field-grown maize (Zea mays L.) subjected to drought were investigated. Plants grown in a field lysimeter on two soil types were subjected to progressive drought during vegetative growth. Leaf ABA content, water status, extension rate, conductance, photosynthesis, nitrogen content, and xylem sap composition were measured daily. Maize responded similarly to progressive drought on both soil types. Effects on loam were less pronounced than on sand. Relative to fully-watered controls, xylem pH increased by about 0.2 units one day after withholding irrigation (DAWI) and conductivity decreased by about 0.25 mS cm(-1) 1-3 DAWI. Xylem nitrate, ammonium, and phosphate concentrations decreased by about 50% at 1-5 DAWI and potassium concentration decreased by about 50% at 7-8 DAWI. Xylem ABA concentration consistently increased by 45-70 pmol ml(-1) at 7 DAWI. Leaf extension rate decreased 5 DAWI, after the changes in xylem chemical composition had occurred. Leaf nitrogen significantly decreased 8-16 DAWI in droughted plants. Midday leaf water potential and photosynthesis were significantly decreased in droughted plants late in the drying period. Xylem nitrate concentration was the only ionic xylem sap component significantly correlated to increasing soil moisture deficit and decreasing leaf nitrogen concentration. Predawn leaf ABA content in droughted plants increased by 100-200 ng g(-1) dry weight at 7 DAWI coinciding with a decrease in stomatal conductance before any significant decrease in midday leaf water potential was observed. Based on the observed sequence, a chain of signal events is suggested eventually leading to stomatal closure and leaf surface reduction through interactive effects of reduced nitrogen supply and plant growth regulators under drought.     

The relations of stomatal closure and reopening to xylem ABA concentration and leaf water potential during soil drying and rewatering

Two tropical tree species, Acacia confusa and Leucaena leucocephala, were used to study the relationships among stomatal conductance, xylem ABA concentration and leaf water potential during a soil drying and rewatering cycle. Stomatal conductance of both A. confusa and L. leucocephala steadily decreased with the decreases in soil water content and pre-dawn leaf water potential. Upon rewatering, soil water content and pre-dawn leaf water potential rapidly returned to the control levels, whereas the reopening of stomata showed an obvious lag time. The length of this lag time was highly dependent not only upon the degree of water stress but also on plant species. The more severe the water stress, the longer the lag time. When A. confusa and L. leucocephala plants were exposed to the same degree of water stress (around –2.0 MPa in pre-dawn leaf water potential), the stomata of A. confusa reopened to the control level 6 days after rewatering. However, it took L. leucocephala about 14 days to reopen fully. A very similar response of leaf photosynthesis to soil water deficit was also observed for both species. Soil drying resulted in a significant increase in leaf and xylem ABA concentrations in both species. The more severe the water stress, the higher the leaf and xylem ABA concentrations. Both leaf ABA and xylem ABA returned to the control level following relief from water deficit and preceded the full recovery of stomata, suggesting that the lag phase of stomatal reopening was not controlled by leaf and/or xylem ABA. In contrast to drying the whole root system, drying half of the root system did not change the leaf water relations, but caused a significant increase in xylem ABA concentration, which could fully explain the decrease of stomatal conductance. After rewatering, the stomatal conductance of plants in which half of the roots were dried recovered more rapidly than those of whole-root dried plants, indicating that the leaf water deficit that occurred during the drying period was related to the post-stress stomatal inhibition. These results indicated that the decrease in stomatal conductance caused by water deficit was closely related to the increase in xylem ABA, but xylem ABA could not fully explain the reopening of stomata after relief of water stress, neither did the leaf ABA. Some unknown physiological and/or morphological processes in the guard cells may be related to the recovery process.     

Can stomatal closure caused by xylem ABA explain the inhibition of leaf photosynthesis under soil drying?

Effects of leaf water deficit and increase in endogenous ABA on photosynthesis of two tropical trees, t Acacia confusa and t Leucaena leucocephala, were investigated with two soil-drying methods, i.e. half or whole root system was subjected to soil drying. Half-root drying was achieved by allowing upper layer of soil column to dry and lower layer of soil column to remain watered. Half-root drying had little effect on leaf water potential, but when compared to the well-watered control, both methods of soil drying substantially increased the ABA concentration in xylem and reduced leaf conductance in both species. There was a significant relationship between leaf conductance and xylem ABA concentrations in both species, which was comparable to the same relationship that was generated by feeding ABA to excised twigs. The rate of photosynthesis was inhibited substantially in both soil-drying treatments and in both species, but photochchemical efficiency, measured as a ratio of variable fluorescence to a peak fluorescence emission of a dark-adapted leaf (F_v/F_m), was not reduced except in the whole root-dried t L. leucocephala plants where leaf water potential was reduced to –2.5 MPa. In all the cases where photosynthesis was inhibited, there was a concomitant reduction in both leaf conductance and calculated internal CO₂ concentration. After two days of rewatering, leaf water potential and xylem ABA concentration rapidly returned to pre-treatment levels, but leaf conductance and photosynthesis of both whole-root and half root dried t L. leucocephala remained inhibited substantially. Rewatering led to a full recovery of both stomatal conductance and photosynthesis in soil-dried t A. confusa, although its photosynthesis of whole-root dried plants did not recover fully but such difference was not significant statistically. These results suggest that drought-induced decline of photosynthesis was mainly a result of the stomatal factor caused by the increase of ABA concentration in the xylem sap. Non-stomatal factors, e.g. reduced photochemical activity and/or carbon metabolic activity, were species-specific and were brought about only at very low water potential.     

土壤温度和水分对长白山不同森林类型土壤呼吸的影响

在实验室条件下,将不同含水量的3种森林类型的土柱分别置于0、5、15、25和35℃条件下,进行土壤呼吸测定．结果表明,在0～35℃范围内。土壤呼吸速率与温度呈正相关．在一定含水量范围内(0．21～0．37kg·kg^-1),土壤呼吸随含水量的增加而升高,当含水量超出该范围,土壤呼吸速率则随含水量的变化而降低．土壤温度和水分对土壤呼吸作用存在明显的交互作用．不同森林类型土壤呼吸作用强弱存在显著差异,大小顺序为阔叶红松林>岳桦林>云冷杉暗针叶林．阔叶红松林土壤呼吸作用的最佳条件是土壤温度35℃、含水量0．37kg·kg^-1;云冷杉暗针叶林下的山地棕色针叶林土壤呼吸作用的最佳条件是25℃、0．21kg·kg^-1;岳桦林土壤呼吸作用的最佳条件是35℃、含水量0．37kg·kg^-1。但是．由于长白山阔叶红松林、云冷杉林和岳桦林处在不同的海拔带上,同期不同森林类型土壤温度各不相同,相差4～5℃,所以野外所测的同期山地棕色针叶林土呼吸速率应低于暗棕色森林土呼吸速率,山地生草森林土呼吸速率应高于山地棕色针叶林土的呼吸速率．     

Fog interception by Sequoia sempervirens (D. Don) crowns decouples physiology from soil water deficit

Although crown wetting events can increase plant water status, leaf wetting is thought to negatively affect plant carbon balance by depressing photosynthesis and growth. We investigated the influence of crown fog interception on the water and carbon relations of juvenile and mature Sequoia sempervirens trees. Field observations of mature trees indicated that fog interception increased leaf water potential above that of leaves sheltered from fog. Furthermore, observed increases in leaf water potential exceeded the maximum water potential predicted if soil water was the only available water source. Because field observations were limited to two mature trees, we conducted a greenhouse experiment to investigate how fog interception influences plant water status and photosynthesis. Pre-dawn and midday branchlet water potential, leaf gas exchange and chlorophyll fluorescence were measured on S. sempervirens saplings exposed to increasing soil water deficit, with and without overnight canopy fog interception. Sapling fog interception increased leaf water potential and photosynthesis above the control and soil water deficit treatments despite similar dark-acclimated leaf chlorophyll fluorescence. The field observations and greenhouse experiment show that fog interception represents an overlooked flux into the soil–plant–atmosphere continuum that temporarily, but significantly, decouples leaf-level water and carbon relations from soil water availability.     

Photosynthesis as related to xylem water potential and carbon dioxide concentration in Sitka spruce

Current-year shoots of Sitka spruce ( Picea sitchensis (Bong.) Carr.) were removed from the forest canopy. After steady-state rates of net photosynthesis were obtained in a leaf chamber, the shoots were excised in air and removed at different times to establish a relationship between net photosynthesis and xylem water potential. The experiment was repeated at five ambient carbon dioxide concentrations.
Net photosynthesis remained constant over a wide range of xylem water potential and increased linearly with ambient carbon dioxide concentration between 20 and 300 cm³ m⁻³. At low water potential net photosynthesis declined at each ambient carbon dioxide concentration and there was little difference in the potential (±0.05 MPa) at which zero photosynthesis was observed.
There was a small increase in the CO₂ compensation concentration at low xylem water potentials, but calculated mesophyll conductance still declined at low water potential after correction for this change in compensation concentration. Mesophyll conductance reached zero within the same range of water potential as net photosynthesis. The results suggested that the non-stomatal contribution to the decline of photosynthesis was approximately 30% until almost complete stomatal closure occurred.     

Water deficits and hydraulic limits to leaf water supply

Many aspects of plant water use -- particularly in response to soil drought -- may have as their basis the alteration of hydraulic conductance from soil to canopy. The regulation of plant water potential (Psi) by stomatal control and leaf area adjustment may be necessary to maximize water uptake on the one hand, while avoiding loss of hydraulic contact with the soil water on the other. Modelling the changes in hydraulic conductance with pressure gradients in the continuum allows the prediction of water use as a function of soil environment and plant architectural and xylem traits. Large differences in water use between species can be attributed in part to differences in their 'hydraulic equipment' that is presumably optimized for drawing water from a particular temporal and spatial niche in the soil environment. A number of studies have identified hydraulic limits as the cause of partial or complete foliar dieback in response to drought. The interactions between root:shoot ratio, rooting depth, xylem properties, and soil properties in influencing the limits to canopy water supply can be used to predict which combinations should optimize water use in a given circumstance. The hydraulic approach can improve our understanding of the coupling of canopy processes to soil environment, and the adaptive significance of stomatal behaviour.