南亚热带丘陵赤红壤—龙眼—大气连续体水分运移力能变化及分布规律

根据田间试验观测资料,分析了南亚热带丘陵赤红壤—龙眼—大气连续体水分运移过程中能量和水流阻力变化及分布规律．结果表明水流在连续体中运移时,其能量主要消耗在由叶部到大气这一环节上,水流阻力主要分布于从叶气孔腔到大气的扩散过程,叶—气系统的水流阻力占连续体水流总阻力的９０．１３％～９８．７１％,叶—气系统的水流阻力是决定连续体中水流速率的主导因素．     

玉米生育期土壤-植物-大气连续体水流阻力与水势的分布

根据玉米生育期的田间试验资料分析了土壤-植物-大气连续体中水势和水流阻力的分布,结果表明土壤与植物叶片之间的水势差在玉米抽雄期前达0.8—1.0MPa,到抽雄期以后达1.0—1.5MPa,叶片与大气之间的水势差则在抽雄期前后分别达80—120MPa和60—80MPa;连续体内的水流阻力主要在叶片与大气之间.建立了连续体中玉米叶片水势的动态模拟公式,模拟叶水势具有较高的精度.最后,揭示了叶片蒸腾速率与叶-气系统水势差和水流阻力的关系,当叶片与大气之间的水势差达90—100MPa之后,蒸腾速率随叶-气间水势差增加而减小.     

坡地赤红壤—芒果—大气连续体水分运移力能关系的田间试验研究

依据田间实测资料,运用水流的电模拟原理,定量分析了坡地赤红壤—芒果—大气连续体水分运移过程中水分势能和水流阻力各分量的大小、变化规律及其相对重要性．结果表明,水流在该连续体中运移时,其能量主要消耗在由叶部到大气这一环节上,水分势能损失达１５．４４９１～５８．４０３６ＭＰａ,水分流经土壤到达叶部,水分热能降低０．２８１８～０．６９７９ＭＰａ;水流阻力主要分布于从叶气孔腔到大气的扩散过程,叶—气系统的水流阻力占该连续体水流总阻力的９５．６８％～９９．０３％,植株体的水流阻力占该连续体水流总阻力的０．９７％～４．３２％,而土壤阻力相对可忽略不计．     

玉米生育期土壤—植物—大气连续体水流阻力与水势的分布

根据玉米生育期的田间试验资料分析了土壤-植物-大气连续体中水势和水流阻力的分布,结果表明土壤与植物叶片之间的水势差在玉米抽雄期前达0.8—1.0MPa,到抽雄期以后达1.0—1.5MPa,叶片与大气之间的水势差则在抽雄期前后分别达80—120MPa和60—80MPa;连续体内的水流阻力主要在叶片与大气之间。建立了连续体中玉米叶片水势的动态模拟公式,模拟叶水势具有较高的精度。最后,揭示了叶片蒸腾速率与叶-气系统水势差和水流阻力的关系,当叶片与大气之间的水势差达90—100MPa之后,蒸腾速率随叶-气间水势差增加而减小。     

陕西渭北旱源土壤—植物—大气连续作中水分运转规律的研究──Ⅲ．生态和生理环境对叶片气孔阻力的影响

在整个生长季内,研究了陕西渭北旱源冬小麦叶气孔阻力与生态和生理因子的关系。结果表明,气孔阻力与大气温度、相对湿度和大气水势及叶温均呈二次曲线相关;与土壤水势呈直线正相关;与叶水势呈指数函数相关;当光量子通量密度小于１５２３μｍｏｌ·ｍ－２·ｓ－１时．气孔阻力与之呈幂函数相关,当光量子通量密度大于１５２３μｍｏｌ·ｍ－２·ｓ－１时,气孔阻力与之呈指数函数相关,此时气孔正处于“午休”期间。试验给出了冬小麦叶气孔阻力与各因素之间的现象模型。通过主要生态因子（气温、光量子通量密度、大气水势和相对湿度）对气孔阻力作用的综合分析表明,在陕西渭北旱塬,诸生态因子对冬小麦叶气孔阻力的重要性依次为大气水势、相对湿度、光量子通量密度和气温。并对其它影响气孔阻力的因素进行了讨论。     

植物气孔阻力及其测定

狭义概念中的气孔是指位于两个保卫细胞之间的缝隙,广义的概念将构成气孔的保卫细胞及副卫细胞也归于气孔结构。二氧化碳、水汽等由大气经过该狭缝进入气孔腔过程中所遇到的机械阻力称为气孔阻力。主要受植物表皮结构、气孔数量及其分布、气孔开张度、小气候因素(尤其是风速、温度、大气相对湿度等)以及大气污染物等因素制约。     

土壤-植物-大气连续体水热动态模拟的研究

本文从能量平衡原理和质量守恒定律出发,描述了土壤-植物-大气连续体中的热量转换和水分输送,模拟了系统中水分和热量的动态变化过程,并用所建立的模拟模型计算了冬小麦群落的冠层温度、叶水势及系统的潜热与显热变化关系,结果表明该模型有一定的可靠性。     

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.     

土壤-植物-大气连续体水热、CO2通量估算模型研究进展

土壤-植物-大气连续体(SPAC)水热、CO2通量的准确估算对理解陆地和大气的物质和能量交换过程有着重要意义.重点阐述了基于过程的土壤-植物-大气连续体水热、CO2通量模型,综述了统计模型、综合模型及基于遥感的模型的发展过程.其中水热通量统计模型包括基于温度和湿度以及基于温度和辐射的方法;CO2通量统计模型包括基于气候因子或蒸散因子以及基于光能利用率的方法.水热通量过程模型包括大叶、双源、多源和多层的水热传输物理模型;CO2通量过程模型包括叶片尺度及由大叶、双叶和多层方法扩展到冠层尺度的生理生态模型以及光合-蒸腾耦合模型.综合模型包括生物物理模型、生物化学模型和生物地理模型.统计模型形式简单,资料易得,对大范围的水热通量模拟具有指导意义;过程模型准确的揭示了水热和CO2通量传输的物理和生理过程,是大尺度综合模型的基础.未来生态系统水热、CO2通量估算模型将集成各种技术手段进行多尺度网络观测和大尺度机理模拟.     

用热脉冲速度记录仪（HPVR）测定树干液流

树木蒸腾耗水是环境生态平衡(水分)的重要因素。由于树体高大,环境、时间、空间变异因素复杂,测定工作十分困难。在林木生态系统中,水分运动的途径是,树木根部吸收土壤水分,通过树干(木质部上升液流)输送到树冠部,从叶表面蒸腾散失到大气中,即所谓“土壤-植物-大气连续系统”。在此过程中,树干是水流通道的咽喉部位,树干液流量的大小制约着冠部蒸腾量的变化。因此,可以用测定树干部液流的方法确定树冠的蒸腾耗水     

The temperature dependence of shoot hydraulic resistance: implications for stomatal behaviour and hydraulic limitation

Recent soil pressurization experiments have shown that stomatal closure in response to high leaf–air humidity gradients can be explained by direct feedback from leaf water potential. The more complex temperature‐by‐humidity interactive effects on stomatal conductance have not yet been explained fully. Measurements of the change in shoot conductance with temperature were made on Phaseolus vulgaris (common bean) to test whether temperature‐induced changes in the liquid‐phase transport capacity could explain these temperature‐ by‐humidity effects. In addition, shoot hydraulic resistances were partitioned within the stem and leaves to determine whether or not leaves exhibit a greater resistance. Changes in hydraulic conductance were calculated based on an Ohm’s law analogy. Whole‐plant gas exchange was used to determine steady‐ state transpiration rates. A combination of in situ psychrometer measurements, Scholander pressure chamber measurements and psychrometric measurements of leaf punches was used to determine water potential differences within the shoot. Hydraulic conductance for each portion of the pathway was estimated as the total flow divided by the water potential difference. Temperature‐induced changes in stomatal conductance were correlated linearly with temperature‐induced changes in hydraulic conductance. The magnitude of the temperature‐induced changes in whole‐plant hydraulic conductance was sufficient to account for the interactive effects of temperature and humidity on stomatal conductance.     

油松人工林SPAC水势梯度时空变化规律及其对边材液流传输的影响

 利用热扩散式边材液流茎流探针（TDP）和微型自动气象站组成的测定系统于2001年4月在北京林业大学妙峰山教学实验林场（39°54′N,116°28′E）对低山油松（Pinus tabulaeformis）人工林土壤-植物-大气体（SPAC）界面水势梯度及油松木质部边材液流传输速率的时空变化规律及其相关因子进行了连续测定。土壤水势随深度下降逐渐升高,日周期波动幅度减小,灌水后上层土壤水势迅速提高,但随着水分扩散和林地持续蒸散,土壤湿度迅速下降并逐渐与对照趋同;叶片水势连日逐渐降低,灌水后水势较对照有一定程度提高;林冠不同层次叶片水势在日周期内不同时间差异显著,但同一层次之间差异不明显;油松人工林土壤、叶片、大气水势梯度比约为1∶5∶30,灌水后SPAC相临界面水势差增大,水势梯度提高至1∶15∶90。大气水分饱和亏缺与土壤水势和叶片水势、以及土壤水势与叶片水势之间均有极显著相关性。干旱春季灌溉对油松木质部边材液流时空波动产生很大影响,灌水后连日树干上位边材液流峰值出现时间推迟1 h,连日平均液流速率提高48.59%,连日平均最大液流速率提高25.12%。木质部边材液流速率日变化和连日变化与SPAC水势和气象因子如空气相对湿度、空气温度、太阳辐射强度密切相关。与对照相比,灌水后边材液流速率与SPAC各介质水势和界面水势差的相关性下降。     

In Situ Estimates of Variable Plant Resistance to Water Flux in Ilex opaca Ait

Xylem pressure potentials and stomatal diffusion resistances were measured in the field in Ilex opaca Ait. during days which differed in temperature and vapor pressure deficit. Water flux into leaves was calculated by combining the field data with laboratory determinations of the relation between tissue water deficit and water potential. Estimates of apparent plant resistance were then calculated from fluxes and differences between soil water potential and xylem tension. The resistance depended strongly on water flux, dropping by a factor of over 7 from low to high water flow rates. This extends the generality of variable plant resistances measured in controlled environment studies to I. opaca as it occurs naturally in the field. The relation of apparent plant resistance to water flux as estimated in this study can be useful in simulation models which calculate water uptake to leaves as a flux driven by a difference in soil and leaf water potentials across a resistance between the bulk soil and the leaf.     

Is stomatal conductance in a tomato crop controlled by soil or atmosphere?

Summary The effects of soil water deficits and air vapour pressure deficits on stomatal conductance of tomato leaves were analysed separately under field conditions in central Portugal. Three conditions were created: low soil and air humidity (A), high soil and air humidity (B) and low soil but high air humidity (C). The results show that the effect of air vapour pressure deficit on stomatal behaviour is more important than the effect of soil water deficit when the predawn leaf water potential is above –0.4 MPa.     

黑河地区绿洲生态条件下麦田生物气象若干特征

观测分析了ＨＥＩＦＥ地区绿洲中麦田的微气候特征,结果表明ＳＰＡＣ中水５势随高度呈显著梯度分布,在土壤－植物以及植物－大气界面,水势值存在两个大的跳跃;水势廓线存在明显的日变化;ＳＰＡＣ各部分水势变化的起伏顺序是大气〉植物〉土壤,说明水势变化受植物水分代谢进程直到气象因子的强烈影响和控制。冠层上方近地面风温湿的时间剖而显示出白天与夜晚相比,大气混合得较好。日出前则大气较为稳定。在典型晴天条件下,麦田     

Plant transpiration at high elevations: Theory,field measurements,and comparisons with desert plants

Summary The influence of elevational changes on plant transpiration was evaluated using leaf energy balance equations and well-known elevational changes in the physical parameters that influence water vapor diffusion. Simulated transpirational fluxes for large leaves with low and high stomatal resistances to water vapor diffusion were compared to small leaves with identical stomatal resistances at elevations ranging from sea level to 4 km. The specific influence of various air temperature lapse rates was also tested. Validation of the simulated results was accomplished by comparing actual field measurements taken at a low elevation (300 m) desert site with similar measurements for a high elevation (2,560 m) mountain research site. Close agreement was observed between predicted and measured values of transpiration for the environmental and leaf parameters tested.Substantial increases in solar irradiation and the diffusion coefficient for water vapor in air (D _wv) occurred with increasing elevation, while air and leaf temperatures, the water vapor concentration difference between the leaf and air, longwave irradiation, and the thermal conductivity coefficient for heat in air decreased with increasing elevation. These changes resulted in temperatures for sunlit leaves that were further above air temperature at higher elevations, especially for large leaves. For large leaves with low stomatal resistances, transpirational fluxes for low-elevation desert plants were close to those predicted for high-elevation plants even though the sunlit leaf temperatures of these mountain plants were over 10°C cooler. Simulating conditions with a low air temperature lapse rate (0.003° C m^-1 and 0.004° C m^-1) resulted in predicted transpirational fluxes that were greater than those calculated for the desert site. Transpiration for smaller leaves decreased with elevation for all lapse rates tested (0.003° C m^-1 to 0.010° C m^-1). However, transpirational fluxes at higher elevations were considerably greater than expected for all leaves, especially larger leaves, due to the strong influence of increased solar heating and a greater D _wv. These results are discussed in terms of similarities in leaf structure and plant habit observed among low-elevation desert plants and high-elevation alpine and subalpine plants.     

Effects of varying air and soil moisture on the water relations and growth of sugar beet

Sugar beet were grown for short periods with different amounts of moisture in the soil and air. Growing plants in wet soil (23 % moisture on dry weight) compared with dry soil (15% moisture) increased growth of the shoots and roots and plant dry weights by 15% in young plants and 10% in mature plants. Growing plants in wet air containing 10.9 g m^-3 of water (equivalent to a saturation deficit of 2.5 mb) compared with dry air containing 6.4 g m^-3 of water (saturation deficit = 8.5 mb) increased the dry weights of both young and mature plants by 8%, mostly by increasing the sizes of their storage roots. Wet air and wet soil increased the net assimilation rates of both young and mature plants. Wet soil, but not wet air, increased leaf areas of young plants by accelerating leaf expansion, and both increased the leaf area of mature plants by slowing senescence of the older leaves. Wet soil increased the water potential of the leaves of both young and mature plants and, by doing so, increased their stomatal conductances and rates of photosynthesis. Wet air also increased stomatal conductances and rates of photosynthesis of leaves of plants of both ages, but without changing their water potentials. Stomatal conductances and photosynthetic rates were greater for young leaves than mature on the same plant and at the same water potential. It is suggested that at certain stages in the crops growth photosynthetic efficiency could be increased by applying additional water as a mist to increase the moisture content of the air around the crop.     

Water relations of crok-oak (Quercus suber L.) under natural conditions

Daily and annual courses of leaf transpiration, stomatal conductance and shoot water potential of four Quercus suber individuals were compared in a semi-natural stand in southwest Portugal, from spring 1989 to early summer 1990.The trees investigated showed annual patterns typical of evergreen sclerophyllous species but varied in their range of stomatal operation. This appeared to be related to differences in hydraulic conductivity in the root-to-leaf pathway.Maximum stomatal conductance and transpiration rates occurred from March to June.Water stress was found to be moderate and winter cold stress due to low air and soil temperatures appeared to have an influence on plant water balance through their effects on flow resistances.Abbreviations g_sw stomatal conductance - g_max maximum stomatal conductance - PAR photosynthetically active radiation - RH relative humidity of the air - T leaf transpiration - Ta air temperature - TL leaf temperature - T_max maximum leaf transpiration - W air-to-leaf vapor pressure difference - shoot water potential - PD predawn shoot water potential - MIN minimum shoot water potential     

土壤干旱胁迫下非水力根信号调控夏玉米气体交换对大气环境的响应

对不同程度土壤干旱胁迫下夏玉米非水力根信号的产生以及气体交换过程对大气环境的响应进行了试验研究。充足底墒播种后采用3个土壤水分处理等级(0~200cm土壤相对湿度为>80%、60%~70%、40%~50%,代号为W T1、W T2和W T3)。生育期内遮去自然降水。试验结果表明,在拔节期轻度和中度土壤干旱胁迫的情况下,玉米根系合成大量ABA传输到地上部分,参与控制气孔开度和气体交换过程对大气环境变化的响应并调节水分消耗。在日变化过程中,当光强和水汽压亏缺较高时,由于蒸腾速率较高,非水力根信号物质向冠层的传输速率也较高,ABA在叶片中的累积影响了气孔开张对光强响应的敏感度,气孔开度受到抑制,并且随着ABA累积和浓度的增加,气孔抑制作用越强;在水汽压亏缺较低的情况下,非水力根信号物质向冠层的传输速率较低,ABA的代谢过程以及再分配过程能够保证这种信号物质保持在低水平,从而保证一定程度的气孔开度和光合、蒸腾速率。这种策略能够使夏玉米在轻、中等干旱条件下保证最大的光合作用,同时在可能的胁迫情况下降低蒸腾作用以提高水分利用效率。     

Leaf and root control of stomatal closure during drying in soybean

The stomatal conductance of an illuminated 2.5 cm² area of an intact soybean leaflet was the same whether the rest of the shoot was in light or darkness. This was true throughout soil drying cycles. Water potential of tissue immediately outside the illuminated area consistently decreased about 0.3 MPa upon illumination of the shoot. This erroneously suggested that stomatal conductance during soil drying did not respond to diurnal reductions in leaf water potential, but was controlled by root or soil water status. Tests showed that the water potential of tissue in the illuminated area did not change in the steady-state upon illumination of the rest of the shoot. Water potentials of shaded sections of leaves were not different from predawn water potentials, and were higher than leaf xylem pressure potentials as determined with a pressure chamber. These steep local gradients of leaf water potential suggest that there is minimal interchange of water among xylem elements leading from roots to different sections of leaves. The relationship between stomatal conductance and leaf water potential was the same whether leaf water potential was reduced by soil drying, application of polyethylene glycol (PEG) to the root system, lowering root temperature, or leaf excision. In the root cooling experiment, there was no soil drying, and with leaf excision, there was no root drying. The similarity of stomatal responses to leaf water potential in all cases strongly suggests control of conductance by a signal produced by local leaf water potential rather than root or soil water status in these experiments.