压力探针技术在植物水分关系研究中的运用

压力探针（pressure probe）技术最初设计时用于测定巨型藻类细胞的膨压,后来转到对高等植物细胞的膨压及其他水分关系参数的测定,现在已发展成为植物生理学和生态学研究中的一种多用途技术。它可以在细胞原位测定水分及溶质跨膜运输及分布情况。能够在不离体的植物中测定水通道的活性。新近发展的木质部压力探针是惟一可以直接测定导管或管胞中负压的技术。文章介绍该技术基本原理及其在植物水分生理学研究中的应用。     

植物木质部水力学研究进展

植物为适应陆地环境进化出木质部维管系统,通过水力学机制高效安全的向光合器官长距离运输水分,木质部水分运输对蒸腾、气孔运动、光合碳同化等生理过程有调控和协调作用,被称为植物生理学的支柱。植物水力学作为木质部水分运输的研究内容和手段,已成为整合植物与生态系统功能的中心枢纽。该文首先概述了植物水分运输的水力学机制、运输系统的局限性,以及木质部结构与功能之间的关系;其次,阐述了木质部栓塞的形成机制并详细介绍了栓塞的诱导方法和测试技术,分析了水分运输系统安全与效率之间的权衡关系,总结了植物对环境的响应和干旱致死的预测模型,讨论了测试技术问题及其引发的当前木质部逆压力修复和指数型木质部栓塞脆弱性曲线有效性的争议;最后,总结了目前植物木质部水力学研究的成果,提出了尚待解决的主要问题,探讨了研究机会与方向。     

林木耗水调控机理研究进展

林木的蒸腾耗水量是造林设计与环境水分研究的重要参数。本文就林木耗水的气孔与非气孔调节机制、木质部空穴和栓塞的发生和恢复机理、树体组织水容等方面进行了综述,对它们在树木水分传输过程中的调控作用和意义开展了探讨。目前在蒸腾气孔调节方面,包括,蒸腾午休、夜间蒸腾、气孔振荡和补偿现象等气孔行为的研究工作有待深入。栓塞木质部和空穴化导管恢复的临界条件与重新充注对植物水分运输的重要生理作用要进一步加强。树体组织水容对树木水分传输和耗水的调控机制问题应加以重视。     

2006年第17届国际生物学奥林匹克竞赛(4)

理论测试单元A 植物解剖学和植物生理学 下列哪组关键词说明木质部水分运输？ A．根毛，阳离子浓度，蒸腾作用 B．蒸腾作用，张力，吐水 C．蒸腾作用．水的内聚力．根压     

植物生理学研究中的压力探针技术

压力探针技术是一种用来测定微系统中压力大小和变化的新技术。其最初被设计用于直接测定巨型藻类的细胞膨压。随着操作装置的进一步微型化和精密化, 后来被应用于测定普通高等植物细胞膨压及其它水分关系参数。该技术的发展建立在一系列相应的流体物理学理论基础上。通过这些物理学公式的计算, 该技术能测定跨细胞膜或器官的水分运输速度以及它们的水力学导度; 测定溶液中水分和溶质的相对运输速度以及它们之间的相互影响; 还可以测定细胞壁的刚性等。目前压力探针技术已成为植物生理学和生态学领域研究中的多用途技术。它可以在细胞水平上原位测定水分及溶质跨膜运输及分布情况, 这对于阐明水通道功能具有极其重要的意义。此外, 木质部压力探针技术是目前唯一可以直接测定导管或管胞中负压的工具。该技术还可以用于单细胞汁液的样品采集, 结合微电极技术测定导管或其它细胞中的pH值、离子浓度以及细胞膜电位。本文重点介绍该技术使用的基本原理和相应的理论基础, 并详细地描述了操作过程中的技术和技巧。     

植物生理学研究中的压力探针技术

压力探针技术是一种用来测定微系统中压力大小和变化的新技术。其最初被设计用于直接测定巨型藻类的细胞膨压。随着操作装置的进一步微型化和精密化,后来被应用于测定普通高等植物细胞膨压及其它水分关系参数。该技术的发展建立在一系列相应的流体物理学理论基础上。通过这些物理学公式的计算,该技术能测定跨细胞膜或器官的水分运输速度以及它们的水力学导度;测定溶液中水分和溶质的相对运输速度以及它们之间的相互影响;还可以测定细胞壁的刚性等。目前压力探针技术已成为植物生理学和生态学领域研究中的多用途技术。它可以在细胞水平上原位测定水分及溶质跨膜运输及分布情况,这对于阐明水通道功能具有极其重要的意义。此外,木质部压力探针技术是目前唯一可以直接测定导管或管胞中负压的工具。该技术还可以用于单细胞汁液的样品采集,结合微电极技术测定导管或其它细胞中的pH值、离子浓度以及细胞膜电位。本文重点介绍该技术使用的基本原理和相应的理论基础,并详细地描述了操作过程中的技术和技巧。     

植物体内水分长距离运输的生理生态学机制

植物体内长距离水分运输是植物生理生态学研究中的一个重要问题,长期为植物生理学家和生理生态学家所关注。木质部探针技术的问世,掀起了近年来植物生理学界最为激烈的一场争论。提出了已经有100多年,风行40年的内聚力-张力(Cohesion-Tension, C-T)学说受到质疑。随后维护派和质疑派围绕木质部探针技术、压力室技术(C-T理论的主要支撑实验技术)的可靠性展开辩论。进一步从物理学原理和各种实验上就C-T理论的3个支柱(木质部导管或管胞中巨大的张力、沿树高的压力梯度、连续水柱)进行争论。这场争论似暂告一段落,C-T理论没有被推翻,但仍留有问题期待以后的研究。     

植物钙素吸收和运转

近年来,钙素在植物体内的吸收和运输研究主要集中在细胞和分子水平,但整株水平上的研究也同样重要.整株水平上的钙吸收和运输包括根细胞的钙吸收、钙离子横向穿过根系并进入木质部、在木质部运输、从木质部移出并进入叶片或果实及在叶片或果实中运转分配等环节,既经过质外体也穿越共质体.钙离子通道、Ca2 -ATP酶和Ca2 /H 反向转运器等参与根细胞的钙吸收.在钙离子横向穿根进入木质部的过程中,需要穿越内皮层和木质部薄壁细胞组织.根系内皮层凯氏带阻挡了Ca2 沿质外体途径由内皮层外侧向内侧的移动,部分Ca2 由此通过离子通道流进内皮层细胞而转入共质体并到达木质部薄壁细胞组织,而由木质部薄壁细胞组织进入中柱质外体可能需要Ca2 -ATP酶驱动;还有一些Ca2 由内皮层细胞运出,沿内皮层内侧的质外体途径进入木质部导管,并通过导管运向枝干.钙离子以螯合态的形式在枝干导管运输;水流速率是影响钙离子沿导管运输的关键因子.钙离子在果实和叶片中的运输和分配不仅通过质外体途径也通过共质体途径.     

维管植物木质部水分传输过程的影响因素及研究进展

维管植物的水分传输过程一直是植物学家关注的重点,木质部是植物体内长距离运输的组织之一,为维管植物提供了一个将水分从根运输到叶的低阻力通道。木质部在结构上形成了一个相互连通的网络管道结构,外部环境要素的改变(水分胁迫、氮沉降、光照等)引起的植物体内水势及木质部网络管道结构的变化直接影响植物的水分传输过程。本文从植物水分传输驱动力和内部木质部微观结构出发,总结了水分传输机理过程,概述了影响木质部水分传输的直接和间接因素,并在全球变化背景下,在植物内部观测技术、考虑多因子的综合作用等研究方面进行了展望。     

PV技术在研究细胞壁弹性调节上的应用

应用压力室测定PV曲线,然后用PV曲线推导、计算水分参数,称为PV技术。这一技术是植物水分生理研究中的重要手段之一,应用也相当广泛「’,”。它可以用于确定植物的相对含水量（RWC）、饱和渗透势（w”）、质外体水（I”。）、共质体水（1”。）、总体容积弹性模量（Ev）等”‘,并可用以阐明植物的渗透调节和植物对干旱的适应性卜”。近年来,植物水分生理研究领域内的学者们越来越意识到细胞壁弹性在维持细胞膨压中具有重要作用,在植物抗旱生理研究中也具有重要意义k－。‘。为此,根据有关资料和我们多年实验,总结出了弹性调节…     

Sap Ascent in Vascular Plants: Challengers to the Cohesion Theory Ignore the Significance of Immature Xylem and the Recycling of Munch Water

In recent years the cohesion theory has been attacked on thegrounds that direct measurements made with the pressure probeindicate that sap tensions are much less (maximum tension approx.0.7 MPa) than indicated by parallel measurements made with themore conventional methods: osmotic methods, pressure bomb, orpsychrometer. It has also been claimed that other direct methodsdo not support the cohesion theory. Thus a re-examination usingthe Renner technique indicated sap tensions of approx. 2.5 MPa.Also an independent method based on mercury penetrometry providesevidence that sap tensions of at least 2.0 MPa can be demonstrateddirectly implying, that serious limitations arise from the pressureprobe method itself. Without tensions exceeding 2.0 MPa mangroveswould be unable to extract fresh water for transpiration fromseawater. It is suggested that the pressure probe is susceptibleto bias because it investigates the least mature xylem conduitswhile they are still under varying degrees of turgor pressureand only partially interconnected with the main xylem system.This supposition is supported by claims that the xylem sap sampledby the probe contains significant concentrations of solutes.Additionally water, supplied by reverse osmosis from the sievetubes (‘Münch water’), is continually beingliberated in the vicinity of the outermost xylem vessels hydratingthem to an atypical degree which can explain several of thediscrepancies claimed. These results, which are supported bythe work of others, demonstrate that the challenges to the cohesiontheory for the ascent of sap are ill-founded. The release ofwater from the phloem can explain not only some discrepanciesclaimed by the cohesion challengers, but also explain the refillingof cavitated xylem conduits: a hitherto unsuspected role forthe phloem transport system. Cohesion theory; sap ascent; cavitation; pressure probe; xylem transport; vessel development; recycled water; reverse osmosis     

Water relations in silver birch during springtime: How is sap pressurised?

• Positive sap pressures are produced in the xylem of birch trees in boreal conditions during the time between the thawing of the soil and bud break. During this period, xylem embolisms accumulated during wintertime are refilled with water. The mechanism for xylem sap pressurization and its environmental drivers are not well known.
• We measured xylem sap flow, xylem sap pressure, xylem sap osmotic concentration, xylem and whole stem diameter changes, and stem and root non‐structural carbohydrate concentrations, along with meteorological conditions at two sites in Finland during and after the sap pressurisation period.
• The diurnal dynamics of xylem sap pressure and sap flow during the sap pressurisation period varied, but were more often opposite to the diurnal pattern after bud burst, i.e. sap pressure increased and sap flow rate mostly decreased when temperature increased. Net conversion of soluble sugars to starch in the stem and roots occurred during the sap pressurisation period. Xylem sap osmotic pressure was small in comparison to total sap pressure, and it did not follow changes in environmental conditions or tree water relations.
• Based on these findings, we suggest that xylem sap pressurisation and embolism refilling occur gradually over a few weeks through water transfer from parenchyma cells to xylem vessels during daytime, and then the parenchyma are refilled mostly during nighttime by water uptake from soil. Possible drivers for water transfer from parenchyma cells to vessels are discussed. Also the functioning of thermal dissipation probes in conditions of changing stem water content is discussed.

     

Applications of the compensating pressure theory of water transport

Some predictions of the recently proposed theory of long-distance water transport in plants (the Compensating Pressure Theory) have been verified experimentally in sunflower leaves. The xylem sap cavitates early in the day under quite small water stress, and the compensating pressure P (applied as the tissue pressure of turgid cells) pushes water into embolized vessels, refilling them during active transpiration. The water potential, as measured by the pressure chamber or psychrometer, is not a measure of the pressure in the xylem, but (as predicted by the theory) a measure of the compensating pressure P. As transpiration increases, P is increased to provide more rapid embolism repair. In many leaf petioles this increase in P is achieved by the hydrolysis of starch in the starch sheath to soluble sugars. At night P falls as starch is reformed. A hypothesis is proposed to explain these observations by pressure-driven reverse osmosis of water from the ground parenchyma of the petiole. Similar processes occur in roots and are manifested as root pressure. The theory requires a pump to transfer water from the soil into the root xylem. A mechanism is proposed by which this pump may function, in which the endodermis acts as a one-way valve and a pressure-confining barrier. Rays and xylem parenchyma of wood act like the xylem parenchyma of petioles and roots to repair embolisms in trees. The postulated root pump permits a re-appraisal of the work done by evaporation during transpiration, leading to the proposal that in tall trees there is no hydrostatic gradient to be overcome in lifting water. Some published observations are re-interpreted in terms of the theory: doubt is cast on the validity of measurements of hydraulic conductance of wood; vulnerability curves are found not to measure the cavitation threshold of water in the xylem, but the osmotic pressure of the xylem parenchyma; if measures of xylem pressure and of hydraulic conductance are both suspect, the accepted view of the hydraulic architecture of trees needs drastic revision; observations that xylem feeding insects feed faster as the water potential becomes more negative are in accord with the theory; tyloses, which have been shown to form in vessels especially vulnerable to cavitation, are seen as necessary for the maintenance of P, and to conserve the supplementary refilling water. Far from being a metastable system on the edge of disaster, the water transport system of the xylem is ultrastable: robust and self-sustaining in response to many kinds of stress.     

High Molecular Weight Organic Compounds in the Xylem Sap of Mangroves: Implications for Long-Distance Water Transport

The rise of sap in mangroves has puzzled plant physiologists for many decades. The current consensus is that negative pressures in the xylem exist which are sufficiently high to exceed the osmotic pressure of seawater (2.5 MPa). This implies that the radial reflection coefficients of the mangrove roots are equal to unity. However, direct pressure probe measurements in xylem vessels of the roots and stems of mangrove (Rhizophora mangle) grown in the laboratory or in the field yielded below-atmospheric, positive (absolute) pressure values. Slightly negative pressure values were recorded only occasionally. Xylem pressure did not change significantly when the plants were transferred from tap water to solutions containing up to 1700 mOsmol kg^?1 NaCl. This indicates that the radial reflection coefficient of the roots for salt, and therefore the effective osmotic pressure of the external solution, was essentially zero as already reported for other halophytes. The low values of xylem tension measured with the xylem pressure probe were consistent with previously published data obtained using the vacuum/leafy twig technique. Values of xylem tension determined with these two methods were nearly two orders of magnitude smaller than those estimated for mangrove using the pressure chamber technique (?3 to ?6MPa). Xylem pressure probe measurements and staining experiments with alcian blue and other dyes gave strong evidence that the xylem vessels contained viscous, mucilage- and/or protein-related compounds. Production of these compounds resulting from wound or other artifactual reactions was excluded. The very low sap flow rates of about 20–50 cm h^?1 measured in these mangrove plants were consistent with the presence of high molecular weight polymeric substances in the xylem sap. The presence of viscous substances in the xylem sap of mangroves has the following implications for traditional xylem pressure measurement techniques, development of xylem tension, and longdistance water transport: (1) high external balancing pressures in the pressure chamber are needed to force xylem sap to the cut surface of the twig; (2) stable tensions much larger than 0.1 MPa can be developed only occasionally because viscous solutions provide nucleation sites for gas bubble formation; (3) the frequent presence of small gas bubbles in viscous solutions allows water transport by interfacial, gravity-independent streaming at gas/water interfaces and (4) the increased density of viscous solutions creates (gravity-dependent) convectional flows. Density-driven convectional flows and interfacial streaming, but also the very low radial reflection coefficient of the roots to NaCl are apparently the means by which R. mangle maintains water transport to its leaves despite the high salinity of the environment.     

The Cohesion-Tension theory of sap ascent: current controversies

In recent years, the Cohesion-Tension (C-T) theory of sap ascentin plants has come under question because of work publishedby Professor Ulrich Zimmermann and colleagues at the Universityof Wrzburg, Germany. The purpose of this review is to (1) statethe essential and testable elements of the C-T theory, (2) summarizethe negative evidence for the C-T theory, and (3) review criticallythe positive evidence for the C-T theory and the evidence thatthe Scholander-Hammel pressure bomb measures xylem pressurepotential (P_x) correctly, because much of the evidence for theC-T theory depends on pressure bomb data. Much of the current evidence negates the conclusions drawn byZimmermann from studies using the xylem pressure probe (XPP),but it is not yet clear in every instance why the XPP resultsdisagree with those of other methods for estimating xylem pressure.There is no reason to reject the XPP as a useful new tool forstudying xylem tensions in the range of 0 to –0.6 MPa.Additional research is needed to test the C-T theory with boththe XPP and traditional methods. Key words: Cohesion-Tension theory, cavitation, embolism, xylem pressure probe, pressure bomb     

A New Theory for the Ascent of Sap--Cohesion Supported by Tissue Pressure

Recent work contradicting both the assumptions of the CohesionTheory, and the tensions measured in the xylem sap by the pressure-chamber,is reviewed. Measurements with the xylem-pressure probe revealpressures in vessels around 0 bar absolute, and no detectablegradients of pressure with tree height. Under high water stress,pressures down to -6 bar were found, but then cavitations occurredvery readily. Also, measurements of the cavitation thresholdsof water show an average threshold of about -2 bar. The uncertainfoundations of the Cohesion Theory are recalled from the yearsbefore 1965. Soon after that date, Scholander's measurementswith the pressure chamber were agreed to have confirmed thetheory and the existence of high tensions in the xylem. Before1965, many experiments over many years pointed to the conclusionsnow rediscovered, viz., no high tensions, and no gradients oftension. A resolution of these paradoxes is offered in the formof a new theory. This proposes that the driving force and thetransmission of the force are the same as in the Cohesion Theory,but the operating pressure of the xylem is raised into a stablerange by compensating tissue pressures pressing upon the trachearyelements. The tissue pressure does not propel the transpirationstream, which is still driven by evaporation, but protects thestream from cavitation. Evidence is presented for the existenceof positive pressures in roots, wood, and leaves. It is shownthat the anatomy of roots, wood, and monocotyledon and cryptogamvascular bundles is organized so that pressure is confined bymechanical barriers, and exerted upon the tracheary elementsby the living cells of the phloem and the xylem parenchyma.The Compensating-Pressure Theory also explains, among otherthings, root pressure, the function of the endodermis, the structureof wood, the constant association of xylem and phloem, the absenceof gas spaces in vascular tissue, the absence of a gravitationalgradient in the xylem, bleeding from cut palm inflorescences,how insects are able to withdraw sap from the xylem, and thevariable that is measured by the pressure chamber. This instrumentmeasures the water potential, but this is the potential notof xylem in tension, but of the compensating pressure appliedto the xylem. The requirements of the Theory are explained,and a number of predictions are made which are open to experimentaltesting.Copyright 1995, 1999 Academic Press Ascent of sap, cavitation, cohesion theory, endodermis, pressure chamber, root pressure, stem pressure, tissue pressure, transpiration, water potential, wood anatomy, xylem pressure     

Tyloses and the Maintenance of Transpiration

During a study of transpiration and embolism-formation in petiolesof sunflower, tyloses were frequently observed in early metaxylemvessels. Tyloses were confined to the inner ends of the xylemarcs, remote from the phloem. Vessels in this position are especiallyvulnerable to embolism. All stages of the invasion of vessellumens by xylem parenchyma cells were observed, from the earlyprotuberance of a cell through a pit to the complete occlusionof the lumen by one to several cells. The lumen space not occupiedby tyloses was seen both filled with xylem sap, or embolizedand gas-filled. Thus, during the early stages of tylosis formationthe vessel remained active in carrying the transpiration stream.Thin-walled vessels of the protoxylem or early metaxylem werenot tylosed, but were squashed and disappeared. These observationsare interpreted as evidence that vessels vulnerable to embolismare decommissioned and replaced by parenchyma tissue, whilenew and less vulnerable vessels are added to the xylem arcsat the cambial side. It is proposed that tylosis formation istriggered by the frequent embolization of the vulnerable vesselsto give, ultimately, an incompressible tissue. Then tyloseswould be necessary to preserve the tissue pressure which expresseswater to refill embolisms in the remaining vessels, and maintaintranspiration, as explained by the compensating pressure theoryof water transport. Compensating pressure theory; embolisms; starch sheath; tissue pressure; transpiration; tyloses; vessel diameter     

Sensing embolism in xylem vessels: the role of sucrose as a trigger for refilling

Refilling of embolized vessels requires a source of water and the release of energy stored in xylem parenchyma cells. Past evidence suggests that embolism presence can trigger a biological response that is switched off upon successful vessel refilling. As embolism formation is a purely physical process and most biological triggers rely on chemical sensors, we hypothesized that accumulation of osmotic compounds in walls of embolized vessels are involved in the embolism sensing mechanism. Analysis of Populus trichocarpa's response to infiltration of sucrose, monosaccharides, polyethylene glycol and potassium chloride into the xylem revealed that only presence of sucrose resulted in a simultaneous physiological and molecular response similar to that induced by embolism. This response included reduction of the starch pool in xylem parenchyma cells and significant correlation of gene expression from aquaporins, amylases and sugar transporter families. The work provides evidence of the ability of plants to sense embolism and suggests that sucrose concentration is the stimulus that allows plants to trigger a biological response to embolism.