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互花米草中的渗透势与膨压维持

Osmotic potential and turgor maintenance in Spartina alterniflora Loisel.

作者信息

Drake B G, Gallagher J L

机构信息

Smithsonian Environmental Research Center, 12441 Parklawn Drive, 20852, Rockville, MD, USA.

College Marine Studies, University of Delaware, 19958, Lewes, DE, USA.

出版信息

Oecologia. 1984 Jun;62(3):368-375. doi: 10.1007/BF00384269.

Abstract

The dependence of leaf water potential (Ψ), osmotic potential (π) and turgor pressure (P) on relative water content (RWC) was determined for leaves of tall and short growth forms of Spartina alterniflora Loisel. from a site on Canary Creek marsh in Lewes, Delaware. Tall plants (ca. 1.5 m) occured along a drainage ditch where interstitial water salinity was approximately 20‰, and short plants (ca. 0.2 m) were 13 m away near a pan and exposed to 80‰ salinity during the most stressful period. Leaves were collected at dawn and pressure-volume measurements were made as they desiccated in the laboratory. Pressure equilibrium was used to measure Ψ, RWC was determined from weight loss and dry weight, π was determined from the pressure volume curve, and P was calculated as the difference between Ψ and π. Physical properties of the bulk leaf tissue that have a role in regulating water balance of the two growth forms were estimated: relative water content of apoplastic water (RWC) relative water content at zero turgor (RWC), the bulk modulus of elasticity (E), and water capacity (C ). There were no detectable temporal trends in any of the parameters measured from Nune through September and no significant differences between the two growth forms when compared on the basis of RWC, RWC, E, and C . There was a clear difference between the two growth forms with respect to π; at RWC, π was-4.5±0.40 MPa for short form plants and-3.3±0.40 MPa for tall form.Turgor pressure of plants in the field (P') was lower in leaves from short form than for the tall form plants with average difference of about 0.4 MPa. In July, P' in short form leaves dropped to zero by mid-morning as expected for leaves experiencing water stress.These results show that S. alterniflora is capable of reducing osmotic potential in response to increased salinity and that turgor pressure was lower in short growth form than in tall forms.

摘要

测定了特拉华州刘易斯市加那利溪沼泽地互花米草(Spartina alterniflora Loisel.)高生长型和矮生长型叶片的叶水势(Ψ)、渗透势(π)和膨压(P)对相对含水量(RWC)的依赖性。高植株(约1.5米)生长在一条排水沟沿岸,那里的间隙水盐度约为20‰,矮植株(约0.2米)生长在距离蒸发皿约13米处,在压力最大的时期暴露于80‰的盐度环境中。黎明时分采集叶片,并在实验室中使其干燥的过程中进行压力-容积测量。利用压力平衡来测量Ψ,通过失重和干重测定RWC,从压力-容积曲线确定π,并将P计算为Ψ与π的差值。估算了在调节两种生长型水分平衡中起作用的叶片组织整体的物理特性:质外体水相对含水量(RWC)、零膨压时相对含水量(RWC)、弹性模量(E)和水容量(C)。从6月到9月测量的任何参数均未检测到时间趋势,并且在基于RWC、RWC、E和C进行比较时,两种生长型之间没有显著差异。两种生长型在π方面存在明显差异;在RWC时,矮生长型植株的π为-4.5±0.40兆帕,高生长型植株的π为-3.3±0.40兆帕。田间植株的膨压(P')在矮生长型叶片中低于高生长型植株,平均差值约为0.4兆帕。7月,矮生长型叶片中的P'在上午中旬降至零,这正如经历水分胁迫的叶片所预期的那样。这些结果表明,互花米草能够响应盐度增加而降低渗透势,并且矮生长型的膨压低于高生长型。

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