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一种用于利用压力探针研究植物细胞水分关系的修订统一的压力钳制/松弛理论:原位测定细胞体积以计算体积弹性模量和水力传导率。

A revised and unified pressure-clamp/relaxation theory for studying plant cell water relations with pressure probes: in-situ determination of cell volume for calculation of volumetric elastic modulus and hydraulic conductivity.

作者信息

Knipfer T, Fei J, Gambetta G A, Shackel K A, Matthews M A

机构信息

Department of Viticulture and Enology, University of California, Davis, USA.

Department of Viticulture and Enology, University of California, Davis, USA.

出版信息

J Theor Biol. 2014 Oct 21;359:80-91. doi: 10.1016/j.jtbi.2014.05.035. Epub 2014 Jun 5.

Abstract

The cell-pressure-probe is a unique tool to study plant water relations in-situ. Inaccuracy in the estimation of cell volume (νo) is the major source of error in the calculation of both cell volumetric elastic modulus (ε) and cell hydraulic conductivity (Lp). Estimates of νo and Lp can be obtained with the pressure-clamp (PC) and pressure-relaxation (PR) methods. In theory, both methods should result in comparable νo and Lp estimates, but this has not been the case. In this study, the existing νo-theories for PC and PR methods were reviewed and clarified. A revised νo-theory was developed that is equally valid for the PC and PR methods. The revised theory was used to determine νo for two extreme scenarios of solute mixing between the experimental cell and sap in the pressure probe microcapillary. Using a fully automated cell-pressure-probe (ACPP) on leaf epidermal cells of Tradescantia virginiana, the validity of the revised theory was tested with experimental data. Calculated νo values from both methods were in the range of optically determined νo (=1.1-5.0nL) for T. virginiana. However, the PC method produced a systematically lower (21%) calculated νo compared to the PR method. Effects of solute mixing could only explain a potential error in calculated νo of <3%. For both methods, this discrepancy in νo was almost identical to the discrepancy in the measured ratio of ΔV/ΔP (total change in microcapillary sap volume versus corresponding change in cell turgor) of 19%, which is a fundamental parameter in calculating νo. It followed from the revised theory that the ratio of ΔV/ΔP was inversely related to the solute reflection coefficient. This highlighted that treating the experimental cell as an ideal osmometer in both methods is potentially not correct. Effects of non-ideal osmotic behavior by transmembrane solute movement may be minimized in the PR as compared to the PC method.

摘要

细胞压力探针是一种用于原位研究植物水分关系的独特工具。细胞体积(νo)估计的不准确是计算细胞体积弹性模量(ε)和细胞水力传导率(Lp)时误差的主要来源。可以通过压力钳制(PC)和压力松弛(PR)方法获得νo和Lp的估计值。理论上,两种方法应得出可比的νo和Lp估计值,但实际情况并非如此。在本研究中,对PC和PR方法现有的νo理论进行了回顾和澄清。开发了一种对PC和PR方法同样有效的修正νo理论。该修正理论用于确定压力探针微毛细管中实验细胞与汁液之间溶质混合的两种极端情况下的νo。使用全自动化细胞压力探针(ACPP)对弗吉尼亚紫露草的叶表皮细胞进行研究,并用实验数据检验了修正理论的有效性。两种方法计算出的νo值都在弗吉尼亚紫露草光学测定的νo(=1.1 - 5.0nL)范围内。然而,与PR方法相比,PC方法计算出的νo系统地低了21%。溶质混合的影响只能解释计算出的νo中<3%的潜在误差。对于两种方法,νo的这种差异几乎与测量的ΔV/ΔP(微毛细管汁液体积的总变化与细胞膨压相应变化的比值)的19%差异相同,而ΔV/ΔP是计算νo的一个基本参数。从修正理论可以得出,ΔV/ΔP的比值与溶质反射系数成反比。这突出表明,在两种方法中将实验细胞视为理想渗透计可能是不正确的。与PC方法相比,跨膜溶质移动引起的非理想渗透行为的影响在PR方法中可能会最小化。

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