Montes J G, Sjodin R A, Yergey A L, Vieira N E
Department of Biophysics, University of Maryland School of Medicine, Baltimore 21201.
Biophys J. 1989 Sep;56(3):437-46. doi: 10.1016/S0006-3495(89)82690-6.
Stable isotopes of Mg were used to measure bidirectional magnesium ion fluxes in single barnacle giant muscle fibers immersed in Ca- and Na-free, isosmotic media. Measurements were made using a mass spectrometric technique, thermal ionization mass spectrometry (TIMS), in conjunction with atomic absorption spectroscopy. Kinetic relations based on a first-order model were developed that permit the determination of unidirectional rate coefficients for Mg influx, ki, and efflux, ke, in the same experiment from knowledge of initial conditions and the initial and final ratios of 26Mg/24Mg and 25Mg/24Mg in ambient solutions (i.e., by isotope dilution). Such determinations were made for three values of the external Mg ion concentration: 5, 25, and 60 mM. At the concentration [Mg+2]o = 5 mM, ki and ke were about equal at a value of 0.01 min-1. At the higher values of [Mg+2]o, the values of ke increased along a curve suggesting saturation, whereas the values of ki remained essentially constant. As could be expected on the basis of a constant ki, the initial influx rate varied in direct linear proportion to [Mg+2]o, and was 11.8 pmol/cm2s when [Mg+2]o was 5 mM. However, the initial efflux rate appeared to increase nonlinearly with [Mg+2]o, varying from 13.4 pmol/cm2s ([ Mg+2]o = 5 mM) to approximately 80 pmol/cm2s ([ Mg+2]o = 60 mM). The results are consistent with a model that assumes Mg influx to be mainly an electrodiffusive inward leak with PMg = 0.07 cm/s and Mg efflux to be almost entirely by active transport processes. Where comparisons can be made, the rate coefficients determined from stable isotope measurements agree with those previously obtained using radioactive Mg. The rate coefficients can be used to correctly predict time-dependent changes in total fiber Mg content. The results support the conclusion that nonradioactive tracers can be used to measure ion fluxes and ion flux ratios in excitable cells; it is expected that this method will greatly assist in the study of Mg regulation in general.
镁的稳定同位素被用于测量浸没在无钙、无钠等渗介质中的单个藤壶巨型肌纤维中的双向镁离子通量。测量使用质谱技术——热电离质谱法(TIMS),并结合原子吸收光谱法进行。基于一级模型建立了动力学关系,通过了解初始条件以及环境溶液中26Mg/24Mg和25Mg/24Mg的初始和最终比率(即通过同位素稀释),可以在同一实验中确定镁流入速率系数ki和流出速率系数ke。针对外部镁离子浓度的三个值进行了此类测定:5、25和60 mM。在浓度[Mg+2]o = 5 mM时,ki和ke约相等,值为0.01 min-1。在较高的[Mg+2]o值时,ke值沿着一条表明饱和的曲线增加,而ki值基本保持恒定。基于恒定的ki,可以预期初始流入速率与[Mg+2]o成直接线性比例变化,当[Mg+2]o为5 mM时为11.8 pmol/cm2s。然而,初始流出速率似乎随[Mg+2]o非线性增加,从13.4 pmol/cm2s([Mg+2]o = 5 mM)变化到约80 pmol/cm2s([Mg+2]o = 60 mM)。结果与一个模型一致,该模型假设镁流入主要是具有PMg = 0.07 cm/s的电扩散内向泄漏,而镁流出几乎完全通过主动运输过程。在可以进行比较的地方,通过稳定同位素测量确定的速率系数与先前使用放射性镁获得的速率系数一致。速率系数可用于正确预测纤维总镁含量随时间的变化。结果支持这样的结论,即非放射性示踪剂可用于测量可兴奋细胞中的离子通量和离子通量比率;预计该方法将极大地有助于一般镁调节的研究。