Shabala Sergey, Shabala Lana, Volkenburgh Elizabeth Van
School of Agricultural Science, University of Tasmania, Private Bag 54, Hobart, Tas. 7001, Australia. Corresponding author; email:
School of Agricultural Science, University of Tasmania, Private Bag 54, Hobart, Tas. 7001, Australia.
Funct Plant Biol. 2003 Jul;30(5):507-514. doi: 10.1071/FP03016.
The effects of various Na / Ca ratios on root growth, development, and ion acquisition patterns were studied in hydroponic experiments with barley (Hordeum vulgare L.) plants. In total, interactions between three different levels of salinity (1, 50 and 100 mM NaCl) and three different levels of Ca (0.1, 1 and 10 mM) were studied (a full factorial experiment). Growth rate and biomass accumulation were significantly lower in salinised roots. In addition to reduction in extension growth, salinity also significantly affected plant developmental processes (for example reduced root hair density and root thickening). Supplemental Ca significantly ameliorated those detrimental effects of salinity. Non-invasive, microelectrode ion-flux (MIFE) measurements showed that the onset of salt stress caused rapid and prolonged efflux of H, K and NH from the root epidermis. This efflux could be significantly reversed, or completely prevented, by the presence of high Ca concentration in the bath solution, even after several days of salt stress. Membrane potential measurements in root epidermal cells showed that high Ca levels in the bath were able to restore (otherwise depolarised) membrane potential back to control level (-120 to -130 mV). At the same time, no significant impact of Ca on net Na uptake in plant roots was found. Some limitations of the MIFE technique for study of Na uptake kinetics under saline conditions, as well as possible ionic mechanisms underlying the ameliorating Ca effects on ion fluxes in roots of salt-stressed plants, are discussed.
在以大麦(Hordeum vulgare L.)植株进行的水培实验中,研究了不同钠/钙比例对根系生长、发育及离子吸收模式的影响。总共研究了三种不同盐度水平(1、50和100 mM NaCl)与三种不同钙水平(0.1、1和10 mM)之间的相互作用(全因子实验)。盐化根系的生长速率和生物量积累显著降低。除了伸长生长减少外,盐度还显著影响植物发育过程(例如根毛密度降低和根加粗)。补充钙显著减轻了盐度的这些有害影响。非侵入性微电极离子通量(MIFE)测量表明,盐胁迫开始时会导致根表皮中的氢离子、钾离子和铵离子快速且持续外流。即使在盐胁迫数天后,通过在浴液中存在高钙浓度,这种外流也可显著逆转或完全阻止。根表皮细胞的膜电位测量表明,浴液中的高钙水平能够将(否则会去极化的)膜电位恢复到对照水平(-120至-130 mV)。同时,未发现钙对植物根系净钠吸收有显著影响。讨论了MIFE技术在研究盐胁迫条件下钠吸收动力学方面的一些局限性,以及钙对盐胁迫植物根系离子通量产生缓解作用的潜在离子机制。