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海生紫菀的耐盐性。III. 完整幼苗中的钠和钾通量。

Salt tolerance in Aster tripolium L. III. Na and K fluxes in intact seedlings.

作者信息

Shennan C

机构信息

Botany School, Downing Street, Cambridge, CB2 3EA, U.K.

出版信息

Plant Cell Environ. 1987 Jan;10(1):75-81. doi: 10.1111/j.1365-3040.1987.tb02082.x.

DOI:10.1111/j.1365-3040.1987.tb02082.x
PMID:28692154
Abstract

Uptake and transport of Na and K was studied using the radioactive tracers Na and K in intact Aster tripolium L. seedlings grown at two salinities CS 10 and CS 100, (containing 10mol m and 100 mol m Na, respectively, together with other major ions in the proportions found in sea water). At both salinities a much greater proportion of the Na than K taken up by the plant was subsequently transported to the shoot. Most K fluxes were reduced by about 40% in CS 100 plants relative to CS 10 except root accumulation which increased. Experiments involving changing the salinity from CS 10 to CS 100 showed that K fluxes remained constant for at least 40 h, indicating that competition with Na for uptake sites was not the cause of the reduced flux in CS 100 plants. Na fluxes responded immediately to a change in salinity with all fluxes increasing six-fold when the salinity was raised. When the salinity was lowered, however, root accumulation returned to the level in CS 10 control plants whereas transport to the shoot was inhibited by the previous high salinity treatment, being reduced to only 35% of the rate in CS 10 plants. The time courses of osmotic adjustment and Na accumulation following an increase in salinity were found to be very similar, with sufficient Na being accumulated to account for the observed increase in sap osmotic pressure.

摘要

利用放射性示踪剂钠和钾,对生长在两种盐度(CS 10和CS 100,分别含有10摩尔/立方米和100摩尔/立方米的钠,以及海水比例的其他主要离子)下的完整海生菊苣幼苗中钠和钾的吸收与运输进行了研究。在这两种盐度下,植物吸收的钠中随后运输到地上部的比例远高于钾。相对于CS 10的植物,CS 100的植物中大多数钾通量降低了约40%,但根系积累增加。涉及将盐度从CS 10改变为CS 100的实验表明,钾通量至少40小时保持恒定,这表明与钠竞争吸收位点不是CS 100植物中通量降低的原因。钠通量对盐度变化立即做出反应,当盐度升高时,所有通量增加六倍。然而,当盐度降低时,根系积累恢复到CS 10对照植物的水平,而运输到地上部则受到先前高盐度处理的抑制,降至CS 10植物中速率的仅35%。发现盐度增加后渗透调节和钠积累的时间进程非常相似,积累了足够的钠以解释观察到的汁液渗透压增加。

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