Department of Agronomy & Range Science, University of California, Davis, California 95616.
Plant Physiol. 1986 Oct;82(2):494-8. doi: 10.1104/pp.82.2.494.
Initial observations showed a 100% increase in H(2)-uptake (Hup) activity of Rhizobium leguminosarum strain 3855 in pea root nodules (Pisum sativum L. cv Alaska) on plants growing in a baked clay substrate relative to those growing in vermiculite, and an investigation of nutrient factors responsible for the phenomenon was initiated. Significantly greater Hup activity was first measured in the clay-grown plants 24 days after germination, and higher activity was maintained relative to the vermiculite treatment until experiments were terminated at day 32. The increase in Hup activity was associated with a decrease in H(2) evolution for plants with comparable rates of acetylene reduction. Analyses of the clay showed that it contained more Na(+) (29 versus 9 milligrams per kilogram) and less K(+) (6 versus 74 milligrams per kilogram) than the vermiculite. Analyses of plants, however, showed a large increase in Na(+) concentration of clay-grown plants with a much smaller reduction in K(+) concentration. In tests with the same organisms in a hydroponic system with controlled pH, 40 millimolar NaCl increased Hup activity more than 100% over plants grown in solutions lacking NaCl. Plants with increased Hup activity, however, did not have greater net carbon or total nitrogen assimilation. KCl treatments from 5 to 80 millimolar produced slight increased in Hup activity at 10 millimolar KCl, and tests with other salts in the hydroponic system indicated that only Na(+) strongly promoted Hup activity. Treating vermiculite with 50 millimolar NaCl increased Na(+) concentration in pea plant tissue and greatly promoted Hup activity of root nodules in a manner analogous to the original observation with the clay rooting medium. A wider generality of the phenomenon was suggested by demonstrating that exogenous Na(+) increased Hup activity of other R. leguminosarum strains and promoted Hup activity of R. meliloti strain B300 in alfalfa (Medicago sativa L.).
初步观察表明,与在珍珠岩中生长的植物相比,在烤粘土基质中生长的豌豆(Pisum sativum L. cv Alaska)根瘤中的根瘤菌 3855 的 H(2)吸收(Hup)活性增加了 100%,并开始研究负责该现象的营养因素。在发芽后 24 天,首先在粘土中生长的植物中测量到更高的 Hup 活性,并且相对于珍珠岩处理,直到实验在第 32 天结束,活性仍保持较高水平。Hup 活性的增加与具有可比乙炔还原率的植物的 H(2)演化减少有关。对粘土的分析表明,与珍珠岩相比,它含有更多的 Na(+)(29 毫克/千克对 9 毫克/千克)和更少的 K(+)(6 毫克/千克对 74 毫克/千克)。然而,对植物的分析表明,与 K(+)浓度相比,粘土中生长的植物的 Na(+)浓度有很大增加。在同一生物体在 pH 可控的水培系统中的测试中,40 毫摩尔/升 NaCl 使 Hup 活性增加了 100%以上,而在缺乏 NaCl 的溶液中生长的植物。然而,具有增加的 Hup 活性的植物并没有具有更高的净碳或总氮同化。在 5 至 80 毫摩尔/升的 KCl 处理下,在 10 毫摩尔/升 KCl 下,Hup 活性略有增加,并且在水培系统中用其他盐进行的测试表明,只有 Na(+)强烈促进 Hup 活性。用 50 毫摩尔/升 NaCl 处理珍珠岩会增加豌豆植物组织中的 Na(+)浓度,并以类似于原始观察到的粘土生根培养基的方式极大地促进根瘤的 Hup 活性。通过证明外源性 Na(+)增加了其他 R. leguminosarum 菌株的 Hup 活性并促进了苜蓿(Medicago sativa L.)中 R. meliloti 菌株 B300 的 Hup 活性,表明该现象具有更广泛的普遍性。