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水势低的大豆幼苗的渗透调节、溶质分布和生长。

Osmoregulation, solute distribution, and growth in soybean seedlings having low water potentials.

机构信息

Science and Education Administration, Agricultural Research, U.S. Department of Agriculture, 61801, Urbana, IL, USA.

出版信息

Planta. 1981 May;151(5):482-9. doi: 10.1007/BF00386543.

Abstract

Soybean (Glycine max (L.) Merr.) seedlings osmoregulate when the supply of water is limited around the roots. The osmoregulation involves solute accumulation (osmotic adjustment) by the elongating region of the hypocotyls. We investigated the relationship between growth, solute accumulation, and the partitioning of solutes during osmoregulation. Darkgrown seedlings were transplanted to vermiculite containing 1/8 (0.13 x) the water of the controls. Within 12-15 h, the osmotic potential of the elongating region had decreased to-12 bar, but it was-7 bar in the controls. This osmoregulation involved a true solute accumulation by the hypocotyls, since cell volume and turgor were virtually the same regardless of the water regime. The hypocotyls having low water potentials elongated slowly but, when deprived of their cotyledons, did not elongate or accumulate solute. This result indicated a cotyledonary origin for the solutes and a dependence of slow growth on osmotic adjustment. The translocation of nonrespired dry matter from the cotyledons to the seedling axis was unaffected by the availability of water, but partitioning was altered. In the first 12 h, dry matter accumulated in the elongating region of the 0.13 x hypocotyls, and osmotic adjustment occurred. The solutes involved were mostly free amino acids, glucose, fructose, and sucrose, and these accounted for most of the increased dry weight. After osmotic adjustment was complete, dry matter ceased to accumulate in the hypocotyls and bypassed them to accumulate in the roots, which grew faster than the control roots. The proliferation of the roots resulted in an increased root/shoot ratio, a common response of plants to dry conditions.Osmotic adjustment occurred in the elongating region of the hypocotyls because solute utilization for growth decreased while solute uptake continued. Adjustment was completed when solute uptake subsequently decreased, and uptake then balanced utilization. The control of osmotic adjustment was therefore the rate of solute utilization and, secondarily, the rate of solute uptake. Elongation was inhibited by unknown factors(s) despite the turgor and substrates associated with osmotic adjustment. The remaining slow elongation depended on osmotic adjustment and represented some optimum between the necessary inhibition for solute accumulation and the necessary growth for seedling establishment.

摘要

大豆(Glycine max(L.)Merr.)幼苗在根部供水受到限制时会进行渗透调节。这种渗透调节涉及到下胚轴伸长区的溶质积累(渗透调节)。我们研究了生长、溶质积累和渗透调节过程中溶质分配之间的关系。黑暗生长的幼苗被移植到含有对照物 1/8(0.13x)水分的珍珠岩中。在 12-15 小时内,伸长区的渗透势下降到-12 巴,但在对照物中为-7 巴。这种渗透调节涉及到下胚轴的真正溶质积累,因为细胞体积和膨压几乎不受水分状况的影响。水势较低的下胚轴伸长缓慢,但如果去除子叶,就不会伸长或积累溶质。这一结果表明,溶质来源于子叶,并且缓慢生长依赖于渗透调节。从子叶到幼苗轴的非呼吸干物质的转运不受水分供应的影响,但分配发生了改变。在最初的 12 小时内,0.13x 下胚轴伸长区积累了干物质,并发生了渗透调节。所涉及的溶质主要是游离氨基酸、葡萄糖、果糖和蔗糖,这些占增加干重的大部分。渗透调节完成后,干物质停止在下胚轴中积累,并绕过下胚轴积累在根中,根的生长速度快于对照根。根的增殖导致根/茎比增加,这是植物对干旱条件的常见反应。渗透调节发生在下胚轴的伸长区,因为生长所需的溶质利用减少,而溶质吸收继续。当溶质吸收随后减少时,调节就完成了,然后吸收就平衡了利用。因此,渗透调节的控制是溶质利用的速度,其次是溶质吸收的速度。尽管与渗透调节相关的膨压和底物存在,但伸长仍受到未知因素的抑制。剩下的缓慢伸长依赖于渗透调节,代表了溶质积累所必需的抑制和幼苗建立所必需的生长之间的某种最佳状态。

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