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大豆种子的吸水模式与动力学

Patterns and kinetics of water uptake by soybean seeds.

作者信息

Meyer Chris J, Steudle Ernst, Peterson Carol A

机构信息

Department of Biology, University of Waterloo, Waterloo, ON, Canada N2L 3G1.

出版信息

J Exp Bot. 2007;58(3):717-32. doi: 10.1093/jxb/erl244. Epub 2006 Dec 21.

Abstract

Soybean [Glycine max (L.) Merr.] plants produce some seeds (called stone or impermeable seeds) that do not take up water for long periods of time. The present investigation confirmed that the stone seed trait is a feature of the seed coat: isolated embryos from both stone and permeable seeds took up water equally quickly. A whole, permeable seed typically imbibed water initially through its dorsal side, forming wrinkles in the seed coat and delivering water to the underlying cotyledons. Later, some lateral movement of water through the coat occurred, presumably through the air spaces of the osteosclereid layer. Imbibition by seeds was a two-phase process, the first dominated by hydration of the seed coat and the second by hydration of the cotyledons, which was rate-limited by the coat. When hydrated, coats of stone seeds were permeable to water but their hydraulic conductivity, as measured with a pressure probe, was smaller than that of coats from permeable seeds by a factor of five. Hydrated coats of both permeable and stone seeds showed weak osmometer properties.

摘要

大豆[Glycine max (L.) Merr.]植株会产生一些种子(称为石籽或不透水种子),这些种子长时间不吸水。本研究证实,石籽性状是种皮的一个特征:从石籽和透水种子中分离出的胚吸水速度相同。完整的透水种子通常最初通过其背面吸水,在种皮上形成皱纹,并将水输送到下面的子叶。后来,水通过种皮发生了一些横向移动,推测是通过骨状石细胞层的气隙。种子的吸水是一个两阶段过程,第一阶段以种皮水合为主,第二阶段以子叶水合为主,后者受种皮限制速率。水合后,石籽的种皮对水是可渗透的,但用压力探针测量时,其水力传导率比透水种子的种皮小五倍。透水种子和石籽的水合种皮均表现出较弱的渗透压计特性。

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