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盐胁迫下小麦的根系水力特性

Root hydraulics in salt-stressed wheat.

作者信息

Fricke Wieland, Bijanzadeh Ehsan, Emam Yahya, Knipfer Thorsten

机构信息

School of Biology and Environmental Science, Science Centre West, University College Dublin, Belfield, Dublin 4, Ireland.

Crop Production Department, College of Agriculture and Natural Resources of Darab, Shiraz University, Shiraz 71345, Iran.

出版信息

Funct Plant Biol. 2014 Apr;41(4):366-378. doi: 10.1071/FP13219.

Abstract

The aim of the present study was to test whether salinity, which can impact through its osmotic stress component on the ability of plants to take up water, affects root water transport properties (hydraulic conductivity) in bread wheat (Triticum aestivum L). Hydroponically grown plants were exposed to 100mM NaCl when they were 10-11 days old. Plants were analysed during the vegetative stage of development when they were 15-17 days old and the root system consisted entirely of seminal roots, and when they were 22-24 days old, by which time adventitious roots had developed. Root hydraulic conductivity (Lp) was determined through exudation experiments (osmotic Lp) on individual roots and the entire plant root system, and through experiments involving intact, transpiring plants (hydrostatic Lp). Salt stress caused a general reduction (40-80%) in Lp, irrespective of whether individual seminal and adventitious roots, entire root systems or intact, transpiring plants were analysed. Osmotic and hydrostatic Lp were in the same range. The data suggest that most radial root water uptake in wheat grown in the presence and absence of NaCl occurs along a pathway that involves the crossing of membranes. As wheat plants develop, a nonmembraneous (apoplast) pathway contributes increasingly to radial water uptake in control but not in NaCl-stressed plants.

摘要

本研究的目的是测试盐度是否会影响面包小麦(Triticum aestivum L)的根系水分运输特性(水力传导率),盐度可通过其渗透胁迫成分影响植物吸收水分的能力。水培种植的植株在10 - 11日龄时暴露于100mM NaCl中。在植株发育的营养阶段,即15 - 17日龄时(此时根系完全由种子根组成)以及22 - 24日龄时(此时不定根已发育)对植株进行分析。通过对单个根系和整个植株根系的渗出实验(渗透水力传导率)以及涉及完整蒸腾植株的实验(静水水力传导率)来测定根系水力传导率(Lp)。无论分析的是单个种子根和不定根、整个根系还是完整的蒸腾植株,盐胁迫都会导致Lp普遍降低(40 - 80%)。渗透水力传导率和静水水力传导率处于同一范围。数据表明,在有和没有NaCl的情况下生长的小麦中,大部分根系径向水分吸收发生在一条涉及跨膜的途径上。随着小麦植株的发育,一条非膜性(质外体)途径在对照植株中对径向水分吸收的贡献越来越大,但在NaCl胁迫的植株中并非如此。

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