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首页> 外文期刊>American-Eurasian Journal of Agricultural and Environmental Sciences >Evaluation Barley Germination in NaCl + CaCl2 Solution, Natural Saline Water and Saline Soil
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Evaluation Barley Germination in NaCl + CaCl2 Solution, Natural Saline Water and Saline Soil

机译:评价NaCl + CaCl2溶液,天然盐水和盐渍土壤中的大麦萌发

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Salinity stress negatively impacts agricultural yield throughout the world affecting production whether it is for subsistence or economic gain. Our objection in this study was to investigate the effect of salinity on barley germination. In this study barley (Hordeum vulgare) was carried out in three different experiments in complete randomize design through 13 treatments and 3 replicates. The salinity levels in all experiments were consisted of control (0.005 dS mG1), 5, 7, 9, 11, 13, 15, 17, 19, 21, 23, 25 and 27dS mG1. Germination in NaCl + CaCl solution, natural saline water and saline soil were studied. The results indicated 2 that the increased salinity, decreased number of both percentage and rate of germination. These were further reduction in natural saline water than the NaCl + CaCl solution. In higher salinities, the germination rate was 2 decreased, while the required time for germination was increased. The seeds could germinate in all salinity treatments in the NaCl + CaCl solution, but germination was successful until 13 dS m in soil and consequently 2 -1 germinated seed decrease rapidly to the degree that in treatment 23 dS mG1 no seed was germinate. Soil inhabits water absorption by the seeds more than solutions and this is due to the matrix potential of soil beside the osmotic potential.
机译:盐分胁迫对全世界的农业产量都产生了负面影响,无论是为了维持生计还是为经济利益而影响生产。我们在这项研究中的目的是调查盐度对大麦发芽的影响。在这项研究中,大麦(Hordeum vulgare)通过三个不同的实验在13个处理和3个重复的完全随机设计中进行。所有实验中的盐度水平由对照(0.005 dS mG1),5、7、9、11、13、15、17、19、21、23、25和27dS mG1组成。研究了NaCl + CaCl溶液,天然盐水和盐渍土壤中的萌发。结果表明2盐度提高,发芽率和发芽率均降低。与NaCl + CaCl溶液相比,这些盐在天然盐水中的含量进一步降低。在较高盐度下,发芽率降低了2,而发芽所需的时间却增加了。种子可以在NaCl + CaCl溶液中的所有盐分处理中发芽,但发芽成功直至土壤中13 dS m,因此2 -1发芽的种子迅速减少,至处理23 dS mG1时没有种子发芽。土壤对种子的吸收比对溶液的吸收要多,这是由于土壤的基质势除渗透势之外。

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