首页> 外文期刊>Russian Journal of Biological Invasions >Threshold Concentrations of Cations in the External EnvironmentRequired for Maintenance of the Ionic Balance between the Organism of the Invader Elodea canadensis Michaux and Fresh Water
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Threshold Concentrations of Cations in the External EnvironmentRequired for Maintenance of the Ionic Balance between the Organism of the Invader Elodea canadensis Michaux and Fresh Water

机译:维持入侵者加拿大伊乐藻生物和淡水之间离子平衡所需的外部环境中的阳离子阈值浓度

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摘要

The content of sodium, potassium, calcium, and magnesium in the invader pondweed Elodea canadensis in field conditions is 14.5 ± 0.7, 56.2 ±0.9,241.5 ± 15.2, and 26.4 ± 0.2 mmol/kgwet mass, respectively; the content of various fractions of water is as follows: general 80.3 ± 0.7%, free 77.5 ± 0.8%, connected 2.73 ± 0.14%. The threshold concentrations of sodium, potassium, calcium, and magnesium in the water necessary to maintain the ionic balance between the plant organism and the medium are 0.0014—0.0021, 0.00013-0.00024, 0.12-0.16, and 0.0056-0.0075 mmol/L, respectively. Reduction of water mineralization is accompanied by a significant drop in the levels of sodium, calcium, and magnesium in plants, as well as by augmentation of concentration gradients of cations between the organism and the medium, thereby enhancing the load on systems for maintenance of the water—salt exchange. Along with that, the amount of dry substance in plants decreases, while that of water increases. Under such intense conditions, the power expenses to maintain the vital activity of the organism dominate the processes of accumulation of organic substances. On the basis of data on threshold cation concentrations in the medium, a comparative analysis for the ability of various species of aquatic organisms to master low-mineralized freshwater reservoirs is presented.
机译:在田间条件下,侵染的加拿大蓝藻Elodea canadensis中钠,钾,钙和镁的含量分别为14.5±0.7、56.2±0.9、241.5±15.2和26.4±0.2 mmol / kg湿重。水各部分的含量如下:一般为80.3±0.7%,游离的为77.5±0.8%,相连的为2.73±0.14%。维持植物有机体和培养基之间离子平衡所必需的水中钠,钾,钙和镁的阈值浓度分别为0.0014-0.0021、0.00013-0.00024、0.12-0.16和0.0056-0.0075 mmol / L 。水矿化的减少伴随着植物中钠,钙和镁含量的显着下降,以及生物体与培养基之间阳离子浓度梯度的增加,从而增加了维持植物体内系统的负荷。水—盐交换。随之,植物中的干物质减少,而水则增加。在如此激烈的条件下,维持有机体生命活动所需的动力费用支配着有机物质的积累过程。根据有关培养基中阳离子浓度阈值的数据,对各种水生生物掌握低矿化淡水水库的能力进行了比较分析。

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