地表水源中氨对河豚毒性的影响(Pallas, 1771)

Е. Аrystarkhova, L. Romantschuk, Y. Dankevych, O. Zhytova
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引用次数: 0

摘要

的目标。揭示来自地表水供应源的氨对其毒性形成的影响,由幼年湖蛙的运动活动指标确定(Rana ridibunda Pallas, 1771)。方法。生物试验采用“时间采样”的方法进行,使个体初步暴露在捷捷列夫河的德尼舍夫斯基储水盆地和奥特谢纳取水口的测试水样中12小时(n=30),并从水管中提取沉淀水样作为对照。通过个体典型和非典型活性反应计算水毒性指标。用奈斯勒试剂光度法测定氨含量。采用标准的计算机程序moexcel2003进行相关分析和回归分析。结果。确定了氨对试验水毒性的影响,并通过3年期间的测定系数值(蓄水池的r2值为0.3893,取水口的r2值为0.2814)和相关性(中等程度的R值分别为0.6240和0.5305)证明了这一点。用线性回归方程(y=52,535x+16,207和y=50,917x+21,067)构建了图,可以预测储水盆地和取水的氨含量对水的毒性水平。结论。结果表明,2014年(Denishevsky流域为0.6939年,Otsechne取水口为0.6803年)水体毒性指标与氨含量的相关性高于2012年(0.6413年和0.4281年)和2013年(0.6556年和0.5083年),这是由于氨化过程的增加所致。氨对这些水的毒性的影响有增加的趋势(在储水盆地的水中从41.12%增加到48.15%,在取水时从18.33%增加到46.28%)。在3年的研究期间,在38,93%的水平上证明了储水区水的毒性存在可靠的氨影响(F=3,0811;p≤0.05,),其在取水中缺失率为28.14% (F=1,5663)。给出了线性回归方程和依赖关系的图形图像,可以计算出湖蛙达到50%水毒性水平时的氨含量(0.58 mg/dm 3和0.64 mg/dm 3)
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Influence of ammonia of waters from the surface sources of water supply on their toxicity for Rana Ridibunda (Pallas, 1771)
Aim . Revelation of the influence of ammonia from surface water supply sources on formation of their toxicity, determined by indices of motor activity of young lacustrine frogs (Rana ridibunda Pallas, 1771). Methods . Biotesting was conducted by the method of «time sampling» with preliminary exposure of individuals for 12 hours (n=30) in test samples of water, taken from the Denishevsky water storage basin and Otsechne water intake of the river Teterev and also in samples of settled water from water pipe as a control. The indices of water toxicity were calculated by reactions of typical and non-typical activity of individuals. The ammonia content was determined by the photometric method with Nessler reagent. The correlation and regression analysis was realized by the standard computer program MO Excel 2003. Results . There are established the effects of the ammonia influence on the toxicity of test waters that is proved by the values of determination coefficients, received for 3-year period (R 2 at level 0,3893 for the water storage basin and 0,2814 for water intake) and correlation (r of middle degree 0,6240 and 0,5305 respectively). There are constructed the graphs, expressed by the equations of rectilinear regression (y=52,535x+16,207 and y=50,917x+21,067), that gives a possibility to prognosticate toxicity levels of waters as to the ammonia content for the water storage basin and water intake. Conclusions . There were revealed the correlations of the indices of toxicity of the testing waters with the ammonia content that in 2014 (0,6939 – in the Denishevsky water storage basin and 0,6803 – in the Otsechne water intake) reached more degree than in 2012 (0,6413 and 0,4281) and 2013 (0,6556 and 0,5083) years, respectively that is conditioned by increasing ammonification processes. There was fixed a tendency of increasing the force of the ammonia influence (from 41,12 to 48,15 % in waters of the water storage basin and from 18,33 to 46,28 % – water intake) on the toxicity of these waters. In the 3-years period of the studies, there was testified the presence of the reliable ammonia influence of the toxicity of waters in the water storage basin at level 38,93 % (F=3,0811; p ≤0,05, ), and also its absence in the water intake  28,14 % (F=1,5663). There were given the equations of rectilinear regression and graphic images of the dependencies that allow to calculate the ammonia content (0,58 mg/dm 3 and 0,64) at reaching 50 % level of water toxicity of lacustrine frogs
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