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chemistry journal of moldova

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V. Gladchi et al./Chem.J.Mold. 2008, 3 (1), 70-76The ammonia ions in the section line <strong>of</strong> Dniester were present in concentrations 0.015 – 0,136 ml NH 4+/l.Starting from Cosauti towards the Dubasari hydroelectrical plant their content was steadily increasing. The maximalcontent was observed below the dam at Dubasari. The seasonal dynamics <strong>of</strong> ammonium nitrogen was manifested by the+increase <strong>of</strong> its concentration in autumn. In spring the NH 4ions were not identified in any site but Bosernita.-In average for the year, the content <strong>of</strong> NO 3in the section lines constituted 5.5 – 7.4 mg NO 3-/l, and the lowest-values were detected in autumn; the highest concentrations <strong>of</strong> NO 3were observed in spring in all the sites butNaslavcea.The nitrites, during the investigation period, were a permanent component <strong>of</strong> Dniester waters. Their absencewas registered only once in May 2006 above and below the Dubasari barrage. The average content <strong>of</strong> nitrites throughoutthe year constituted between 0.027 and 0.058 mg NO 2-/l. In summer the content <strong>of</strong> nitrites in Dniester waters wasincreasing, while in spring it was decreasing. The permanent presence <strong>of</strong> nitrites in the background <strong>of</strong> low content or-complete absence <strong>of</strong> ammonium nitrogen can occur due to unfavorable oxidation state and slow oxidation <strong>of</strong> NO 2toNO 3-.3-The phosphates were present in the river in quantities 0.11 – 3.22 mg PO 4/l. Their average concentrations in3-the sections lines varied in the range 0.48-0.73 mg 4/l. The maximal pollution with phosphates was observed in3-the summer <strong>of</strong> 2006 at Cosauti and Bosernita sites, and constituted respectively 3.22 and 1.37 mg 4/l. The seasonaldynamics have shown an increase <strong>of</strong> the phosphates content in the segment Naslavcea – Mereseuca in spring, anotherincrease being detected in summer between Cosauti and Dubasari.The average content <strong>of</strong> organic compounds according to the BOD 5in the section lines <strong>of</strong> the investigated sector<strong>of</strong> Dniester constituted 3.1 – 3.9 mg O 2/l. In summer this indicator was rising above the yearly average at Mereseucaand Cosauti sites and constituted respectively 4.6 and 3.7 mg O 2/l, in spring – at the Dubasari water reservoir (Bosernita– Dubasari, lower reach) and constituted respectively 6.1 – 5.0 mg O 2/l. At Naslavcea the maximal amount <strong>of</strong> organiccompounds was 4.45 mg O 2/l that was detected in spring.The hydrogen peroxide and the redox state <strong>of</strong> watersThe analyses <strong>of</strong> the waters <strong>of</strong> the sector under investigation have never detected an oxidant state throughout theperiod <strong>of</strong> research (table 2). The most favorable state, according to this parameter, was registered in September 2005when hydrogen peroxide was detected in the samples collected from all the sites (the range <strong>of</strong> concentrations: 1.44·10 -6 M– 9.52·10 -6 M) except Naslavchea. At that site the waters were continuously in reducing state, the hydrogen peroxidewas missing and only the organic substances <strong>of</strong> peroxidazic type that are easily titrated by hydrogen peroxide werepresent. The reducing state <strong>of</strong> water below the Naslavchea dam could be caused by a shift from the equilibrium statein the waters <strong>of</strong> the accumulation reservoir above the dam resulting from the inflow <strong>of</strong> substantial amounts <strong>of</strong> reducingperoxidazic substances. The negative impact <strong>of</strong> the resulted disequilibria has been attenuated along the investigationsegment <strong>of</strong> the river, that was confirmed by the presence <strong>of</strong> hydrogen peroxide in the waters <strong>of</strong> the Mereseuca site,where its concentration was the lowest (1.19 . 10 -6 M) in the hole investigated part <strong>of</strong> the river. The detection <strong>of</strong> hydrogenperoxide can be related to the occurrence in the segment Naslavcea – Mereseuca (18 km) <strong>of</strong> self-purification processesthat lead to the total oxidation <strong>of</strong> peroxidazic substances and to the low excess <strong>of</strong> hydrogen peroxide.The maximal content <strong>of</strong> H 2O 2in September 2005 was registered below and above the Dubasari dam (8.48· 10 -6 Mand 9.52·10 -6 M), that can be explained by the existence <strong>of</strong> large quantities <strong>of</strong> micr<strong>of</strong>lora that eliminates metabolic H 2O 2in the surrounding environment.Table 2The content <strong>of</strong> hydrogen peroxide and reducing substances (H 2O 2·10 -6 M/Red·10 -6 M) in the waters <strong>of</strong> Dniester River)Month, year Naslavcea Mereseuca Cosauti Bosernita Dubasari, above Dubasari, belowthe dam the dam09.2005 -1,191,771,449,528,481,10-----10.2005 1,241,051,90-1,52-------11.2005 0,320,350,70-0,330,42------03.2006 ----------0,900,9205.2006 0,30-0,50-0,500,40-0,30----06.2006 4,805,441,26------0,500,460,6408.2006 0,500,490,480,490,490,48------72

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