Specific features of photometric determination of organic carbon in bottom sediments
Organic matter in bottom sediments originates from plants and animals as a metabolic byproduct; it determines biological productivity of a water body and physical and chemical properties of its bottom soils, enriches its aquatic environment with biogenic elements, and provides nutrients for its benthic communites, on which, in turn, feed benthophagous fish species. The most reprepresentative indicator of the organic matter in bottom sediments is organic carbon. Currently, for determination of the organic carbon directly in bottom sediments, either expensive equipment or certified methods approved for soils are used. This work presents the results of development and validation of the method for quantitative determination of organic carbon in bottom sediments. The developed modification of I.V. Tyurin’s method is based on photometric detection of trivalent chrome that is equivalent to the content of oranic carbon after oxidation of the organic matter in bottom sediments in chromosulfuric acid. Chloride interference was precluded with silver sulphate; as a reference standard, the State Standard Sample of glucose was used for the first time. This method has been tested on the bottom sediments of the Azov Sea, and the results are found to be in compliance with those obtained from the investigations conducted by the traditional Tyurin’s method with silver sulphate. This method does not require expensive equipment and is applicable for mass determination. Based on the results of this investigation, a metrological certification of the developed method has been conducted; it regulates the procedure for determination of carbon mass fractions in the bottom sediments of water bodies in the range from 0.3 to 16.0 %.
Main Authors: | , |
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Format: | Journal Contribution biblioteca |
Language: | Russian |
Published: |
2023
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Subjects: | Органическое вещество, Разработанная методика, Bottom sediments, Methodology, Metrological certification, Biological productivity, Chemical properties, Photometric detection method, Chromosulfuric acid, Carbon mass fractions, ASFA_2015::O::Organic carbon, ASFA_2015::P::Photometry, ASFA_2015::B::Biogenic deposits, |
Online Access: | http://hdl.handle.net/1834/42878 |
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Органическое вещество Разработанная методика Bottom sediments Methodology Metrological certification Biological productivity Chemical properties Photometric detection method Chromosulfuric acid Carbon mass fractions ASFA_2015::O::Organic carbon ASFA_2015::P::Photometry ASFA_2015::B::Biogenic deposits Органическое вещество Разработанная методика Bottom sediments Methodology Metrological certification Biological productivity Chemical properties Photometric detection method Chromosulfuric acid Carbon mass fractions ASFA_2015::O::Organic carbon ASFA_2015::P::Photometry ASFA_2015::B::Biogenic deposits |
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Органическое вещество Разработанная методика Bottom sediments Methodology Metrological certification Biological productivity Chemical properties Photometric detection method Chromosulfuric acid Carbon mass fractions ASFA_2015::O::Organic carbon ASFA_2015::P::Photometry ASFA_2015::B::Biogenic deposits Органическое вещество Разработанная методика Bottom sediments Methodology Metrological certification Biological productivity Chemical properties Photometric detection method Chromosulfuric acid Carbon mass fractions ASFA_2015::O::Organic carbon ASFA_2015::P::Photometry ASFA_2015::B::Biogenic deposits Shevtsova, E.A. Burdina, E.I. Specific features of photometric determination of organic carbon in bottom sediments |
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Organic matter in bottom sediments originates from plants and animals as a metabolic byproduct; it determines biological productivity of a water body and physical and chemical properties of its bottom soils, enriches its aquatic environment with biogenic elements, and provides nutrients for its benthic communites, on which, in turn, feed benthophagous fish species. The most reprepresentative indicator of the organic matter in bottom sediments is organic carbon. Currently, for determination of the organic carbon directly in bottom sediments, either expensive equipment or certified methods approved for soils are used. This work presents the results of development and validation of the method for quantitative determination of organic carbon in bottom sediments. The developed modification of I.V. Tyurin’s method is based on photometric detection of trivalent chrome that is equivalent to the content of oranic carbon after oxidation of the organic matter in bottom sediments in chromosulfuric acid. Chloride interference was precluded with silver sulphate; as a reference standard, the State Standard Sample of glucose was used for the first time. This method has been tested on the bottom sediments of the Azov Sea, and the results are found to be in compliance with those obtained from the investigations conducted by the traditional Tyurin’s method with silver sulphate. This method does not require expensive equipment and is applicable for mass determination. Based on the results of this investigation, a metrological certification of the developed method has been conducted; it regulates the procedure for determination of carbon mass fractions in the bottom sediments of water bodies in the range from 0.3 to 16.0 %. |
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Journal Contribution |
topic_facet |
Органическое вещество Разработанная методика Bottom sediments Methodology Metrological certification Biological productivity Chemical properties Photometric detection method Chromosulfuric acid Carbon mass fractions ASFA_2015::O::Organic carbon ASFA_2015::P::Photometry ASFA_2015::B::Biogenic deposits |
author |
Shevtsova, E.A. Burdina, E.I. |
author_facet |
Shevtsova, E.A. Burdina, E.I. |
author_sort |
Shevtsova, E.A. |
title |
Specific features of photometric determination of organic carbon in bottom sediments |
title_short |
Specific features of photometric determination of organic carbon in bottom sediments |
title_full |
Specific features of photometric determination of organic carbon in bottom sediments |
title_fullStr |
Specific features of photometric determination of organic carbon in bottom sediments |
title_full_unstemmed |
Specific features of photometric determination of organic carbon in bottom sediments |
title_sort |
specific features of photometric determination of organic carbon in bottom sediments |
publishDate |
2023 |
url |
http://hdl.handle.net/1834/42878 |
work_keys_str_mv |
AT shevtsovaea specificfeaturesofphotometricdeterminationoforganiccarboninbottomsediments AT burdinaei specificfeaturesofphotometricdeterminationoforganiccarboninbottomsediments AT shevtsovaea osobennostifotometričeskogoopredeleniâorganičeskogouglerodavdonnyhotloženiâh AT burdinaei osobennostifotometričeskogoopredeleniâorganičeskogouglerodavdonnyhotloženiâh |
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dig-aquadocs-1834-428782023-12-09T02:14:00Z Specific features of photometric determination of organic carbon in bottom sediments Особенности фотометрического определения органического углерода в донных отложениях Shevtsova, E.A. Burdina, E.I. Органическое вещество Разработанная методика Bottom sediments Methodology Metrological certification Biological productivity Chemical properties Photometric detection method Chromosulfuric acid Carbon mass fractions ASFA_2015::O::Organic carbon ASFA_2015::P::Photometry ASFA_2015::B::Biogenic deposits Organic matter in bottom sediments originates from plants and animals as a metabolic byproduct; it determines biological productivity of a water body and physical and chemical properties of its bottom soils, enriches its aquatic environment with biogenic elements, and provides nutrients for its benthic communites, on which, in turn, feed benthophagous fish species. The most reprepresentative indicator of the organic matter in bottom sediments is organic carbon. Currently, for determination of the organic carbon directly in bottom sediments, either expensive equipment or certified methods approved for soils are used. This work presents the results of development and validation of the method for quantitative determination of organic carbon in bottom sediments. The developed modification of I.V. Tyurin’s method is based on photometric detection of trivalent chrome that is equivalent to the content of oranic carbon after oxidation of the organic matter in bottom sediments in chromosulfuric acid. Chloride interference was precluded with silver sulphate; as a reference standard, the State Standard Sample of glucose was used for the first time. This method has been tested on the bottom sediments of the Azov Sea, and the results are found to be in compliance with those obtained from the investigations conducted by the traditional Tyurin’s method with silver sulphate. This method does not require expensive equipment and is applicable for mass determination. Based on the results of this investigation, a metrological certification of the developed method has been conducted; it regulates the procedure for determination of carbon mass fractions in the bottom sediments of water bodies in the range from 0.3 to 16.0 %. Органическое вещество донных осадков является продуктом жизнедеятельности растительных и животных организмов, определяет физико-химические свойства грунтов и биологическую продуктивность водоема, обогащает водную среду биогенными элементами, а также служит источником питательных веществ для бентосных сообществ, которыми, в свою очередь, питаются рыбы-бентофаги. Наиболее репрезентативным показателем органического вещества в донных отложениях является органический углерод. В настоящий момент органический углерод непосредственно в донных отложениях определяется на дорогостоящем оборудовании либо с использованием методик, аттестованных для почв. В работе проводилась разработка и аттестация методики количественного определения органического углерода в донных осадках. Разработанная модификация метода Тюрина основана на фотометрическом определении трехвалентного хрома, эквивалентного содержанию органического углерода после окисления органического вещества донных отложений в хромовой смеси. Мешающее влияние хлоридов устраняли с помощью сульфата серебра; в качестве стандартного образца впервые использовали ГСО глюкозы. Методика опробована на донных отложениях Азовского моря, результаты измерений согласуются с исследованиями, проведенными классическим методом Тюрина в присутствии сульфата серебра. Разработанная методика не требует дорогостоящего оборудования и пригодна для массовых определений. По результатам работы была проведена метрологическая аттестация разработанной методики, которая регламентирует порядок определения массовых долей углерода в донных отложениях водных объектов в диапазоне от 0,3 до 16,0 %. Published Refereed 2023-12-08T12:13:47Z 2023-12-08T12:13:47Z 2023 Journal Contribution 2618-8147 print 2619-1024 online 10.47921/2619-1024_2023_6_4_43 http://hdl.handle.net/1834/42878 ru https://journal.azniirkh.ru/uploads/files/2023/12/05/44_51_%D1%826_N4_2023-3.pdf Attribution 4.0 International http://creativecommons.org/licenses/by/4.0/ pp.43–50 Azov Sea Азовское море |