BIOTRANSFORMATION OF HYDROCARBONS IN THE GROUND SINKING

The processes of biotransformation of non-polar hydrocarbons are examined in the article. The ground sinking of off-shore area of north part of the Black sea was probed. The standards of the ground fallouts were taken away in the Sevastopol bay and in the off-shore area of Karadagsky of natural pres...

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Date:2016
Main Authors: Shkapenko, V.V., Kadoshnikov, V.M., Musich, E.G., Pisanskaya, I.R.
Format: Article
Language:Russian
Published: Institute of Geological Sciences, NAS of Ukraine 2016
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Online Access:http://geojournal.igs-nas.org.ua/article/view/97273
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Geological journal
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author Shkapenko, V.V.
Kadoshnikov, V.M.
Musich, E.G.
Pisanskaya, I.R.
author_facet Shkapenko, V.V.
Kadoshnikov, V.M.
Musich, E.G.
Pisanskaya, I.R.
author_sort Shkapenko, V.V.
baseUrl_str
collection OJS
datestamp_date 2018-03-15T11:00:09Z
description The processes of biotransformation of non-polar hydrocarbons are examined in the article. The ground sinking of off-shore area of north part of the Black sea was probed. The standards of the ground fallouts were taken away in the Sevastopol bay and in the off-shore area of Karadagsky of natural preserve. Mineral composition of sandy faction of the selected standards is presented kalcitom and kvarcem with the negligible quantity of pelitic faction (no more than 2%).  The standards of silt deposits mineral composition of which was presented montmorillonitom were taken away in deep-water part of the Sevastopol bay, illitom, kaolinite and vysokodispersnym kal'citom and kvarcem, and also by the particles of feldspars (analcin).The organic matter of silt deposits was presented humic acids (3%) and oil hydrocarbons (0,25%). A betweenness by humic acids and oil-products in the ground sinking of the Sevastopol bay grounds to consider that under the action of microorganisms oil-products is transformed in humic acids. This conclusion is confirmed the results of laboratory researches. For the design of this process was developed and prepared series of preparations, containing hydrocarbons mineral phase and bio-preparation in different correlations. The got mixture was maintained in a thermostat at permanent humidity 60-70% and to the temperature of 37±1oS is 21 day. It was set by the method of IK-spectroscopy, that as a result of action of microorganisms, containing cyclic structures which are identified as benzol rings are in aromatic hydrocarbons, appear in a chloroform extract. It is expressed appearance of bars of absorption in area of 1170 sm-1 and 1270 sm-1, on the IK-spectrums of standards additionally bars in area of 1715 sm-1 and 1735 sm-1 appear proper the valency vibrations of S=O, that characteristically for the processes of oxidization on spectrums. Essential influence on the process of transformation of hydrocarbons is rendered by the ions of ammonium, which in the conditions of lack of oxygen, promotes in anaerobic oxidization of hydrocarbons nitrates and nitrites with formation of ammonium. Restoration amination of intermediate oxidates hydrocarbons with formation of the nitrogenated organic compounds, including amino acid, assumes possibility of including of surplus carbon in the complement of organic matter. Being of high- dispersion mineral phase in the ground sinking accelerates the process of mineralizacii and partly results in the accumulation of guminosimilar polymers. It is experimentally well-proven that only during the certain concentration of clay minerals in a cultural environment it is possible to attain optimum terms for transformation of hydrocarbons.  The special composition, containing the complex of microorganisms and bentonito's clay allowing effectively to remove oil contaminations from mineral surfaces, is developed. The offered composition can be used for cleaning of hard mineral surfaces of both natural and technogenic objects.
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spelling mcm-mathkpnueduua-article-972732018-03-15T11:00:09Z BIOTRANSFORMATION OF HYDROCARBONS IN THE GROUND SINKING БИОТРАНСФОРМАЦИЯ УГЛЕВОДОРОДОВ В ДОННЫХ ОСАДКАХ БІОТРАНСФОРМАЦІЯ ВУГЛЕВОДНІВ У ДОННИХ ОСАДАХ Shkapenko, V.V. Kadoshnikov, V.M. Musich, E.G. Pisanskaya, I.R. hydrocarbons petroleum products transformation biodestructors microorganisms углеводороды нефтепродукты трансформация биодеструкторы микроорганизмы вуглеводні нафтопродукти трансформація біодеструктори мікроорганізми 550.4 551.462.32(262.5) The processes of biotransformation of non-polar hydrocarbons are examined in the article. The ground sinking of off-shore area of north part of the Black sea was probed. The standards of the ground fallouts were taken away in the Sevastopol bay and in the off-shore area of Karadagsky of natural preserve. Mineral composition of sandy faction of the selected standards is presented kalcitom and kvarcem with the negligible quantity of pelitic faction (no more than 2%).  The standards of silt deposits mineral composition of which was presented montmorillonitom were taken away in deep-water part of the Sevastopol bay, illitom, kaolinite and vysokodispersnym kal'citom and kvarcem, and also by the particles of feldspars (analcin).The organic matter of silt deposits was presented humic acids (3%) and oil hydrocarbons (0,25%). A betweenness by humic acids and oil-products in the ground sinking of the Sevastopol bay grounds to consider that under the action of microorganisms oil-products is transformed in humic acids. This conclusion is confirmed the results of laboratory researches. For the design of this process was developed and prepared series of preparations, containing hydrocarbons mineral phase and bio-preparation in different correlations. The got mixture was maintained in a thermostat at permanent humidity 60-70% and to the temperature of 37±1oS is 21 day. It was set by the method of IK-spectroscopy, that as a result of action of microorganisms, containing cyclic structures which are identified as benzol rings are in aromatic hydrocarbons, appear in a chloroform extract. It is expressed appearance of bars of absorption in area of 1170 sm-1 and 1270 sm-1, on the IK-spectrums of standards additionally bars in area of 1715 sm-1 and 1735 sm-1 appear proper the valency vibrations of S=O, that characteristically for the processes of oxidization on spectrums. Essential influence on the process of transformation of hydrocarbons is rendered by the ions of ammonium, which in the conditions of lack of oxygen, promotes in anaerobic oxidization of hydrocarbons nitrates and nitrites with formation of ammonium. Restoration amination of intermediate oxidates hydrocarbons with formation of the nitrogenated organic compounds, including amino acid, assumes possibility of including of surplus carbon in the complement of organic matter. Being of high- dispersion mineral phase in the ground sinking accelerates the process of mineralizacii and partly results in the accumulation of guminosimilar polymers. It is experimentally well-proven that only during the certain concentration of clay minerals in a cultural environment it is possible to attain optimum terms for transformation of hydrocarbons.  The special composition, containing the complex of microorganisms and bentonito's clay allowing effectively to remove oil contaminations from mineral surfaces, is developed. The offered composition can be used for cleaning of hard mineral surfaces of both natural and technogenic objects. Рассмотрены процессы биотрансформации неполярных углеводородов. Изучение органического вещества донных осадков Севастопольской бухты показало, что нефтепродукты, накапливаясь в высокодисперсной фракции донных осадков, частично минерализуются, а частично трансформируются в ароматические соединения и гуминоподобные полимеры. В лабораторных условиях подтверждена трансформация линейных алифатических углеводородов, которые под действием микроорганизмов частично минерализуются, а частично трансформируются в ароматические циклические соединения. Показано влияние минеральной фазы на накопление и эффективность биотрансформации неполярных углеводородов.   Розглядаються процеси біотрансформації неполярних вуглеводнів. Вивчення органічної речовини донних осадів Севастопольської бухти показало, що нафтопродукти, накопичуючись в високодисперсній фракції донних осадів, частково мінералізуються, а частково трансформуються в ароматичні сполуки і гуміноподібні полімери. У лабораторних умовах підтверджена трансформація лінійних аліфатичних вуглеводнів, які під дією мікроорганізмів частково мінералізуються, а частково трансформуються в ароматичні циклічні сполуки. Показано вплив мінеральної фази на накопичення й ефективність біотрансформації неполярних вуглеводнів.   Institute of Geological Sciences, NAS of Ukraine 2016-08-11 Article Article application/pdf http://geojournal.igs-nas.org.ua/article/view/97273 10.30836/igs.1025-6814.2016.2.97273 Geologìčnij žurnal (Geological Journal); No. 2 (2016); ст. 43 - 54 Геологический журнал; № 2 (2016); ст. 43 - 54 Геологічний журнал; № 2 (2016); ст. 43 - 54 2522-4107 1025-6814 rus http://geojournal.igs-nas.org.ua/article/view/97273/92616 Авторське право (c) 2021 V.V. Shkapenko, V.M. Kadoshnikov, E.G. Musich, I.R. Pisanskaya
spellingShingle hydrocarbons
petroleum products
transformation
biodestructors
microorganisms
Shkapenko, V.V.
Kadoshnikov, V.M.
Musich, E.G.
Pisanskaya, I.R.
BIOTRANSFORMATION OF HYDROCARBONS IN THE GROUND SINKING
title BIOTRANSFORMATION OF HYDROCARBONS IN THE GROUND SINKING
title_alt БИОТРАНСФОРМАЦИЯ УГЛЕВОДОРОДОВ В ДОННЫХ ОСАДКАХ
БІОТРАНСФОРМАЦІЯ ВУГЛЕВОДНІВ У ДОННИХ ОСАДАХ
title_full BIOTRANSFORMATION OF HYDROCARBONS IN THE GROUND SINKING
title_fullStr BIOTRANSFORMATION OF HYDROCARBONS IN THE GROUND SINKING
title_full_unstemmed BIOTRANSFORMATION OF HYDROCARBONS IN THE GROUND SINKING
title_short BIOTRANSFORMATION OF HYDROCARBONS IN THE GROUND SINKING
title_sort biotransformation of hydrocarbons in the ground sinking
topic hydrocarbons
petroleum products
transformation
biodestructors
microorganisms
topic_facet hydrocarbons
petroleum products
transformation
biodestructors
microorganisms
углеводороды
нефтепродукты
трансформация
биодеструкторы
микроорганизмы
вуглеводні
нафтопродукти
трансформація
біодеструктори
мікроорганізми
550.4
551.462.32(262.5)
url http://geojournal.igs-nas.org.ua/article/view/97273
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AT kadoshnikovvm biotransformationofhydrocarbonsinthegroundsinking
AT musicheg biotransformationofhydrocarbonsinthegroundsinking
AT pisanskayair biotransformationofhydrocarbonsinthegroundsinking
AT shkapenkovv biotransformaciâuglevodorodovvdonnyhosadkah
AT kadoshnikovvm biotransformaciâuglevodorodovvdonnyhosadkah
AT musicheg biotransformaciâuglevodorodovvdonnyhosadkah
AT pisanskayair biotransformaciâuglevodorodovvdonnyhosadkah
AT shkapenkovv bíotransformacíâvuglevodnívudonnihosadah
AT kadoshnikovvm bíotransformacíâvuglevodnívudonnihosadah
AT musicheg bíotransformacíâvuglevodnívudonnihosadah
AT pisanskayair bíotransformacíâvuglevodnívudonnihosadah