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Mineralization of dimethylsilanediol by microorganisms isolated from soil

Previous studies have shown that polydimethylsiloxane is hydrolyzed in soil to dimethylsilanediol and that dimethylsilanediol is biodegraded in soil. Previously, two soil microorganisms capable of biodegrading dimethylsilanediol were isolated and identified. In this paper, the extent of [(14)C]dimet...

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Published in:Environmental toxicology and chemistry 1999-09, Vol.18 (9), p.1913-1919
Main Authors: Sabourin, C.L, Carpenter, J.C, Leib, T.K, Spivack, J.L
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description Previous studies have shown that polydimethylsiloxane is hydrolyzed in soil to dimethylsilanediol and that dimethylsilanediol is biodegraded in soil. Previously, two soil microorganisms capable of biodegrading dimethylsilanediol were isolated and identified. In this paper, the extent of [(14)C]dimethylsilanediol biodegradation by these two soil microorganisms, Fusarium oxysporum Schlechtendahl and an Arthrobacter species, is investigated. The silicon-containing products of dimethylsilanediol biodegradation in liquid culture were identified by high-performance liquid chromatography coupled to argon plasma emission spectrometry (HPLC-ICP). The biodegradation of [(14)C]methylsilanetriol was investigated in liquid cultures and in soil by monitoring the production of (14)CO2. The sorption coefficient of [(14)C]methylsilanetriol was determined, and the sorption coefficient of [(14)C]dimethylsilanediol was estimated, by measuring the amount of (14)C counts in the water phase of a water-soil mixture. Methylsilanetriol was found to be mineralized in liquid cultures of F. oxysporum Schlecht. and the Arthrobacter sp. that were supplied with a primary carbon source. However, the production of (14)CO2 from [(14)]methylsilanetriol in soil experiments never exceeded the level of possible [(14)C]-containing impurities in the methylsilanetriol. Methylsilanetriol was found to be more strongly sorbed to soil, which might have reduced its bioavailability. Previous evidence has shown that polydimethylsiloxane is hydrolyzed in soil to the monomer dimethylsilanediol, which is biodegraded in soil. Now mineralization of dimethylsilanediol to inorganic silicate has been demonstrated.
doi_str_mv 10.1002/etc.5620180907
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Previously, two soil microorganisms capable of biodegrading dimethylsilanediol were isolated and identified. In this paper, the extent of [(14)C]dimethylsilanediol biodegradation by these two soil microorganisms, Fusarium oxysporum Schlechtendahl and an Arthrobacter species, is investigated. The silicon-containing products of dimethylsilanediol biodegradation in liquid culture were identified by high-performance liquid chromatography coupled to argon plasma emission spectrometry (HPLC-ICP). The biodegradation of [(14)C]methylsilanetriol was investigated in liquid cultures and in soil by monitoring the production of (14)CO2. The sorption coefficient of [(14)C]methylsilanetriol was determined, and the sorption coefficient of [(14)C]dimethylsilanediol was estimated, by measuring the amount of (14)C counts in the water phase of a water-soil mixture. Methylsilanetriol was found to be mineralized in liquid cultures of F. oxysporum Schlecht. and the Arthrobacter sp. that were supplied with a primary carbon source. However, the production of (14)CO2 from [(14)]methylsilanetriol in soil experiments never exceeded the level of possible [(14)C]-containing impurities in the methylsilanetriol. Methylsilanetriol was found to be more strongly sorbed to soil, which might have reduced its bioavailability. Previous evidence has shown that polydimethylsiloxane is hydrolyzed in soil to the monomer dimethylsilanediol, which is biodegraded in soil. 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Methylsilanetriol was found to be mineralized in liquid cultures of F. oxysporum Schlecht. and the Arthrobacter sp. that were supplied with a primary carbon source. However, the production of (14)CO2 from [(14)]methylsilanetriol in soil experiments never exceeded the level of possible [(14)C]-containing impurities in the methylsilanetriol. Methylsilanetriol was found to be more strongly sorbed to soil, which might have reduced its bioavailability. Previous evidence has shown that polydimethylsiloxane is hydrolyzed in soil to the monomer dimethylsilanediol, which is biodegraded in soil. 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Previously, two soil microorganisms capable of biodegrading dimethylsilanediol were isolated and identified. In this paper, the extent of [(14)C]dimethylsilanediol biodegradation by these two soil microorganisms, Fusarium oxysporum Schlechtendahl and an Arthrobacter species, is investigated. The silicon-containing products of dimethylsilanediol biodegradation in liquid culture were identified by high-performance liquid chromatography coupled to argon plasma emission spectrometry (HPLC-ICP). The biodegradation of [(14)C]methylsilanetriol was investigated in liquid cultures and in soil by monitoring the production of (14)CO2. The sorption coefficient of [(14)C]methylsilanetriol was determined, and the sorption coefficient of [(14)C]dimethylsilanediol was estimated, by measuring the amount of (14)C counts in the water phase of a water-soil mixture. Methylsilanetriol was found to be mineralized in liquid cultures of F. oxysporum Schlecht. and the Arthrobacter sp. that were supplied with a primary carbon source. However, the production of (14)CO2 from [(14)]methylsilanetriol in soil experiments never exceeded the level of possible [(14)C]-containing impurities in the methylsilanetriol. Methylsilanetriol was found to be more strongly sorbed to soil, which might have reduced its bioavailability. Previous evidence has shown that polydimethylsiloxane is hydrolyzed in soil to the monomer dimethylsilanediol, which is biodegraded in soil. Now mineralization of dimethylsilanediol to inorganic silicate has been demonstrated.</abstract><cop>Hoboken</cop><pub>Wiley Periodicals, Inc</pub><doi>10.1002/etc.5620180907</doi><tpages>7</tpages></addata></record>
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ispartof Environmental toxicology and chemistry, 1999-09, Vol.18 (9), p.1913-1919
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subjects Animal, plant and microbial ecology
Applied sciences
Arthrobacter
Biodegradation
biological activity in soil
Biological and medical sciences
Biological and physicochemical properties of pollutants. Interaction in the soil
contaminants
Dimethylsilanediol
Earth sciences
Earth, ocean, space
Engineering and environment geology. Geothermics
Exact sciences and technology
Fundamental and applied biological sciences. Psychology
Fusarium oxysporum
Methylsilanetriol
Microbial ecology
Pollution
Pollution, environment geology
Silicone
Soil
Soil and sediments pollution
title Mineralization of dimethylsilanediol by microorganisms isolated from soil
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