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Nitrobacter As an Indicator of Toxicity in Wastewater
State Water Survey Division WATER QUALITY SECTION AT Illinois Department of PEORIA, ILLINOIS Energy and Natural Resources SWS Contract Report 326 NITROBACTER AS AN INDICATOR OF TOXICITY IN WASTEWATER by Wuncheng Wang and Paula Reed Prepared for and funded by the Illinois Department of Energy and Natural Resources September 1983 CONTENTS PAGE Abstract 1 Introduction 1 Scope of study 3 Acknowledgments 3 Literature review 3 Microbial nitrification 3 Influence of toxicants on nitrification 5 Materials and methods 10 Culture 10 Methods 11 Results 12 Preliminary tests 13 Metal toxicity 13 Organic compounds toxicity 16 Time effect 22 Discussion 22 References 27 NITROBACTER AS AN INDICATOR OF TOXICITY IN WASTEWATER by Wuncheng Wang and Paula Reed ABSTRACT This report presents the results of a study of the use of Nitrobacter as an indicator of toxicity. Nitrobacter are strictly aerobic, autotrophic, and slow growing bacteria. Because they convert nitrite to nitrate, the effects that toxins have on them can be detected easily by monitoring changes in their nitrite consumption rate. The bacterial cultures were obtained from two sources — the Peoria and Princeton (Illinois) wastewater treatment plants — and tests were con• ducted to determine the effects on the cultures of inorganic ions and organic compounds. The inorganic ions included cadmium, copper, lead, and nickel. The organic compounds were phenol, chlorophenol (three derivatives), dichlo- rophenol (two derivatives), and trichlorophenol. The bioassay procedure is relatively simple and the results are repro• ducible . The effects of these chemical compounds on Nitrobacter were not dramatic. For example, of the compounds tested, 2,4,6-trichlorophenol was the most toxic to Nitrobacter. -
Cometabolic Biodegradation of Halogenated Aliphatic Hydrocarbons by Ammonia-Oxidizing Microorganisms Naturally Associated with Wetland Plant Roots
Wright State University CORE Scholar Browse all Theses and Dissertations Theses and Dissertations 2015 Cometabolic Biodegradation of Halogenated Aliphatic Hydrocarbons by Ammonia-oxidizing Microorganisms Naturally Associated with Wetland Plant Roots Ke Qin Wright State University Follow this and additional works at: https://corescholar.libraries.wright.edu/etd_all Part of the Environmental Sciences Commons Repository Citation Qin, Ke, "Cometabolic Biodegradation of Halogenated Aliphatic Hydrocarbons by Ammonia-oxidizing Microorganisms Naturally Associated with Wetland Plant Roots" (2015). Browse all Theses and Dissertations. 1430. https://corescholar.libraries.wright.edu/etd_all/1430 This Dissertation is brought to you for free and open access by the Theses and Dissertations at CORE Scholar. It has been accepted for inclusion in Browse all Theses and Dissertations by an authorized administrator of CORE Scholar. For more information, please contact [email protected]. COMETABOLIC BIODEGRADATION OF HALOGENATED ALIPHATIC HYDROCARBONS BY AMMONIA-OXIDIZING MICROORGANISMS NATURALLY ASSOCIATED WITH WETLAND PLANT ROOTS A dissertation submitted in partial fulfillment of the requirements for the degree of Doctor of Philosophy By KE QIN MRes., University of York, 2008 2014 Wright State University i COPYRIGHT BY KE QIN 2014 ii WRIGHT STATE UNIVERSITY GRADUATE SCHOOL JANUARY 12, 2015 I HEREBY RECOMMEND THAT THE DISSERTATION PREPARED UNDER MY SUPERVISION BY Ke Qin ENTITLED Cometabolic Biodegradation of Halogenated Aliphatic Hydrocarbons by Ammonia-Oxidizing Microorganisms Naturally Associated with Wetland Plant Roots BE ACCEPTED IN PARTIAL FULFILLMENT OF THE REQUIREMENTS FOR THE DEGREE OF Doctor of Philosophy. ________________________________ Abinash Agrawal, Ph.D. Dissertation Director ________________________________ Donald Cipollini, Ph.D. Director, ES Ph.D. Program ________________________________ Committee on Robert E.W. -
Hydrogen Isotope Fractionation in Lipids of the Methane-Oxidizing Bacterium Methylococcus Capsulatus
Geochimica et Cosmochimica Acta, Vol. 66, No. 22, pp. 3955–3969, 2002 Copyright © 2002 Elsevier Science Ltd Pergamon Printed in the USA. All rights reserved 0016-7037/02 $22.00 ϩ .00 PII S0016-7037(02)00981-X Hydrogen isotope fractionation in lipids of the methane-oxidizing bacterium Methylococcus capsulatus 1, 2 3 1 ALEX L. SESSIONS, *LINDA L. JAHNKE, ARNDT SCHIMMELMANN, and JOHN M. HAYES 1Department of Geology and Geophysics, Woods Hole Oceanographic Institution, Woods Hole, MA 02543, USA 2Exobiology Branch, NASA-Ames Research Center, Moffett Field, CA 94035, USA 3Biogeochemical Laboratories, Department of Geological Sciences, Indiana University, Bloomington, IN 47405, USA (Received December 10, 2001; accepted in revised form June 7, 2002) Abstract—Hydrogen isotopic compositions of individual lipids from Methylococcus capsulatus, an aerobic, methane-oxidizing bacterium, were analyzed by hydrogen isotope-ratio-monitoring gas chromatography–mass spectrometry (GC-MS). The purposes of the study were to measure isotopic fractionation factors between methane, water, and lipids and to examine the biochemical processes that determine the hydrogen isotopic composition of lipids. M. capsulatus was grown in six replicate cultures in which the ␦D values of methane and water were varied independently. Measurement of concomitant changes in ␦D values of lipids allowed estimation of the proportion of hydrogen derived from each source and the isotopic fractionation associated with the utilization of each source. All lipids examined, including fatty acids, sterols, and hopanols, derived 31.4 Ϯ 1.7% of their hydrogen from methane. This was apparently true whether the cultures were harvested during exponential or stationary phase. Examination of the relevant biochemical pathways indicates that no hydrogen is transferred directly (with C-H bonds intact) from methane to lipids. -
Reduced Net Methane Emissions Due to Microbial Methane Oxidation in a Warmer Arctic
LETTERS https://doi.org/10.1038/s41558-020-0734-z Reduced net methane emissions due to microbial methane oxidation in a warmer Arctic Youmi Oh 1, Qianlai Zhuang 1,2,3 ✉ , Licheng Liu1, Lisa R. Welp 1,2, Maggie C. Y. Lau4,9, Tullis C. Onstott4, David Medvigy 5, Lori Bruhwiler6, Edward J. Dlugokencky6, Gustaf Hugelius 7, Ludovica D’Imperio8 and Bo Elberling 8 Methane emissions from organic-rich soils in the Arctic have bacteria (methanotrophs) and the remainder is mostly emitted into been extensively studied due to their potential to increase the atmosphere (Fig. 1a). The methanotrophs in these wet organic the atmospheric methane burden as permafrost thaws1–3. soils may be low-affinity methanotrophs (LAMs) that require However, this methane source might have been overestimated >600 ppm of methane (by moles) for their growth and mainte- without considering high-affinity methanotrophs (HAMs; nance23. But in dry mineral soils, the dominant methanotrophs are methane-oxidizing bacteria) recently identified in Arctic min- high-affinity methanotrophs (HAMs), which can survive and grow 4–7 eral soils . Herein we find that integrating the dynamics of at a level of atmospheric methane abundance ([CH4]atm) of about HAMs and methanogens into a biogeochemistry model8–10 1.8 ppm (Fig. 1b)24. that includes permafrost soil organic carbon dynamics3 leads Quantification of the previously underestimated HAM-driven −1 to the upland methane sink doubling (~5.5 Tg CH4 yr ) north of methane sink is needed to improve our understanding of Arctic 50 °N in simulations from 2000–2016. The increase is equiva- methane budgets. -
General Introduction
Physiological Characteristics and Genomic Properties of Nitrosomonas mobilis Isolated from Nitrifying Granule of Wastewater Treatment Bioreactor December 2016 Soe Myat Thandar ソー ミャット サンダー Physiological Characteristics and Genomic Properties of Nitrosomonas mobilis Isolated from Nitrifying Granule of Wastewater Treatment Bioreactor December 2016 Waseda University Graduate School of Advanced Science and Engineering Department of Life Science and Medical Bioscience Research on Environmental Biotechnology Soe Myat Thandar ソー ミャット サンダー Contents Abbreviations ................................................................................................................... i Chapter 1-General introduction .................................................................................... 1 1.1. Nitrification and wastewater treatment system .......................................................... 3 1.2. Important of Nitrosomonas mobilis ........................................................................... 8 1.3. Objectives and outlines of this study ....................................................................... 12 1.4. Reference.................................................................................................................. 12 Chapter 2- Physiological characteristics of Nitrosomonas mobilis Ms1 ................... 17 2.1. Introduction .............................................................................................................. 19 2.2. Material and methods .............................................................................................. -
Human Alteration of the Global Nitrogen Cycle
What is Nitrogen? Human Alteration of the Nitrogen is the most abundant element in Global Nitrogen Cycle the Earth’s atmosphere. Nitrogen makes up 78% of the troposphere. Nitrogen cannot be absorbed directly by the plants and animals until it is converted into compounds they can use. This process is called the Nitrogen Cycle. Heather McGraw, Mandy Williams, Suzanne Heinzel, and Cristen Whorl, Give SIUE Permission to Put Our Presentation on E-reserve at Lovejoy Library. The Nitrogen Cycle How does the nitrogen cycle work? Step 1- Nitrogen Fixation- Special bacteria convert the nitrogen gas (N2 ) to ammonia (NH3) which the plants can use. Step 2- Nitrification- Nitrification is the process which converts the ammonia into nitrite ions which the plants can take in as nutrients. Step 3- Ammonification- After all of the living organisms have used the nitrogen, decomposer bacteria convert the nitrogen-rich waste compounds into simpler ones. Step 4- Denitrification- Denitrification is the final step in which other bacteria convert the simple nitrogen compounds back into nitrogen gas (N2 ), which is then released back into the atmosphere to begin the cycle again. How does human intervention affect the nitrogen cycle? Nitric Oxide (NO) is released into the atmosphere when any type of fuel is burned. This includes byproducts of internal combustion engines. Production and Use of Nitrous Oxide (N2O) is released into the atmosphere through Nitrogen Fertilizers bacteria in livestock waste and commercial fertilizers applied to the soil. Removing nitrogen from the Earth’s crust and soil when we mine nitrogen-rich mineral deposits. Discharge of municipal sewage adds nitrogen compounds to aquatic ecosystems which disrupts the ecosystem and kills fish. -
Characterization of a Microbial Community Capable of Nitrification At
Bioresource Technology 101 (2010) 491–500 Contents lists available at ScienceDirect Bioresource Technology journal homepage: www.elsevier.com/locate/biortech Characterization of a microbial community capable of nitrification at cold temperature Thomas F. Ducey *, Matias B. Vanotti, Anthony D. Shriner, Ariel A. Szogi, Aprel Q. Ellison Coastal Plains Soil, Water, and Plant Research Center, Agricultural Research Service, USDA, 2611 West Lucas Street, Florence, SC 29501, United States article info abstract Article history: While the oxidation of ammonia is an integral component of advanced aerobic livestock wastewater Received 5 February 2009 treatment, the rate of nitrification by ammonia-oxidizing bacteria is drastically reduced at colder temper- Received in revised form 30 July 2009 atures. In this study we report an acclimated lagoon nitrifying sludge that is capable of high rates of nitri- Accepted 30 July 2009 fication at temperatures from 5 °C (11.2 mg N/g MLVSS/h) to 20 °C (40.4 mg N/g MLVSS/h). The Available online 5 September 2009 composition of the microbial community present in the nitrifying sludge was investigated by partial 16S rRNA gene sequencing. After DNA extraction and the creation of a plasmid library, 153 partial length Keywords: 16S rRNA gene clones were sequenced and analyzed phylogenetically. Over 80% of these clones were Nitrite affiliated with the Proteobacteria, and grouped with the b- (114 clones), - (7 clones), and -classes (2 Ammonia-oxidizing bacteria c a Nitrosomonas clones). The remaining clones were affiliated with the Acidobacteria (1 clone), Actinobacteria (8 clones), Activated sludge Bacteroidetes (16 clones), and Verrucomicrobia (5 clones). The majority of the clones belonged to the genus 16S rRNA gene Nitrosomonas, while other clones affiliated with microorganisms previously identified as having floc forming or psychrotolerance characteristics. -
The Ratio of Methanogens to Methanotrophs and Water-Level Dynamics Drive Methane Exchange Velocity in a Temperate Kettle-Hole Peat Bog
Biogeosciences Discuss., https://doi.org/10.5194/bg-2019-116 Manuscript under review for journal Biogeosciences Discussion started: 23 April 2019 c Author(s) 2019. CC BY 4.0 License. The ratio of methanogens to methanotrophs and water-level dynamics drive methane exchange velocity in a temperate kettle-hole peat bog Camilo Rey-Sanchez1,4, Gil Bohrer1, Julie Slater2, Yueh-Fen Li3, Roger Grau-Andrés2, Yushan Hao2, 5 Virginia I. Rich3, & G. Matt Davies2 1Department of Civil and Environmental Engineering and Geodetic Science, The Ohio State University, Columbus, Ohio, 43210, USA 2School of Environment and Natural Resources, The Ohio State University, Columbus, Ohio, 43210, USA 3Department of Microbiology, The Ohio State University, Columbus, Ohio, 43210, USA 10 4Current address, Department of Environmental Science, Management and Policy, University of California- Berkeley, California, 94720, USA Correspondence to: Camilo Rey-Sanchez ([email protected]) 15 Abstract. Peatlands are a large source of methane (CH4) to the atmosphere, yet the uncertainty around the estimates of CH4 flux from peatlands is large. To better understand the spatial heterogeneity in temperate peatland CH4 emissions and their response to physical and biological drivers, we studied CH4 dynamics throughout the growing seasons of 2017 and 2018 in Flatiron Lake Bog, a kettle-hole peat bog in Ohio. The site is composed of six different hydro-biological zones: an open water zone, four concentric vegetation zones surrounding the open water, and a restored zone connected to the main bog by a narrow 20 channel. At each of these locations, we monitored water level (WL), CH4 pore-water concentration at different peat depths, CH4 fluxes from the ground and from representative plant species using chambers, and microbial community composition with focus here on known methanogens and methanotrophs. -
Nitrogen Removal Training Program
Nitrogen Removal Training Program Module 1 Nitrogen in the Aquatic Environment • Forms of Nitrogen and Nitrogen Transformations • Nitrogen in Surface Waters • Water Quality Impacts of Nitrogen Discharges • Nitrogen in Wastewater Module 1 Transparency 1 Nitrogen Removal Training Program Module 1 Forms of Nitrogen and Nitrogen Transformations Module 1 Transparency 2 Forms of Nitrogen in the Environment Unoxidized Forms Oxidized Forms of Nitrogen of Nitrogen Nitrite (NO -) • Nitrogen Gas (N2) • 2 + Nitrate (NO -) • Ammonia (NH4 , NH3) • 3 • Organic Nitrogen (urea, • Nitrous Oxide (N2O) amino acids, peptides, proteins, etc...) • Nitric Oxide (NO) • Nitrogen Dioxide (NO2) Module 1 Transparency 3 Nitrogen Fixation • Biological Fixation - Use of atmospheric nitrogen by certain photosynthetic blue-green algae and bacteria for growth. Nitrogen Gas Organic Nitrogen (N2) • Lightning Fixation - Conversion of atmospheric nitrogen to nitrate by lightning. lightning Nitrogen Gas + Ozone Nitrate - (N2) (O3)(NO3 ) • Industrial Fixation - Conversion of nitrogen gas to ammonia and nitrate-nitrogen (used in the manufacture of fertilizers and explosives). Module 1 Transparency 4 Biological Nitrogen Fixation Nitrogen Gas (N2) Bacteria Blue-green Algae Organic N Organic N Certain blue-green algae and bacteria use atmospheric nitrogen to produce organic nitrogen compounds. Module 1 Transparency 5 Atmospheric Fixation Lightning converts Nitrogen Gas and Ozone to Nitrate. Nitrogen Gas Nitrate Module 1 Transparency 6 Industrial Fixation N2 Nitrogen gas is converted to ammonia and nitrate in the production of fertilizer and explosives. NH3 - NO3 Module 1 Transparency 7 Ammonification and Assimilation Ammonification - Conversion of organic nitrogen to ammonia-nitrogen resulting from the biological decomposition of dead plant and animal tissue and animal fecal matter. -
Recycling of Vitamin B12 and NAD+ Within the Pdu Microcompartment of Salmonella Enterica Shouqiang Cheng Iowa State University
Iowa State University Capstones, Theses and Graduate Theses and Dissertations Dissertations 2010 Recycling of vitamin B12 and NAD+ within the Pdu microcompartment of Salmonella enterica Shouqiang Cheng Iowa State University Follow this and additional works at: https://lib.dr.iastate.edu/etd Part of the Biochemistry, Biophysics, and Structural Biology Commons Recommended Citation Cheng, Shouqiang, "Recycling of vitamin B12 and NAD+ within the Pdu microcompartment of Salmonella enterica" (2010). Graduate Theses and Dissertations. 11713. https://lib.dr.iastate.edu/etd/11713 This Dissertation is brought to you for free and open access by the Iowa State University Capstones, Theses and Dissertations at Iowa State University Digital Repository. It has been accepted for inclusion in Graduate Theses and Dissertations by an authorized administrator of Iowa State University Digital Repository. For more information, please contact [email protected]. + Recycling of vitamin B12 and NAD within the Pdu microcompartment of Salmonella enterica by Shouqiang Cheng A dissertation submitted to the graduate faculty in partial fulfillment of the requirements for the degree of DOCTOR OF PHILOSOPHY Major: Biochemistry Program of Study Committee: Thomas A. Bobik, Major Professor Alan DiSpirito Basil Nikolau Reuben Peters Gregory J. Phillips Iowa State University Ames, Iowa 2010 Copyright © Shouqiang Cheng, 2010. All rights reserved. ii Table of contents Abstract............................................................................................................................. -
Nitrification and Nitrifying Bacteria in a Coastal Microbial
ORIGINAL RESEARCH published: 01 December 2015 doi: 10.3389/fmicb.2015.01367 Nitrification and Nitrifying Bacteria in a Coastal Microbial Mat Haoxin Fan 1, Henk Bolhuis 1 and Lucas J. Stal 1, 2* 1 Department of Marine Microbiology, Royal Netherlands Institute for Sea Research, Yerseke, Netherlands, 2 Department of Aquatic Microbiology, Institute of Biodiversity and Ecosystem Dynamics, University of Amsterdam, Amsterdam, Netherlands The first step of nitrification, the oxidation of ammonia to nitrite, can be performed by ammonia-oxidizing archaea (AOA) or ammonium-oxidizing bacteria (AOB). We investigated the presence of these two groups in three structurally different types of coastal microbial mats that develop along the tidal gradient on the North Sea beach of the Dutch barrier island Schiermonnikoog. The abundance and transcription of amoA, a gene encoding for the alpha subunit of ammonia monooxygenase that is present in both AOA and AOB, were assessed and the potential nitrification rates in these mats were measured. The potential nitrification rates in the three mat types were highest in autumn and lowest in summer. AOB and AOA amoA genes were present in all three mat types. The composition of the AOA and AOB communities in the mats of the tidal and intertidal stations, based on the diversity of amoA, were similar and clustered separately from the supratidal microbial mat. In all three mats AOB amoA genes were significantly more abundant than AOA amoA genes. The abundance of neither AOB nor AOA amoA genes correlated with the potential nitrification rates, but AOB amoA transcripts were Edited by: Hongyue Dang, positively correlated with the potential nitrification rate. -
Organic Matter Decomposition in Simulated Aquaculture Ponds Group Fish Culture and Fisheries Daily Supervisor(S) Dr
O rganic matter decomposition in simulated aquaculture ponds Beatriz Torres Beristain Promotor: Prof. Dr. J.A .J. V erreth H oogleraar in de V isteelt en V isserij W ageningen U niversiteit C o-promotor: Dr. M .C .J. V erdegem U niversitair docent bij the Leerstoelgroep V isteelt en V isserij W ageningen U niversiteit Samenstelling promotiecommissie: Prof. Dr. Y . A vnimelech Technion, Israel Institute of Technology Prof. Dr. Ir. H .J. Gijzen U N ESC O -IH E, Delf, N etherlands Prof. Dr. Ir. M . W .A . V erstegen W ageningen U niversiteit Prof. Dr. Ir. A .A . K oelmans W ageningen U niversiteit Dit onderzoek is uitgevoerd binnen de onderzoekschool W IA S O rganic matter decomposition in simulated aquaculture ponds Beatriz Torres Beristain Proefschrift Ter verkrijging van de graad van doctor O p gezag van de rector magnificus van W ageningen U niversiteit, Prof. Dr. Ir. L. Speelman, In het openbaar te verdedigen O p dinsdag 15 A pril 2005 des namiddags te half tw ee in de A ula Torres Beristain, B. O rganic matter decomposition in simulated aquaculture ponds PhD thesis, Fish C ulture and Fisheries Group, W ageningen Institute of A nimal Sciences. W ageningen U niversity, P.O . Box 338, 6700 A H W ageningen, The N etherlands. - W ith R ef. œW ith summary in Spanish, Dutch and English ISBN : 90-8504-170-8 A Domingo, Y olanda y A lejandro Table of contents C hapter 1 General introduction. 1 C hapter 2 R eview microbial ecology and role in aquaculture ponds.