Anammox) in the Cape Fear River Estuary
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Deammonification
Deammonification MARCH 2019 The Deammonification Compendium was prepared in 2012 and later updated in 2014 as part of the Nutrient Removal Challenge. The Deammonification Compendium serves as a succinct primer on the deammonification process and applications in water resource recovery facilities. This 2019 compendium updates prior versions based on reports and documents generated by the Nutrient Removal Challenge. As such, updates are limited in scope and not intended to capture all recent industry and research activity related to deammonification. ACKNOWLEDGMENTS We acknowledge the following contributors and reviewers (alphabetically). The findings from the Nutrient Removal Challenge were incorporated into this 2019 edition by: Bryce Figdore JB Neethling David Stensel HDR Inc. HDR Inc. University of Washington The following individuals contributed to earlier versions of this compendium: Charles Bott Sudhir Murthy Julian Sandino Hampton Roads Sanitation DC Water CH2M Hill District JB Neethling David Stensel Gregory Bowden HDR Inc. University of Washington AECOM Amit Pramanik Ryujiro Tsuchihashi Ramesh Goel The Water Research AECOM University of Utah Foundation Please use the following citation for this document: WRF (The Water Research Foundation). 2019. “Deammonification” from the Nutrient Removal Challenge. 1199 North Fairfax Street, Suite 900 6666 West Quincy Avenue Alexandria, VA 22314-1445 Denver, CO 80235-3098 [email protected] www.waterrf.org TABLE OF CONTENTS DEAMMONIFICATION | 1 1 | What is deammonification? DEAMMONIFICATION PROCESS -
Isolation and Identification of Denitrifying Bacteria and Its Growth and Metabolism Characteristics
2017 2nd International Conference on Environmental Science and Energy Engineering (ICESEE 2017) ISBN: 978-1-60595-417-2 Isolation and Identification of Denitrifying Bacteria and Its Growth and Metabolism Characteristics Xin-ran JIANG, Dian JIAO, Lei ZHANG and Li-na ZHENG College of Marine Technology and Environmental, Dalian Ocean University, Dalian 116023, China Keywords: Denitrification, Nitrate, Isolation and identification, Activity research. Abstract. A denitrifying bacterium DN20 was isolated from the biofilm after centrifugation in the aquaculture purification system of a aquaculture base, and the denitrification characteristics of the strain were further studied. The strain was identified by 16S rDNA sequence analysis, the effects of temperature, salinity, pH, substrate concentration and C/N ratio on denitrification activity were studied. Introduction Denitrifying bacteria are a kind of bacteria that can cause denitrification. Biological denitrification is the use of denitrifying bacteria, nitrate nitrogen into gaseous products to remove, is considered to be the most economical and effective way of nitrogen removal [1]-[2]. The application of denitrifying bacteria and the removal of nitrate in water have become the research focus[3]-[5], many methods have been reported [6]-[8]. In recent years, some studies on salt tolerant and halophilic denitrifying bacteria have been reported abroad [9]-[10]. In this study, the sludge from the culture pond was taken as the main separation source, and the enrichment, separation and purification were carried out.To obtain a highly efficient nitrate removal ability of denitrifying bacteria, named strain DN20. The aim of this study is to provide effective bacteria source for practical application of nitrate-N treatment in aquaculture water. -
Bacteria and Cyanobacteria
Bacteria and Cyanobacteria Bacteria represent an amazingly diverse group of organisms that are of great ecological, economic, agricultural, and medical importance. Cyanobacteria, also known as blue-green bacteria, contain thylakoid membranes with photosynthetic pigments (chlorophyll a and phycobilins) and are capable to oxygenic photosynthesis. Purple bacteria and green sulfur bacteria occupy habitats in the presence of hydrogen sulfide and oxidize and release sulfur gas rather than oxygen. Nitrogen fixing and denitrifying bacteria have an exceptionally important role in nitrogen cycling in terrestrial plant communities. Many vascular plants such as legumes and an aquatic fern have a symbiotic relationship with nitrogen fixing bacteria. Bacteria are also important carbon recyclers in the environment by assisting in the decomposition of dead organisms. Bacteria are considered Prokaryotes (before the nucleus) and represent a lineage that is ancient and possess a number of novel features. Bacteria generally lack internal compartmentalized organelles that are bound by membranes. Organelles such as Golgi bodies (dictyosomes), chloroplasts, mitochondria, and nuclei are regarded as unique to Eukaryotic (true nucleus) organisms. Recently, evolutionary biologists have determined that two major kingdoms of bacteria are present on the planet. Eubacteria represent the true bacteria and contain many of the groups that we are most familiar with such as cyanobacteria. E. coli, Streptococcus, and Rhizobium. Archaebacteria represent an ancient lineage whose members occupy rather inhospitable habitats such as deep sea thermal vents and miles deep in the Earth=s crust, but are also found in more normal environments. The objective of this lab is to examine the morphology, structure, and ecology of bacteria and cyanobacteria. -
Spatiotemporal Distributions and Environmental Drivers Of
Journal of Oceanology and Limnology Vol. 37 No. 4, P. 1211-1228, 2019 https://doi.org/10.1007/s00343-019-8200-3 Spatiotemporal distributions and environmental drivers of diversity and community structure of nosZ -type denitrifi ers and anammox bacteria in sediments of the Bohai Sea and North Yellow Sea, China* CAI Youjun 1 , ZHANG Xiaoli 2 , LI Guihao 2, 3 , DONG Jun 3, 4 , YANG Anjing 2, 3 , WANG Guangyu 5 , ** , ZHOU Xiaojian 1 , ** 1 College of Environmental Sciences and Engineering, Yangzhou University, Yangzhou 225000, China 2 Key Laboratory of Coastal Environmental Processes and Ecological Remendation, Yantai Institute of Coastal Zone Research, Chinese Academy of Sciences, Yantai 264003, China 3 University of Chinese Academy of Sciences, Beijing 100049, China 4 Shenzhen Lightsun Technology Co. Ltd., Shenzhen 518000, China 5 Department of Bioengineering, School of Marine Science and Technology, Harbin Institute of Technology, Weihai 264209, China Received Jul. 26, 2018; accepted in principle Sep. 5, 2018; accepted for publication Oct. 23, 2018 © Chinese Society for Oceanology and Limnology, Science Press and Springer-Verlag GmbH Germany, part of Springer Nature 2019 Abstract Denitrifi cation and anammox processes are major nitrogen removal processes in coastal ecosystems. However, the spatiotemporal dynamics and driving factors of the diversity and community structure of involved functional bacteria have not been well illustrated in coastal environments, especially in human-dominated ecosystems. In this study, we investigated the distributions of denitrifi ers and anammox bacteria in the eutrophic Bohai Sea and the northern Yellow Sea of China in May and November of 2012 by constructing clone libraries employing nosZ and 16S rRNA gene biomarkers. -
Isolation and Characterization of a Novel Denitrifying Bacterium with High Nitrate Removal: Pseudomonas Stutzeri
Iran. J. Environ. Health. Sci. Eng., 2010, Vol. 7, No. 4, pp. 313-318 ISOLATION AND CHARACTERIZATION OF A NOVEL DENITRIFYING BACTERIUM WITH HIGH NITRATE REMOVAL: PSEUDOMONAS STUTZERI *1A. Rezaee, 2H. Godini, 1S. Dehestani, 1S. Kaviani 1 Department of Environmental Health, Faculty of Medical Sciences, Tarbiat Modares University, Tehran, Iran 2 Department of Environmental Health, School of Public Health, Lorestan University of Medical Sciences, Khoramabbad, Iran Received 16 August 2009; revised 13 Jully 2010; accepted 20 August 2010 ABSTRACT The aim of this study was to isolate and characterize a high efficiency denitrifier bacterium for reducing nitrate in wastewater. Six denitrifier bacteria with nitrate removal activities were isolated from a petrochemical industry effluent with high salinity and high nitrogen concentrations without treatment. The isolated bacteria were tested for nitrate reomoval activity. One of the bacterium displayed the highest reduction of nitrate. The strain was preliminarily identified using biochemical tests and further identified based on similarity of PCR-16S rRNA using universal primers. Biochemical and molecular experiments showed that the best bacterium with high nitrate removal potential was Pseudomonas stutzeri, a member of the α subclass of the class Proteobacteria. The extent of nitrate removal efficiency was 99% at 200 mg/L NO3 and the nitrite content of the effluent was in the prescribed limit. The experiments showed the ability of Pseudomonas stutzeri to rapidly remove nitrate under anoxic conditions. The strain showed to be potentially good candidate for biodenitrification of high nitrate solutions. Key words: Pseudomonas stutzeri; Denitrification; Polymerase Chain Reaction, Isolation; Characterization INTRODUCTION Biological denitrification is a process carried to respire anaerobically using nitrogen oxides as out by numerous genera of bacteria. -
Enrichment of Denitrifying Bacterial Community Using Nitrite As an Electron Acceptor for Nitrogen Removal from Wastewater
water Article Enrichment of Denitrifying Bacterial Community Using Nitrite as an Electron Acceptor for Nitrogen Removal from Wastewater Renda Yao, Quan Yuan and Kaijun Wang * State Key Joint Laboratory of Environment Simulation and Pollution Control, School of Environment, Tsinghua University, Beijing 100084, China; [email protected] (R.Y.); [email protected] (Q.Y.) * Correspondence: [email protected]; Tel.: +86-10-6278-9411 Received: 31 October 2019; Accepted: 17 December 2019; Published: 20 December 2019 Abstract: This work aimed to enrich a denitrifying bacterial community for economical denitrification via nitrite to provide the basic objects for enhancing nitrogen removal from wastewater. A sequencing batch reactor (SBR) with continuous nitrite and acetate feeding was operated by reasonably adjusting the supply rate based on the reaction rate, and at a temperature of 20 2 C, pH of 7.5 0.2, ± ◦ ± and dissolved oxygen (DO) of 0 mg/L. The results revealed that the expected nitrite concentration can be achieved during the whole anoxic reaction period. The nitrite denitrification rate of nitrogen removal from synthetic wastewater gradually increased from approximately 10 mg/(L h) to 275.35 mg/(L h) over 12 days (the specific rate increased from 3.83 mg/(g h) to 51.80 mg/(g h)). Correspondingly, the chemical oxygen demand/nitrogen (COD/N) ratio of reaction decreased from 7.9 to 2.7. Both nitrite and nitrate can be used as electron acceptors for denitrification. The mechanism of this operational mode was determined via material balance analysis of substrates in a typical cycle. High-throughput sequencing showed that the main bacterial community was related to denitrification, which accounted for 84.26% in the cultivated sludge, and was significantly higher than the 2.16% in the seed sludge. -
Influence of Denitrification in Aquatic Sediments on the Nitrogen Content of Natural Waters J
6 / c__ Influence of denitrification in aquatic sediments on the nitrogen content of natural waters J. F. van Kessel Influence of denitrification in aquatic sedimentso n the nitrogen content of naturalwater s Proefschrift ter verkrijging van degraa d van doctor in de landbouwwetenschappen, op gezagva n derecto r magnificus, dr. ir. J. P.H .va n derWant , hoogleraar in devirologie , in het openbaar te verdedigen opvrijda g 8oktobe r 1976 desnamiddag s te vier uur in de aula van de Landbouwhogeschool te Wageningen Centrefor Agriculture Publishingand Documentation Wageningen —1976 Abstract Kessel, J. F. van (1976) Influence of denitrification in aquatic sediments on the nitrogen content of natural waters. Agric. Res. Rep. (Versl. landbouwk. Onderz.) 858. Pudoc, Wageningen. ISBN 90 220062 04 . (vi)+ 5 2 p.: 12figs ; 14 tables;Eng .an d Dutch summaries. Forms part of a doctoral thesis, Wageningen ((vii) + 104 p., 43 figs, 28 tables). Other parts are published in Water Research,bu t are summarized in the Agric.Res .Rep . A study was made of microbiological processes, particularly denitrification, leading to the elimi nation of nitrogen from natural waters. As denitrification is an anaerobic process and natural waters mostly contain dissolved oxygen, this process was suggested to proceed in the anaerobic sediment at the bottom of natural waters. Two widely differing types of aquatic sediments were tested in the laboratory for effects of temperature, oxygen and nitrate in the overlying water, and thickness of the sediment layer on the rate of denitrification. During disappearance of nitrate from the overlying water, by far most of thenitrat e was converted to molecular nitrogen by denitrification and only a small part of the nitrate was utilized for cell synthesis (immobilization). -
Microbial Function on Climate Change Addis Ababa, Ethiopia – a Review Received: 14 March, 2018 Accepted: 28 April, 2018 Published: 30 April, 2018
vv ISSN: 2690-0777 DOI: https://dx.doi.org/10.17352/ojeb LIFE SCIENCES GROUP Endeshaw Abatenh*, Birhanu Gizaw, Zerihun Tsegaye and Genene Tefera Review Article Endeshaw Abatenh, Ethiopia Biodiversity Institute, Department of Microbiology, Comoros Street, 0000, Microbial Function on Climate Change Addis Ababa, Ethiopia – A Review Received: 14 March, 2018 Accepted: 28 April, 2018 Published: 30 April, 2018 *Corresponding author: Endeshaw Abatenh, Ethiopia Abstract Biodiversity Institute, Department of Microbiology, Comoros Street, 0000, Addis Ababa, Ethiopia, Greenhouse gases concentration is increased through time within different human and natural E-mail: [email protected] factors. Such as combustion of coal, oil and other fossil fuels, decay of plant matter and biomass burning. Now a day’s climate change and global warming is the major problem in the world. It is damage Keywords: Green House Gases (GHGs); Climate (destroy) a number of biotic componets. It have also effect on microbial comunity stracture, function change; Microbial comunity; Biogeochemical cycle; and their metablolic activity. In order to fi ght (compromize) climate change using a number of methods Methanotropic. are listed here. For example, microorganisms and other biological componets have many potential role https://www.peertechz.com for mitigation by contribute forward response. Microorganisms have a wide function especialy used in greenhouse gas treatment and reduction through nutrient recycling processes. It act as either generators or users of these gases in a good manner. It provide to reduce environment hazards which is caused by nature and antropogenic activity. In overall biogeochemical cycles and climate changes are never see separately. Introduction of a certain region, including temperature, rainfall, and wind. -
16S Rrna and Hydrazine Gene-Based Profiling of the Candidatus Scalindua Community from the Arabian Sea Hypoxic Sediments
RESEARCH ARTICLES 16S rRNA and hydrazine gene-based profiling of the Candidatus Scalindua community from the Arabian Sea hypoxic sediments Jovitha Lincy* and Cathrine Sumathi Manohar Biological Oceanography Division, CSIR-National Institute of Oceanography, Goa 403 004, India and Academy of Scientific and Innovative Research, Ghaziabad 201 002 India The nitrogen loss contribution of anammox to the total Anammox bacterial diversity and abundance were denitrification in marine sediments can range from near studied from the organic-rich hypoxic sediments of 7 the Arabian Sea utilizing the partial 16S rRNA, and 0% to 80%, especially in deposits underlying ODZ . In hydrazine synthase, hzsA and hydrazine oxidoreduc- the southeastern Arabian Sea, benthic nitrogen metabo- 8 tase, hzo genes. Among all the clades obtained, phylo- lism is driven by sinking organic matter which is excep- typic diversity was high within the Candidatus genus tionally high during the southwest monsoon period9. The Scalindua with an abundance of ≤7 × 104 copies/g dry prevailing conditions are assumed to favour heterotrophic wt. As such, Scalindua is known to play a significant denitrifying communities that rely on organic sources10. role in fixed nitrogen removal through anaerobic Hence the possible occurrence of a chemolithoautotroph ammonium oxidation (anammox) pathway. From these like anammox microbes is not studied thoroughly. Be- analyses, it is inferred that searching for hzo gene sides ammonium ion available in situ11, dissimilatory yields robust evidence for detecting anammox com- nitrate reduction to ammonia (DNRA) is reported1. In the munity than the widely used 16S rRNA gene marker. Oman coast of the Arabian Sea, a coupling of DNRA to anammox resulted in intense nitrogen loss12, suggesting Keywords: Anammox, community gene-based profil- that anammox occurrence is controlled by the availability ing, hydrazine, hypoxic sediments, Scalindua. -
Neoproterozoic Iron Formation: an Evaluation of Its Temporal, Environmental and Tectonic Significance
ÔØ ÅÒÙ×Ö ÔØ Neoproterozoic Iron Formation: An evaluation of its temporal, environmental and tectonic significance Grant M. Cox, Galen P. Halverson, William G. Minarik, Daniel P. Le Heron, Francis A. Macdonald, Eric J. Bellefroid, Justin V. Strauss PII: S0009-2541(13)00349-5 DOI: doi: 10.1016/j.chemgeo.2013.08.002 Reference: CHEMGE 16961 To appear in: Chemical Geology Received date: 2 November 2012 Revised date: 29 July 2013 Accepted date: 5 August 2013 Please cite this article as: Cox, Grant M., Halverson, Galen P., Minarik, William G., Le Heron, Daniel P., Macdonald, Francis A., Bellefroid, Eric J., Strauss, Justin V., Neo- proterozoic Iron Formation: An evaluation of its temporal, environmental and tectonic significance, Chemical Geology (2013), doi: 10.1016/j.chemgeo.2013.08.002 This is a PDF file of an unedited manuscript that has been accepted for publication. As a service to our customers we are providing this early version of the manuscript. The manuscript will undergo copyediting, typesetting, and review of the resulting proof before it is published in its final form. Please note that during the production process errors may be discovered which could affect the content, and all legal disclaimers that apply to the journal pertain. ACCEPTED MANUSCRIPT Neoproterozoic Iron Formation: An evaluation of its temporal, environmental and tectonic significance Grant M. Cox 1* , Galen P. Halverson 1, William G. Minarik 1, Daniel P. Le Heron 2, Francis A. Macdonald 3, Eric J. Bellefroid 1, Justin V. Strauss 3 *Corresponding author 1-McGill University, Montreal, Quebec, Canada 2-Royal Holloway, University of London, United Kingdom 3-Harvard University, Massachusetts, U.S.A. -
1 Single Cell Genomic and Transcriptomic Evidence for the Use of Alternative Nitrogen
1 Single cell genomic and transcriptomic evidence for the use of alternative nitrogen 2 substrates by anammox bacteria 3 4 Contributors: Sangita Ganesh1,2*, Anthony D. Bertagnolli1*, Laura A. Bristow3, Cory C. 5 Padilla1, Nigel Blackwood4, Montserrat Aldunate5,6, Annie Bourbonnais7,8, Mark A. Altabet8, 6 Rex R. Malmstrom9, Tanja Woyke9, Osvaldo Ulloa6, Konstantinos T. Konstantinidis10, Bo 7 Thamdrup11, Frank J. Stewart1# 8 9 Affiliations and footnotes: 10 11 * These authors contributed equally to this work. 12 # Corresponding author. Mailing address: School of Biological Sciences, Georgia Institute of 13 Technology, Ford ES&T Building, Rm 1242, 311 Ferst Drive, Atlanta GA 30332 14 Email: [email protected] 15 16 1 School of Biological Sciences, Georgia Institute of Technology, Atlanta GA, USA, 30332 17 2 Radiant Genomics, Emeryville CA, USA, 94608 18 3 Biogeochemistry Group, Max Planck Institute for Marine Microbiology, Bremen, Germany 19 4 Department of Biology, University of Pennsylvania, Philadelphia PA, USA, 19104 20 5 Graduate Program in Oceanography, Department of Oceanography, Faculty of Natural Sciences 21 and Oceanography, University of Concepción, Casilla 160-C, Concepción, Chile 22 6 Departamento de Oceanografía, Universidad de Concepción, Casilla 160-C, 4070386, 23 Concepción, Chile 24 7 Marine Chemistry & Geochemistry, Woods Hole Oceanographic Institution, 266 Woods Hole 25 Road, Woods Hole MA, USA, 02543 26 8 School for Marine Science and Technology, University of Massachusetts Dartmouth, 706 27 Rodney French -
The Interplay of Microbially Mediated and Abiotic Reactions in the Biogeochemical Fe Cycle
REVIEWS The interplay of microbially mediated and abiotic reactions in the biogeochemical Fe cycle Emily D. Melton, Elizabeth D. Swanner, Sebastian Behrens, Caroline Schmidt and Andreas Kappler Abstract | Many iron (Fe) redox processes that were previously assumed to be purely abiotic, such as photochemical Fe reactions, are now known to also be microbially mediated. Owing to this overlap, discerning whether biotic or abiotic processes control Fe redox chemistry is a major challenge for geomicrobiologists and biogeochemists alike. Therefore, to understand the network of reactions within the biogeochemical Fe cycle, it is necessary to determine which abiotic or microbially mediated reactions are dominant under various environmental conditions. In this Review, we discuss the major microbially mediated and abiotic reactions in the biogeochemical Fe cycle and provide an integrated overview of biotic and chemically mediated redox transformations. Fe speciation The environmental abundance of iron (Fe) and its pos‑ and temporal distribution of Fe redox species in some Refers to the redox state of session of electrons in d orbitals with π‑character, which environments, such as heterogeneous sediments, plant iron (Fe) and the identity of its can form complexes with carbon (C), oxygen (O), nitro‑ rhizospheres and microbial mats6, and abiotic Fe trans‑ ligands. The two most common gen (N) and sulphur (S) species, make it an essential ele‑ formations with biologically produced intermediates environmental Fe redox ment for nearly all living organisms. Fe occurs in two must be taken into account7,8. species are Fe(II) and Fe(III). main redox states in the environment: oxidized ferric Fe Despite our growing knowledge of the wide‑ (Fe(iii)), which is poorly soluble at circumneutral pH; spread environmental occurrence and the importance and reduced ferrous Fe (Fe(ii)), which is easily soluble of microbial Fe redox cycling for the degradation and and therefore more bioavailable.