Effects of Four Aromatic Organic Pollutants on Microbial Glucose Metabolism and Thymidine Incorporation in Marine Sedimentst JAMES E

Total Page:16

File Type:pdf, Size:1020Kb

Effects of Four Aromatic Organic Pollutants on Microbial Glucose Metabolism and Thymidine Incorporation in Marine Sedimentst JAMES E APPLIED AND ENVIRONMENTAL MICROBIOLOGY, Apr. 1985, p. 828-835 Vol. 49, No. 4 0099-2240/85/040828-08$02.OO/0 Copyright C 1985, American Society for Microbiology Effects of Four Aromatic Organic Pollutants on Microbial Glucose Metabolism and Thymidine Incorporation in Marine Sedimentst JAMES E. BAUER AND DOUGLAS G. CAPONE* Marine Sciences Research Center, State University of New York, Stony Brook, New York 11794 Received 18 October 1984/Accepted 21 January 1985 The metabolism of D-[U-14C]glucose and the incorporation of [methyl-3H]thymidine by aerobic and anaerobic marine sediment microbes exposed to 1 to 1,000 ppm anthracene, naphthalene, p,p'-dichlorodiphenyltri- chloroethane, and pentachlorophenol were examined. Cell-specific rates of [14C]glucose metabolism averaged 1.7 x 10-21 and 0.5 x 10-21 mol/min per cell for aerobic and anaerobic sediment slurries, respectively; [3Hlthymidine incorporation rates averaged 43 x 10-24 and 9 x 10-24 mol/min per cell for aerobic and anaerobic slurries, respectively. Aerobic sediments exposed to three of the organic pollutants for 2 to 7 days showed recovery of both activities. Anaerobic sediments showed little recovery after 2 days of pre-exposure to the pollutants. We conclude that (i) anaerobic sediments are more sensitive than aerobic sediments to pollutant additions; (ii) [3HJthymidine incorporation is more sensitive to pollutant additions than is [14C]glucose metabolism; and (iii) the toxicity of the pollutants increased in the following order: anthracene, p,p'- dichlorodiphenyltrichloroethane, naphthalene, and pentachlorophenol. Coastal marine sediments, which are sites of intensive and Sediments for aerobic studies were obtained by scraping important microbial activities (8), accumulate organic pollut- the top 0 to 2 mm of sediment with a sterile spatula and ants (2, 4, 16). The effects of organic pollutants on the placing the sample in a sterile glass beaker. Sediment for sediment biota, although possibly substantial, generally have anaerobic studies was collected from depths of 5 to 10 cm not been considered. Several studies have examined the and maintained anoxically until return to the Marine Sci- acute and chronic effects of complex organic mixtures such ences Research Center, within 1 h from the time of collec- as fuel oils (10, 11, 14) on organic carbon metabolism by tion. Flax Pond seawater, with a salinity of about 28 parts sedimentary microorganisms. A few studies have considered per thousand, was obtained from Flax Pond laboratory the alteration of activities in marine sediments as a result of where it had undergone coarse (10 ,um) filtration through individual pollutants (5, 18; J. Slater and D. G. Capone, in I. nylon cartridge filters. Duedall, ed., Wastes in the Ocean, vol. 9: Proceedings of Sediment subsamples were diluted 1:100 (volume the Fourth Ocean Disposal Symposium, in press). sediment:volume seawater) in filtered seawater (0.45-R,m, In the present investigation, we assessed the effects of type GA-6; Gelman Sciences, Inc., Ann Arbor, Mich.) and four aromatic organic pollutants, anthracene, naphthalene, kept well mixed on a magnetic stirrer while slurry was p,p'-dichlorodiphenyltrichloroethane (DDT), and pentachlo- dispensed. For anoxic sediments, all diluent seawater was rophenol (PCP), on two microbial activities common to both purged of oxygen by bubbling with nitrogen gas for at least oxic and anoxic coastal marine sediments. Anthracene and 30 min before dilution. All vessels containing anoxic slurries naphthalene are polycyclic aromatic hydrocarbons, whereas were immediately stoppered (butyl rubber stoppers; Thomas DDT and PCP are representative chlorinated aromatic pol- Scientific Co., Philadelphia, Pa.) after they were dispensed, lutants. The activities chosen for study were D-[U- and the headspace was purged with nitrogen gas for 1 min. 14C]glucose metabolism and [methyl-3H]thymidine ([3H]TdR) All experimental slurries were maintained at 25°C in the dark incorporation. The study allows comparison of the sensitiv- in temperature-controlled water baths with rotary shaking to ity of [3H]TdR incorporation relative to [14C]glucose metab- ensure rapid equilibration between the gas and liquid phases olism in toxicity studies involving sedimentary systems, and dispersal of pollutants. comparison of the sensitivity of aerobic and anaerobic Pollutant effects studies. The effects of anthracene, naph- marine sediments to pollutants, and assessment of the rela- thalene (Eastman Kodak Co., Rochester, N.Y.), DDT tive toxicity of the four pollutant compounds tested. (R.F.R. Corp., Hope, R.I.), and PCP (Aldrich Chemical Co., Milwaukee, Wis.) on D-[U-_4C]glucose metabolism and MATERIALS AND METHODS [3H]TdR incorporation were examined in short-term acute Sampling and sample preparation. Sediments for all labo- and longer term experiments. All comparisons of rates of ratory studies were obtained from an intertidal mudflat of activities among treatments were analyzed by single classi- Flax Pond Saltmarsh, Old Field, N.Y. The mud consisted of fication analysis of variance (23). Significance levels were set a fine organic-mineral mixture (3 to 7% loss on ignition) at the at P < 0.05 for all analyses. sediment-water interface which became more mineral-rich at In acute pollutant effects 5 ml depths of 5 to 10 cm. The depth of the oxidized surface layer studies, of diluted sediment varied seasonally from approximately 1 to 3 mm in summer slurry was transferred from batch preparations to 20 ml of to as much as 3 cm in winter. acid-washed borosilicate scintillation vials (Wheaton Indus- tries, Millville, N. J.). Controls received 5 Rl of pure acetone carrier. It was found in preliminary experiments that this volume of acetone did not alter significantly either [3H]TdR * Corresponding author. incorporation or [14C]glucose metabolism compared with t Contribution no. 467 of the Marine Sciences Research Center. samples that received no acetone. Pollutants were added to 828 VOL. 49, 1985 ORGANIC POLLUTANT EFFECTS ON SEDIMENTARY MICROBIOTA 829 treatment slurries in 5-,l acetone solutions; final concentra- filters with their light coating of collected sediment were tions ranged from 1 to 1,000 ppm (micrograms of pollutant removed and placed in 20-ml scintillation vials. Ethyl acetate per milliliter of slurry). Samples were shaken continuously (1 ml) was added to dissolve the filters, after which Protosol and incubated for 1 to 2 h before activity assays were tissue digester (1 ml; New England Nuclear Corp., Boston, performed. In addition, subsamples were taken for the Mass.) was also added. Vials were then capped, and diges- estimation of total bacterial numbers (20) and determination tion proceeded overnight at 25 to 30°C. The next day, 10 ml of cell-specific activity rates. of Econofluor scintillation cocktail (New England Nuclear) The effects of longer term exposures of the four pollutants was added to each vial. Samples were thoroughly shaken, on oxic ["'Ciglucose assimilation were assessed by preparing and the light floc was allowed to settle. large batch slurries (ca. 600 ml) of diluted sediment and The radioactivity in each sample was quantified by count- dispensing 100 ml into 125- or 250-ml Erlenmeyer flasks. ing in a Packard Tri-Carb scintillation counter. Quench Individual flasks then received 100 ,ul of acetone or organic curves were constructed by the external standards method. stock solutions containing one of the four pollutants (100 Counting efficiency was relatively low (8 to 10%) in these ppm final concentration). Triplicate subsamples were taken samples because of color quenching which could not be from each flask and assayed for ["'C]glucose metabolism in removed by 10% benzoyl peroxide oxidation. scintillation vials at selected intervals over a 7-day period. To ensure that all single time point measurements of Single flasks were deemed suitable for each experimental [3H]TdR incorporation were representative of linear uptake level on the basis of preliminary results, from which no kinetics, periodic time series of incorporation were per- significant differences among subsamples from replicate formed. Both oxic and anoxic incorporation were linear for flasks (receiving no treatment) with respect to total at least 60 min (data not shown). Generally, oxic experi- ["'C]glucose metabolism or percent respired to 1'CO2 or ments were conducted for 30 to 45 min, whereas anoxic [3H]TdR incorporation were found. experiments never exceeded 60 min. To investigate possible acclimation of microbial popula- ["'C]glucose metabolism assays. The format for assaying tions to pollutants through previous exposure, as well as the the metabolism of [14C]glucose was similar to that described effects of additional inputs on activities, 100-ml batch slur- above for the [3H]TdR assays. An autoclaved filtered seawa- ries were prepared as described above and dosed with 1 to ter solution (10 ,ul) of 5 ,uCi of (18.0 mCi mmoI-1) D-[U- 1,000 ppm of the pollutants or acetone. After 2 days, 14C]glucose (New England Nuclear) per ml was added to triplicate 5-ml subsamples of both control and pretreated each 5-ml sediment slurry subsample through the stopper batches were dispensed into scintillation vials. Initial con- with a microliter syringe. The final amount of glucose to be trols then received either S RI of acetone (control) or organic added was determined by a preliminary study which as- pollutant stock to the same level as the parallel pretreated sessed the kinetics of uptake, as suggested by Griffiths et al. samples (dosed, no pretreatment). Pretreated batch (13). Glucose uptake appeared to be saturated at glucose subsamples received either 5 1±l of acetone (pretreatment concentrations of about 100 pug/liter of slurry, and this control) or an additional quantity of organic pollutant iden- concentration was used in all subsequent incubations. In tical to the pretreatment concentration (pretreatment plus preliminary experiments, uptake of [14C]glucose (100 pig/liter retreatment). of slurry) by oxic sediment slurries (5 ml) remained linear for [3HJTdR incorporation. The incorporation of [3H]TdR to at least 60 min.
Recommended publications
  • Stabilization and Destabilization of Soil Organic Matter: Mechanisms and Controls
    13F7H GEODERLIA ELSEVIER Geoderma 74 (1996) 65-105 • Stabilization and destabilization of soil organic matter: mechanisms and controls Phillip Sollins, Peter Homann, Bruce A. Caldwell Department of Forest Science Oregon State University Corvallis, OR 97331, USA Receed 1 December 1993; revised 26 July 1995; accepted 3 April 1996 Abstract We present a conceptual model of the processes by which plant leaf and root litter is transformed to soil organic C and CO 2. Stabilization of a portion of the litter C yields material that resists further transformation; destabilization yields material that is more susceptible to microbial respiration. Stability of the organic C is viewed as resulting from three general sets of characteristics. Recalcitrance comprises, molecular-level characteristics of organic substances, including elemental composition, presence of functional groups, and molecular conformation, that influence their degradation by microbes and enzymes. Interactions refers to the inter-molecular interactions between organics and either inorganic substances or other organic substances that alter the rate of degradation of those organics or synthesis of new organics. Accessibility refers to the location of organic substances with respect to microbes and enzymes. Mechanisms by which these three characteristics change through time are reviewed along with controls on those mechanisms. This review suggests that the following changes in the study of soil organic matter dynamics would speed progress: (1) increased effort to incorporate results
    [Show full text]
  • Tracking Hidden Organic Carbon in Rocks Using Chemometrics And
    www.nature.com/scientificreports OPEN Tracking hidden organic carbon in rocks using chemometrics and hyperspectral imaging Received: 4 October 2017 Céline Pisapia 1,2, Frédéric Jamme2, Ludovic Duponchel3 & Bénédicte Ménez1 Accepted: 25 January 2018 Finding traces of life or organic components of prebiotic interest in the rock record is an appealing goal Published: xx xx xxxx for numerous felds in Earth and space sciences. However, this is often hampered by the scarceness and highly heterogeneous distribution of organic compounds within rocks. We assess here an innovative analytical strategy combining Synchrotron radiation-based Fourier-Transform Infrared microspectroscopy (S-FTIR) and multivariate analysis techniques to track and characterize organic compounds at the pore level in complex oceanic rocks. S-FTIR hyperspectral images are analysed individually or as multiple image combinations (multiset analysis) using Principal Component Analyses (PCA) and Multivariate Curve Resolution – Alternating Least Squares (MCR-ALS). This approach allows extracting simultaneously pure organic and mineral spectral signatures and determining their spatial distributions and relationships. MCR-ALS analysis provides resolved S-FTIR signatures of 8 pure mineral and organic components showing the close association at a micrometric scale of organic compounds and secondary clays formed during rock alteration and known to catalyse organic synthesis. These results highlights the potential of the serpentinizing oceanic lithosphere to generate and preserve organic compounds of abiotic origin, in favour of the hydrothermal theory for the origin of life. Spectroscopic techniques and especially Synchrotron-based Fourier-Transform Infrared microspectroscopy (S-FTIR) have been used in geosciences for decades1–3. S-FTIR has notably been proven efcient for determining at the micrometer scale the mineral, fuid and organic phases contained in interplanetary dust particles, meteor- ites and terrestrial material4–10.
    [Show full text]
  • Carbon Mineral Ecology: Predicting the Undiscovered Minerals of Carbon
    American Mineralogist, Volume 101, pages 889–906, 2016 Carbon mineral ecology: Predicting the undiscovered minerals of carbon ROBERT M. HAZEN1,*, DANIEL R. HUMMER1, GRETHE HYSTAD2, ROBERT T. DOWNS3, AND JOSHUA J. GOLDEN3 1Geophysical Laboratory, Carnegie Institution, 5251 Broad Branch Road NW, Washington, D.C. 20015, U.S.A. 2Department of Mathematics, Computer Science, and Statistics, Purdue University Calumet, Hammond, Indiana 46323, U.S.A. 3Department of Geosciences, University of Arizona, 1040 East 4th Street, Tucson, Arizona 85721-0077, U.S.A. ABSTRACT Studies in mineral ecology exploit mineralogical databases to document diversity-distribution rela- tionships of minerals—relationships that are integral to characterizing “Earth-like” planets. As carbon is the most crucial element to life on Earth, as well as one of the defining constituents of a planet’s near-surface mineralogy, we focus here on the diversity and distribution of carbon-bearing minerals. We applied a Large Number of Rare Events (LNRE) model to the 403 known minerals of carbon, using 82 922 mineral species/locality data tabulated in http://mindat.org (as of 1 January 2015). We find that all carbon-bearing minerals, as well as subsets containing C with O, H, Ca, or Na, conform to LNRE distributions. Our model predicts that at least 548 C minerals exist on Earth today, indicating that at least 145 carbon-bearing mineral species have yet to be discovered. Furthermore, by analyzing subsets of the most common additional elements in carbon-bearing minerals (i.e., 378 C + O species; 282 C + H species; 133 C + Ca species; and 100 C + Na species), we predict that approximately 129 of these missing carbon minerals contain oxygen, 118 contain hydrogen, 52 contain calcium, and more than 60 contain sodium.
    [Show full text]
  • 7 30(1) 0007 Włodarczyk-Makuła
    CIVIL AND ENVIRONMENTAL ENGINEERING REPORTS E-ISSN 2450-8594 CEER 2020; 30 (1): 074-086 DOI: 10.2478/ceer-2020-0007 Original Research Article CHARACTERISTICS OF PETROLEUM COMPOUNDS AND THEIR REMOVAL FROM THE AQUATIC ENVIRONMENT Maria WŁODARCZYK – MAKUŁA 1 Czestochowa University of Technology, Department of Environmental Engineering Czestochowa, Poland A b s t r a c t The aim of the study was to characterize the components of crude oil, with particular emphasis on those that have a toxic effect on organisms, and to describe the sources of pollution and the methodology for determining these compounds in aqueous solutions. In addition, the study presents the legal provisions in the field of petroleum compounds and practical methods for their removal in the event of uncontrolled emission of these compounds into the aquatic environment as well as methods used in the treatment of wastewater loaded with these compounds. Keywords: water, wastewater, surface water, soil petroleum compounds, BTX, PAH 1. INTRODUCTION Crude oil, both unprocessed and its products, pose a serious threat in the event of uncontrolled emissions to the aquatic and ground environment. This threat results from the possibility of migration of these compounds, relative stability and bioaccumulation in organisms inhabiting the aquatic or ground environment [1,2]. The crude oil includes paraffin (alkanes), naphthenic (cycloalkanes) and aromatic hydrocarbons, including polycyclic. The crude oil also contains elements such as sulphur, oxygen, nitrogen, iron, silicon, vanadium, sodium and 1 Corresponding author : Czestochowa University of Technology, 42 – 200 Czestochowa, 69 Dabrowskiego Str., +48 3250919, email: [email protected] CHARACTERISTICS OF PETROLRUM COMPOUNDS AND THEIR REMOVAL 75 FROM THE AQUATIC ENVIRONMENT nickel as well as organometallic and mineral compounds [2].
    [Show full text]
  • Nanostructural Origin of Blue Fluorescence in the Mineral Karpatite
    Potticary, J. , Jensen, T. T., & Hall, S. R. (2017). Nanostructural origin of blue fluorescence in the mineral karpatite. Scientific Reports, 7(1), [9867]. https://doi.org/10.1038/s41598-017-10261-w Publisher's PDF, also known as Version of record License (if available): CC BY Link to published version (if available): 10.1038/s41598-017-10261-w Link to publication record in Explore Bristol Research PDF-document This is the final published version of the article (version of record). It first appeared online via Nature at https://www.nature.com/articles/s41598-017-10261-w. Please refer to any applicable terms of use of the publisher. University of Bristol - Explore Bristol Research General rights This document is made available in accordance with publisher policies. Please cite only the published version using the reference above. Full terms of use are available: http://www.bristol.ac.uk/red/research-policy/pure/user-guides/ebr-terms/ www.nature.com/scientificreports OPEN Nanostructural origin of blue fuorescence in the mineral karpatite Received: 9 June 2017 Jason Potticary 1,2, Torsten T. Jensen 1,3 & Simon R. Hall1 Accepted: 7 August 2017 The colour of crystals is a function of their atomic structure. In the case of organic crystals, it is the Published: xx xx xxxx spatial relationships between molecules that determine the colour, so the same molecules in the same arrangement should produce crystals of the same colour, regardless of whether they arise geologically or synthetically. There is a naturally-occurring organic crystal known as karpatite which is prized for its beautiful blue fuorescence under ultra-violet illumination.
    [Show full text]
  • Deep Carbon Through Deep Time Data-Driven Insights Robert M
    20 Deep Carbon through Deep Time Data-Driven Insights robert m. hazen, yana bromberg, robert t. downs, ahmed eleish, paul g. falkowski, peter fox, donato giovannelli, daniel r. hummer, grethe hystad, joshua j. golden, andrew h. knoll, congrui li, chao liu, eli k. moore, shaunna m. morrison, a.d. muscente, anirudh prabhu, jolyon ralph, michelle y. rucker, simone e. runyon, lisa a. warden, and hao zhong 20.1 Introduction: Data and the Deep Carbon Observatory For most of the history of science, data-driven discovery has been difficult and time- consuming: a lifetime of meticulous data collection and thoughtful synthesis was required to recognize previously hidden, higher-dimensional trends in multivariate data. Recognition of processes such as biological evolution by natural selection (1,2), continental evolution by plate tectonics (3,4), atmospheric and ocean oxygenation by photosynthesis (5,6), and climate change (7,8) required decades of integrated data synthesis preceding the discovery and acceptance of critical Earth phenomena. How- ever, we stand at the precipice of a unique opportunity: to dramatically accelerate scientific discovery by coupling hard-won data resources with advanced analytical and visualization techniques (9,10). Today, Earth and life sciences are generating a multi- tude of data resources in numerous subdisciplines. Integration and synthesis of these diverse data resources will lead to an abductive, data-driven approach to investigating Earth’s mineralogical and geochemical history, as well as the coevolution of the geosphere and biosphere (11–13). In this chapter, we examine applications of data science in deep carbon research through three “use cases.” The first example focuses on geochemical and mineralogical anomalies from a period in Earth history (~1.3 to 0.9 Ga) when the supercontinent Rodinia was being assembled from previously scattered continental blocks.
    [Show full text]
  • The Impact of Drying on Structure of Sedimentary Organic Matter in Wetlands: Probing with Native and Amended Polycyclic
    See discussions, stats, and author profiles for this publication at: https://www.researchgate.net/publication/303849557 The impact of drying on structure of sedimentary organic matter in wetlands: Probing with native and amended polycyclic... Article in Science of The Total Environment · October 2016 DOI: 10.1016/j.scitotenv.2016.05.184 CITATIONS READS 2 29 5 authors, including: Zucheng Wang Zhanfei Liu Northeast Normal University University of Texas at Austin 10 PUBLICATIONS 155 CITATIONS 66 PUBLICATIONS 1,103 CITATIONS SEE PROFILE SEE PROFILE Some of the authors of this publication are also working on these related projects: PROOF-PECHE View project All content following this page was uploaded by Zhanfei Liu on 08 November 2016. The user has requested enhancement of the downloaded file. Science of the Total Environment 568 (2016) 42–51 Contents lists available at ScienceDirect Science of the Total Environment journal homepage: www.elsevier.com/locate/scitotenv The impact of drying on structure of sedimentary organic matter in wetlands: Probing with native and amended polycyclic aromatic hydrocarbons Zucheng Wang a,b,c, Zhanfei Liu a,⁎,MinLiub,KehuiXud,e, Lawrence M. Mayer f a Marine Science Institute, The University of Texas at Austin, Port Aransas, TX 78373, USA b Department of Geography, Key Laboratory of Geographic Information Science of the Ministry of Education, East China Normal University, Shanghai, China c Institute for Peat and Mire, Northeast Normal University, Changchun, China d Department of Oceanography and Coastal Sciences, Louisiana State University, Baton Rouge, LA 70803, USA e Coastal Studies Institute, Louisiana State University, Baton Rouge, LA 70803, USA f Darling Marine Center, University of Maine, Walpole, ME 04573, USA HIGHLIGHTS GRAPHICAL ABSTRACT • Native PAHs were released into solution after sediments suffering dry-wet cycles.
    [Show full text]
  • Interaction of Natural Organic Matter with Layered Minerals: Recent Developments in Computational Methods at the Nanoscale
    Minerals 2014, 4, 519-540; doi:10.3390/min4020519 OPEN ACCESS minerals ISSN 2075-163X www.mdpi.com/journal/minerals Review Interaction of Natural Organic Matter with Layered Minerals: Recent Developments in Computational Methods at the Nanoscale Jeffery A. Greathouse 1,*, Karen L. Johnson 2 and H. Christopher Greenwell 3 1 Geochemistry Department, Sandia National Laboratories, P.O. Box 0754, Albuquerque, NM 87185-0754, USA 2 School of Engineering and Computing Sciences, Durham University, South Road, Durham DH1 3LE, UK; E-Mail: [email protected] 3 Department of Earth Sciences, Durham University, South Road, Durham DH1 3LE, UK; E-Mail: [email protected] * Author to whom correspondence should be addressed; E-Mail: [email protected]; Tel.: +1-505-284-4895; Fax: +1-505-844-7354. Received: 5 March 2014; in revised form: 3 May 2014 / Accepted: 14 May 2014 / Published: 6 June 2014 Abstract: The role of mineral surfaces in the adsorption, transport, formation, and degradation of natural organic matter (NOM) in the biosphere remains an active research area owing to the difficulties in identifying proper working models of both NOM and mineral phases present in the environment. The variety of aqueous chemistries encountered in the subsurface (e.g., oxic vs. anoxic, variable pH) further complicate this field of study. Recently, the advent of nanoscale probes such as X-ray adsorption spectroscopy and surface vibrational spectroscopy applied to study such complicated interfacial systems have enabled new insight into NOM-mineral interfaces. Additionally, due to increasing capabilities in computational chemistry, it is now possible to simulate molecular processes of NOM at multiple scales, from quantum methods for electron transfer to classical methods for folding and adsorption of macroparticles.
    [Show full text]
  • The Composition and Stability of Clay-Associated Organic Matter Along a Soil Profile
    Article The Composition and Stability of Clay-Associated Organic Matter along a Soil Profile Chunmei Chen 1,*, Peter Leinweber 2, Kai-Uwe Eckhardt 2 and Donald L. Sparks 1 1 Delaware Environmental Institute, Department of Plant and Soil Science, University of Delaware, Newark, DE 19716, USA; [email protected] 2 Soil Science, University of Rostock, Justus-von-Liebig-Weg 6, 18051 Rostock, Germany; [email protected] (P.L.); [email protected] (K.-U.E.) * Correspondence: [email protected]; Tel.: +1-302-983-3299 Received: 19 February 2018; Accepted: 13 March 2018; Published: 14 March 2018 Abstract: Organic carbon in subsoil generally has longer turnover times than that in surface soil, but little is known about how the stability of the specific organic compound classes changes with soil depth. The objective of this study was to analyze the composition and thermal stability of clay-associated organic matter (OM) at varying soil depths in the summit and footslope of a pasture hillslope using C X-ray absorption near edge structure (XANES) and pyrolysis-field ionization mass spectrometry (Py-FIMS). C XANES showed aromatic C was relatively enriched in the subsoil, relative to the surface soil. Py-FIMS demonstrated a relative enrichment of phenols/lignin monomers and alkylaromatics with increasing profile depth in the summit soil, and to a greater extent in the footslope soil, followed by a decreasing abundance of sterols. In surface soil, the thermostability of clay-associated OM increases in the order: carbohydrates and N compounds < phenols/lignin monomers < lignin dimers and alkylaromatics, suggesting the intrinsic chemical nature of OM as a major driver for OM persistent in surface soil.
    [Show full text]
  • Deep Carbon Observatory
    DEEP CARBON OBSERVATORY DCO EARLY CAREER SCIENTIST WORKSHOP Hotel Biancaneve, Nicolosi Mount Etna, Italy 28 August – 2 September 2017 SPONSORS AGENDA MEETING HASHTAG: #DCOECS17 Sunday, 27 August 2017 ______________________________________________________________________________ All day Arrival at Hotel Biancaneve, Nicolosi All day; transportation from Catania Fontanarossa Airport (CTA) will be provided where possible. Check-in, registration, and badge pick up. Monday, 28 August ______________________________________________________________________________ Until 16:00 Arrival at Hotel Biancaneve, Nicolosi All day; transportation from Catania Fontanarossa Airport (CTA) will be provided where possible. Check-in, registration, and badge pick up. ______________________________________________________________________________ 16:30 Welcome and Icebreaker Members of the organizing committee. 16:30 – 16:45 Welcome to the Third DCO Early Career Scientist Workshop Vincenzo Stagno, Workshop PI, Sapienza University of Rome, Italy 16:45 – 17:00 An introduction to the Deep Life Community Melitza Crespo-Medina, Co-Organizer, CECIA – Inter American University of Puerto Rico 17:00 – 17:15 An introduction to the Deep Energy Community Riikka Kietäväinen, Co-Organizer, Geological Survey of Finland 17:15 – 17:30 An introduction to the Extreme Physics and Chemistry Community Valerio Cerantola, Co-Organizer, ESRF Grenoble, France 17:30 – 17:45 An introduction to the Reservoirs and Fluxes Community Peter Barry, Co-Organizer, University of Oxford, UK 17:45 – 18:00
    [Show full text]
  • The Importance of Degradation in the Fate of Selected Organic Compounds in the Environment
    Polish Journal of Environmental Studies Vol. 13, No. 6 (2004), 617-626 Review The Importance of Degradation in the Fate of Selected Organic Compounds in the Environment. Part II. Photodegradation and Biodegradation D. Dąbrowska, A. Kot-Wasik, J. Namieśnik* Department of Analytical Chemistry, Chemical Faculty, Gdańsk University of Technology, 11/12 Narutowicz Str., 80-952 Gdańsk, Poland Received: 12 December 2003 Accepted: 3 June 2004 Abstract Compounds characterized by a slow degradation rate in the environment, i.e. resistant to biodegrada- tion, and photolysis processes, are classified as persistent and have often been considered as potential environmental problems. A more exacting approach recognizes that a compound released to the environ- ment has a tendency to accumulate in one medium more than in others. Hence, partitioning, transport, and transformation rates of any particular compound will differ in each medium. Degradation processes in the dominant medium (where the compound is preferentially accumulated) are expected to have more effect on overall persistence of the measured compound than degradation processes in the other media. Photo- degradation and biodegradation are the degradation processes which can naturaly clean up the environ- ment. Biodegradation is expected to be the major mechanism of loss for most chemicals released into the environment. In this study, photodegradation and biodegradation processes of selected organic pollutants in different media have been reviewed. Keywords: organic pollutants, photodegradation, biodegradation, products of degradation Introduction layers of soil. The intensity of UV radiation depends on many factors, among others, a time of the year, a time of the Persistent organic pollutants (POPs) can cause serious day, latitude, height above the sea level, air density, cloud problems in various environmental compartments due to cover or the size of the ozone hole [1].
    [Show full text]
  • Comparison of Inorganic and Organic Trace Mineral Supplementation on the Growth, Performance and Fecal Mineral Excretion in Phase-Fed, Grow-Finish Swine
    Iowa State University Capstones, Theses and Retrospective Theses and Dissertations Dissertations 1-1-2006 Comparison of inorganic and organic trace mineral supplementation on the growth, performance and fecal mineral excretion in phase-fed, grow-finish swine Jeremy Lenn Burkett Iowa State University Follow this and additional works at: https://lib.dr.iastate.edu/rtd Recommended Citation Burkett, Jeremy Lenn, "Comparison of inorganic and organic trace mineral supplementation on the growth, performance and fecal mineral excretion in phase-fed, grow-finish swine" (2006). Retrospective Theses and Dissertations. 19370. https://lib.dr.iastate.edu/rtd/19370 This Thesis 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 Retrospective Theses and Dissertations by an authorized administrator of Iowa State University Digital Repository. For more information, please contact [email protected]. Comparison of inorganic and organic trace mineral supplementation on the growth, performance and fecal mineral excretion in phase-fed, grow- finish swine by Jeremy Lenn Burkett A thesis submitted to the graduate faculty in partial fulfillment of the requirements for the degree of MASTER OF SCIENCE Major: Animal Science Program of Study Committee: Kenneth Stalder, Co-major Professor Thomas J. Baas, Co-major Professor Wendy J. Powers Theodore Bailey Iowa State University Ames, Iowa 2006 Copyright ©Jeremy Lenn Burkett, 2006. All rights reserved. 11 Graduate College Iowa State University This is to certify the master's thesis of Jeremy Lenn Burkett has met the thesis requirements of Iowa State University Signatures have been redacted for privacy Signatures have been redacted for privacy 111 TABLE OF CONTENTS LIST OF TABLES v CHAPTER 1.
    [Show full text]