Fate and Reactivity of Natural and Manufactured Nanoparticles in Soil/Water Environments Allison Vandevoort Clemson University, [email protected]
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Biogeochemistry of Mediterranean Wetlands: a Review About the Effects of Water-Level Fluctuations on Phosphorus Cycling and Greenhouse Gas Emissions
water Review Biogeochemistry of Mediterranean Wetlands: A Review about the Effects of Water-Level Fluctuations on Phosphorus Cycling and Greenhouse Gas Emissions Inmaculada de Vicente 1,2 1 Departamento de Ecología, Universidad de Granada, 18071 Granada, Spain; [email protected]; Tel.: +34-95-824-9768 2 Instituto del Agua, Universidad de Granada, 18071 Granada, Spain Abstract: Although Mediterranean wetlands are characterized by extreme natural water level fluctu- ations in response to irregular precipitation patterns, global climate change is expected to amplify this pattern by shortening precipitation seasons and increasing the incidence of summer droughts in this area. As a consequence, a part of the lake sediment will be exposed to air-drying in dry years when the water table becomes low. This periodic sediment exposure to dry/wet cycles will likely affect biogeochemical processes. Unexpectedly, to date, few studies are focused on assessing the effects of water level fluctuations on the biogeochemistry of these ecosystems. In this review, we investigate the potential impacts of water level fluctuations on phosphorus dynamics and on greenhouse gases emissions in Mediterranean wetlands. Major drivers of global change, and specially water level fluctuations, will lead to the degradation of water quality in Mediterranean wetlands by increasing the availability of phosphorus concentration in the water column upon rewetting of dry sediment. CO2 fluxes are likely to be enhanced during desiccation, while inundation is likely to decrease cumulative CO emissions, as well as N O emissions, although increasing CH emissions. Citation: de Vicente, I. 2 2 4 Biogeochemistry of Mediterranean However, there exists a complete gap of knowledge about the net effect of water level fluctuations Wetlands: A Review about the Effects induced by global change on greenhouse gases emission. -
The Global Marine Phosphorus Cycle: Sensitivity to Oceanic Circulation
Biogeosciences, 4, 155–171, 2007 www.biogeosciences.net/4/155/2007/ Biogeosciences © Author(s) 2007. This work is licensed under a Creative Commons License. The global marine phosphorus cycle: sensitivity to oceanic circulation C. P. Slomp and P. Van Cappellen Department of Earth Sciences – Geochemistry, Faculty of Geosciences, Utrecht University, P.O. Box 80021, 3508 TA Utrecht, The Netherlands Received: 4 September 2006 – Published in Biogeosciences Discuss.: 5 October 2006 Revised: 8 January 2007 – Accepted: 20 February 2007 – Published: 22 February 2007 Abstract. A new mass balance model for the coupled ma- stand long-term variations in marine biological activity, at- rine cycles of phosphorus (P) and carbon (C) is used to ex- mospheric composition and climate (Holland, 1984; Van amine the relationships between oceanic circulation, primary Cappellen and Ingall, 1996; Petsch and Berner, 1998; Bjer- productivity, and sedimentary burial of reactive P and partic- rum and Canfield, 2002). Important forcings include the sup- ulate organic C (POC), on geological time scales. The model ply of reactive P from the continents, oceanic circulation and explicitly represents the exchanges of water and particulate sea level fluctuations (Follmi,¨ 1996; Compton et al., 2000; matter between the continental shelves and the open ocean, Handoh and Lenton, 2003; Wallmann, 2003; Bjerrum et al., and it accounts for the redox-dependent burial of POC and 2006). the various forms of reactive P (iron(III)-bound P, particu- Upward transport of nutrient-rich water sustains biologi- late organic P (POP), authigenic calcium phosphate, and fish cal activity in marine surface waters. Vertical mixing, how- debris). Steady state and transient simulations indicate that ever, also controls the ventilation of the deeper ocean waters, a slowing down of global ocean circulation decreases pri- which in turn has a major effect on the sedimentary burial mary production in the open ocean, but increases that in the of phosphorus. -
Asbestos, So That the Statement That
Br J Ind Med: first published as 10.1136/oem.48.6.430 on 1 June 1991. Downloaded from 430 Forum 49 Muehleck E. Letter to WWF Sheperd bles paranoia. In the so that the statement (Turner and Newall). 8 March, 1943. fully developed asbestos, that 50 Hardy HL. Personal communications, form of this psychosis the individual the disease was "discovered by the 1982, 1989. adopts a false premise and then uses ancients," while adding historical 51 Brown V. Letter to E Muehleck (Keas- every device of selection and bias to colour and apparent verisimilitude, is bey & Mattison Co) and JFD Rohr- bach (Raybestos-Manhattan). 22 support it. In the case of a person who manifest nonsense. October, 1948. thinks he is Napoleon or she is the This temptation to dramatise and 52 Brown V. Letter to sponsors (Amer Virgin Mary it is easy to recognise the emotionalise is apparent throughout Brake Shoe, Gatke Corp, Keasbey false premise. is the whole book. I have not and Mattison, Raybestos-Manhattan, It less easy with a counted the Thermoid Corp, Union Asbestos and subject which has been ventilated in emotional adjectives but the book is Rubber Co, Russell Manufacturing the media over the last 25 years to such liberally besprinkled with them while Co, United States Gypsum Co). 27 an extent that the average man in the the author flogs himselfinto a lather of October 1948. 53 Brown V. Letter to WT Kelly (Amer street tends to agree with the premise indignation. One early example is a Brake Shoe). 12 November, 1948. -
Earth Systems and Interactions
The Earth System Earth Systems and Interactions Key Concepts • How do Earth systems What do you think? Read the three statements below and decide interact in the carbon whether you agree or disagree with them. Place an A in the Before column cycle? if you agree with the statement or a D if you disagree. After you’ve read • How do Earth systems this lesson, reread the statements to see if you have changed your mind. interact in the phosphorus Before Statement After cycle? 1. The amount of water on Earth remains constant over time. 2. Hydrogen makes up the hydrosphere. 3. Most carbon on Earth is in the atmosphere. 3TUDY#OACH Earth Systems Make a Table Contrast the carbon cycle and the Your body contains many systems. These systems work phosphorus cycle in a two- together and make one big system—your body. Earth is a column table. Label one system, too. Like you, Earth has smaller systems that work column Carbon Cycle and together, or interact, and make the larger Earth system. Four the other column Phosphorus of these smaller systems are the atmosphere, the Cycle. Complete the table hydrosphere, the geosphere, and the biosphere. as you read this lesson. The Atmosphere Reading Check The outermost Earth system is a mixture of gases and 1. Identify What systems particles of matter called the atmosphere. It forms a layer make up the larger Earth around the other Earth systems. The atmosphere is mainly system? nitrogen and oxygen. Gases in the atmosphere move freely, helping transport matter and energy among Earth systems. -
Effects of Fertilisation on Phosphorus Pools in the Volcanic Soil of a Managed Tropical Forest
Forest Ecology and Management 258 (2009) 2199–2206 Contents lists available at ScienceDirect Forest Ecology and Management journal homepage: www.elsevier.com/locate/foreco Effects of fertilisation on phosphorus pools in the volcanic soil of a managed tropical forest Dean F. Meason a,*, Travis W. Idol a, J.B. Friday a, Paul G. Scowcroft b a Department of Natural Resources and Environmental Management, College of Tropical Agriculture and Human Resources, Sherman Laboratory, University of Hawaii, 1910 East West Road, Honolulu, HI 96822, USA b Institute of Pacific Islands Forestry, Pacific Southwest Research Station, USDA Forest Service, 60 Nowelo Street, Hilo, HI 96720, USA ARTICLE INFO ABSTRACT Article history: Acacia koa forests benefit from phosphorus fertilisation, but it is unknown if fertilisation is a short or long Received 31 July 2008 term effect on P availability. Past research suggests that P cycling in soils with high P sorption capacity, Received in revised form 30 March 2009 such as Andisols, was through organic pathways. We studied leaf P and soil P fractions in a tropical forest Accepted 2 April 2009 Andisol for 3 years after fertilisation with triple super phosphate. Leaf P concentration and labile P remained high after fertilisation. Fertilisation had increased all the inorganic P fractions over the length Keywords: of the study, while organic P fractions had not. The results suggested that the organic P fractions had a Hedley fractionation reduced role as a source of labile P after fertilisation. The size and dynamics of the sodium hydroxide- and Phosphorus fertilization hydrochloric acid-extractable P pools would suggest that either pool could be major sources of labile P. -
Prevention of Osteonecrosis of the Jaw (ONJ) in Patients On
Guideline Department of Health, NSW 73 Miller Street North Sydney NSW 2060 Locked Mail Bag 961 North Sydney NSW 2059 Telephone (02) 9391 9000 Fax (02) 9391 9101 http://www.health.nsw.gov.au/policies/ space space Prevention of Osteonecrosis of the Jaw (ONJ) in Patients on Bisphosphonate Therapies space Document Number GL2010_010 Publication date 23-Jul-2010 Functional Sub group Clinical/ Patient Services - Dental/Oral Clinical/ Patient Services - Pharmaceutical Clinical/ Patient Services - Medical Treatment Summary This document provides a consensus based guideline, drawing on current documented best practices, for the undertaking of invasive dental/oral surgical procedures on patients taking bisphosphonate agents so as to minimise the risk, or prevent the development of osteonecrosis of the jaws. Replaces Doc. No. Bisphosphonate Related Osteonecrosis of the Jaws - Prevention [GL2008_010] Author Branch Centre for Oral Health Strategy Branch contact Peter List 8821 4310 Applies to Area Health Services/Chief Executive Governed Statutory Health Corporation, Board Governed Statutory Health Corporations, Affiliated Health Organisations - Non Declared, Affiliated Health Organisations - Declared, Community Health Centres, Dental Schools and Clinics, Public Hospitals Audience Public Oral Health Practitioners, Medical Practitioners, Private Dental Practitioners Distributed to Public Health System, Divisions of General Practice, Government Medical Officers, NSW Ambulance Service, NSW Department of Health, Private Hospitals and Day Procedure Centres, -
Consumption, Silicosis, and the Social Construction of Industrial Disease
City University of New York (CUNY) CUNY Academic Works Publications and Research Baruch College 1991 Consumption, silicosis, and the social construction of industrial disease. D. Rosner CUNY Bernard M Baruch College G. Markowitz CUNY Bernard M Baruch College How does access to this work benefit ou?y Let us know! More information about this work at: https://academicworks.cuny.edu/bb_pubs/24 Discover additional works at: https://academicworks.cuny.edu This work is made publicly available by the City University of New York (CUNY). Contact: [email protected] THE YALE JOURNAL OF BIOLOGY AND MEDICINE 64 (1991), 481-498 Consumption, Silicosis, and the Social Construction of Industrial Disease* DAVID ROSNER, Ph.D.,a AND GERALD MARKOWITZ, Ph.D." aProfessor ofHistory, Baruch College and CUNYGraduate Center, New York; "Professor ofHistory, John Jay College, City University ofNew York New York, New York Received September 10, 1991 In the wake of the bacterial revolution after Robert Koch identified the tuberculosis bacillus, medical and public health professionals classified the various forms of consumption and phthisis as a single disease-tuberculosis. In large measure, historians have adopted that perspective. While there is undoubtedly a great deal of truth in this conceptualization, we argue that it obscures almost as much as it illuminates. By collapsing the nineteenth-century terms phthisis and consumption into tuberculosis, we maintain that historians have not understood the effect of non-bacterial consumption on working-class populations who suffered from the symptoms of coughing, wasting away, and losing weight. In this essay, we explore how, in the nineteenth century, what we now recognize as silicosis was referred to as miners' "con," stonecutters' phthisis, and other industry-specific forms of phthisis and consumption. -
Development of the International and Egyptian Occupational Diseases’ Lists - Review
Egyptian Journal of Occupational Medicine, 2012; 36 (2) : 215-237 DEVELOPMENT OF THE INTERNATIONAL AND EGYPTIAN OCCUPATIONAL DISEASES’ LISTS - REVIEW By Abo El-Ata GA Department of Occupational and Environmental Medicine, Faculty of Medicine, Cairo University. Abstract: An occupational disease is typically identified when it is shown that it is more prevalent in a given group of workers than in the general population, or in other worker populations. The present review study aims at eliciting development of the occupational diseases concepts and lists in Egypt and internationally, in order to anticipate the future trends in enhancing the supportive activities targeting healthcare activities of the Egyptian workers. The historical and present situation of occupational diseases are carefully reviewed and discussed, emphasizing the foot prints of related conceptions in Egypt and ILO. Future ambitions are expressed by the current study. Adopt the ILO list as well as its future amendments. In addition, re-formatting the schedule, in a similar way the ILO list is organized in three categories of occupational diseases: 1) Diseases caused by agents (chemical, physical, biological) ; 2) Diseases of target organ systems (respiratory, skin and mucous membranes, musculoskeletal, liver, kidney, endocrine, etc.) ; and 3) Occupational cancer. Restructure the basic occupational health services (BOHS) to insure provision of comprehensive and continuous benefits for every worker in his workplace. A series of guidelines and codes of practice should be issued to facilitate adoption of BOHS with detailed required procedures. The study recommended continued improving the Egyptian schedule, with establishment of proper guidelines and codes of practice to lead surveillance of the worker’s health and the workplace, an important item in basic occupational health services (BOHS). -
Flows and Human Interferences
P1: FXZ/VEN October 16, 2000 12:3 Annual Reviews AR118-03 Annu. Rev. Energy Environ. 2000. 25:53–88 Copyright c 2000 by Annual Reviews. All rights reserved PHOSPHORUS IN THE ENVIRONMENT: Natural Flows and Human Interferences Vaclav Smil Department of Geography, University of Manitoba, Winnipeg, Manitoba R3T 2N2 Canada; e-mail: [email protected] Key Words biogeochemical cycling, phosphates, fertilizers, eutrophication ■ Abstract Phosphorus has a number of indispensable biochemical roles, but it does not have a rapid global cycle akin to the circulations of C or N. Natural mobilization of the element, a part of the grand geotectonic denudation-uplift cycle, is slow, and low solubility of phosphates and their rapid transformation to insoluble forms make the element commonly the growth-limiting nutrient, particularly in aquatic ecosystems. Human activities have intensified releases of P.By the year 2000 the global mobilization of the nutrient has roughly tripled compared to its natural flows: Increased soil erosion and runoff from fields, recycling of crop residues and manures, discharges of urban and industrial wastes, and above all, applications of inorganic fertilizers (15 million tonnes P/year) are the major causes of this increase. Global food production is now highly dependent on the continuing use of phosphates, which account for 50–60% of all P supply; although crops use the nutrient with relatively high efficiency, lost P that reaches water is commonly the main cause of eutrophication. This undesirable process affects fresh and ocean waters in many parts of the world. More efficient fertilization can lower nonpoint P losses. Although P in sewage can be effectively controlled, such measures are often not taken, and elevated P is common in treated wastewater whose N was lowered by denitrification. -
Croet 2001 Annual Report
PuttingCROET science to work for working Oregonians CROET 2001 ANNUAL REPORT Where Healing, Teaching and Discovery Come Together Mission, Purpose, and Table of Contents Mandate CROET, the Center for Research on Occupational and Overview . 2 Environmental Toxicology at OHSU, is dedicated to Mission, Purpose, and Mandate the promotion of health and safety in the workforce. Through basic and applied research, education, and Message from the Director . 3 outreach, CROET seeks to prevent disease and disability among working Oregonians and their CROET — A Resource for Oregon . 4 families, during their employment years and throughout retirement. Advisory Committees . 5 CROET’s Areas of Emphasis . 6 2001 CROET Highlights . 7-9 Financial Summary . 10 Staff and Contact Information . 11 2 Message from the Director Dear Fellow Oregonians, “CROET - Putting Science to Work for Working Oregonians!” Many will have heard this message broadcast over public radio in an effort to increase awareness among Oregonians of the treasure trove of talent and information available to Oregonians through CROET at OHSU. This simple message proved most effective as judged by the dramatic increase in use of our information-packed website, www.croetweb.com. There are many other messages that CROET wishes to broadcast, but time and space are always limited. We have used this report to illustrate some of the basic mechanistic and applied workplace research initiatives that are underway at CROET. Brief study of our Financial Summary reveals the various research activities that are supported by workers’ compensation funds and leveraged federal grant support. On average, a single Oregon dollar leverages four federal dollars for basic and applied research at CROET! This speaks to the quality of CROET’s scientists and staff in competing successfully for highly competitive research dollars from federal agencies such as the National Institutes of Health (NIH). -
Chapter 15 Biogeochemical Cycles
Climate Change Impacts in the United States CHAPTER 15 BIOGEOCHEMICAL CYCLES Convening Lead Authors James N. Galloway, University of Virginia William H. Schlesinger, Cary Institute of Ecosystem Studies Lead Authors Christopher M. Clark, U.S. Environmental Protection Agency Nancy B. Grimm, Arizona State University Robert B. Jackson, Duke University Beverly E. Law, Oregon State University Peter E. Thornton, Oak Ridge National Laboratory Alan R. Townsend, University of Colorado Boulder Contributing Author Rebecca Martin, Washington State University Vancouver Recommended Citation for Chapter Galloway, J. N., W. H. Schlesinger, C. M. Clark, N. B. Grimm, R. B. Jackson, B. E. Law, P. E. Thornton, A. R. Townsend, and R. Martin, 2014: Ch. 15: Biogeochemical Cycles. Climate Change Impacts in the United States: The Third National Climate Assessment, J. M. Melillo, Terese (T.C.) Richmond, and G. W. Yohe, Eds., U.S. Global Change Research Program, 350-368. doi:10.7930/J0X63JT0. On the Web: http://nca2014.globalchange.gov/report/sectors/biogeochemical-cycles INFORMATION DRAWN FROM THIS CHAPTER IS INCLUDED IN THE HIGHLIGHTS REPORT AND IS IDENTIFIED BY THIS ICON 350 15 BIOGEOCHEMICAL CYCLES KEY MESSAGES 1. Human activities have increased atmospheric carbon dioxide by about 40% over pre-industrial levels and more than doubled the amount of nitrogen available to ecosystems. Similar trends have been observed for phosphorus and other elements, and these changes have major consequences for biogeochemical cycles and climate change. 2. In total, land in the United States absorbs and stores an amount of carbon equivalent to about 17% of annual U.S. fossil fuel emissions. U.S. forests and associated wood products account for most of this land sink. -
The Anthropocene: a Conspicuous Stratigraphical Signal of 10.1002/2015EF000339 Anthropogenic Changes in Production and Consumption
Earth’s Future REVIEW The Anthropocene: a conspicuous stratigraphical signal of 10.1002/2015EF000339 anthropogenic changes in production and consumption Key Points: across the biosphere • Humans refashioning relationship between production and consumption Mark Williams1, Jan Zalasiewicz1, Colin N. Waters2, Matt Edgeworth3, Carys Bennett1, Anthony D. in the biosphere Barnosky4, Erle C. Ellis5, Michael A. Ellis2, Alejandro Cearreta6, Peter K. Haff7, Juliana A. Ivar do Sul8, • Biosphere characterized by pattern of 9 10 11 12 13 global energy flow pervasively Reinhold Leinfelder , John R. McNeill , Eric Odada , Naomi Oreskes , Andrew Revkin , Daniel influenced by humans deB Richter7, Will Steffen14, Colin Summerhayes15, James P.Syvitski16, Davor Vidas17, Michael • Changes consistent with the Wagreich18,ScottL.Wing19, Alexander P.Wolfe20, and An Zhisheng21 biosphere entering a new stage of its evolution 1Department of Geology, University of Leicester, Leicester, UK, 2Environmental Science Centre, British Geological Survey, Nottingham, UK, 3School of Archaeology and Ancient History, University of Leicester, Leicester, UK, Supporting Information: 4Department of Integrative Biology, Museum of Paleontology, Museum of Vertebrate Zoology, University of California, • Supporting Information S1 Berkeley, California, USA, 5Department of Geography and Environmental Systems, University of Maryland Baltimore County, Baltimore, Maryland, USA, 6Departamento de Estratigrafía y Paleontología, Facultad de Ciencia y Tecnología, 7 Corresponding author: Universidad del País Vasco UPV/EHU, Bilbao, Spain, Division of Earth and Ocean Sciences, Nicholas School of the M. Williams, [email protected] Environment, Duke University, Durham, North Carolina, USA, 8Association of Polar Early Career Scientists (APECS-Brazil), Rio Grande do Sul, Brazil, 9Department of Geological Sciences, Freie Universität Berlin, Berlin, Germany, 10Georgetown University, Washington DC, USA, 11Department of Geology, University of Nairobi, Nairobi, Kenya, 12Department of the Citation: 13 Williams, M.