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Comparison of Lead Calcium and Lead Selenium Alloys
A COMPARISON OF LEAD CALCIUM & LEAD SELENIUM ALLOYS Separating Fact From Fiction By: Carey O’Donnell & Chuck Finin Background Debate between lead antimony vs. lead calcium has been ongoing for almost 70 years Both are mature ‘technologies’, with major battery producers and users in both camps Batteries based on both alloy types have huge installed bases around the globe Time to take another look for US applications: • New market forces at work • Significant improvements in alloy compositions • Recognize that users are looking for viable options Objectives Provide a brief history of the development and use of both lead selenium (antimony) and lead calcium; objectively compare and contrast the performance and characteristics of each type To attempt to draw conclusions about the performance, reliability, and life expectancy of each alloy type; suitability of each for use in the US Then & Now: Primary Challenges in Battery Manufacturing The improvement of lead alloy compositions for increased tensile strength, improved casting, & conductive performance Developing better compositions & processes for the application and retention of active material on the grids Alloy Debate: Lead Calcium Vs. Lead Selenium Continues to dominate & define much of the technical and market debate in US Good reasons for this: • Impacts grid & product design, long-term product performance & reliability • Directly affects physical strength & hardness of grid; manufacturability • Influences grid corrosion & growth, retention of active material History of Antimony First -
7.014 Handout PRODUCTIVITY: the “METABOLISM” of ECOSYSTEMS
7.014 Handout PRODUCTIVITY: THE “METABOLISM” OF ECOSYSTEMS Ecologists use the term “productivity” to refer to the process through which an assemblage of organisms (e.g. a trophic level or ecosystem assimilates carbon. Primary producers (autotrophs) do this through photosynthesis; Secondary producers (heterotrophs) do it through the assimilation of the organic carbon in their food. Remember that all organic carbon in the food web is ultimately derived from primary production. DEFINITIONS Primary Productivity: Rate of conversion of CO2 to organic carbon (photosynthesis) per unit surface area of the earth, expressed either in terns of weight of carbon, or the equivalent calories e.g., g C m-2 year-1 Kcal m-2 year-1 Primary Production: Same as primary productivity, but usually expressed for a whole ecosystem e.g., tons year-1 for a lake, cornfield, forest, etc. NET vs. GROSS: For plants: Some of the organic carbon generated in plants through photosynthesis (using solar energy) is oxidized back to CO2 (releasing energy) through the respiration of the plants – RA. Gross Primary Production: (GPP) = Total amount of CO2 reduced to organic carbon by the plants per unit time Autotrophic Respiration: (RA) = Total amount of organic carbon that is respired (oxidized to CO2) by plants per unit time Net Primary Production (NPP) = GPP – RA The amount of organic carbon produced by plants that is not consumed by their own respiration. It is the increase in the plant biomass in the absence of herbivores. For an entire ecosystem: Some of the NPP of the plants is consumed (and respired) by herbivores and decomposers and oxidized back to CO2 (RH). -
Oregon Department of Human Services HEALTH EFFECTS INFORMATION
Oregon Department of Human Services Office of Environmental Public Health (503) 731-4030 Emergency 800 NE Oregon Street #604 (971) 673-0405 Portland, OR 97232-2162 (971) 673-0457 FAX (971) 673-0372 TTY-Nonvoice TECHNICAL BULLETIN HEALTH EFFECTS INFORMATION Prepared by: Department of Human Services ENVIRONMENTAL TOXICOLOGY SECTION Office of Environmental Public Health OCTOBER, 1998 CALCIUM CARBONATE "lime, limewater” For More Information Contact: Environmental Toxicology Section (971) 673-0440 Drinking Water Section (971) 673-0405 Technical Bulletin - Health Effects Information CALCIUM CARBONATE, "lime, limewater@ Page 2 SYNONYMS: Lime, ground limestone, dolomite, sugar lime, oyster shell, coral shell, marble dust, calcite, whiting, marl dust, putty dust CHEMICAL AND PHYSICAL PROPERTIES: - Molecular Formula: CaCO3 - White solid, crystals or powder, may draw moisture from the air and become damp on exposure - Odorless, chalky, flat, sweetish flavor (Do not confuse with "anhydrous lime" which is a special form of calcium hydroxide, an extremely caustic, dangerous product. Direct contact with it is immediately injurious to skin, eyes, intestinal tract and respiratory system.) WHERE DOES CALCIUM CARBONATE COME FROM? Calcium carbonate can be mined from the earth in solid form or it may be extracted from seawater or other brines by industrial processes. Natural shells, bones and chalk are composed predominantly of calcium carbonate. WHAT ARE THE PRINCIPLE USES OF CALCIUM CARBONATE? Calcium carbonate is an important ingredient of many household products. It is used as a whitening agent in paints, soaps, art products, paper, polishes, putty products and cement. It is used as a filler and whitener in many cosmetic products including mouth washes, creams, pastes, powders and lotions. -
Terrestrial Decomposition
Terrestrial Decomposition • Objectives – Controls over decomposition • Litter breakdown • Soil organic matter formation and dynamics – Carbon balance of ecosystems • Soil carbon storage 1 Overview • In terrestrial ecosystems, soils (organic horizon + mineral soil) > C than in vegetation and atmosphere combined 2 Overview • Decomposition is: 1. Major pathway for C loss from ecosystems 2. Central to ecosystem C loss and storage 3 Overview 4 Incorporation 1 year later Overview • Predominant controls on litter decomposition are fairly well constrained 1. Temperature and moisture 2. Litter quality • N availability • Lignin concentration • Lignin:N • Mechanisms for soil organic matter stabilization: 1. Recalcitrance (refers to chemistry) 2. Physical protection • Within soil aggregates • Organo-mineral associations 3. Substrate supply regulation (energetic limitation) 5 Overview • Disturbance can override millenia in a matter of days or years: 1. Land use change 2. Invasive species 3. Climate change • Understanding the mechanistic drivers of decomposition, soil organic matter formation, and carbon stabilization help us make management decisions, take mitigation steps, and protect resources. 6 Overview Native Ōhiʻa - Koa forest Conversion to Reforestation in grass-dominated pasture (80 yr) Eucalyptus plantation (10 yr) Conventional sugar cane harvest. 20° C 18° C 16° C 14° C 7 Sustainable ratoon harvest. Decomposition • Decomposition is the biological, physical and chemical breakdown of organic material – Provides energy for microbial growth -
Thermophilic Lithotrophy and Phototrophy in an Intertidal, Iron-Rich, Geothermal Spring 2 3 Lewis M
bioRxiv preprint doi: https://doi.org/10.1101/428698; this version posted September 27, 2018. The copyright holder for this preprint (which was not certified by peer review) is the author/funder, who has granted bioRxiv a license to display the preprint in perpetuity. It is made available under aCC-BY-NC-ND 4.0 International license. 1 Thermophilic Lithotrophy and Phototrophy in an Intertidal, Iron-rich, Geothermal Spring 2 3 Lewis M. Ward1,2,3*, Airi Idei4, Mayuko Nakagawa2,5, Yuichiro Ueno2,5,6, Woodward W. 4 Fischer3, Shawn E. McGlynn2* 5 6 1. Department of Earth and Planetary Sciences, Harvard University, Cambridge, MA 02138 USA 7 2. Earth-Life Science Institute, Tokyo Institute of Technology, Meguro, Tokyo, 152-8550, Japan 8 3. Division of Geological and Planetary Sciences, California Institute of Technology, Pasadena, CA 9 91125 USA 10 4. Department of Biological Sciences, Tokyo Metropolitan University, Hachioji, Tokyo 192-0397, 11 Japan 12 5. Department of Earth and Planetary Sciences, Tokyo Institute of Technology, Meguro, Tokyo, 13 152-8551, Japan 14 6. Department of Subsurface Geobiological Analysis and Research, Japan Agency for Marine-Earth 15 Science and Technology, Natsushima-cho, Yokosuka 237-0061, Japan 16 Correspondence: [email protected] or [email protected] 17 18 Abstract 19 Hydrothermal systems, including terrestrial hot springs, contain diverse and systematic 20 arrays of geochemical conditions that vary over short spatial scales due to progressive interaction 21 between the reducing hydrothermal fluids, the oxygenated atmosphere, and in some cases 22 seawater. At Jinata Onsen, on Shikinejima Island, Japan, an intertidal, anoxic, iron- and 23 hydrogen-rich hot spring mixes with the oxygenated atmosphere and sulfate-rich seawater over 24 short spatial scales, creating an enormous range of redox environments over a distance ~10 m. -
Micronutrients and the Nutrient Status of Soils: a Global Study
FAO SOILS BULLETIN 48 micron utrients and the nutrient status of SOUS: a global study by mikko sillanpAl FOOD AND AGRICULTURE ORGANIZATION OF THE UNITED NATIONS FAO SOILS BULLETIN 48 micronutrients and the nutrient status of soils: a global study by mikko sillanpäd sponsored by the government of finland executed at the institute of soil science agricultural research centre jokioinen, finland and soil resources, management and conservation service land and water development division FAO FOOD AND AGRICULTURE ORGANIZATION OF THE UNITED NATIO-NS Rome 1982 The designations employed and the presentation of material in this publication do not imply the expression of any opinion whatsoever on the part of the Food and Agriculture Organization oftheUnitedNations concerningthelegal status of any country, territory, city or area or of its authorities, or concerning the delimitation of its frontiers or boundaries. M-52 ISBN 92-5-101193-1 Allrights reserved. No part ofthispublication may be reproduced, stored in a retrieval system, or transmitted in any form or by any means, electronic,mechanical, photocopyingor otherwise, without theprior permission of the copyright owner. Applications for such permission, with a statement of the purpose and extent of the reproduction, should be addressed to the Director, Publications Division, Food and Agriculture Organization of the United Nations, Via delle Terme diCaracalla, 00100 Rome, Italy. C) FAO 1982 Printed in Finland by Werner Söderström Osakeyhtiö. Foreword During the last two decades, the increasing use of mineral fertilizers and organic manures of different types has led to impressive yield incrcases in developing countries. Major emphasis was given to the supply of the main macronutrients, nitrogen, phosphate and potash. -
Growth and Micronutrient Needs of Adolescents
European Journal of Clinical Nutrition (2000) 54, Suppl 1, S11±S15 ß 2000 Macmillan Publishers Ltd All rights reserved 0954±3007/00 $15.00 www.nature.com/ejcn Growth and micronutrient needs of adolescents B Olmedilla* and F Granado Servicio de NutricioÂn, Unidad de Vitaminas, ClõÂnica Puerta de Hierro, 28035-Madrid, Spain Objective: This paper focuses on micronutrients in relation to needs throughout adolescence, a period which involved growth and development that occur through a complex interaction of genetic instructions, hormones and environmental in¯uences, many of them of dietary origin. In the context of micronutrient `needs' it is of special importance to differentiate between the `nutritional needs' and `metabolic needs'. Two main questions arise in relation to the micronutrient needs: (1) why are micronutrients necessary? and (2) how are their needs assessed? Results: The `necessary' amount will differ according to the objectives pursued: (a) to achieve a satisfactory rate of growth and development; and (b) to maintain `optimal health'. The assesment of micronutrient needs and status has proved to be dif®cult, but when elucidating and establishing them, it is imperative to arrive at the estimates in the light of their interdependent role in metabolism and functions. The knowledge of micronutrient metabolic needs can be approached through epidemiological observations, bioavailability studies and clinical trials. However, there is a nearly total absence of reports on the particular metabolic and dietary needs of adolescents. Conclusion: Thus more studies are required in relation to the effect of features associated with adolescence on `needs', evaluating their impact on bioavailablility and turnover (storage and losses), and the interactions among micronutrients in the assessment of metabolic and nutritional needs. -
Guidelines on Food Fortification with Micronutrients
GUIDELINES ON FOOD FORTIFICATION FORTIFICATION FOOD ON GUIDELINES Interest in micronutrient malnutrition has increased greatly over the last few MICRONUTRIENTS WITH years. One of the main reasons is the realization that micronutrient malnutrition contributes substantially to the global burden of disease. Furthermore, although micronutrient malnutrition is more frequent and severe in the developing world and among disadvantaged populations, it also represents a public health problem in some industrialized countries. Measures to correct micronutrient deficiencies aim at ensuring consumption of a balanced diet that is adequate in every nutrient. Unfortunately, this is far from being achieved everywhere since it requires universal access to adequate food and appropriate dietary habits. Food fortification has the dual advantage of being able to deliver nutrients to large segments of the population without requiring radical changes in food consumption patterns. Drawing on several recent high quality publications and programme experience on the subject, information on food fortification has been critically analysed and then translated into scientifically sound guidelines for application in the field. The main purpose of these guidelines is to assist countries in the design and implementation of appropriate food fortification programmes. They are intended to be a resource for governments and agencies that are currently implementing or considering food fortification, and a source of information for scientists, technologists and the food industry. The guidelines are written from a nutrition and public health perspective, to provide practical guidance on how food fortification should be implemented, monitored and evaluated. They are primarily intended for nutrition-related public health programme managers, but should also be useful to all those working to control micronutrient malnutrition, including the food industry. -
Plant Species Effects on Nutrient Cycling: Revisiting Litter Feedbacks
Review Plant species effects on nutrient cycling: revisiting litter feedbacks Sarah E. Hobbie Department of Ecology, Evolution and Behavior, University of Minnesota, St. Paul, MN 55108, USA In a review published over two decades ago I asserted reinforce those gradients and patterns of NPP, focusing that, along soil fertility gradients, plant traits change in on feedbacks operating through plant litter decomposition. ways that reinforce patterns of soil fertility and net Specifically, I evaluate two key assumptions underlying primary productivity (NPP). I reevaluate this assertion the plant litter feedback idea: (i) plant litter traits vary in light of recent research, focusing on feedbacks to NPP predictably along fertility gradients, and (ii) such variation operating through litter decomposition. I conclude that reinforces soil fertility gradients through effects on decom- mechanisms emerging since my previous review might position and litter N release. Given the number of synthetic weaken these positive feedbacks, such as negative cross-site analyses of plant traits and their consequences effects of nitrogen on decomposition, while others for nutrient cycling over the past two decades, the time is might strengthen them, such as slower decomposition ripe for revisiting my original assertions. Indeed, I show of roots compared to leaf litter. I further conclude that that my original assertion is more nuanced and complex predictive understanding of plant species effects on than originally claimed. In particular, I discuss the need to nutrient cycling will require developing new frameworks consider leaf litter decomposition more carefully and move that are broadened beyond litter decomposition to con- beyond consideration of leaf litter feedbacks to a more sider the full litter–soil organic matter (SOM) continuum. -
Vitamin and Mineral Requirements in Human Nutrition
P000i-00xx 3/12/05 8:54 PM Page i Vitamin and mineral requirements in human nutrition Second edition VITPR 3/12/05 16:50 Page ii WHO Library Cataloguing-in-Publication Data Joint FAO/WHO Expert Consultation on Human Vitamin and Mineral Requirements (1998 : Bangkok, Thailand). Vitamin and mineral requirements in human nutrition : report of a joint FAO/WHO expert consultation, Bangkok, Thailand, 21–30 September 1998. 1.Vitamins — standards 2.Micronutrients — standards 3.Trace elements — standards 4.Deficiency diseases — diet therapy 5.Nutritional requirements I.Title. ISBN 92 4 154612 3 (LC/NLM Classification: QU 145) © World Health Organization and Food and Agriculture Organization of the United Nations 2004 All rights reserved. Publications of the World Health Organization can be obtained from Market- ing and Dissemination, World Health Organization, 20 Avenue Appia, 1211 Geneva 27, Switzerland (tel: +41 22 791 2476; fax: +41 22 791 4857; e-mail: [email protected]). Requests for permis- sion to reproduce or translate WHO publications — whether for sale or for noncommercial distri- bution — should be addressed to Publications, at the above address (fax: +41 22 791 4806; e-mail: [email protected]), or to Chief, Publishing and Multimedia Service, Information Division, Food and Agriculture Organization of the United Nations, 00100 Rome, Italy. The designations employed and the presentation of the material in this publication do not imply the expression of any opinion whatsoever on the part of the World Health Organization and the Food and Agriculture Organization of the United Nations concerning the legal status of any country, territory, city or area or of its authorities, or concerning the delimitation of its frontiers or boundaries. -
Micronutrient Management in Nebraska Bijesh Maharjan, Tim M
NebGuide Nebraska Extension Research-Based Information That You Can Use G1830MR · Index: Crops, Soil Management Revised February 2018 Micronutrient Management in Nebraska Bijesh Maharjan, Tim M. Shaver, Charles S. Wortmann, Charles A. Shapiro, Richard B. Ferguson, Brian T. Krienke, and Zachary P. Stewart Extension Soils Specialists This NebGuide addresses issues of micronutrient fertilizer use Table 1. Estimates of micronutrient uptake (whole plant) by with a focus on zinc and iron. crops. Of the 17 elements known to be essential for plant Micronutrient 200 Bu Corn 60 Bu Soybean 6 Ton Alfalfa growth, eight are used in very small amounts and, with the lb/acre lb/acre lb/acre exception of iron, have an uptake of less than 1 pound per Iron 2.4 1.7 1.8 acre per year (Table 1). These elements are classified as mi- Manganese 0.4 0.6 0.6 cronutrients and include zinc (Zn), iron (Fe), manganese Zinc 0.4 0.2 0.2 (Mn), copper (Cu), boron (B), molybdenum (Mo), chlo- Boron 0.2 0.1 0.3 rine (Cl), and nickel (Ni). Interest in micronutrients has Copper 0.1 0.1 0.06 Molybdenum 0.01 0.01 0.02 increased because of accelerated rates of nutrient removal Nickel 0.01 0.01 0.01 due to greater yields and the availability of alternative mi- Adapted from: Role of Micronutrients in Efficient Crop Production, D.B. Mengel, Purdue cronutrient products. University AY- 239. https:// www .extension .purdue .edu /extmedia /AY /AY - 239 .html Micronutrient Availability Some micronutrients are supplied to plants when 1). -
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.