BOD Analysis: Basics and Particulars
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Water Quality: a Field-Based Quality Testing Program for Middle Schools and High Schools
DOCUMENT RESUME ED 433 223 SE 062 606 TITLE Water Quality: A Field-Based Quality Testing Program for Middle Schools and High Schools. INSTITUTION Massachusetts State Water Resources Authority, Boston. PUB DATE 1999-00-00 NOTE 75p. PUB TYPE Guides Classroom - Teacher (052) EDRS PRICE MF01/PC03 Plus Postage. DESCRIPTORS Bacteria; Environmental Education; *Field Studies; High Schools; Middle Schools; Physical Environment; Pollution; *Science Activities; *Science and Society; Science Instruction; Scientific Concepts; Temperature; *Water Pollution; *Water Quality; Water Resources IDENTIFIERS pH ABSTRACT This manual contains background information, lesson ideas, procedures, data collection and reporting forms, suggestions for interpreting results, and extension activities to complement a water quality field testing program. Information on testing water temperature, water pH, dissolved oxygen content, biochemical oxygen demand, nitrates, total dissolved solids and salinity, turbidity, and total coliform bacteria is also included.(WRM) ******************************************************************************** * Reproductions supplied by EDRS are the best that can be made * * from the original document. * ******************************************************************************** SrE N N Water A Field-Based Water Quality Testing Program for Middle Schools and High Schools U.S. DEPARTMENT OF EDUCATION Office of Educational Research and Improvement PERMISSION TO REPRODUCE AND EDUCATIONAL RESOURCES INFORMATION DISSEMINATE THIS MATERIAL -
Oxygen Concentration of Blood: PO
Oxygen Concentration of Blood: PO2, Co-Oximetry, and More Gary L. Horowitz, MD Beth Israel Deaconess Medical Center Boston, MA Objectives • Define “O2 Content”, listing its 3 major variables • Define the limitations of pulse oximetry • Explain why a normal arterial PO2 at sea level on room air is ~100 mmHg (13.3 kPa) • Describe the major features of methemogobin and carboxyhemglobin O2 Concentration of Blood • not simply PaO2 – Arterial O2 Partial Pressure ~100 mm Hg (~13.3 kPa) • not simply Hct (~40%) – or, more precisely, Hgb (14 g/dL, 140 g/L) • not simply “O2 saturation” – i.e., ~89% O2 Concentration of Blood • rather, a combination of all three parameters • a value labs do not report • a value few medical people even know! O2 Content mm Hg g/dL = 0.003 * PaO2 + 1.4 * [Hgb] * [%O2Sat] = 0.0225 * PaO2 + 1.4 * [Hgb] * [%O2Sat] kPa g/dL • normal value: about 20 mL/dL Why Is the “Normal” PaO2 90-100 mmHg? • PAO2 = (FiO2 x [Patm - PH2O]) - (PaCO2 / R) – PAO2 is alveolar O2 pressure – FiO2 is fraction of inspired oxygen (room air ~0.20) – Patm is atmospheric pressure (~760 mmHg at sea level) o – PH2O is vapor pressure of water (47 mmHg at 37 C) – PaCO2 is partial pressure of CO2 – R is the respiratory quotient (typically ~0.8) – 0.21 x (760-47) - (40/0.8) – ~100 mm Hg • Alveolar–arterial (A-a) O2 gradient is normally ~ 10, so PaO2 (arterial PO2) should be ~90 mmHg NB: To convert mm Hg to kPa, multiply by 0.133 Insights from PAO2 Equation (1) • PaO2 ~ PAO2 = (0.21x[Patm-47]) - (PaCO2 / 0.8) – At lower Patm, the PaO2 will be lower • that’s -
Oxygenation and Oxygen Therapy
Rules on Oxygen Therapy: Physiology: 1. PO2, SaO2, CaO2 are all related but different. 2. PaO2 is a sensitive and non-specific indicator of the lungs’ ability to exchange gases with the atmosphere. 3. FIO2 is the same at all altitudes 4. Normal PaO2 decreases with age 5. The body does not store oxygen Therapy & Diagnosis: 1. Supplemental O2 is an FIO2 > 21% and is a drug. 2. A reduced PaO2 is a non-specific finding. 3. A normal PaO2 and alveolar-arterial PO2 difference (A-a gradient) do NOT rule out pulmonary embolism. 4. High FIO2 doesn’t affect COPD hypoxic drive 5. A given liter flow rate of nasal O2 does not equal any specific FIO2. 6. Face masks cannot deliver 100% oxygen unless there is a tight seal. 7. No need to humidify if flow of 4 LPM or less Indications for Oxygen Therapy: 1. Hypoxemia 2. Increased work of breathing 3. Increased myocardial work 4. Pulmonary hypertension Delivery Devices: 1. Nasal Cannula a. 1 – 6 LPM b. FIO2 0.24 – 0.44 (approx 4% per liter flow) c. FIO2 decreases as Ve increases 2. Simple Mask a. 5 – 8 LPM b. FIO2 0.35 – 0.55 (approx 4% per liter flow) c. Minimum flow 5 LPM to flush CO2 from mask 3. Venturi Mask a. Variable LPM b. FIO2 0.24 – 0.50 c. Flow and corresponding FIO2 varies by manufacturer 4. Partial Rebreather a. 6 – 10 LPM b. FIO2 0.50 – 0.70 c. Flow must be sufficient to keep reservoir bag from deflating upon inspiration 5. -
Oxygen Saturation in High-Altitude Pulmonary Edema
Oxygen Saturation In High-Altitude Pulmonary J Am Board Fam Pract: first published as 10.3122/jabfm.5.4.429 on 1 July 1992. Downloaded from Edema James]. Bachman, M.D., Todd Beatty, M.D., and Daniel E. Levene High altitude, defined as elevations greater than Methods or equal to 8000 feet (2438 m) above sea level, is The 126 subjects for this study were all patients responsible for a variety of medical problems both who came to the Summit Medical Center Emer chronic and acute. The spectrum of altitude ill gency Department or to the Frisco Medical ness ranges from the common, mild symptoms of Center. Both units serve Summit County, Colo acute mountain sickness, such as insomnia, head rado. The base elevation of Summit County ache, and nausea, to severe and potentially fatal ranges from roughly 9000 to 11,000 feet (2743 to conditions, such as high-altitude pulmonary 3354 m). Between 1 November 1990 and 26Janu edema (HAPE) and high-altitude cerebral edema ary 1991, a record was maintained of the age, sex, (RACE).l room air pulse oximeter measure of oxygen satu HAPE is a noncardiogenic form of pulmonary ration (Sa 02)' chest radiograph findings, and final edema that predominantly affects young, physi diagnoses of all patients who underwent a chest cally active, previously healthy individuals who radiograph examination. arrived at high altitude between 1 and 4 days There were 152 patients who underwent chest before developing symptoms. Symptoms of early, radiography during the study period. Twenty-six milder cases include dry nonproductive cough, patients were excluded from the study: 18 had no decreased exercise tolerance, and dyspnea on ex oxygen saturation measurement taken or re ertion. -
Guidelines and Standard Procedures for Continuous Water-Quality Monitors: Station Operation, Record Computation, and Data Reporting
Guidelines and Standard Procedures for Continuous Water-Quality Monitors: Station Operation, Record Computation, and Data Reporting Techniques and Methods 1–D3 U.S. Department of the Interior U.S. Geological Survey Front Cover. Upper left—South Fork Peachtree Creek at Johnson Road near Atlanta, Georgia, site 02336240 (photograph by Craig Oberst, USGS) Center—Lake Mead near Sentinel Island, Nevada, site 360314114450500 (photograph by Ryan Rowland, USGS) Lower right—Pungo River at channel light 18, North Carolina, site 0208455560 (photograph by Sean D. Egen, USGS) Back Cover. Lake Mead near Sentinel Island, Nevada, site 360314114450500 (photograph by Ryan Rowland, USGS) Guidelines and Standard Procedures for Continuous Water-Quality Monitors: Station Operation, Record Computation, and Data Reporting By Richard J. Wagner, Robert W. Boulger, Jr., Carolyn J. Oblinger, and Brett A. Smith Techniques and Methods 1–D3 U.S. Department of the Interior U.S. Geological Survey U.S. Department of the Interior P. Lynn Scarlett, Acting Secretary U.S. Geological Survey P. Patrick Leahy, Acting Director U.S. Geological Survey, Reston, Virginia: 2006 For product and ordering information: World Wide Web: http://www.usgs.gov/pubprod Telephone: 1-888-ASK-USGS For more information on the USGS—the Federal source for science about the Earth, its natural and living resources, natural hazards, and the environment: World Wide Web: http://www.usgs.gov Telephone: 1-888-ASK-USGS Any use of trade, product, or firm names is for descriptive purposes only and does not imply endorsement by the U.S. Government. Although this report is in the public domain, permission must be secured from the individual copyright owners to reproduce any copyrighted materials contained within this report. -
A Primer on Limnology, Second Edition
BIOLOGICAL PHYSICAL lake zones formation food webs variability primary producers light chlorophyll density stratification algal succession watersheds consumers and decomposers CHEMICAL general lake chemistry trophic status eutrophication dissolved oxygen nutrients ecoregions biological differences The following overview is taken from LAKE ECOLOGY OVERVIEW (Chapter 1, Horne, A.J. and C.R. Goldman. 1994. Limnology. 2nd edition. McGraw-Hill Co., New York, New York, USA.) Limnology is the study of fresh or saline waters contained within continental boundaries. Limnology and the closely related science of oceanography together cover all aquatic ecosystems. Although many limnologists are freshwater ecologists, physical, chemical, and engineering limnologists all participate in this branch of science. Limnology covers lakes, ponds, reservoirs, streams, rivers, wetlands, and estuaries, while oceanography covers the open sea. Limnology evolved into a distinct science only in the past two centuries, when improvements in microscopes, the invention of the silk plankton net, and improvements in the thermometer combined to show that lakes are complex ecological systems with distinct structures. Today, limnology plays a major role in water use and distribution as well as in wildlife habitat protection. Limnologists work on lake and reservoir management, water pollution control, and stream and river protection, artificial wetland construction, and fish and wildlife enhancement. An important goal of education in limnology is to increase the number of people who, although not full-time limnologists, can understand and apply its general concepts to a broad range of related disciplines. A primary goal of Water on the Web is to use these beautiful aquatic ecosystems to assist in the teaching of core physical, chemical, biological, and mathematical principles, as well as modern computer technology, while also improving our students' general understanding of water - the most fundamental substance necessary for sustaining life on our planet. -
Environmental Dissolved Oxygen Values Above 100 Percent Air Saturation
Technical Note YSI, a Xylem brand • T602-01 Environmental Dissolved Oxygen VALUES GREATER THAN 100% AIR SATURATION Some of YSI’s customers are occasionally concerned about observing “Percent Air Saturation” dissolved oxygen readings in environmental water (lakes, streams, estuaries, etc.) that are above 100%. The issue is usually one of semantics. How can something be more than 100% saturated? To understand the overall concept, it is necessary to consider the sources of dissolved oxygen in environmental water and to appreciate that equilibration between air and water is rarely perfect in environmental situations. Air is certainly one source of dissolved oxygen in environmental water. If air were the only source of oxygen and if environmental water equilibrated with the air above it instantly during temperature changes, then it would indeed be impossible to observe values above 100% air saturation unless the sensor was in error. Neither of these “if statements” is true, however, for most bodies of water. ...it is necessary to consider the sources of dissolved oxygen in Figure 1. Photosynthetically-active species produce pure oxygen environmental water and to (not air) during photosynthesis. appreciate that equilibration between air and water is rarely perfect in environmental situations. Oxygen Sources Photosynthetically-active species (plants, algae, etc.) are common additional sources of dissolved oxygen in the environment and, in many bodies of water, can, in fact, be the dominant factor in determining the dissolved oxygen content. It is important to remember that these organisms produce pure oxygen (not air) during photosynthesis. Air is approximately 21% oxygen and thus it contains about five times less oxygen than the pure gaseous element produced during photosynthesis. -
Marine Primary Productivity: Measurements and Variability
Marine Primary Productivity: Measurements and Variability Matt Church Department of Oceanography MSB 612 Sunlight CO2 + 2H2OCH2O + O2 + H2O + heat Photosynthesis Gross Primary Production (GPP): The rate of organic carbon production via the reduction of CO2 inclusive of all respiratory losses. Net Primary Production (NPP): Gross primary production less photosynthetic respiration (RA): NPP = PN –RA Net Community Production (NCP): Gross primary production less all autotrophic and heterotrophic losses due to respiration (RA+H). NCP = PG –RA+H **If we are interested in carbon available for export or consumption by higher trophic levels, NCP is the key term. If we want to know how much total energy was captured by photosynthesis, we need to know GPP. What methods would you use to measure primary production in the sea? ∆O2 ∆CO2 ∆Organic matter Isotopic tracers of C and/or O2 What methods are most suitable for measuring aquatic primary production? • Typical rates of photosynthesis in the ocean range between 0.2-2 µmol C L-1 d-1 or -1 -1 0.3-3 µmol O2 L d -1, • Concentrations of DIC ~2000 µmol C L O2 ~220 µmol L-1, and TOC ~80-100 µmol L-1 • Analytical sensitivity of carbon and oxygen determinations: -1 –CO2 by coulometry = 1 µmol C L -1 –O2 by Winkler titration = 0.4 to 2 µmol O2 L –TOC by HTC = 2-4 µmol C L-1 **Measuring very small signals against large background pools** Commonly used methods for measuring aquatic photosynthesis • Changes in O2 concentrations – incubations (Gaarder and Gran 1927) and in situ dynamics. • CO2 assimilation: stable or radioisotopes of carbon (13C or 14C) – technique first applied by Steeman- Nielsen 1951. -
Seepage Chemistry Manual
RECLAMManagAingTWateIr iOn theNWest Report DSO-05-03 Seepage Chemistry Manual Dam Safety Technology Development Program U.S. Department of the Interior Bureau of Reclamation Technical Service Center Denver, Colorado December 2005 Form Approved REPORT DOCUMENTATION PAGE OMB No. 0704-0188 The public reporting burden for this collection of information is estimated to average 1 hour per response, including the time for reviewing instructions, searching existing data sources, gathering and maintaining the data needed, and completing and reviewing the collection of information. Send comments regarding this burden estimate or any other aspect of this collection of information, including suggestions for reducing the burden, to Department of Defense, Washington Headquarters Services, Directorate for Information Operations and Reports (0704-0188), 1215 Jefferson Davis Highway, Suite 1204, Arlington, VA 22202-4302. Respondents should be aware that notwithstanding any other provision of law, no person shall be subject to any penalty for failing to comply with a collection of information if it does not display a currently valid OMB control number. PLEASE DO NOT RETURN YOUR FORM TO THE ABOVE ADDRESS. 1. REPORT DATE (DD-MM-YYYY) 2. REPORT TYPE 3. DATES COVERED (From - To) 12-2005 Technical 4. TITLE AND SUBTITLE 5a. CONTRACT NUMBER Seepage Chemistry Manual 5b. GRANT NUMBER 5c. PROGRAM ELEMENT NUMBER 6. AUTHOR(S) 5d. PROJECT NUMBER Craft, Doug 5e. TASK NUMBER 5f. WORK UNIT NUMBER 7. PERFORMING ORGANIZATION NAME(S) AND ADDRESS(ES) 8. PERFORMING ORGANIZATION REPORT Bureau of Reclamation, Technical Service Center, D-8290, PO Box 25007, NUMBER Denver CO 80225 DSO-05-03 9. SPONSORING/MONITORING AGENCY NAME(S) AND ADDRESS(ES) 10. -
Oxygen, Apparent Oxygen Utilization, and Dissolved Oxygen Saturation
NOAA Atlas NESDIS 83 WORLD OCEAN ATLAS 2018 Volume 3: Dissolved Oxygen, Apparent Oxygen Utilization, and Dissolved Oxygen Saturation Silver Spring, MD July 2019 U.S. DEPARTMENT OF COMMERCE National Oceanic and Atmospheric Administration National Environmental Satellite, Data, and Information Service National Centers for Environmental Information NOAA National Centers for Environmental Information Additional copies of this publication, as well as information about NCEI data holdings and services, are available upon request directly from NCEI. NOAA/NESDIS National Centers for Environmental Information SSMC3, 4th floor 1315 East-West Highway Silver Spring, MD 20910-3282 Telephone: (301) 713-3277 E-mail: [email protected] WEB: http://www.nodc.noaa.gov/ For updates on the data, documentation, and additional information about the WOA18 please refer to: http://www.nodc.noaa.gov/OC5/indprod.html This document should be cited as: Garcia H. E., K.W. Weathers, C.R. Paver, I. Smolyar, T.P. Boyer, R.A. Locarnini, M.M. Zweng, A.V. Mishonov, O.K. Baranova, D. Seidov, and J.R. Reagan (2019). World Ocean Atlas 2018, Volume 3: Dissolved Oxygen, Apparent Oxygen Utilization, and Dissolved Oxygen Saturation. A. Mishonov Technical Editor. NOAA Atlas NESDIS 83, 38pp. This document is available on-line at https://www.nodc.noaa.gov/OC5/woa18/pubwoa18.html NOAA Atlas NESDIS 83 WORLD OCEAN ATLAS 2018 Volume 3: Dissolved Oxygen, Apparent Oxygen Utilization, and Dissolved Oxygen Saturation Hernan E. Garcia, Katharine W. Weathers, Chris R. Paver, Igor Smolyar, Timothy P. Boyer, Ricardo A. Locarnini, Melissa M. Zweng, Alexey V. Mishonov, Olga K. Baranova, Dan Seidov, James R. -
La Niña's Effect on the Primary Productivity of Phytoplankton in The
La Niña’s effect on the primary productivity of phytoplankton in the equatorial Pacific Stephen R. Pang University of Washington School of Oceanography, Box 357940 Seattle, WA 98195-7940 Email: [email protected] March 4th, 2011 Pang, La Niña’s Affect on Productivity Summary Phytoplankton form the base of the food chain in the world’s oceans; their declining or increasing populations can have major impacts on the abundance of other marine species. An important question to be asked is: how might a major oceanic change, such as a La Niña event, affect the primary productivity of phytoplankton communities? Primary productivity is a measure of the rate at which new organic matter is produced through photosynthesis by primary producers such as phytoplankton. The rate at which primary production occurs in the ocean is largely controlled by two major physical factors: solar radiation availability and the physical forces that bring nutrients up from deep water. This study wants to determine if the latter can be influenced by a La Niña event. A La Niña event is defined by lower sea surface temperatures in the equatorial Pacific. Typically, water in the ocean is characterized by warmer, less dense water residing on top of colder, denser water. The lower sea surface temperatures induced by a La Niña event could reduce the intensity of this layering, or stratification, in the upper water column. With the stratification weakened, water is more likely to move vertically throughout the water column. Water that is normally deeper, denser, and colder than the overlying water is now much more likely to move upwards toward the surface in a phenomenon that is called upwelling. -
Oxygen Delivering Processes in Groundwater and Their Relevance for Iron -Related Well Clogging Processes – a Case Study on the Quaternary Aquifers of Berlin
OXYGEN DELIVERING PROCESSES IN GROUNDWATER AND THEIR RELEVANCE FOR IRON -RELATED WELL CLOGGING PROCESSES – A CASE STUDY ON THE QUATERNARY AQUIFERS OF BERLIN Dissertation zur Erlangung des akademischen Grades Dr. rer. nat. eingereicht am Fachbereich Geowissenschaften der Freien Universität Berlin vorgelegt von Christian Menz aus Friedberg/Hessen 2016 1. Gutachter: Prof. Dr. Michael Schneider 2. Gutachter: Priv.-Doz. Dr. Christoph Merz Disputation am 06.07.2016 3 Summary Redox condition, in particular the amount of oxygen in groundwater used for drinking water supply, is a key factor for the drinking water quality as well as for the production well’s lifecycle. Thus, a process-based and quantitative understanding about the oxygen fluxes in groundwater systems is fundamental in order to predict e.g. the removal capacity of pollutants or in particular the likelihood of iron-related well clogging. Such well ageing is a major thread for well operators and objective in practice and science. The formation of iron oxides responsible for well clogging is mainly known for wells abstracting groundwater from unconsolidated aquifers with a distinct redox zonation. The accumulation of precipitates is primarily taking place at the slots of the well screens, but also affects aquifers, pumps and collector pipes. Several studies already identified interacting hydro-chemical and microbiological processes as major cause for the development of iron oxides in wells. They develop in the presence of dissolved species of iron and oxygen in the water. The co-occurrence of both, the dissolved iron and oxygen, is the result of a mixing of groundwater with different redox states. The abstraction of groundwater by wells is known to promote such mixing processes.