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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 -
O2 Secretion in the Eye and Swimbladder of Fishes
1641 The Journal of Experimental Biology 209, 1641-1652 Published by The Company of Biologists 2007 doi:10.1242/jeb.003319 Historical reconstructions of evolving physiological complexity: O2 secretion in the eye and swimbladder of fishes Michael Berenbrink School of Biological Sciences, The University of Liverpool, Biosciences Building, Crown Street, Liverpool, L69 7ZB, UK e-mail: [email protected] Accepted 12 March 2007 Summary The ability of some fishes to inflate their compressible value of haemoglobin. These changes predisposed teleost swimbladder with almost pure oxygen to maintain neutral fishes for the later evolution of swimbladder oxygen buoyancy, even against the high hydrostatic pressure secretion, which occurred at least four times independently several thousand metres below the water surface, has and can be associated with increased auditory sensitivity fascinated physiologists for more than 200·years. This and invasion of the deep sea in some groups. It is proposed review shows how evolutionary reconstruction of the that the increasing availability of molecular phylogenetic components of such a complex physiological system on a trees for evolutionary reconstructions may be as important phylogenetic tree can generate new and important insights for understanding physiological diversity in the post- into the origin of complex phenotypes that are difficult to genomic era as the increase of genomic sequence obtain with a purely mechanistic approach alone. Thus, it information in single model species. is shown that oxygen secretion first evolved in the eyes of fishes, presumably for improved oxygen supply to an Glossary available online at avascular, metabolically active retina. Evolution of this http://jeb.biologists.org/cgi/content/full/210/9/1641/DC1 system was facilitated by prior changes in the pH dependence of oxygen-binding characteristics of Key words: oxygen secretion, Root effect, rete mirabile, choroid, haemoglobin (the Root effect) and in the specific buffer swimbladder, phylogenetic reconstruction. -
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. -
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. -
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. -
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. -
Pulse Oximetry Pulse Oximetry Is a Way to Measure How Much Oxygen Your Blood Is Carrying
American Thoracic Society PATIENT EDUCATION | INFORMATION SERIES Pulse Oximetry Pulse oximetry is a way to measure how much oxygen your blood is carrying. By using a small device called a pulse oximeter, your blood oxygen level can be checked without needing to be stuck with a needle. The blood oxygen level measured with an oximeter is called your oxygen saturation level (abbreviated O2sat or SaO2). This is a percentage of how much oxygen your blood is carrying compared to the maximum it is capable of carrying. Normally, more than 89% of your red blood should be carrying oxygen. Why is it important to have my blood is carrying oxygen. It also provides a reading of your oxygen level checked? heart rate (pulse). To make sure the oximeter is giving If you have a lung disease, your blood oxygen level may you a good reading, count your pulse for one minute be lower than normal. This is important to know because and compare the number you get to the pulse number when your oxygen level is low, the cells in your body can on the oximeter. If they are the same, you are getting a have a hard time working properly. Oxygen is the “gas” good signal. that makes your body “go,” and if you are low on “gas,” Should I get a pulse oximeter? your body does not run smoothly. Having a very low Most people do not normally need a pulse oximeter, blood oxygen level also can put a strain on your heart and brain. though during the COVID-19 pandemic, many people are using them to check their oxygen levels. -
Dissolved Oxygen and Biochemical Oxygen Demand in the Waters Close to the Quelimane Sewage Discharge
Dissolved Oxygen and Biochemical Oxygen Demand in the waters close to the Quelimane sewage discharge. Jeremias Joaquim Mocuba Master thesis in Chemical Oceanography NOMA Supervisors: Eva Falck Geophysical Institute, University of Bergen – Norway António Mubango Hoguane School of Marine and Coastal Sciences, Eduardo Mondlane University –Quelimane June 2010 Acknowledgements First I would like to thank my supervisors Eva Falck and António Mubango Hoguane, for their determined contribution, monitoring, and encouragement on this work; it was good to work with them. Very thanks to Tor Gammelsrød, NOMA project manager, for his valuable support throughout the master studies and for his complete hospitality in Bergen. I am immensely thankful to the NOMA program for the scholarship received and the opportunity to study in Norway. I am grateful to Kristin Kalvik, Marie Louise Ljones and Knut Barthel for their assisting in student affairs at the Bergen University. I would like to address with special thanks to my teachers Tor Gammelsrød, Truls Johannessen, Christoph Heinze, Ingunn Skjelvan, Eva FalcK, Knut Barthel, Øyvind Breivik, Svein Sundby, Solfrid Hjøllo Sætre, Ana Lucas and all those who contributed directly and indirectly in my studies. I am grateful to my classmates Ahmed, Elfatih, Salma, Waleed, Cândida, Naftal, and Valentina for their company in Bergen. Abstract The River dos Bons Sinais Estuary is one of the most important estuaries in the central region of the Mozambican coast. It is situated between the confluence of Cuácua and Licuári rivers and the Mozambican Channel in the Indian Ocean. The climate is subtropical with the rain season generally from November to April. -
BOD Analysis: Basics and Particulars
BOD Analysis: Basics and Particulars George Bowman sponsored by: Inorganics Supervisor State Laboratory of Hygiene Rick Mealy Regional Certification Coordinator DNR-Laboratory Certification Disclaimer Any reference to product or company names does not constitute endorsement by the Wisconsin State Laboratory of Hygiene, the University of Wisconsin, or the Department of Natural Resources. April 2001 InformationInformation UpdatesUpdates Watch for…. Text highlighted like this indicates additional or updated information that is NOT on your handouts …be sure to annotate your handouts!!! Session Objectives Discuss Importance and Use of BOD Review Method and QC requirements Troubleshoot: QA/QC problems Identify Common Problems Experienced Troubleshoot: Common Problems Demonstrate: calibration, seeding, probe maintenance Troubleshoot: GGA and dilution water issues Discuss documentation required Provide necessary tools to pass audits Course Outline Overview Sampling/Sample Handling Equipment O2 Measurement Techniques Calibration Method Details Quality Control Troubleshooting Documentation BOD Basics What is it? • Bioassay technique • used to assess the relative strength of a waste −the amount of oxygen required −to stabilize it if discharged to a surface water. Significance of the BOD Test • Most commonly required test on WPDES and NPDES discharge permits. • Widely used in facility planning • Assess waste loading on surface waters • Characterized as the “Test everyone loves to hate” The test everyone loves to hate Rick George BOD Test: Limitations Test period is too long not good for process control Test is imprecise and unpredictable The test is simply not very easy - a lot of QC makes it time-consuming - can take years of experience to master it Cannot evaluate accuracy no universally accepted standard other than GGA accuracy at 200 ppm vs.