11 Total Dissolved Solids (TDS)
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World Bank Document
WATER GLOBAL PRACTICE QUALITY UNKNOWN BACKGROUND PAPER Public Disclosure Authorized Determinants of Public Disclosure Authorized Essayas Ayana Declining Water Quality Public Disclosure Authorized Public Disclosure Authorized About the Water Global Practice Launched in 2014, the World Bank Group’s Water Global Practice brings together financing, knowledge, and implementation in one platform. By combining the Bank’s global knowledge with country investments, this model generates more firepower for transformational solutions to help countries grow sustainably. Please visit us at www.worldbank.org/water or follow us on Twitter at @WorldBankWater. About GWSP This publication received the support of the Global Water Security & Sanitation Partnership (GWSP). GWSP is a multidonor trust fund administered by the World Bank’s Water Global Practice and supported by Australia’s Department of Foreign Affairs and Trade, the Bill & Melinda Gates Foundation, the Netherlands’ Ministry of Foreign Affairs, Norway’s Ministry of Foreign Affairs, the Rockefeller Foundation, the Swedish International Development Cooperation Agency, Switzerland’s State Secretariat for Economic Affairs, the Swiss Agency for Development and Cooperation, U.K. Department for International Development, and the U.S. Agency for International Development. Please visit us at www.worldbank.org/gwsp or follow us on Twitter #gwsp. Determinants of Declining Water Quality Essayas Ayana © 2019 International Bank for Reconstruction and Development / The World Bank 1818 H Street NW, Washington, DC 20433 Telephone: 202-473-1000; Internet: www.worldbank.org This work is a product of the staff of The World Bank with external contributions. The findings, interpretations, and conclusions expressed in this work do not necessarily reflect the views of The World Bank, its Board of Executive Directors, or the governments they represent. -
Plants in Constructed Wetlands Help to Treat Agricultural Processing Wastewater
UC Agriculture & Natural Resources California Agriculture Title Plants in constructed wetlands help to treat agricultural processing wastewater Permalink https://escholarship.org/uc/item/67s9p4z8 Journal California Agriculture, 65(2) ISSN 0008-0845 Authors Grismer, Mark E Shepherd, Heather L Publication Date 2011 Peer reviewed eScholarship.org Powered by the California Digital Library University of California ReseaRch aRticle ▼ Plants in constructed wetlands help to treat agricultural processing wastewater by Mark E. Grismer and Heather L. Shepherd Over the past three decades, winer- ies in the western United States and sugarcane processing for ethanol in Central and South America have experienced problems related to the treatment and disposal of pro- cess wastewater. Both winery and sugarcane (molasses) wastewaters are characterized by large organic loadings that change seasonally and are detrimental to aquatic life. We examined the role of plants for treating these wastewaters in constructed wetlands. In the green- house, subsurface-flow flumes with agricultural processing wastewaters may have high concentrations of organic matter that volcanic rock substrates and plants contaminate surface waters when discharged downstream. at imagery estate Winery in Glen ellen, constructed wetlands with plants were tested for their ability to remove pollutants. steadily removed approximately 80% of organic-loading oxygen demand Shepherd et al. (2001) described the sugarcane and winery wastewater from sugarcane process wastewater negative impacts of winery wastewater Sugarcane, food-processing, winery after about 3 weeks of plant growth; downstream, which led to requirements and other distilleries generate waste- for its control and on-site treatment. waters from processing and equipment unplanted flumes removed about Similarly, downstream degradation wash-down. -
Great Salt Lake Brine Chemistry Database, 1966–2011
GREAT SALT LAKE BRINE CHEMISTRY DATABASE, 1966–2011 by Andrew Rupke and Ammon McDonald OPEN-FILE REPORT 596 UTAH GEOLOGICAL SURVEY a division of UTAH DEPARTMENT OF NATURAL RESOURCES 2012 GREAT SALT LAKE BRINE CHEMISTRY DATABASE, 1966–2011 by Andrew Rupke and Ammon McDonald Cover photo: The Southern Pacific Railroad rock causeway. The view is to the east, and the north arm of Great Salt Lake is on the left. OPEN-FILE REPORT 596 UTAH GEOLOGICAL SURVEY a division of UTAH DEPARTMENT OF NATURAL RESOURCES 2012 STATE OF UTAH Gary R. Herbert, Governor DEPARTMENT OF NATURAL RESOURCES Michael Styler, Executive Director UTAH GEOLOGICAL SURVEY Richard G. Allis, Director PUBLICATIONS contact Natural Resources Map & Bookstore 1594 W. North Temple Salt Lake City, UT 84116 telephone: 801-537-3320 toll-free: 1-888-UTAH MAP website: mapstore.utah.gov email: [email protected] UTAH GEOLOGICAL SURVEY contact 1594 W. North Temple, Suite 3110 Salt Lake City, UT 84116 telephone: 801-537-3300 website: geology.utah.gov This open-file release makes information available to the public that may not conform to UGS technical, edito- rial, or policy standards; this should be considered by an individual or group planning to take action based on the contents of this report. Although this product represents the work of professional scientists, the Utah Department of Natural Resources, Utah Geological Survey, makes no warranty, expressed or implied, regarding its suitability for a particular use. The Utah Department of Natural Resources, Utah Geological Survey, shall not be liable under any circumstances for any direct, indirect, special, incidental, or consequential damages with respect to claims by users of this product. -
Aquarius Salinity & Density Bead Activity
Floating in a Salty Sea JPL Aquarius Workshop Background If there is one thing that just about everyone knows about the ocean, it’s that it is salty. The two most common elements in sea water, after oxygen and hydrogen, are sodium and chloride. Sodium and chloride combine to form what we know as table salt. If you allow the wind to dry your skin after swimming in the ocean, you will see a light coasting of salt that has been left behind when the water evaporated. Salinity is a measure of how much salt is in the water. Sea water salinity is expressed as a ratio of salt (in grams) to liter of water. In sea water there is typically close to 35 grams of dissolved salts in each liter. Scientists describe salinity using Practical Salinity Units (PSU) which defines salinity in terms of a conductivity ratio, so it is dimensionless. Salinity was formerly expressed in terms of parts per thousand or by weight (written as ppt or ‰). That is, a salinity of 35 ppt meant 35 grams of salt per 1,000 ml (1 liter) of sea-water. The normal range of open ocean salinity is between 32-37 grams per liter (32‰ - 37‰). Salinity affects density. Density is the mass per unit volume (mass/volume) of a substance. Salty waters are denser than fresh water at the same temperature. Both salt and temperature are important influences on density: density increases with increased salinity and decreases with increased temperature. As you might expect, in the ocean there are areas of high and low salinity. -
Total Dissolved Solids in Drinking-Water
WHO/SDE/WSH/03.04/16 English only Total dissolved solids in Drinking-water Background document for development of WHO Guidelines for Drinking-water Quality __________________ Originally published in Guidelines for drinking-water quality, 2nd ed. Vol. 2. Health criteria and other supporting information. World Health Organization, Geneva, 1996. © World Health Organization 2003 All rights reserved. Publications of the World Health Organization can be obtained from Marketing and Dissemination, World Health Organization, 20 Avenue Appia, 1211 Geneva 27, Switzerland (tel: +41 22 791 2476; fax: +41 22 791 4857; email: [email protected]). Requests for permission to reproduce or translate WHO publications - whether for sale or for noncommercial distribution - should be addressed to Publications, at the above address (fax: +41 22 791 4806; email: [email protected]). 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 concerning the legal status of any country, territory, city or area or of its authorities, or concerning the delimitation of its frontiers or boundaries. The mention of specific companies or of certain manufacturers’ products does not imply that they are endorsed or recommended by the World Health Organization in preference to others of a similar nature that are not mentioned. Errors and omissions excepted, the names of proprietary products are distinguished by initial capital letters. The World Health -
Investigation of Total Dissolved Solids Regulation In
Investigation of Total Dissolved Solids Regulation in the Appalachian Plateau Physiographic Province: A Case Study from Pennsylvania and Recommendations for the Future by Mark Wozniak A project submitted to the Graduate Faculty of North Carolina State University in partial fulfillment of the requirements for the degree of Masters of Environmental Assessment Raleigh, North Carolina 2011 Advisory Chair: Linda Taylor ii ABSTRACT WOZNIAK, MARK. Investigation of Total Dissolved Solids Regulation in the Appalachian Plateau Physiographic Province: A Case Study from Pennsylvania and Recommendations for the Future. (Under the direction of Linda Taylor and Dr. Chris Hofelt). Total dissolved solids (TDS) are a natural constituent of surface water throughout the world. The World Health Organization, U.S. Environmental Protection Agency, and most states regulate TDS as a secondary drinking water criteria, affecting taste and odor, limiting discharges to 500 mg/L. This method of regulation fails to account for the conservative nature of TDS, with in-stream concentrations increasing with each addition, as well as impacts to aquatic life. New sources of TDS are further stressing historically contaminated waterways throughout the Appalachian Plateau, leaving them unable to assimilate additional TDS. With these new sources only projected to increase, it is necessary, now more than ever, for the states to develop total maximum daily loads for the affected waterways. This is the most effective method for regulating TDS to ensure the sustained health of the regional aquatic communities and human health. iii BIOGRAPHY Mark Wozniak has lived in western Pennsylvania all his life, where he attained an interest in all aspects of the natural environment at an early age. -
Treatability of a Highly-Impaired, Saline Surface Water for Potential Urban Water Use
water Article Treatability of a Highly-Impaired, Saline Surface Water for Potential Urban Water Use Frederick Pontius Department of Civil Engineering and Construction Management, Gordon and Jill Bourns College of Engineering, California Baptist University, Riverside, CA 92504, USA; [email protected]; Tel.: +1-951-343-4846 Received: 14 January 2018; Accepted: 14 March 2018; Published: 15 March 2018 Abstract: As freshwater sources of drinking water become limited, cities and urban areas must consider higher-salinity waters as potential sources of drinking water. The Salton Sea in the Imperial Valley of California has a very high salinity (43 ppt), total dissolved solids (70,000 mg/L), and color (1440 CU). Future wetlands and habitat restoration will have significant ecological benefits, but salinity levels will remain elevated. High salinity eutrophic waters, such as the Salton Sea, are difficult to treat, yet more desirable sources of drinking water are limited. The treatability of Salton Sea water for potential urban water use was evaluated here. Coagulation-sedimentation using aluminum chlorohydrate, ferric chloride, and alum proved to be relatively ineffective for lowering turbidity, with no clear optimum dose for any of the coagulants tested. Alum was most effective for color removal (28 percent) at a dose of 40 mg/L. Turbidity was removed effectively with 0.45 µm and 0.1 µm microfiltration. Bench tests of Salton Sea water using sea water reverse osmosis (SWRO) achieved initial contaminant rejections of 99 percent salinity, 97.7 percent conductivity, 98.6 percent total dissolved solids, 98.7 percent chloride, 65 percent sulfate, and 99.3 percent turbidity. -
Water Quality Salinity Standards
Water quality standards Electrical conductivity is a measure of the saltiness of the water and is measured on a scale from 0 to 50,000 uS/cm. Electrical conductivity is measured in microsiemens per centimeter (uS/cm). Freshwater is usually between 0 and 1,500 uS/cm and typical sea water has a conductivity value of about 50,000 uS/cm. Low levels of salts are found naturally in waterways and are important for plants and animals to grow. When salts reach high levels in freshwater it can cause problems for aquatic ecosystems and complicated human uses. μS/cm Use 0 - 800 • Good drinking water for humans (provided there is no organic pollution and not too much suspended clay material) • Generally good for irrigation, though above 300μS/cm some care must be, particularly with overhead sprinklers, which may cause leaf, scorch on some salt sensitive plants. • Suitable for all livestock 800 - 2500 • Can be consumed by humans, although most would prefer water in the lower half of this range if available • When used for irrigation, requires special management including suitable soils, good drainage and consideration of salt tolerance of plants • Suitable for all livestock 2500 -10,000 • Not recommended for human consumption, although water up to 3000 μS/cm can be consumed • Not normally suitable for irrigation, although water up to 6000 μS/cm can be used on very salt tolerant crops with very special management techniques. Over 6000 μS/cm, occasional emergency may be possible with care • When used for drinking water by poultry and pigs, the salinity should be limited to about 6000 μS/cm. -
Urban-Salinity-Groundwater-Basics.Pdf
First published 2005 © Department of Infrastructure, Planning and Natural Resources Groundwater Basics for Understanding Urban Salinity Local Government Salinity Initiative - Booklet No.9 ISBN: 07347 5441 8 Contents 1. Introduction 3 2. What is Groundwater? 3 3. The Importance of Groundwater 5 4. The Hydrological Cycle 6 5. Water Table Changes 7 5.1 Changes Over Time 7 5.2 Regional Shape of the Water Table 9 5.3 Water Balance and Water Table Rises 9 6. Porosity 10 7. Porosity in Sediments and Different Rock Types 11 7.1 Primary Porosity 11 7.2 Secondary Porosity 12 8. Permeability 13 8.1 Non-Porous Permeable Materials 13 8.2 Porous Impermeable Materials 13 8.3 Poorly Connected Pores 14 9. Aquifers 14 10. Salt Accumulation, How Does it Happen? 18 11. How does the Groundwater Reach the Earth’s Surface? 19 11.1 Capillary Rise 19 11.2 Faults 20 11.3 Restrictions to Groundwater Flow 20 11.4 Contrasts of Permeability 21 12. The Development of Urban Salinity 23 13. Managing Urban Salinity 24 14. References 25 1 2 dug, water from the saturated soil will flow 1. Introduction into the excavated hole. This booklet is part of the “Local Government Salinity Initiative” series and presents some basic groundwater concepts necessary for understanding urban salinity processes. Other booklets in the series contain information on urban salinity identification, investigation, impacts and management. 2. What is Groundwater? If a hole is dug in loose earth material such as soil or sand, we may find that just below the surface the earth feels moist. -
Salinity Experiment Teacher Notes
Teacher’s Notes EXPERIMENT 1 THE EFFECTS OF SALT ON CUT VEGETABLES AIM: To see what happens to cut vegetables in water when salt is added to the water. MATERIALS: You will need – • 4 cups, jars or bowls of water — big enough to hold 500 ml • 2 Litres of water • 4 bunches of spinach (baby spinach with roots is best) • 7 teaspoons of salt METHOD: Step 1 — Label each of the 4 containers with the numbers 1, 2, 3 & 4. Step 2 — Pour 500 ml of water into each container. Step 3 — Add 1 teaspoon of salt (approx. 5 ml) to container 1 Add 2 teaspoons of salt (approx. 10 ml) to container 2, Add 4 teaspoons of salt (approx. 20 ml) to container 3, Do not add any salt to container 4. It should hold water only. Step 4 — Place one bunch of spinach into each of the 4 containers. RESULTS: Write down what each bunch of the spinach looks like. Describe its position, colour and any other observations you make. Bunch 1: Some wilti ng of spinach Bunch 2: Wilti ng of spinach – more than bunch 1 Bunch 3: A lot of wilti ng of spinach – more than bunch 1 & 2 Bunch 4: Litt le wilti ng of spinach if any at all EXPERIMENT 1 : THE EFFECTS OF SALT ON CUT VEGETABLES EXPECTED RESULTS: Each bunch of spinach, apart from the fi rst one in freshwater, will show some sign of wilti ng and/or discolourati on. The bunch in the highest concentrati on of salt will show greatest signs of damage. -
Summary of Water Quality Indicators-Surface Waters Page 2 Around 9 Mg/L
HOW WATER QUALITY INDICATORS WORK Following are summaries of water quality indicators from several sources collated by the International Water Institute. They provide information about how the specific water quality indicators describe river health and factors affecting them. Other sources: http://ga.water.usgs.gov/edu/characteristics.html, and http://bcn.boulder.co.us/basin/data/NUTRIENTS/info/ *************************************************************************************** Following from FM RIVER at: http://www.undeerc.org/watman/FMRiver/PPTV/factsheets.asp Electrical Conductivity The electrical conductivity of water is directly related to the concentration of dissolved solids in the water. Ions from the dissolved solids in water influence the ability of that water to conduct an electrical current, which can be measured using a conductivity meter. When correlated with laboratory TDS measurements, electrical conductivity can provide an accurate estimate of the TDS concentration. Conductivity measurements for the Red River correlate very closely to the TDS determinations. Water in the Red River is usually below the 900 microsiemens/cm (red line on graph) set for drinking water by EPA's National Secondary Water Standards even before entering the local The Red River contains 1/70th the water treatment plants. dissolved minerals found in seawater. Graph of electrical conductivity (μS/cm) for the Red River in the FM metro area for the period July 2001 to April 2003 in relation to the EPA guideline (900 μS/cm; red line) for drinking water. Dissolved Oxygen Dissolved oxygen (DO) refers to the amount of oxygen (O2) dissolved in water. Because fish and other aquatic organisms cannot survive without oxygen, DO is one of the most important water quality parameters. -
Increasing Salinity Affects on Heavy Metal Concentration
INCREASING SALINITY AFFECTS ON HEAVY METAL CONCENTRATION CHEYENE KENISTON California State University of Sacramento, 6000 J Street, Sacramento, CA 95819 USA MENTOR SCIENTIST: DR. STUART FINDLAY Cary Institute of Ecosystem Studies, Millbrook, NY 12545 USA Abstract. Global climate change is being accelerated because of many anthropogenic reasons. This contributes to many ecosystems alterations throughout the world. Warmer temperatures and melting sea ice are two factors that contribute greatly to sea level rise, which is causing salt-water intrusion into many ecotones. The Hudson River wetland ecosystems will potentially experience this salt intrusion phenomenon. Salinity is increasing within tidal freshwater wetlands, altering these important ecosystems and their functionality. Wetlands along the Hudson River have also historically experienced high levels of heavy metal pollution; therefore, the sediments have stored heavy metals. The questions that I addressed are: 1) Will an increase in water salinity within the Tivoli wetlands draw stored lead out of the sediment? 2) Will the increase in salinity affect the lead absorption properties of the sediment? My hypothesis is that an increase in water salinity at the Tivoli wetlands will displace the lead stored in the sediment, increasing the heavy metal concentrations in the water and also decreasing the sediment’s capacity to absorb lead from the overlaying water. Through a manipulative experiment, I tested the effects of multiple saline and lead solutions on Tivoli wetland sediment cores. There was not a significant increase of lead, within the overlaying water, that leached out of the sediment exposed to different salinities. Although all sediment cores continued to have lead absorption properties after the saline soak, there was a significant relationship between an increased saline water level and less absorption of lead from the overlaying water.