4. Physical Removal Processes: Sedimentation and Filtration
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Circle Reverse Osmosis System
CIRCLE REVERSE OSMOSIS SYSTEM KEY FEATURES Water Saving Technology – Patented technology eliminates backpressure The RC100 conforms to common in conventional RO systems making the Circle up to 10 times more NSF/ANSI 42, 53 and efficient than existing products. 58 for the reduction of Saves You Money – Conventional RO systems waste up to 24 gallons of Aesthetic Chlorine, Taste water per every 1 gallon of filtered water produced. The Circle only wastes and Odor, Cyst, VOCs, an average of 2.1 gallons of water per 1 gallon of filtered water produced, Fluoride, Pentavalent Arsenic, Barium, Radium 226/228, Cadmium, Hexavalent saving you water and money over the life of the product!. Chromium, Trivalent Chromium, Lead, RO Filter Auto Flushing – Significantly extends life of RO filter. Copper, Selenium and TDS as verified Chrome Faucet Included – With integrated LED filter change indicator. and substantiated by test data. The RC100 conforms to NSF/ANSI 372 for Space Saving Compact Design – Integrated rapid refill tank means more low lead compliance. space under the sink. SPECIFICATIONS Product Name H2O+ Circle Reverse Osmosis Water Filtration System Model / SKU RC100 Installation Undercounter Sediment Filter, Pre-Carbon Plus Filter, Post Carbon Block Filter (RF-20): 6 months Filters & Lifespan RO Membrane Filter (RF-40): 24 months Tank Capacity 6 Liters (refills fully in less than one hour) Dimensions 9.25” (W) x 16.5” (H) x 13.75” (D) Net weight 14.6 lbs Min/Max Operating Pressure 40 psi – 120 psi (275Kpa – 827Kpa) Min/Max Water Feed Temp 41º F – 95º F (5º C – 35º C) Faucet Flow Rate 0.26 – 0.37 gallons per minute (gpm) at incoming water pressure of 20–100 psi Rated Service Flow 0.07 gallons per minute (gpm) Warranty One Year Warranty PO Box 470085, San Francisco CA, 94147–0085 brondell.com 888-542-3355. -
Sediment Transport in the San Francisco Bay Coastal System: an Overview
Marine Geology 345 (2013) 3–17 Contents lists available at ScienceDirect Marine Geology journal homepage: www.elsevier.com/locate/margeo Sediment transport in the San Francisco Bay Coastal System: An overview Patrick L. Barnard a,⁎, David H. Schoellhamer b,c, Bruce E. Jaffe a, Lester J. McKee d a U.S. Geological Survey, Pacific Coastal and Marine Science Center, Santa Cruz, CA, USA b U.S. Geological Survey, California Water Science Center, Sacramento, CA, USA c University of California, Davis, USA d San Francisco Estuary Institute, Richmond, CA, USA article info abstract Article history: The papers in this special issue feature state-of-the-art approaches to understanding the physical processes Received 29 March 2012 related to sediment transport and geomorphology of complex coastal–estuarine systems. Here we focus on Received in revised form 9 April 2013 the San Francisco Bay Coastal System, extending from the lower San Joaquin–Sacramento Delta, through the Accepted 13 April 2013 Bay, and along the adjacent outer Pacific Coast. San Francisco Bay is an urbanized estuary that is impacted by Available online 20 April 2013 numerous anthropogenic activities common to many large estuaries, including a mining legacy, channel dredging, aggregate mining, reservoirs, freshwater diversion, watershed modifications, urban run-off, ship traffic, exotic Keywords: sediment transport species introductions, land reclamation, and wetland restoration. The Golden Gate strait is the sole inlet 9 3 estuaries connecting the Bay to the Pacific Ocean, and serves as the conduit for a tidal flow of ~8 × 10 m /day, in addition circulation to the transport of mud, sand, biogenic material, nutrients, and pollutants. -
Sedimentation and Clarification Sedimentation Is the Next Step in Conventional Filtration Plants
Sedimentation and Clarification Sedimentation is the next step in conventional filtration plants. (Direct filtration plants omit this step.) The purpose of sedimentation is to enhance the filtration process by removing particulates. Sedimentation is the process by which suspended particles are removed from the water by means of gravity or separation. In the sedimentation process, the water passes through a relatively quiet and still basin. In these conditions, the floc particles settle to the bottom of the basin, while “clear” water passes out of the basin over an effluent baffle or weir. Figure 7-5 illustrates a typical rectangular sedimentation basin. The solids collect on the basin bottom and are removed by a mechanical “sludge collection” device. As shown in Figure 7-6, the sludge collection device scrapes the solids (sludge) to a collection point within the basin from which it is pumped to disposal or to a sludge treatment process. Sedimentation involves one or more basins, called “clarifiers.” Clarifiers are relatively large open tanks that are either circular or rectangular in shape. In properly designed clarifiers, the velocity of the water is reduced so that gravity is the predominant force acting on the water/solids suspension. The key factor in this process is speed. The rate at which a floc particle drops out of the water has to be faster than the rate at which the water flows from the tank’s inlet or slow mix end to its outlet or filtration end. The difference in specific gravity between the water and the particles causes the particles to settle to the bottom of the basin. -
Estuarine and Coastal Sedimentation Problems1
ESTUARINE AND COASTAL SEDIMENTATION PROBLEMS1 Leo C. van Rijn Delft Hydraulics and University of Utrecht, The Netherlands. E•mail: [email protected] Abstract: This Keynote Lecture addresses engineering sedimentation problems in estuarine and coastal environments and practical solutions of these problems based on the results of field measurements, laboratory scale models and numerical models. The three most basic design rules are: (1) try to understand the physical system based on available field data; perform new field measurements if the existing field data set is not sufficient (do not reduce on the budget for field measurements); (2) try to estimate the morphological effects of engineering works based on simple methods (rules of thumb, simplified models, analogy models, i.e. comparison with similar cases elsewhere); and (3) use detailed models for fine•tuning and determination of uncertainties (sensitivity study trying to find the most influencial parameters). Engineering works should be designed in a such way that side effects (sand trapping, sand starvation, downdrift erosion) are minimum. Furthermore, engineering works should be designed and constructed or built in harmony rather than in conflict with nature. This ‘building with nature’ approach requires a profound understanding of the sediment transport processes in morphological systems. Keywords: Sedimentation, sediment transport, morphological modelling 1. INTRODUCTION This lecture addresses sedimentation and erosion engineering problems in estuaries and coastal seas and practical solutions of these problems based on the results of field measurements, laboratory scale models and numerical models. Often, the sedimentation problem is a critical element in the economic feasibility of a project, particularly when each year relatively large quantities of sediment material have to be dredged and disposed at far•field locations. -
A Lexicon of Alchemy
A Lexicon of Alchemy by Martin Rulandus the Elder Translated by Arthur E. Waite John M. Watkins London 1893 / 1964 (250 Copies) A Lexicon of Alchemy or Alchemical Dictionary Containing a full and plain explanation of all obscure words, Hermetic subjects, and arcane phrases of Paracelsus. by Martin Rulandus Philosopher, Doctor, and Private Physician to the August Person of the Emperor. [With the Privilege of His majesty the Emperor for the space of ten years] By the care and expense of Zachariah Palthenus, Bookseller, in the Free Republic of Frankfurt. 1612 PREFACE To the Most Reverend and Most Serene Prince and Lord, The Lord Henry JULIUS, Bishop of Halberstadt, Duke of Brunswick, and Burgrave of Luna; His Lordship’s mos devout and humble servant wishes Health and Peace. In the deep considerations of the Hermetic and Paracelsian writings, that has well-nigh come to pass which of old overtook the Sons of Shem at the building of the Tower of Babel. For these, carried away by vainglory, with audacious foolhardiness to rear up a vast pile into heaven, so to secure unto themselves an immortal name, but, disordered by a confusion and multiplicity of barbarous tongues, were ingloriously forced. In like manner, the searchers of Hermetic works, deterred by the obscurity of the terms which are met with in so many places, and by the difficulty of interpreting the hieroglyphs, hold the most noble art in contempt; while others, desiring to penetrate by main force into the mysteries of the terms and subjects, endeavour to tear away the concealed truth from the folds of its coverings, but bestow all their trouble in vain, and have only the reward of the children of Shem for their incredible pain and labour. -
Coastal and Shelf Sediment Transport: an Introduction
Downloaded from http://sp.lyellcollection.org/ by guest on September 28, 2021 Coastal and shelf sediment transport: an introduction MICHAEL B. COLLINS 1'3 & PETER S. BALSON 2 1School of Ocean & Earth Science, University of Southampton, Southampton Oceanography Centre, European Way, Southampton S014 3ZH, UK (e-mail." mbc@noc, soton, ac. uk) 2Marine Research Division, AZTI Tecnalia, Herrera Kaia, Portu aldea z/g, Pasaia 20110, Gipuzkoa, Spain 3British Geological Survey, Kingsley Dunham Centre, Keyworth, Nottingham NG12 5GG, UK. Interest in sediment dynamics is generated by the (a) no single method for the determination of need to understand and predict: (i) morphody- sediment transport pathways provides the namic and morphological changes, e.g. beach complete picture; erosion, shifts in navigation channels, changes (b) observational evidence needs to be gathered associated with resource development; (ii) the in a particular study area, in which contem- fate of contaminants in estuarine, coastal and porary and historical data, supported by shelf environment (sediments may act as sources broad-based measurements, is interpreted and sinks for toxic contaminants, depending by an experienced practitioner (Soulsby upon the surrounding physico-chemical condi- 1997); tions); (iii) interactions with biota; and (iv) of (c) the form and internal structure of sedimen- particular relevance to the present Volume, inter- tary sinks can reveal long-term trends in pretations of the stratigraphic record. Within this transport directions, rates and magnitude; context of the latter interest, coastal and shelf (d) complementary short-term measurements sediment may be regarded as a non-renewable and modelling are required, to (b) (above) -- resource; as such, their dynamics are of extreme any model of regional sediment transport importance. -
Settling Velocities of Particulate Systems†
Settling Velocities of Particulate Systems† F. Concha Department of Metallurgical Engineering University of Concepción.1 Abstract This paper presents a review of the process of sedimentation of individual particles and suspensions of particles. Using the solutions of the Navier-Stokes equation with boundary layer approximation, explicit functions for the drag coefficient and settling velocities of spheres, isometric particles and arbitrary particles are developed. Keywords: sedimentation, particulate systems, fluid dynamics Discrete sedimentation has been successful to 1. Introduction establish constitutive equations in processes using Sedimentation is the settling of a particle, or sus- sedimentation. It establishes the sedimentation prop- pension of particles, in a fluid due to the effect of an erties of a certain particulate material in a given fluid. external force such as gravity, centrifugal force or Nevertheless, to analyze a sedimentation process and any other body force. For many years, workers in to obtain behavioral pattern permitting the prediction the field of Particle Technology have been looking of capacities and equipment design procedures, an- for a simple equation relating the settling velocity of other approach is required, the so-called continuum particles to their size, shape and concentration. Such approach. a simple objective has required a formidable effort The physics underlying sedimentation, that is, the and it has been solved only in part through the work settling of a particle in a fluid is known since a long of Newton (1687) and Stokes (1844) of flow around time. Stokes presented the equation describing the a particle, and the more recent research of Lapple sedimentation of a sphere in 1851 and that can be (1940), Heywood (1962), Brenner (1964), Batchelor considered as the starting point of all discussions of (1967), Zenz (1966), Barnea and Mitzrahi (1973) the sedimentation process. -
Soil Erosion, Runoff, and Sedimentation Construction Site Fact Sheet No
Soil Erosion, Runoff, and Sedimentation Construction Site Fact Sheet No. 1 What Is Soil Erosion? What Problems Happen On Construction Soil erosion is the detachment and movement of soil Sites? particles by water, wind, ice, or gravity. Safety and Nuisance Issues – Sediment on roadways and in the air can cause safety hazards. Flooding– Excessive sediment accumulation in drainage systems can create blockages that promote flooding. Sediment Build‐Up – Sediment that accumulates in streams, lakes, and bays can only be remediated by costly dredging. Increased Costs – Uncontrolled erosion and sedimentation requires costly maintenance and What Is Sedimentation? repair. It is cheaper and easier to PREVENT Sediment is the result of erosion. Sedimentation is erosion than to fix sedimentation problems. the build‐ up of eroded soil particles that are transported in runoff from their site of origin and Negative Public Perception ‐Observing muddy deposited in drainage systems, on other ground water flowing from construction sites negatively surfaces, or in bodies of water or wetlands. effects public perception. Why Should I Care? It’s the Law– Federal, State and local regulations require construction sites to be compliant with the Clean Water Act. Water Quality‐Erosion from construction projects can be a non‐point source pollutant that deteriorates the health of our lakes, streams and Narragansett Bay. Soil Loss ‐ Much of the total sediment loss that occurs each year is generated by highway construction and land development projects. Quality of Life‐ If you enjoy fishing, eating local Sediment‐filled runoff from a RIDOT construction site shellfish or swimming at one of Rhode Island’s beautiful beaches, this pollution can threaten your quality of life. -
CIVL 1101 Introduction to Filtration 1/15
CIVL 1101 Introduction to Filtration 1/15 Water Treatment Water Treatment Water treatment describes those industrial-scale The goal of all water treatment process is to processes used to make water more acceptable remove existing contaminants in the water, or for a desired end-use. reduce the concentration of such contaminants so These can include use for drinking water, industry, the water becomes fit for its desired end-use. medical and many other uses. One such use is returning water that has been used back into the natural environment without adverse ecological impact. Water Treatment Water Treatment Basis water treatment consists Coagulation of four processes: This process helps removes Coagulation/Flocculation particles suspended in water. Sedimentation Chemicals are added to water to form tiny sticky particles Filtration called "floc" which attract the Disinfection particles. Water Treatment Water Treatment Flocculation Sedimentation Flocculation refers to water The heavy particles (floc) treatment processes that settle to the bottom and the combine or coagulate small clear water moves to filtration. particles into larger particles, which settle out of the water as sediment. CIVL 1101 Introduction to Filtration 2/15 Water Treatment Water Treatment Filtration Disinfection The water passes through A small amount of chlorine is filters, some made of layers of added or some other sand, gravel, and charcoal disinfection method is used to that help remove even smaller kill any bacteria or particles. microorganisms that may be in the water. Water Treatment Water Treatment 1. Coagulation 1. Coagulation - Aluminum or iron salts plus chemicals 2. Flocculation called polymers are mixed with the water to make the 3. -
REFERENCE GUIDE to Treatment Technologies for Mining-Influenced Water
REFERENCE GUIDE to Treatment Technologies for Mining-Influenced Water March 2014 U.S. Environmental Protection Agency Office of Superfund Remediation and Technology Innovation EPA 542-R-14-001 Contents Contents .......................................................................................................................................... 2 Acronyms and Abbreviations ......................................................................................................... 5 Notice and Disclaimer..................................................................................................................... 7 Introduction ..................................................................................................................................... 8 Methodology ................................................................................................................................... 9 Passive Technologies Technology: Anoxic Limestone Drains ........................................................................................ 11 Technology: Successive Alkalinity Producing Systems (SAPS).................................................. 16 Technology: Aluminator© ............................................................................................................ 19 Technology: Constructed Wetlands .............................................................................................. 23 Technology: Biochemical Reactors ............................................................................................. -
Membrane Filtration
Membrane Filtration A membrane is a thin layer of semi-permeable material that separates substances when a driving force is applied across the membrane. Membrane processes are increasingly used for removal of bacteria, microorganisms, particulates, and natural organic material, which can impart color, tastes, and odors to water and react with disinfectants to form disinfection byproducts. As advancements are made in membrane production and module design, capital and operating costs continue to decline. The membrane processes discussed here are microfiltration (MF), ultrafiltration (UF), nanofiltration (NF), and reverse osmosis (RO). MICROFILTRATION Microfiltration is loosely defined as a membrane separation process using membranes with a pore size of approximately 0.03 to 10 micronas (1 micron = 0.0001 millimeter), a molecular weight cut-off (MWCO) of greater than 1000,000 daltons and a relatively low feed water operating pressure of approximately 100 to 400 kPa (15 to 60psi) Materials removed by MF include sand, silt, clays, Giardia lamblia and Crypotosporidium cysts, algae, and some bacterial species. MF is not an absolute barrier to viruses. However, when used in combination with disinfection, MF appears to control these microorganisms in water. There is a growing emphasis on limiting the concentrations and number of chemicals that are applied during water treatment. By physically removing the pathogens, membrane filtration can significantly reduce chemical addition, such as chlorination. Another application for the technology is for removal of natural synthetic organic matter to reduce fouling potential. In its normal operation, MF removes little or no organic matter; however, when pretreatment is applied, increased removal of organic material can occur. -
Sedimentary Rock Formation Models
Sedimentary Rock Formation Models 5.7 A Explore the processes that led to the formation of sedimentary rock and fossil fuels. The Formation Process Explained • Formation of these rocks is one of the important parts of the rock cycle. For millions of years, the process of deposition and formation of these rocks has been operational in changing the geological structure of earth and enriching it. Let us now see how sedimentary rocks are formed. Weathering The formation process begins with weathering of existent rock exposed to the elements of nature. Wind and water are the chisels and hammers that carve and sculpt the face of the Earth through the process of weathering. The igneous and metamorphic rocks are subjected to constant weathering by wind and water. These two elements of nature wear out rocks over a period of millions of years creating sediments and soil from weathered rocks. Other than this, sedimentation material is generated from the remnants of dying organisms. Transport of Sediments and Deposition These sediments generated through weathering are transported by the wind, rivers, glaciers and seas (in suspended form) to other places in the course of flow. They are finally deposited, layer over layer by these elements in some other place. Gravity, topographical structure and fluid forces decide the resting place of these sediments. Many layers of mineral, organics and chemical deposits accumulate together for years. Layers of different deposits called bedding features are created from them. Crystal formation may also occur in these conditions. Lithification (Compaction and Cementation) Over a period of time, as more and more layers are deposited, the process of lithification begins.