Preliminary Estimates of Residence Times and Apparent Ages of Ground Water in the Chesapeake Bay Watershed

Total Page:16

File Type:pdf, Size:1020Kb

Preliminary Estimates of Residence Times and Apparent Ages of Ground Water in the Chesapeake Bay Watershed PreliminaryEstimatesofResidenceTimes andApparentAgesofGroundWaterinthe ChesapeakeBayWatershed,andWater- QualityDataFromaSurveyofSprings Water-ResourcesInvestigationsReport97-4225 U.S.DepartmentoftheInterior U.S.GeologicalSurvey U.S.DepartmentoftheInterior U.S.GeologicalSurvey PreliminaryEstimatesofResidenceTimes andApparentAgesofGroundWaterinthe ChesapeakeBayWatershed,andWater- QualityDataFromaSurveyofSprings byM.J.Focazio,L.N.Plummer,J. K. Bohlke,EurybiadesBusenberg,L.J.Bachman,andD.S.Powars Water-ResourcesInvestigationsReport97-4225 Richmond,Virginia September1998 U.S.DepartmentoftheInterior BruceBabbitt,Secretary U.S.GeologicalSurvey ThomasJ.Casadevall,ActingDirector Theuseoftrade,product,orfirmnamesinthisreportisfor descriptivepurposesonlyanddoesnotimplyendorsement bytheU.S.GeologicalSurvey. UnitedStatesGovernmentPrintingOffice:1998 Foradditionalinformationcontact: DistrictChief U.S.GeologicalSurvey,WRD 8987YellowBrickRoad Baltimore,MD21237 Copiesofthisreportcanbepurchasedfrom: U.S.GeologicalSurvey BranchofInformationServices Box25286 Denver,CO80225-0286 CONTRIBUTING U.S. GEOLOGICAL SURVEY STAFF TECHNICAL SUPPORT TECHNICAL REVIEWERS OR ADVISORS Richard J. Ahlin, Hydrologic Technician Joel E. Dysart, Hydrologist Gerolamo C. Casile, Hydrologist David L. Nelms, Hydrologist Douglas C. Chichester, Hydrologist Dennis W. Risser, Ground-Water Specialist Michael W. Doughten, Chemist Scott W. Phillips, Chesapeake Bay Coordinator Janet E. Hannon, Physical Science Technician Henry M. Johnson, Hydrologist Bruce D. Lindsey, Hydrologist Dennis J. Low, Hydrologist Mastin M. Mount, Hydrologic Technican Cody W. Reinitz, Student Trainee Andrew Stock, Student Trainee Julian E. Wayland, Hydrologist Peggy K. Widman, Physical Science Technician TEXT PREPARATION R. Brent Banks, Cartographic Trainee Judith A. McFarland, Technical Publications Editor Donna Knight, Editorial Assistant CONTENTS Abstract........................................................................................................................................................ 1 Introduction .................................................................................................................................................2 Purpose and scope ...............................................................................................................................3 Description of study area.....................................................................................................................3 Acknowledgments...............................................................................................................................3 Study methods ............................................................................................................................................. 3 Delineation of hydrogeomorphic regions............................................................................................3 Chlorofluorocarbon analysis ...............................................................................................................5 Nitrogen isotope analysis ....................................................................................................................8 Major ion and nutrient analyses ..........................................................................................................8 Estimation of residence time by application of a simple reservoir model. .........................................8 Water-quality data and general nitrogen chemistry of spring water from selected hydrogeomorphic regions ..............................................................................................10 Preliminary estimates of residence times and apparent ages of ground water in the Chesapeake Bay watershed..........................................................................................................11 Hydrologic conditions during sampling............................................................................................16 Coastal Plain hydrogeomorphic region .............................................................................................18 Piedmont crystalline hydrogeomorphic region .................................................................................21 Piedmont carbonate hydrogeomorphic region ..................................................................................26 Mesozoic Lowland hydrogeomorphic region ...................................................................................32 Blue Ridge hydrogeomorphic region ................................................................................................35 Valley and Ridge siliciclastic hydrogeomorphic region ...................................................................39 Valley and Ridge carbonate hydrogeomorphic region......................................................................43 Appalachian Plateau siliciclastic hydrogeomorphic region ..............................................................43 Discussion..................................................................................................................................................49 Conclusions ...............................................................................................................................................51 Selected references ....................................................................................................................................52 Appendixes................................................................................................................................................57 A. Field parameters of spring water collected in the Chesapeake Bay watershed, September and November 1996 ...............................................................................................58 B. Apparent ages of water collected from springs and ancillary data used for modeled recharge dates ...........................................................................................................61 C. Concentrations of CFC-11, 12, and 113 in all samples................................................................65 D. Concentrations of major ions in water from springs collected in the Chesapeake Bay watershed, September and November 1996 .................................................70 FIGURES 1- 2. Maps showing: 1. Chesapeake Bay watershed study area and representative geologic section..........................4 2. Locations of springs in the Chesapeake Bay watershed sampled in September and November 1996 .........................................................................................6 iii FIGURES—Continued 3- 4. Generalized sections showing: 3. Ground-water-flow path through a shallow Coastal Plain aquifer.......................................7 4. Possible ground-water-flow path associated with a tubular spring in carbonate rock.......................................................................................8 5- 6. Graphs showing relation of: 5. Nitrate and delta 15 nitrogen in water collected from springs in the Chesapeake Bay watershed in September and November 1996.......................................11 6. Concentration of chlorofluorocarbon to ground-water residence time ...............................12 7. Map showing apparent ages of water collected from springs in the Chesapeake Bay watershed in September and November 1996...................................14 8. Bar graph showing apparent ages of water collected from springs in the Chesapeake Bay watershed in September and November 1996...................................15 9. Hydrographs of (A) ground water and (B) surface water index sites in the study area ....................................................................................................................17 10. Generalized section showing the shallow aquifer in the Coastal Plain with apparent ages of ground water......................................................................................20 11. Diagrammatic section showing the shallow aquifer in the Coastal Plain with apparent ages of ground water................................................................21 12. Graph showing ranges of aquifer properties, associated residence times, and apparent ages of water collected from springs in the Coastal Plain hydrogeomorphic region.......................................................................23 13. Conceptual ground-water-flow diagram showing the Piedmont crystalline hydrogeomorphic region.....................................................................24 14. Diagram showing the shallow aquifer in the Piedmont crystalline hydrogeomorphic region and apparent ages of ground water...............................................25 15. Graph showing ranges of aquifer properties, associated residence times, and apparent ages of water collected from springs in the Piedmont crystalline hydrogeomorphic region...........................................................28 16. Conceptual ground-water-flow diagram showing the Piedmont carbonate and Valley and Ridge carbonate hydrogeomorphic regions .....................................................................................................29 17. Graph showing ranges of aquifer properties, associated residence times, and apparent ages of water collected from springs in the Piedmont carbonate hydrogeomorphic region ...............................................................31 18. Conceptual ground-water-flow diagram
Recommended publications
  • Residence Time, Chemical and Isotopic Analysis of Nitrate in The
    Residence Time, Chemical and Isotopic Analysis of Nitrate in the Groundwater and Surface Water of a Small Agricultural Watershed in the Coastal Plain, Bucks Branch, Sussex County, Delaware John Clune ([email protected]) Judy Denver ([email protected]) Introduction Introduction Problem/Need Resource managers need a practical perspective on travel time of groundwater to streams, detailed understanding of the sources of nitrogen for targeting management efforts and to better quantify water-quality improvements Introduction High TN Bucks Branch has some of the highest measured concentrations of total nitrogen in any stream in the State (Delaware Department of Natural Resources and Environmental Control, 2010) and most of the nitrogen is in the form of nitrate. Introduction Sources The vast majority of nitrogen inputs in this part of Sussex County, Delaware are from manure and fertilizer Purpose/Objectives The purpose of this study was to present (1) estimated residence times of groundwater and (2) and provide a chemical and isotopic analysis of nitrate in the groundwater and surface water of the Bucks Branch watershed Purpose/Objectives The purpose of this study was to present Concentrations of sulfur (1) estimated residence times hexafluoride (SF6), dissolved gases and silica of groundwater and (2) and provide a in groundwater and chemical and isotopic analysis of nitrate surface water to in the groundwater and surface water of determine the apparent the Bucks Branch watershed age of groundwater in the aquifer and to estimate the average residence
    [Show full text]
  • Estimation of Groundwater Mean Residence Time in Unconfined Karst Aquifers Using Recession Curves
    A. Kavousi and E. Raeisi – Estimation of groundwater mean residence time in unconfined karst aquifers using recession curves. Journal of Cave and Karst Studies, v. 77, no. 2, p. 108–119. DOI: 10.4311/2014ES0106 ESTIMATION OF GROUNDWATER MEAN RESIDENCE TIME IN UNCONFINED KARST AQUIFERS USING RECESSION CURVES ALIREZA KAVOUSI AND EZZAT RAEISI Dept. of Earth Sciences, College of Sciences, Shiraz University, 71454 Shiraz, Iran, [email protected], [email protected] Abstract: A new parsimonious method is proposed to estimate the mean residence time of groundwater emerging at any specific time during recession periods from karst springs. The method is applicable to unconfined karstic aquifers with no-flow boundaries. The only required data are numerous consecutive spring hydrographs involving a wide range of discharge from high to low flow and the relevant precipitation hyetographs. First, a master recession curve is constructed using the matching-strip method. Then, discharge components corresponding to the individual hydrographs at any desired time are estimated by extrapolation of recession curves based on the master curve. Residence times are also taken from the time elapsed since the events’ centroids. Finally, the mean residence time is calculated by a discharge-weighted average. The proposed method was evaluated for the Sheshpeer Spring in Iran. There are 259 sinkholes in the catchment area of the Sheshpeer unconfined aquifer, and all the boundaries are physically no-flow. The mean residence time calculated by the proposed method was about one year longer than that of uranine dye tracer. The tracer mean time is representative of flowing water between the injection and emergence points, but the mean time by the proposed method is representative of all active circulating water throughout the entire aquifer.
    [Show full text]
  • Stocks, Flows, and Residence Times Box Models
    Box Models: Stocks, Flows, and Residence Times IPOL 8512 Reservoirs • Natural systems can be characterized by the transport or transformation of matter (e.g. water, gases, nutrients, toxics), energy, and organisms in and out of a reservoir. • Reservoirs can be physical (e.g. a human body, the atmosphere, ocean mixed layer), chemical (different chemical species), or biological (e.g. populations, live biomass, dead organic matter) • Transport/transformation can involve bulk movement of matter, diffusion, convection, conduction, radiation, chemical or nuclear reactions, phase changes, births and deaths, etc. Box Models • We make a simple model of a system by representing the reservoirs with a “box” and the transport/transformation with arrows. • We usually assume the box is well-mixed, and we usually are not concerned with internal details. Stock, S Inflow, Fin Outflow, Fout • Stock = the amount of stuff (matter, energy, electric charge, chemical species, organisms, pollutants, etc.) in the reservoir • Flows = the amount of stuff flowing into and out of the reservoir as a function of time Why Use Box Models? To understand or predict: • Concentrations of pollutants in various environmental reservoirs as a function of time: e.g. water pollution, outdoor/ indoor air pollution • Concentrations of toxic substance in organs after inhalation or ingestion; setting standards for toxic exposure or intake • Population dynamics, predator-prey and food- chain models, fisheries, wildlife management • Biogeochemical cycles and climate dynamics (nutrients, energy, air, trace gases, water) How Box Models Work Basic rule of box models: change in stock over time = inflow – outflow S/t = Fin –Fout Situation 1: Equilibrium Fin = Fout S/t = 0 Situation 2: Non-equilibrium Fin > Fout S/t > 0 F < F S/ t < 0 in out 5 Equilibrium: The Balance • In many problems in environmental science, it is reasonable to start with the assumption that a particular stock is in equilibrium, meaning that the stock does not change over time.
    [Show full text]
  • Wastewater Residence Time in Sewers
    October 1969 Report No. EVE 19-69-7 THE EFFECT AND REGULATION OF WASTEWATER RESIDENCE TIME IN SEWERS David R. O'Toole and Donald Dean Adrian, Project Investigator Partially Funded by Office of Water Resources Research Grant WR-BO 11-MASS and Federal Water Pollution Control Administration Training Grant 5T1-WP-77-04 ENVIRONMENTAL ENGINEERING DEPARTMENT OF CIVIL ENGINEERING UNIVERSITY OF MASSACHUSETTS AMHERST, MASSACHUSETTS TKE EFFECT AND REGULATION OF WASTEWATER RESIDENCE TIME IN SEWERS by ! David R. O'Toole and Donald Dean Adrian, Project Investigator October 1969 THE AUTHORS w David Richard O'Toole received his B.S. degree in 0 Civil Engineering from the University of Massachusetts in June 1968, After a summer working for a consulting engineering firm he enroiled as a graduate student in the Environmental Engineering Program, Department of Civil Engineering, University of Massachusetts. Upon receipt of his Master's degree in September 1969, he was "commissioned by the U. S. Public Health Service to work as an Assistant Sanitary Engineer with the Indian Health Service in Portland, Oregon. Donald Dean Adrian received his B.A. degree in Liberal Arts and his B.S. degree in Civil Engineering from the University of Notre Dame in 1957 and 1958, respectively. He enrolled in the graduate program in Sanitary Engineering at the University of California at Berkeley and was awarded the M.S. degree in 1959. The Ph.D. was obtained from Stanford University in Civil Engineering in 1964. Experience has been obtained with the California Health Department, Vanderbilt University and the University of Massachusetts. He is presently an Associate Professor of Civil Engineering.
    [Show full text]
  • 14C Mean Residence Time and Its Relationship with Thermal Stability
    Geoderma 308 (2017) 1–8 Contents lists available at ScienceDirect Geoderma journal homepage: www.elsevier.com/locate/geoderma 14C mean residence time and its relationship with thermal stability and MARK molecular composition of soil organic matter: A case study of deciduous and coniferous forest types ⁎ Tsutomu Ohnoa, , Katherine A. Heckmanb, Alain F. Plantec, Ivan J. Fernandezd, Thomas B. Parre a School of Food and Agriculture, University of Maine, Orono, ME 04469, USA b USDA Forest Service, Northern Research Station, Houghton, MI 49931, USA c Department of Earth and Environmental Sciences, University of Pennsylvania, Philadelphia, PA 19104, USA d School of Forest Resources, University of Maine, Orono, ME 04469, USA e Department of Biology, University of Oklahoma, Norman, OK 73019, USA ARTICLE INFO ABSTRACT Keywords: Soil organic matter (SOM) plays a critical role in the global terrestrial carbon cycle, and a better understanding Soil organic carbon of soil processes involved in SOM stability is essential to determine how projected climate-driven changes in soil Carbon sequestration processes will influence carbon dynamics. We used 14C signature, analytical thermal analysis, and ultrahigh Soil minerals resolution mass spectrometry to determine the influence of deciduous and coniferous forest vegetation type and Radiocarbon dating soil depth on the stability of soil C. The 14C mean residence time (MRT) of the illuvial B horizon soils averaged Thermal analysis 1350 years for the deciduous soils and 795 years for the coniferous soils. The difference of MRT between mineral Ultrahigh resolution mass spectrometry soils by forest type may be due to the saturation of extractable Fe and Al minerals binding sites by SOM in the coniferous soils, allowing greater transport of modern SOM from the O horizon down the soil profile, as com- pared with the non-saturated minerals in the deciduous soil profile.
    [Show full text]
  • The Activated Sludge Process Part II Revised October 2014
    Wastewater Treatment Plant Operator Certification Training Module 16: The Activated Sludge Process Part II Revised October 2014 This course includes content developed by the Pennsylvania Department of Environmental Protection (Pa. DEP) in cooperation with the following contractors, subcontractors, or grantees: The Pennsylvania State Association of Township Supervisors (PSATS) Gannett Fleming, Inc. Dering Consulting Group Penn State Harrisburg Environmental Training Center MODULE 16: THE ACTIVATED SLUDGE PROCESS – PART II Topical Outline Unit 1 – Process Control Strategies I. Key Monitoring Locations A. Plant Influent B. Primary Clarifier Effluent C. Aeration Tank D. Secondary Clarifier E. Internal Plant Recycles F. Plant Effluent II. Key Process Control Parameters A. Mean Cell Residence Time (MCRT) B. Food/Microorganism Ratio (F/M Ratio) C. Sludge Volume Index (SVI) D. Specific Oxygen Uptake Rate (SOUR) E. Sludge Wasting III. Daily Process Control Tasks A. Record Keeping B. Review Log Book C. Review Lab Data Unit 2 – Typical Operational Problems I. Process Operational Problems A. Plant Changes B. Sludge Bulking C. Septic Sludge D. Rising Sludge E. Foaming/Frothing F. Toxic Substances II. Process Troubleshooting Guide Bureau of Safe Drinking Water, Department of Environmental Protection i Wastewater Treatment Plant Operator Training MODULE 16: THE ACTIVATED SLUDGE PROCESS – PART II III. Equipment Operational Problems and Maintenance A. Surface Aerators B. Air Filters C. Blowers D. Air Distribution System E. Air Header/Diffusers F. Motors G. Gear Reducers Unit 3 – Microbiology of the Activated Sludge Process I. Why is Microbiology Important in Activated Sludge? A. Activated Sludge is a Biological Process B. Tools for Process Control II. Microorganisms in Activated Sludge A.
    [Show full text]
  • Cropland Has Higher Soil Carbon Residence Time Than Grassland In
    Soil & Tillage Research 174 (2017) 130–138 Contents lists available at ScienceDirect Soil & Tillage Research journal homepage: www.elsevier.com/locate/still Cropland has higher soil carbon residence time than grassland in the MARK subsurface layer on the Loess Plateau, China ⁎ Ding Guoa, Jing Wanga, Hua Fua, , Haiyan Wena, Yiqi Luob a State Key Laboratory of Grassland Agro-Ecosystems, College of Pastoral Agriculture Science and Technology, Lanzhou University, Lanzhou 730020, China b Department of Microbiology and Plant Biology, University of Oklahoma, Norman, OK 73019, USA ARTICLE INFO ABSTRACT Keywords: Carbon (C) residence time is one of the key factors that determine the capacity of C storage and the potential C Carbon mineralization loss in soil, but it has not been well quantified. Assessing C residence time is crucial for an improved under- Inverse analysis standing of terrestrial C dynamics. To investigate the responses of C residence time to land use, soil samples were Residence time collected from millet cropland (MC) and enclosed grassland (EG) on the Loess Platea, China. The soil samples were incubated at 25 °C for 182 days. A Bayesian inverse analysis was applied to evaluate the residence times of different C fractions based on the information contained in the time-series data from laboratory incubation. Our results showed that soil organic carbon (SOC) mineralization rates and the amount of SOC mineralized sig- nificantly was increased after the conversion of cropland into grassland due to the increase in labile C fraction. At the end of the incubation study, 2.1%–6.8% of the initial SOC was released.
    [Show full text]
  • Evaluation of the Influence of Individual Clay Minerals on Biochar
    Article Evaluation of the Influence of Individual Clay Minerals on Biochar Carbon Mineralization in Soils Qingzhong Zhang 1, Claudia Keitel 2 and Balwant Singh 2,* 1 Key Laboratory of Agricultural Environment, Ministry of Agriculture, Sino-Australian Joint Laboratory for Sustainable Agro-Ecosystems, Institute of Environment and Sustainable Development in Agriculture, Chinese Academy of Agricultural Sciences, Beijing 100081, China; [email protected] 2 School of Life and Environmental Sciences, Faculty of Science, The University of Sydney, Sydney NSW 2006, Australia; [email protected] * Correspondence: [email protected]; Tel.: +61-2-8627-1140 Received: 26 August 2019; Accepted: 28 November 2019; Published: 3 December 2019 Abstract: Although association between mineral and biochar carbon have been speculated in some studies, still there is no direct evidence for the influence of individual clay minerals on the mineralization of biochar carbon in soils. To address this, we conducted an incubation study using monomineralic soils constituted by separately mixing pure minerals, i.e., smectite, kaolinite, and goethite, with a sandy soil. Switch grass biochar (400 ◦C) was added to the artificial soils and samples were incubated for 90 days at 20 ◦C in the laboratory. The CO2-C mineralized from the control, and biochar amended soil was captured in NaOH traps and the proportion of C mineralized from biochar was determined using δ13C isotopic analysis. The clay minerals significantly decreased the cumulative total carbon mineralized during the incubation period, whereas biochar had no effect on this. The least amount of total C was mineralized in the presence of goethite and biochar amended soil, where only 0.6% of the native soil organic carbon (SOC) (compared to 4.14% in control) and 2.9% of the biochar-C was mineralized during the 90 days incubation period.
    [Show full text]
  • Chapter 2 - WATER QUALITY
    Water Quality Monitoring - A Practical Guide to the Design and Implementation of Freshwater Quality Studies and Monitoring Programmes Edited by Jamie Bartram and Richard Ballance Published on behalf of United Nations Environment Programme and the World Health Organization © 1996 UNEP/WHO ISBN 0 419 22320 7 (Hbk) 0 419 21730 4 (Pbk) Chapter 2 - WATER QUALITY This chapter was prepared by M. Meybeck, E. Kuusisto, A. Mäkelä and E. Mälkki “Water quality” is a term used here to express the suitability of water to sustain various uses or processes. Any particular use will have certain requirements for the physical, chemical or biological characteristics of water; for example limits on the concentrations of toxic substances for drinking water use, or restrictions on temperature and pH ranges for water supporting invertebrate communities. Consequently, water quality can be defined by a range of variables which limit water use. Although many uses have some common requirements for certain variables, each use will have its own demands and influences on water quality. Quantity and quality demands of different users will not always be compatible, and the activities of one user may restrict the activities of another, either by demanding water of a quality outside the range required by the other user or by lowering quality during use of the water. Efforts to improve or maintain a certain water quality often compromise between the quality and quantity demands of different users. There is increasing recognition that natural ecosystems have a legitimate place in the consideration of options for water quality management. This is both for their intrinsic value and because they are sensitive indicators of changes or deterioration in overall water quality, providing a useful addition to physical, chemical and other information.
    [Show full text]
  • Biogeochemical Cycles (Saleska) A
    Biogeochemistry: Key concepts and methods SWES 410/510 Jan. 31, 2014 I. Biogeochemical cycles (Saleska) A. Method: Box models & Residence time B. Budgets and cycles: water, carbon, nitrogen C. Ecological Stoichiometry II. Thermodynamics of Biogeochemical Reactions (guest Prof. Chorover) I. What is Biogeochemistry? Biogeochemistry = the study of how the cycling of elements through the earth system (water, air, living organisms, soil and rock) is governed by physical, chemical, geological and biological processes hydrosphere atmosphere biosphere pedosphere lithosphere Key Names Vladimir Vernadsky (1863-1945): Russian scientist known as the “father of biogeochemistry”, invented the terms geosphere, biosphere, and “noosphere” G. Evelyn Hutchinson (1903-1991): famous limnologist (considered to be founder of limnology) (also studied the question of how biological species coexist) 1 A. Box models and Residence times Steady-state: when flow (of water, nutrients, energy) through a ‘box’ (a lake, the atmosphere, a population or organisms) is steady, i.e.: inflow (Fin) = outflow (Fout) box size (or stock S) doesn’t change Then residence time (the time it would take for the flow to fill the box if the box were empty) is the ratio of the stock in the box, to the flow: (using consistent units) grams grams sec-1 A. Box models and Residence times Example 1: Students at University Given 30,000 student-body population (stock), about how many graduate each year? (what is the flow?) Example 2: Land and sea autotrophs have roughly equal global productivities (NPPland 60 PgC/yr; NPPsea 50 PgC/yr), but big differences in total biomass carbon (560 PgC on land vs 3 PgC in the sea) Why? Residence time! Land: 10 ; Sea: 0.06 / / (24 days) Example 3: Zooplankton (residence time 6 mo) graze phytoplankton (residence time 2 weeks) in a lake.
    [Show full text]
  • Aerobic Treatment Process
    Industrial Water Pollution Control 19. AEROBIC SECONDARY TREATMENT OF WASTEWATER 19.1 Activated Sludge Process Conventional biological treatment of wastewater under aerobic conditions includes activated sludge process (ASP) and Trickling Filter. The ASP was developed in England in 1914. The activated sludge process consists of an aeration tank, where organic matter is stabilized by the action of bacteria under aeration and a secondary sedimentation tank (SST), where the biological cell mass is separated from the effluent of aeration tank and the settle sludge is recycled partly to the aeration tank and remaining is wasted (Figure 19.1). Recycling is necessary for activated sludge process. The aeration conditions are achieved by the use of diffused or mechanical aeration. Diffusers are provided at the tank bottom, and mechanical aerators are provided at the surface of water, either floating or on fixed support. Settled raw wastewater and the returned sludge enter the head of the tank, and cross the tank following the spiral flow pattern, in case of diffuse air aeration, or get completely mixed in case of completely mixed reactor. The air supply may be tapered along the length in case of plug flow aeration tank, to match the quantity of oxygen demand. The effluent is settled in the settling tank and the sludge is returned at a desired rate. Settled sewage Aeration Tank SST Effluent Excess sludge Return Sludge Figure 19.1 Conventional Activated Sludge Process Loading Rate: The organic matter loading rate applied to the reactor is quantified as kg of BOD applied per unit volume of the reactor per day, called as volumetric loading rate, or kg of BOD applied per day per unit mass of microorganisms present in the reactor (i.e.
    [Show full text]
  • Basic Principles of Wastewater Treatment
    TREATMENT SERIES TREATMENT BIOLOGICAL WASTEWATER BIOLOGICAL WASTEWATER BIOLOGICAL WASTEWATER TREATMENT SERIES VOLUME 2 Basic Principles of Wastewater Treatment is the second volume in the series Biological Wastewater Treatment, and focuses on the unit operations and processes associated with biological wastewater treatment. The major VOLUME 2 topics covered are: • microbiology and ecology of wastewater treatment BASIC PRINCIPLES • reaction kinetics and reactor hydraulics • conversion of organic and inorganic matter • sedimentation and TREATMENT WASTEWATER OF WASTEWATER • aeration. BASIC PRINCIPLES OF The theory presented in this volume forms the basis upon which the other books of the series are built. TREATMENT The Biological Wastewater Treatment series is based on the book Biological Wastewater Treatment in Warm Climate Regions and on a highly acclaimed set of best selling textbooks. This international version is comprised by six textbooks giving a state-of-the-art presentation of the science and technology of biological wastewater treatment. Books in the Biological Wastewater Treatment series are: • Volume 1: Wastewater Characteristics, Treatment and Disposal • Volume 2: Basic Principles of Wastewater Treatment • Volume 3: Waste Stabilisation Ponds • Volume 4: Anaerobic Reactors • Volume 5: Activated Sludge and Aerobic Biofilm Reactors • Volume 6: Sludge Treatment and Disposal von Sperling Marcos 1843391627 Marcos von Sperling 6.14 x 9.21.440 6.14 x 9.21 Basic Principles of Wastewater Treatment Biological Wastewater Treatment Series The Biological Wastewater Treatment series is based on the book Biological Wastewater Treatment in Warm Climate Regions and on a highly acclaimed set of best selling textbooks. This international version is comprised by six textbooks giving a state-of-the-art presentation of the science and technology of biological wastewater treatment.
    [Show full text]