Introduction to Ponds, Lagoons, and Natural Systems Study Guide December 2013 Edition
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Thesis, Dissertation
AN EXPLORATION OF SMALL TOWN SENSIBILTIES by Lucas William Winter A thesis submitted in partial fulfillment of the requirements for the degree of Master of Architecture in Architecture MONTANA STATE UNIVERSITY Bozeman, Montana April 2010 ©COPYRIGHT by Lucas William Winter 2010 All Rights Reserved ii APPROVAL of a thesis submitted by Lucas William Winter This thesis has been read by each member of the thesis committee and has been found to be satisfactory regarding content, English usage, format, citation, bibliographic style, and consistency and is ready for submission to the Division of Graduate Education. Steven Juroszek Approved for the Department of Architecture Faith Rifki Approved for the Division of Graduate Education Dr. Carl A. Fox iii STATEMENT OF PERMISSION TO USE In presenting this thesis in partial fulfillment of the requirements for a master’s degree at Montana State University, I agree that the Library shall make it available to borrowers under rules of the Library. If I have indicated my intention to copyright this thesis by including a copyright notice page, copying is allowable only for scholarly purposes, consistent with “fair use” as prescribed in the U.S. Copyright Law. Requests for permission for extended quotation from or reproduction of this thesis in whole or in parts may be granted only by the copyright holder. Lucas William Winter April 2010 iv TABLE OF CONTENTS 1. THESIS STATEMENT AND INRO…...........................................................................1 2. HISTORY…....................................................................................................................4 3. INTERVIEW - WARREN AND ELIZABETH RONNING….....................................14 4. INTERVIEW - BOB BARTHELMESS.…………………...…....................................20 5. INTERVIEW - RUTH BROWN…………………………...…....................................27 6. INTERVIEW - VIRGINIA COFFEE …………………………...................................31 7. CRITICAL REGIONALISM AS RESPONSE TO GLOBALIZATION…………......38 8. -
The Biological Treatment Method for Landfill Leachate
E3S Web of Conferences 202, 06006 (2020) https://doi.org/10.1051/e3sconf/202020206006 ICENIS 2020 The biological treatment method for landfill leachate Siti Ilhami Firiyal Imtinan1*, P. Purwanto1,2, Bambang Yulianto1,3 1Master Program of Environmental Science, School of Postgraduate Studies, Diponegoro University, Semarang - Indonesia 2Department of Chemical Engineering, Faculty of Engineering, Diponegoro University, Semarang - Indonesia 3Department of Marine Sciences, Faculty of Fisheries and Marine Sciences, Diponegoro University, Semarang - Indonesia Abstract. Currently, waste generation in Indonesia is increasing; the amount of waste generated in a year is around 67.8 million tons. Increasing the amount of waste generation can cause other problems, namely water from the decay of waste called leachate. Leachate can contaminate surface water, groundwater, or soil if it is streamed directly into the environment without treatment. Between physical and chemical, biological methods, and leachate transfer, the most effective treatment is the biological method. The purpose of this article is to understand the biological method for leachate treatment in landfills. It can be concluded that each method has different treatment results because it depends on the leachate characteristics and the treatment method. These biological methods used to treat leachate, even with various leachate characteristics, also can be combined to produce effluent from leachate treatment below the established standards. Keywords. Leachate treatment; biological method; landfill leachate. 1. Introduction Waste generation in Indonesia is increasing, as stated by the Minister of Environment and Forestry, which recognizes the challenges of waste problems in Indonesia are still very large. The amount of waste generated in a year is around 67.8 million tons and will continue to grow in line with population growth [1]. -
Trickling Filter Technology for Treating Abattoir Wastewater
Trickling Filter Technology for Treating Abattoir Wastewater Project code: 2014 /1016 Prepared by: GHD Pty Ltd Date Published: April 2015 Published by: Australian Meat Processor Corporation Disclaimer: The information contained within this publication has been prepared by a third party commissioned by Australian Meat Processor Corporation Ltd (AMPC). It does not necessarily reflect the opinion or position of AMPC. Care is taken to ensure the accuracy of the information contained in this publication. However, AMPC cannot accept responsibility for the accuracy or completeness of the information or opinions contained in this publication, nor does it endorse or adopt the information contained in this report. No part of this work may be reproduced, copied, published, communicated or adapted in any form or by any means (electronic or otherwise) without the express written permission of Australian Meat Processor Corporation Ltd. All rights are expressly reserved. Requests for further authorisation should be directed to the Chief Executive Officer, AMPC, Suite 1, Level 5, 110 Walker Street Sydney NSW. Table of Contents Executive Summary 4 1. Introduction 6 1.1 Project Background 6 1.2 Objectives 6 1.3 Workscope and Basis 6 1.4 Overview 7 2. Treatment of Abattoir Wastewater 11 2.1 Characterisation of Wastewater 11 2.2 Typical Treatment Train 11 2.3 Treatment 12 3. Trickling Filtration 15 3.1 General 15 3.2 Description 15 3.3 Trickling Filter Media 17 3.4 Construction 18 3.5 Recirculation 19 3.6 Air Access / Circulation 19 3.7 Broad Design 19 3.8 Activated Sludge Versus Trickling Filters 22 4. -
Helpful Study Guide (PDF)
WASTEWATER STABILIZATION POND (WWSP) STUDY GUIDE ALASKA DEPARTMENT OF ENVIRONMENTAL CONSERVATION DIVISION OF WATER OPERATOR TRAINING AND CERTIFICATION PROGRAM http://dec.alaska.gov/water/opcert/index.htm Phone: (907) 465-1139 Email: [email protected] January 2011 Edition Introduction This study guide is made available to examinees to prepare for the Wastewater Stabilization Pond (WWSP) certification exam. This study guide covers only topics concerning non-aerated WWSPs. The WWSP certification exam is comprised of 50 multiple choice questions in various topics. These topics will be addressed in this study guide. The procedure to apply for the WWSP certification exam is available on our website at: http://www.dec.state.ak.us/water/opcert/LargeSystem_Operator.htm. It is highly recommended that an examinee complete one of the following courses to prepare for the WWSP certification exam. 1. Montana Water Center Operator Basics 2005 Training Series, Wastewater Lagoon module; 2. ATTAC Lagoons online course; or 3. CSUS Operation of Wastewater Treatment Plants, Volume I, Wastewater Stabilization Pond chapter. If you have any questions, please contact the Operator Training and Certification Program staff at (907) 465-1139 or [email protected]. Definitions 1. Aerobic: A condition in which “free” or dissolved oxygen is present in an aquatic environment. 2. Algae: Simple microscopic plants that contain chlorophyll and require sunlight; they live suspended or floating in water, or attached to a surface such as a rock. 3. Anaerobic: A condition in which “free” or dissolved oxygen is not present in an aquatic environment. 4. Bacteria: Microscopic organisms consisting of a single living cell. -
Safety Evaluation of the Zhaoli Tailings Dam a Seepage, Deformation and Stability Analysis with Geostudio
UPTEC ES 16 031 Examensarbete 30 hp September 2016 Safety Evaluation of the Zhaoli Tailings Dam A seepage, deformation and stability analysis with GeoStudio Johan Bäckström Malin Ljungblad Abstract Safety Evaluation of the Zhaoli Tailings Dam Johan Bäckström and Malin Ljungblad Teknisk- naturvetenskaplig fakultet UTH-enheten The mining industry produce large amount of mine waste, also called tailings, which must be kept in tailings dams. In this thesis the safety and stability of a tailings dam Besöksadress: have been studied, where some of the tailing material is being used as filling material. Ångströmlaboratoriet Lägerhyddsvägen 1 The dam has been modelled and simulated using the software Geostudio. To evaluate Hus 4, Plan 0 the safety and stability of the dam seepage, stress and strain as well as slope stability have been simulated with SEEP/W, SIGMA/W and SLOPE/W, which are different Postadress: modules in the Geostudio software. Box 536 751 21 Uppsala The results show that the dam is stable for all tested scenarios. However, in this Telefon: thesis many simplifications and assumptions have been made so it is recommended to 018 – 471 30 03 do a more detailed study to confirm the safety of the dam. The dam should also be Telefax: simulated for earthquakes before a definite evaluation can be made. 018 – 471 30 00 This master thesis has been conducted in cooperation with Vattenfall AB, Energiforsk Hemsida: AB, Uppsala University and Tsinghua University in Beijing, China. The project has http://www.teknat.uu.se/student been carried out on the planned Zhaoli ditch tailing dam in the Shanxi Province, China. -
General Sewer Plan
CITY OF GRANDVIEW GENERAL SEWER PLAN Prepared by PROJECT NO. 08032 January 2009 CITY OF GRANDVIEW GENERAL SEWER PLAN Prepared by PROJECT NO. 08032 January 2009 TABLE OF CONTENTS Page No. INTRODUCTION AND EXECUTIVE SUMMARY ......................................................................................... 1 INTRODUCTION ............................................................................................................................... 2 REQUIREMENTS.............................................................................................................................. 2 PURPOSE AND OBJECTIVE OF PLAN ........................................................................................... 2 SUMMARY OF RECOMMENDED IMPROVEMENTS ...................................................................... 3 SCHEDULE OF IMPROVEMENTS ................................................................................................... 3 ESTIMATED COSTS AND PROPOSED SEWER SYSTEM FINANCIAL PROGRAM ..................... 3 CHAPTER 1 - BASIC PLANNING INFORMATION ...................................................................................... 4 1.1 BACKGROUND INFORMATION .............................................................................................. 5 Wastewater System Ownership .......................................................................................... 5 Geography ........................................................................................................................... 5 Wastewater -
Pond Infiltration and Watertable Mounding
GEO-SLOPE International Ltd, Calgary, Alberta, Canada www.geo-slope.com Pond Infiltration and Watertable Mounding 1 Introduction The objective of this illustration is show how to model the filling of a pond with a liner. The zone below the liner remains unsaturated and the watertable deep in the profile mounds, due to percolation from the base of the pond. The modeling can help evaluate the effectiveness of lining the reservoir with a clay liner. Not only can the final, steady-state condition be established for both scenarios, but the rise in the watertable with time can be determined by conducting a transient analysis. Feature Highlights Transient boundary conditions Watertable viewing over time Unit flux boundary conditions Unsaturated flow 2 Geometry and boundary conditions The containment facility is located on top of a hill, with a stream at the bottom of the embankment, as shown below. Since the change in the regional system needs to be evaluated with time, a transient analysis will be conducted. 12 11 10 9 ) 8 m ( 7 n o i 6 t a v 5 e l E 4 3 2 1 0 0 2 4 6 8 10 12 14 16 18 20 22 24 26 28 30 Distance (m) Figure 1 Problem configuration Before conducting a transient analysis, it is sometimes helpful to know the long-term, steady-state solution, so you know the conditions where the system is eventually going to stabilize. It can also be helpful as a point of reference to compare against your transient results, which can help you determine if the steady-state solution is reasonable or too far in the future to be considered obtainable. -
Surface Water Management Plan Water Resources | City of St
Surface Water Management Plan Water Resources | City of St. Louis Park Proposals are due 4:00 p.m. April 24, 2017 Executive Summary City of St. Louis Park Surface Water Management Plan Executive Summary Located in Hennepin County just west of Minneapolis, the 10.7-square-mile City of St. Louis Park is a fully developed suburban community. The population of St. Louis Park is approximately 48,000 residents, making it the 20th largest city in Minnesota. St. Louis Park contains a variety of physical and water resources including several wetlands and small lakes, wooded areas, parks, and recreational lands, as well as the Minnehaha Creek corridor. Two watershed management organizations (WMOs) cover St. Louis Park, each with its own governing body: the Bassett Creek Watershed Management Commission (BCWMC) and the Minnehaha Creek Watershed District (MCWD). This local Surface Water Management Plan (SWMP) was prepared in accordance with Minnesota Statute 103B.235 and Minnesota Rules 8410 and is intended to replace the 2009 plan. The purpose of this SWMP includes objectives outlined in Minnesota Statute 103B.201 for metropolitan water management programs. According to the statute, the purposes of these water management programs are to: • protect, preserve, and properly use natural surface and groundwater storage and retention systems; • minimize public capital expenditures needed to correct flooding and water quality problems; • identify and plan for means to effectively protect and improve surface and groundwater quality; • establish more uniform local policies and official controls for surface and groundwater management; • prevent the erosion of soil into surface water systems; • promote effective groundwater recharge; • protect and enhance fish and wildlife habitats and water recreational facilities; and • secure the other benefits associated with the proper management of surface and groundwater. -
Evaporation Pond Seepage Soil Solution
from the soil surface. The subcores were fitted and sealed with plexiglass ends and set up to measure Permeability. Drainage water having an electrical conductivity (EC) of 10 dS/m (6100 ppm total dissolved salts) was applied to the cores for three days to ensure saturation and uniform electrolyte concentration. Biological activity was minimized in some of the cores by the addition of chlo- roform to the percolating drain water. Percolating drainage water having pro- gressively larger EC values was applied over periods of one to five days in an effort to exaggerate variations in evaporation pond salinity resulting from evaporation lnfiltrometers (left)were installed in Kings County and fresh drain water additions. The sa- evaporation pond to estimate seepage. Rainfall, evaporation, drainage flows, and changes in pond linity of inflow and outflow water was water levels (herebeing checked by co-author Blake measured periodically along with the per- McCullough-Sanden)were also measured. meability of each subcore. The sodium adsorption ratio (SAR) is an index of the relative concentration of sodium, calcium, and magnesium in the Evaporation pond seepage soil solution. When soil salinity is low, permeability has been shown to increase Mark E. Grismer o Blake L. McCullough-Sanden as the SAR value of the inflow solution in- creases. Past studies, however, have typi- cally considered SAR values of 30 or less. Rates of seepage from operating evaporation In this study, SAR values of the inflow so- ponds decline substantially as they age and as lution increased in the same stepwise fashion as EC, with values ranging from salinity increases 210 to 660. -
Imaging Hydrologic Processes in Headwater Riparian Seeps with Time-Lapse Electrical Resistivity
Case Study/ Imaging Hydrological Processes in Headwater Riparian Seeps with Time-Lapse Electrical Resistivity by Mark R. Williams1, Anthony R. Buda2, Kamini Singha3, Gordon J. Folmar2, Herschel A. Elliott4,and John P. Schmidt5 Abstract Delineating hydrologic and pedogenic factors influencing groundwater flow in riparian zones is central in understanding pathways of water and nutrient transport. In this study, we combined two-dimensional time-lapse electrical resistivity imaging (ERI) (depth of investigation approximately 2 m) with hydrometric monitoring to examine hydrological processes in the riparian area of FD-36, a small (0.4 km2) agricultural headwater basin in the Valley and Ridge region of east-central Pennsylvania. We selected two contrasting study sites, including a seep with groundwater discharge and an adjacent area lacking such seepage. Both sites were underlain by a fragipan at 0.6 m. We then monitored changes in electrical resistivity, shallow groundwater, and nitrate-N concentrations as a series of storms transitioned the landscape from dry to wet conditions. Time-lapse ERI revealed different resistivity patterns between seep and non-seep areas during the study period. Notably, the seep displayed strong resistivity reductions (∼60%) along a vertically aligned region of the soil profile, which coincided with strong upward hydraulic gradients recorded in a grid of nested piezometers (0.2- and 0.6-m depth). These patterns suggested a hydraulic connection between the seep and the nitrate-rich shallow groundwater system below the fragipan, which enabled groundwater and associated nitrate-N to discharge through the fragipan to the surface. In contrast, time-lapse ERI indicated no such connections in the non-seep area, with infiltrated rainwater presumably perched above the fragipan. -
Reclamation of Tailings Ponds
Journal American Society of Mining and Reclamation, 2012 Volume 1, Issue 1, COMPARISON OF HYDROLOGIC CHARACTERISTICS FROM TWO DIFFERENTLY RECLAIMED TAILINGS PONDS; GRAVES MOUNTAIN, LINCOLNTON, GA1 Gwendelyn Geidel2 Abstract: This study compares and evaluates the hydrologic characteristics between two kyanite ore process tailings ponds that were reclaimed with different reclamation strategies; one reclaimed with an impermeable membrane and the other with an open, surface reconfiguration (OSR) methodology. During the extraction and processing of kyanite ore from the Graves Mountain mine, Lincoln County, Georgia, fine grained tailings were produced. The tailings were transported by slurry pipeline to various tailings ponds which were created by the construction of dams using on-site materials. The first study site, referred to as the Pyrite Pond (PP), was constructed and filled during the 1960’s and early 1970’s. In early 1992, the PP was capped with an impermeable membrane, covered with a thin soil veneer and vegetated and in 1998 the upslope reclamation was completed. The second tailings pond, referred to as the East Tailings Pond (ETP), was constructed and filled in the 1970’s and early 1980’s and was reclaimed in 1995-96 by surface reconfiguration and the addition of soil amendments. Piezometers and wells were installed into the two tailings ponds and also in close proximity to the tailings ponds. While the initial study was aimed at comparing the two reclamation strategies, it became apparent that the ground water was a dominant factor. Results of the evaluation of the potentiometric surface data for varying depths within each tailings pond indicate that while both tailings ponds exhibit delayed response to precipitation events suggesting infiltration effects, the delay in the ETP deep wells and PP wells could not be adequately described by a surface infiltration model. -
Salinity in Livestock Ponds Summary Report Brian Hauschild, 2020 Big Sky Watershed Corps Musselshell Watershed Coalition
Salinity in Livestock Ponds Summary Report Brian Hauschild, 2020 Big Sky Watershed Corps Musselshell Watershed Coalition Introduction Much of Central Montana is underlain by salt-laden, Cretaceous marine shales. Saline conditions in Petroleum County are concentrated in the Colorado Group bedrock formation, as shown in Figure 4. The formation is characterized by shallow soils with highly soluble salt loads in the groundwater. In 2011, catastrophic floods flushed salts out of the groundwater and into the surface water. This geological condition can be compounded by certain land-use practices. Cropping systems, especially the prominent crop-fallow patterns, can also create a local perched water table to enhance surface evaporation, leaving salt to concentrate on the soil surface. The saline groundwater and saline surface run-off contribute soluble salts to the local watersheds and ponded water. When land-use management creates local saline conditions, the condition is known as saline seep. Dryland saline seeps, which can impair soil and water quality, were recognized as an issue in the latter half of the 20th century. Impacted areas are dependent upon local stratigraphy and geomorphology, but fallow periods in cultivated fields during wet years can be a major factor for their presence. After 2011, saline seeps became noticeably more prevalent and many livestock ponds have become unusable. This has been a major burden for producers who rely on potable water for their cattle. Seeps and ponds can sometimes be reclaimed through techniques like planting perennial forage in groundwater recharge areas to reduce salt leaching. However, climatic factors may enable the underlying problem to persist well into the 21st century, so collecting and understanding data is critical.