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Dhamori Village Development Plan
This presentation premiered at WaterSmart Innovations watersmartinnovations.com Translating Historical Water Wisdom to Contemporary Challenges Leslie A. Johnson, 2018 MLA Capstone Chair: Professor John Koepke Department of Landscape Architecture, University of Minnesota Project Advisor: Alpa Nawre, University of Florida Agenda 1. Contemporary Issues in India & the Relationship to Traditional Water Management 2. Site Visit to Dhamori, India & Project Background 3. Water Wisdom: Capstone Research & Design 4. Lessons Learned & Broader Applications Image Credit: Dhamori Village - Leslie A. Johnson Part I. Contemporary Issues in India & the Relationship to Traditional Water Management India today faces a wide variety of social, environmental, and cultural issues related to water issues. • Conflicts between domestic and productive water use • Farmer suicides in rural communities Image Credit: Maharashtra Farmer during Drought - Jagadeesh NV, European Press Photo Agency / Relocated Workers - “Drought in Maharashtra,” Mumbai Mirror / Farmer Suicides - India You, 2011 Part I. Contemporary Issues in India & the Relationship to Traditional Water Management • Threats to food security • Seasonal migration to cities • During the monsoon, there can be too much water, but during the dry season, there can be too little Challenges stem from water mismanagement as much, or more so, as from water scarcity. Yet India has a rich history of water conservation strategies, so how is it that these current issues came to be? Image Credit: In wait for water - Mumbai Mirror / Stepwell – Atlas Obscura Part I. Contemporary Issues in India & the Relationship to Traditional Water Management What is ”traditional water management?” Broadly, water systems present prior to industrialization, specifically those systems derived from the vernacular of their landscapes and needs of a particular group of people. -
Full Document (Pdf 1196
Final Report GeoEngineers On-Call Agreement Y-7717 Task Order AU AN APPROACH FOR ESTIMATING INFILTRATION RATES FOR STORMWATER INFILTRATION DRY WELLS by Joel Massmann, Ph.D., P.E. Washington State Department of Transportation Technical Monitor Glorilyn Maw Washington State Transportation Commission Department of Transportation and in cooperation with U.S. Department of Transportation Federal Highway Administration April 2004 TECHNICAL REPORT STANDARD TITLE PAGE 1. REPORT NO. 2. GOVERNMENT ACCESSION NO. 3. RECIPIENT'S CATALOG NO. WA-RD 589.1 4. TITLE AND SUBTITLE 5. REPORT DATE AN APPROACH FOR ESTIMATING INFILTRATION April 2004 RATES FOR STORMWATER INFILTRATION DRY WELLS 6. PERFORMING ORGANIZATION CODE 7. AUTHOR(S) 8. PERFORMING ORGANIZATION REPORT NO. Joel Massmann, Ph.D., P.E. 9. PERFORMING ORGANIZATION NAME AND ADDRESS 10. WORK UNIT NO. 11. CONTRACT OR GRANT NO. Agreement Y7717, Task AU 12. SPONSORING AGENCY NAME AND ADDRESS 13. TYPE OF REPORT AND PERIOD COVERED Research Office Final Research Report Washington State Department of Transportation Transportation Building, MS 47372 Olympia, Washington 98504-7372 14. SPONSORING AGENCY CODE Keith Anderson, Project Manager, 360-709-5405 15. SUPPLEMENTARY NOTES This study was conducted in cooperation with the U.S. Department of Transportation, Federal Highway Administration. 16. ABSTRACT This report describes an approach for estimating infiltration rates for dry wells that are constructed using standard configurations developed by the Washington State Department of Transportation. The approach was developed recognizing that the performance of these dry wells depends upon a combination of subsurface geology, groundwater conditions, and dry well geometry. The report focuses on dry wells located in unconsolidated geologic materials. -
Water Balances
On website waterlog.info Agricultural hydrology is the study of water balance components intervening in agricultural water management, especially in irrigation and drainage/ Illustration of some water balance components in the soil Contents • 1. Water balance components • 1.1 Surface water balance 1.2 Root zone water balance 1.3 Transition zone water balance 1.4 Aquifer water balance • 2. Speficic water balances 2.1 Combined balances 2.2 Water table outside transition zone 2.3 Reduced number of zones 2.4 Net and excess values 2.5 Salt Balances • 3. Irrigation and drainage requirements • 4. References • 5. Internet hyper links Water balance components The water balance components can be grouped into components corresponding to zones in a vertical cross-section in the soil forming reservoirs with inflow, outflow and storage of water: 1. the surface reservoir (S) 2. the root zone or unsaturated (vadose zone) (R) with mainly vertical flows 3. the aquifer (Q) with mainly horizontal flows 4. a transition zone (T) in which vertical and horizontal flows are converted The general water balance reads: • inflow = outflow + change of storage and it is applicable to each of the reservoirs or a combination thereof. In the following balances it is assumed that the water table is inside the transition zone. If not, adjustments must be made. Surface water balance The incoming water balance components into the surface reservoir (S) are: 1. Rai - Vertically incoming water to the surface e.g.: precipitation (including snow), rainfall, sprinkler irrigation 2. Isu - Horizontally incoming surface water. This can consist of natural inundation or surface irrigation The outgoing water balance components from the surface reservoir (S) are: 1. -
Single Family Residential Stormwater Management Plan Dry Well (Infiltration) Construction Inspections
Single Family Residential Stormwater Management Plan DRY WELL (INFILTRATION) Definition : A dry well is an excavated pit filled with gravel and sand that provides temporary storage of runoff from roofs and allows for infiltration of that runoff over a 48 hour period. Constraints : • Dry wells should not be used in areas where their operation may create a risk for basement flooding, interfere with septic sewage disposal systems, or cause downslope seepage problems • May not be installed on slopes greater than 20% • Drainage area to each dry well shall not exceed 1000 square feet • Dry wells may not be used in HSG D or if the infiltration rate of the soil is less than 0.27 inches per hour • Dry wells are intended to capture rooftop runoff only Design Guidance: • Dry wells must be installed in accordance with the attached detail • Dry wells should not intercept water table, bedrock, fragipan or other confining layer • Dry wells must be located down gradient of building structures and set back at least 10 feet from buildings, 50 feet from water supply wells and 25 feet from septic systems • Dry wells must be set back at least 50 feet from fill slopes of 25% or steeper • Soils will be evaluated during excavation by ASCD representative to evaluate soil suitability assumed in original design which may alter type of practice to be constructed Installation: • Minimize compaction of dry well bottom and sidewalls • Collection pipes from downspouts shall be 4”-6” PVC installed at min. slope of 1% • The bottom of the dry well excavation should be -
Subsurface Drainage Manual for Pavements in Minnesota
Subsurface Drainage Manual for Pavements in Minnesota 2009-17 Take the steps... Research ...K no wle dge...Innovativ e S olu ti on s! Transportation Research Technical Report Documentation Page 1. Report No. 2. 3. Recipients Accession No. MN/RC 2009-17 4. Title and Subtitle 5. Report Date Subsurface Drainage Manual for Pavements in Minnesota June 2009 6. 7. Author(s) 8. Performing Organization Report No. Caleb N. Arika, Dario J. Canelon, John L. Nieber 9. Performing Organization Name and Address 10. Project/Task/Work Unit No. Department of Bioproducts and Biosystems Engineering University of Minnesota 11. Contract (C) or Grant (G) No. Biosystems and Agricultural Engineering Building (c) 89261 (wo) 10 1390 Eckles Avenue St. Paul, Minnesota 55108 12. Sponsoring Organization Name and Address 13. Type of Report and Period Covered Minnesota Department of Transportation Final Report 395 John Ireland Boulevard Mail Stop 330 14. Sponsoring Agency Code St. Paul, Minnesota 55155 15. Supplementary Notes http://www.lrrb.org/PDF/200917.pdf 16. Abstract (Limit: 250 words) A guide for evaluation of highway subsurface drainage needs and design of subsurface drainage systems for highways has been developed for application to Minnesota highways. The guide provides background information on the benefits of subsurface drainage, methods for evaluating the need for subsurface drainage at a given location, selection of the type of drainage system to use, design of the drainage system, guidelines on how to construct/install the subsurface drainage systems for roads, and guidance on the value of maintenance and how to maintain such drainage systems. 17. Document Analysis/Descriptors 18. -
Basic Equations
- The concentration of salt in the groundwater; - The concentration of salt in the soil layers above the watertable (i.e. in the unsaturated zone); - The spacing and depth of the wells; - The pumping rate of the wells; i - The percentage of tubewell water removed from the project area via surface drains. The first two of these factors are determined by the natural conditions and the past use of the project area. The remaining factors are engineering-choice variables (i.e. they can be adjusted to control the salt build-up in the pumped aquifer). A common practice in this type of study is to assess not only the project area’s total water balance (Chapter 16), but also the area’s salt balance for different designs of the tubewell system and/or other subsurface drainage systems. 22.4 Basic Equations Chapter 10 described the flow to single wells pumping extensive aquifers. It was assumed that the aquifer was not replenished by percolating rain or irrigation water. In this section, we assume that the aquifer is replenished at a constant rate, R, expressed as a volume per unit surface per unit of time (m3/m2d = m/d). The well-flow equations that will be presented are based on a steady-state situation. The flow is said to be in a steady state as soon as the recharge and the discharge balance each other. In such a situation, beyond a certain distance from the well, there will be no drawdown induced by pumping. This distance is called the radius of influence of the well, re. -
Infiltration Trench & Soakaway
An Infiltration Trench System includes an inlet pipe or water source, catch basin sump, perforated DESIGN PRINCIPLES distribution pipe, infiltration trench and overflow to the storm drainage system. ■ Infiltration Trench System: A Soakaway Manhole (Sump, or Dry Well) System includes an inlet pipe, a sedimentation manhole, and one or more infiltration shafts with connecting pipes. Use of Infiltration Shaft will be limited by hydro- a) Locate infiltration trench at least 3m geotechnical conditions in much of GVRD. from any building, 1.5m from Limitations of Infiltration Trench or Soakaway Manholes: property lines, and 6m from adjacent a) To avoid groundwater pollution, do not direct un-treated polluted runoff to Infiltration Trench or Shaft: infiltration facilities (or as recommended by a geotechnical ▪ Direct clean runoff (roof, non-automobile paving) to Infiltration Trench or Shaft. engineer). ▪ For polluted runoff (roads > 1000 vehicles / day, parking areas, other pollution sources), provide upstream source control for pollutant reduction prior to release to Infiltration Trench or Shaft. b) Sump: Provide a lid for periodic b) Use infiltration trench or shaft only in areas with footing drains. inspection and cleanout. Include a 1. Grass or Other Planting T-inlet pipe to trap oils, sediments 2. Finish Grade and debris. 3. Growing Medium Backfill 4. 100mm Dia PVC DR28 Perforated 19 c) Infiltration Trench: installation of Pipe distribution pipe and bottom of 5. Light Non-woven Polyester drainrock to be level. If more than Geotextile c/w Min. 400mm Laps one section of infiltration trench is 9 1 required, design so that underground 6. 50mm Drain Rock or Rock of water is temporarily ‘ponded’ in each Equal Porosity infiltration section. -
A Study on Agricultural Drainage Systems
International Journal of Application or Innovation in Engineering & Management (IJAIEM) Web Site: www.ijaiem.org Email: [email protected] Volume 4, Issue 5, May 2015 ISSN 2319 - 4847 A Study On Agricultural Drainage Systems 1T.Subramani , K.Babu2 1Professor & Dean, Department of Civil Engineering, VMKV Engg. College, Vinayaka Missions University, Salem, India 2PG Student of Irrigation Water Management and Resources Engineering , Department of Civil Engineering in VMKV Engineering College, Department of Civil Engineering, VMKV Engg. College, Vinayaka Missions University, Salem, India ABSTRACT Integration of remote sensing data and the Geographical Information System (GIS) for the exploration of groundwater resources has become an innovation in the field of groundwater research, which assists in assessing, monitoring, and conserving groundwater resources. In the present paper, groundwater potential zones for the assessment of groundwater availability in Salem and Namakkal districts of TamilNadu have been delineated using remote sensing and GIS techniques. The spatial data are assembled in digital format and properly registered to take the spatial component referenced. The namely sensed data provides more reliable information on the different themes. Hence in the present study various thematic maps were prepared by visual interpretation of satellite imagery, SOI Top sheet. All the thematic maps are prepared 1:250,000, 1:50,000 scale. For the study area, artificial recharge sites had been identified based on the number of parameters loaded such as 4, 3, 2, 1 & 0 parameters. Again, the study area was classified into priority I, II, III suggested for artificial recharge sites based on the number of parameters loaded using GIS integration. These zones are then compared with the Land use and Land cover map for the further adopting the suitable technique in the particular artificial recharge zones. -
Comparing Drain and Well Spacings in Deep Semi-Confined Aquifers for Water Table and Soil Salinity Control R.J
Comparing drain and well spacings in deep semi-confined aquifers for water table and soil salinity control R.J. Ooosterbaan, 16-09-2019. On www.waterlog.info public domain Abstract For the control of the water table in a thick soil layer with low hydraulic conductivity underlain by a deep aquifer with high hydraulic conductivity, it may be recommendable to use a pumped well drainage system (vertical drainage) instead of a horizontal subsurface drainage system by ditches, tiles or pipes owing to the relatively large well spacings compared to the drain spacings. The drainage by wells can also help in soil salinity control. This article shows the calculation of the required well and drain spacings in the kind of semi confined aquifer described. In those aquifers the drainage by wells may be more economical due to the large spacings, but when the horizontal drainage can be done by gravity, the well drainage system has the disadvantage of pumping costs. Contents 1. Introduction 2. Horizontal drainage 3. Vertical drainage 4. Comparison 5. Conclusion 6. References 1. Introduction Subsurface drainage systems are used for the control of the water table in otherwise waterlogged soils. They are also used to control the soil salinity by evacuating saline soil moisture. Subsurface drainage is usually done by horizontally placing drain pipes at some depth below the soil surface ,often around 1 to 1.2 m depth, but sometimes also shallower or deeper than that. The water removed by the drainage system may have a gravity outlet, but in low lands pumping may be required to evacuate the drainage water. -
Philadelphia Stormwater Manual V2.1 Philadelphia Stormwater Manual V2.1 This Pageintentionallyleftblank Simplified Approach Design Criteria Rooftop Systems
7 Stormwater Management Practice Design Guidelines 7.1 Green Roofs 7.2 Rain Barrels and Cisterns 7.3 Filter Strips 7.4 Filters 7.5 Bioinfiltration / Bioretention 7.6 Detention Basins 7.7 Berms and Retentive Grading 7.8 Swales 7.9 Constructed Wetlands (see PA Stormwater BMP Manual) 7.10 Ponds & Wet Basins (see PA Stormwater BMP Manual) 7.11 Subsurface Vaults 7.12 Subsurface Infiltration 7.13 Porous Pavement 7.14 Pre-fabricated and Proprietary Designs (see PA Stormwater BMP Manual) 7.15 Inlet and Outlet Controls Philadelphia Stormwater Manual v2.1 This Page Intentionally Left Blank Philadelphia Stormwater Manual v2.1 Simplified Approach Design Criteria Rooftop Systems This section provides the following information about eco-roofs and roof gardens: S Typical cross section S Description S General specifications S Checklist of minimal information to be shown on the permit drawings S Construction inspection requirements and schedule S Link to landscaping requirements S Link to example landscaping plans S Link to operation and maintenance requirements S Link to photos 7.1 S Link to drawings 7.1 S Eco-roof Central City F.A.R. bonus guidelines Green roofs (vegetated roof/eco roof/roof garden) consist of a layer of vegetation that completely covers an otherwise conventional flat or pitched roof. The hydrologic response of a green roof bears closer resemblance to a lawn or meadow than impervious surface. The green roof system is composed of multiple layers including waterproofing, a drainage City of Portland, OR layer, engineered planting media, and specially selected plants. Vegetated roof covers can be optimized to achieve water quantity and quality benefits. -
Continuous Simulation of an Infiltration Trench Best Management Practice
Villanova University The Graduate School Department of Civil and Environmental Engineering Continuous Simulation of an Infiltration Trench Best Management Practice A Thesis in Civil Engineering by Hans M. Benford Submitted in partial fulfillment of the requirements for the degree of Master of Science in Water Resources and Environmental Engineering May 2009 Continuous Simulation of an Infiltration Trench Best Management Practice By Hans Benford May 2009 Robert G. Traver, Ph.D., P.E. Date Professor of Civil and Environmental Engineering Bridget M. Wadzuk, Ph.D. Date Assistant Professor of Civil and Environmental Engineering Ronald A. Chadderton, Ph.D., P.E. Date Chairman, Department of Civil and Environmental Engineering Gary A. Gabriele, Ph.D. Date Dean, College of Engineering A copy of this thesis is available for research purposes at Falvey Memorial Library. Acknowledgements I would like to thank those who have supported me in my academic and personal life during my time at Villanova University as a graduate student. Without their continual support, I would not have been able to complete this study. First of all, I have to thank Dr. Traver for giving me the opportunity to join the Villanova Urban Stormwater Partnership as a graduate student. His ability to motivate and organize people of all types has shown the value of strong leadership as it pertains to progress, specifically in the field of stormwater. In addition to Dr. Traver, I need to thank the entire Villanova University Civil Engineering faculty and staff for my undergraduate education. Dr. Wadzuk, thank you for your valuable advice and guidance through my graduate studies. -
City of Elk Grove Dry Well Project Guidance and Lessons
City of Elk Grove Dry Well Project Guidance and Lessons Learned Document 2/28/2017 CITY OF ELK GROVE DRY WELL PROJECT Guidance Document Guidance and Lesson Learned from the Elk Grove Dry Well Project The Elk Grove Dry Well Project (project) was a four-year study to investigate the risk of groundwater contamination associated with the use of infiltrating stormwater through dry wells. The project involved a large field component that included the installation of two dry wells with pretreatment and a network of groundwater monitoring wells. The project has two study sites located in Elk Grove, California. The first site was the City of Elk Grove’s Corporation Yard, a 0.6-acre parking facility that is a bus fleet servicing area and maintenance yard, and the second site was the Strawberry Detention Basin, a water quality basin that collects stormwater from a 168-acre residential neighborhood. As part of the project study, stormwater and groundwater samples were collected for two years and analyzed for over 200 contaminants. Estimates of infiltration rates were also made. A companion modeling study of the fate and transport of contaminants through the vadose zone was performed. Scientific and government reports evaluating the risk to groundwater quality associated with dry well use were reviewed and compiled in a literature review (annotated bibliography). Lastly, information from other states with developed dry well programs, often known as underground injection control systems, was summarized in fact sheets with the goal of understanding the regulations, permitting, siting, and design guidelines used elsewhere. This guidance document summarizes some of the key lessons learned from this work.