Dewatering Well Assessment for the Highway Drainage System at Five Sites in the East St
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Dewatering Behavior of a Wood-Cellulose Nanofibril
www.nature.com/scientificreports OPEN Dewatering Behavior of a Wood- Cellulose Nanofbril Particulate System Received: 6 May 2019 Ezatollah (Nima) Amini1, Mehdi Tajvidi1, Douglas W. Bousfeld2, Douglas J. Gardner1 & Accepted: 26 September 2019 Stephen M. Shaler1 Published: xx xx xxxx The novel use of aqueous suspensions of cellulose nanofbrils (CNF) as an adhesive/binder in lignocellulosic-based composite manufacture requires the removal of a considerable amount of water from the furnish during processing, necessitating thorough understanding of the dewatering behavior referred to as “contact dewatering”. The dewatering behavior of a wood-CNF particulate system (wet furnish) was studied through pressure fltration tests, centrifugation, and characterization of hard-to- remove (HR) water, i.e. moisture content in the wet furnish at the transition between constant rate part and the falling rate part of evaporative change in mass from an isothermal thermogravimetric analysis (TGA). The efect of wood particle size thereby particle specifc surface area on the dewatering performance of wet furnish was investigated. Permeability coefcients of wet furnish during pressure fltration experiments were also determined based on Darcy’s law for volumetric fow through a porous medium. Results revealed that specifc particle surface area has a signifcant efect on the dewatering of wet furnish where dewatering rate signifcantly increased at higher specifc particle surface area levels. While the permeability of the systems decreased over time in almost all cases, the most signifcant portion of dewatering occurred at very early stages of dewatering (less than 200seconds) leading to a considerable increase in instantaneous dewatering when CNF particles come in contact with wood particles. -
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. -
Bedrock Dewatering for Construction of Marmet and Soo Lock Projects
Bedrock Dewatering for Construction of Marmet and Soo Lock Projects Michael Nield Engineering Geologist Dam Safety Production Center, Huntington, WV August 2012 US Army Corps of Engineers BUILDING STRONG® BEDROCK DEWATERING FOR CONSTRUCTION OUTLINE 1. Marmet Lock Replacement Project (construction) - Project Description - Site Geology - Permeability and Groundwater Inflow - Dewatering Provisions 2. Soo Lock Replacement Project (design) - Project Description - Site Geology - Permeability and Predicted Groundwater Inflow - Impact to Design BUILDING STRONG® MARMET LOCK - PROJECT DESCRIPTION . Located on Kanawha River, OHIIO RIVER near Charleston, West GREAT LAKES DIVISION Virginia. Permits economic river transportation of coal, MARMET aggregate and chemicals. LOCKS & DAM . Construction of the new replacement lock was completed in 2009 BUILDING STRONG® “Busiest Lock in USA” Prior to New Lock Twin 56’ X 360’ Chambers Completed in 1934 Aerial View – Original Locks BUILDING STRONG® New 110’ X 800’ Lock Chamber Original Locks New Guard Wall New Guide Walls Aerial View – New Replacement Lock BUILDING STRONG® MARMET LOCK - SITE GEOLOGY . 157 TOTAL BORINGS . 10,200’ TOTAL DRILLING . 3,700’ ROCK CORE . 294 PRESSURE TESTS Subsurface Exploration – Boring Location Plan BUILDING STRONG® General Geology . Soil thickness 40 to 60 feet . Relatively flat top of rock surface at elev. 552 ± 3’ . Sedimentary rock of the Pennsylvanian-aged Kanawha Formation Sandstone member (23 to 43 feet thick) Shale member (19 to 33 feet thick) . Low angled bedding with 0o-10o dip to the Northwest . Slightly fractured with occasional high angled joints (70o-90o) BUILDING STRONG® Bedrock Units - Sandstone Member . Light gray . Moderately hard to hard . Medium to fine grained . Average unconfined compressive strength 8,442 psi . -
Dewatering Mechanisms of Compressible Filter Cakes
Dewatering mechanisms of compressible filter cakes Sarah Strubel, Harald Anlauf, Hermann Nirschl, Institute of Mechanical Process Engineering (MVM), Karlsruhe Institute of Technology (KIT) For designing filtration processes, a correlation between applied pressure and filter cake saturation is required. This correlation is provided by the capillary pressure curve, and depends on the pore size distribution of the filter cake. Many materials form compressible filter cakes: The porosity - and pore size distribution - changes with applied pressure. To determine the capillary pressure curve, a saturated filter cake is dewatered by gradually increasing the gas pressure. Below the capillary entry pressure the filter cake will consolidate. Above, desaturation of pores will occur in addition to further consolidation. In industrial filtration processes in contrary, the filter cake is subjected to constant gas pressure and therefore consolidation and desaturation occur simultaneously. With desaturation though, the tensile strength of the filter cake and therefore the resistance to consolidation increases. It is therefore interesting to investigate, if desaturation of an already consolidated cake, as in a capillary pressure experiment, will actually result in the same porosity and saturation as in a conventional filtration experiment, where both mechanisms occur at once. In this work, filter cake porosity, saturation and residual moisture are compared for two sets of filtration experiments. The first experiment is a standard filtration test, where the filter cake is formed and desaturated by gas pressure. In the second experiment a filter cake is first formed and consolidated and subsequently desaturated by applying gas pressure to the filter cake. The obtained results show a difference in porosity for the two types of experiments with in all other respects comparable filtration conditions. -
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. -
Dewatering – Deep Well Systems
Dewatering – Deep well systems GEO-SLOPE International Ltd. | www.geo-slope.com 1200, 700 - 6th Ave SW, Calgary, AB, Canada T2P 0T8 Main: +1 403 269 2002 | Fax: +1 888 463 2239 Introduction The objective of dewatering is to lower the groundwater table to prevent significant groundwater flow into an excavation, and/or to ensure slope stability. The preferred dewatering system will depend on hydrogeological conditions and construction requirements. In the case of slopes and excavations, the groundwater table can be lowered using a combination of methods, such as deep wells, wellpoints, vacuum wells, and horizontal wells. Deep well systems are often used for dewatering slopes and excavations when large drawdowns are required. This type of system generally consists of an array of pumping wells located near the excavation or slope. The combined effect of the array lowers the groundwater table over a wide area. The active pumping system must be set below the groundwater table whereas the bottom of the wells must be set deep enough to allow flow without excessive head loss. The objective of this example is to illustrate how to model deep well systems in three-dimensional environments, and to verify the water-flow formulation against a well-known benchmark. To do so, the example will discuss a specific deep well system, and provide insight into an approach for modeling pumping wells. Numerical Simulation The deep well system, taken from Mansur and Kaufman’s (1962) chapter on dewatering, consists of a large, 770 foot-long by 370 foot-wide, 40 foot-deep excavation in a 90 foot-deep unconfined sandy aquifer. -
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. -
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. -
Groundwater Flow in Low-Permeability Environments
WATER RESOURCES RESEARCH, VOL. 22, NO. 8, PAGES 1163-1195, AUGUST 1986 Groundwater Flow in Low-Permeability Environments Water Resources Division, U.S. Geological Survey, Reston, Virginia Certain geologic media are known to have small permeability; subsurface environments composed of these media and lacking well developed secondary permeability have groundwat'er flow sytems with many distinctive characteristics. Moreover, groundwater flow in these environments appears to influence the evolution of certain hydrologic, geologic, and geochemical systems, may affect the accumulation of pertroleum and ores, and probably has a role in the structural evolution of parts of the crust. Such environments are also important in the context of waste disposal. This review attempts to synthesize the diverse contributions of various disciplines to the problem of flow in low-permeability environments. Problems hindering analysis are enumerated together with suggested approaches to overcoming them. A common thread running through the discussion is the significance of size- and time-scale limitations of the ability to directly observe flow behavior and make measurements of parameters. These limitations have resulted in rather distinct small- and large-scale approaches to the problem. The first part of the review considers experimental investigations of low-permeability flow, including in situ testing; these are generally conducted on temporal and spatial scales which are relatively small compared with those of interest. Results from this work have provided increasingly detailed information about many aspects of the flow but leave certain questions unanswered. Recent advances in laboratory and in situ testing techniques have permitted measurements of permeability and storage properties in progressively "tight- er" media and investigation of transient flow under these conditions. -
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. -
Rotary Vacuum-Drum Filter
Rotary vacuum-drum filter Rotary vacuum filter drum consists of a drum rotating in a tub of liquid to be filtered. The technique is well suited to slurries, and liquids with a high solid content, which could clog other forms of filter. The drum is pre-coated with a filter aid, typically of diatomaceous earth (DE) or Perlite. After pre-coat has been applied, the liquid to be filtered is sent to the tub below the drum. The drum rotates through the liquid and the vacuum sucks liquid and solids onto the drum pre-coat surface, the liquid portion is "sucked" by the vacuum through the filter media to the internal portion of the drum, and the filtrate pumped away. The solids adhere to the outside of the drum, which then passes Oliver-type rotary vacuum-drum filter. a knife, cutting off the solids and a small portion of the filter media to reveal a fresh media surface that will enter the liquid as the drum rotates. The knife advances automatically as the surface is removed. Contents Basic fundamentals Rotary vacuum drum filter Range of application Advantages and limitations Advantages Disadvantages Designs available Belt discharge Scraper discharge Roll discharge String discharge Pre coat discharge Main process characteristics and assessment Heuristics design process Basic operation parameters heuristics Discharge mechanism adjustment heuristics Endless belt Scraper Roll String Pre coat Pre coat filter operation heuristics Advanced blade Necessary post treatment for waste stream for thicker Chlorination UV radiation Ozonation Necessary post treatment for waste stream for clarifier Land reclamation Incineration New Development See also References Further reading External links Basic fundamentals Rotary vacuum drum filter Rotary vacuum drum filter (RVDF), patented in 1872,[1] is one of the oldest filters used in the industrial liquid-solids separation.