Groundwater Unit Table of Contents
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Urban Flooding Mitigation Techniques: a Systematic Review and Future Studies
water Review Urban Flooding Mitigation Techniques: A Systematic Review and Future Studies Yinghong Qin 1,2 1 College of Civil Engineering and Architecture, Guilin University of Technology, Guilin 541004, China; [email protected]; Tel.: +86-0771-323-2464 2 College of Civil Engineering and Architecture, Guangxi University, 100 University Road, Nanning 530004, China Received: 20 November 2020; Accepted: 14 December 2020; Published: 20 December 2020 Abstract: Urbanization has replaced natural permeable surfaces with roofs, roads, and other sealed surfaces, which convert rainfall into runoff that finally is carried away by the local sewage system. High intensity rainfall can cause flooding when the city sewer system fails to carry the amounts of runoff offsite. Although projects, such as low-impact development and water-sensitive urban design, have been proposed to retain, detain, infiltrate, harvest, evaporate, transpire, or re-use rainwater on-site, urban flooding is still a serious, unresolved problem. This review sequentially discusses runoff reduction facilities installed above the ground, at the ground surface, and underground. Mainstream techniques include green roofs, non-vegetated roofs, permeable pavements, water-retaining pavements, infiltration trenches, trees, rainwater harvest, rain garden, vegetated filter strip, swale, and soakaways. While these techniques function differently, they share a common characteristic; that is, they can effectively reduce runoff for small rainfalls but lead to overflow in the case of heavy rainfalls. In addition, most of these techniques require sizable land areas for construction. The end of this review highlights the necessity of developing novel, discharge-controllable facilities that can attenuate the peak flow of urban runoff by extending the duration of the runoff discharge. -
Porosity and Permeability Lab
Mrs. Keadle JH Science Porosity and Permeability Lab The terms porosity and permeability are related. porosity – the amount of empty space in a rock or other earth substance; this empty space is known as pore space. Porosity is how much water a substance can hold. Porosity is usually stated as a percentage of the material’s total volume. permeability – is how well water flows through rock or other earth substance. Factors that affect permeability are how large the pores in the substance are and how well the particles fit together. Water flows between the spaces in the material. If the spaces are close together such as in clay based soils, the water will tend to cling to the material and not pass through it easily or quickly. If the spaces are large, such as in the gravel, the water passes through quickly. There are two other terms that are used with water: percolation and infiltration. percolation – the downward movement of water from the land surface into soil or porous rock. infiltration – when the water enters the soil surface after falling from the atmosphere. In this lab, we will test the permeability and porosity of sand, gravel, and soil. Hypothesis Which material do you think will have the highest permeability (fastest time)? ______________ Which material do you think will have the lowest permeability (slowest time)? _____________ Which material do you think will have the highest porosity (largest spaces)? _______________ Which material do you think will have the lowest porosity (smallest spaces)? _______________ 1 Porosity and Permeability Lab Mrs. Keadle JH Science Materials 2 large cups (one with hole in bottom) water marker pea gravel timer yard soil (not potting soil) calculator sand spoon or scraper Procedure for measuring porosity 1. -
Comparison of Two Methods for Estimating Base Flow in Selected Reaches of the South Platte River, Colorado
Prepared in cooperation with the Colorado Water Conservation Board Comparison of Two Methods for Estimating Base Flow in Selected Reaches of the South Platte River, Colorado Scientific Investigations Report 2012–5034 U.S. Department of the Interior U.S. Geological Survey Comparison of Two Methods for Estimating Base Flow in Selected Reaches of the South Platte River, Colorado By Joseph P. Capesius and L. Rick Arnold Prepared in cooperation with the Colorado Water Conservation Board Scientific Investigations Report 2012–5034 U.S. Department of the Interior U.S. Geological Survey U.S. Department of the Interior KEN SALAZAR, Secretary U.S. Geological Survey Marcia K. McNutt, Director U.S. Geological Survey, Reston, Virginia: 2012 For more information on the USGS—the Federal source for science about the Earth, its natural and living resources, natural hazards, and the environment, visit http://www.usgs.gov or call 1–888–ASK–USGS. For an overview of USGS information products, including maps, imagery, and publications, visit http://www.usgs.gov/pubprod To order this and other USGS information products, visit http://store.usgs.gov Any use of trade, product, or firm names is for descriptive purposes only and does not imply endorsement by the U.S. Government. Although this report is in the public domain, permission must be secured from the individual copyright owners to reproduce any copyrighted materials contained within this report. Suggested citation: Capesius, J.P., and Arnold, L.R., 2012, Comparison of two methods for estimating base flow in selected reaches of the South Platte River, Colorado: U.S. Geological Survey Scientific Investigations Report 2012–5034, 20 p. -
How Do Atmospheres Change Over Time? the Greenhouse Effect
Activity #5 How Do Atmospheres Change Over Time? The Greenhouse Effect [Adult] Adapted from: Global Warming & The Greenhouse Effect, Great Explorations in Math and Science (GEMS) Lawrence Hall of Science, 1997, by the Regents of the University of California ISBN: 0-912511-75-3. Unless otherwise noted, all images are courtesy of SETI Institute. 1. Introduction In this activity, Cadettes will observe how the greenhouse effect can change an atmosphere on Mars or on Earth. They will “Think like a scientist. Be a scientist!” 2. Science Objectives You will: • construct models to test ideas about processes that cannot be directly studied on Earth or Mars; • appreciate that the atmosphere is a large and complex system, so experiments concerning it are difficult to perform; and • use skills you have learned about atmospheric composition and apply that knowledge to new situations. 3. Materials For each group of 4–6 Cadettes. • [2] 2 liter (0.5 gal) clear soda bottles with labels removed and tops cut off. These are the Atmosphere Model Chambers. Advance preparation required (see page 2). • [1] pair of scissors for constructing a set of Atmosphere Model Chambers • [1] black permanent marker for constructing a set of Atmosphere Model Chambers • [2] identical thermometers, one for each chamber; view on Amazon.com: http://tinyurl.com/lkrvzvq • sufficient cardboard to prepare backing for each thermometer • 5–10 cm (about 4 in) of clear tape to attach thermometers to cardboard and to inside of each chamber • [1] piece of plastic wrap approximately 15 cm x 15 cm (6 x 6 in) • [1] rubber band large enough to fit the circumference of chamber and secure plastic wrap • chart of electromagnetic spectrum of light (EMS); print in advance • 250-watt infrared heat lamp (bulb) in a fixture with hood. -
Biogeochemical and Metabolic Responses to the Flood Pulse in a Semi-Arid Floodplain
View metadata, citation and similar papers at core.ac.uk brought to you by CORE provided by DigitalCommons@USU 1 Running Head: Semi-arid floodplain response to flood pulse 2 3 4 5 6 Biogeochemical and Metabolic Responses 7 to the Flood Pulse in a Semi-Arid Floodplain 8 9 10 11 with 7 Figures and 3 Tables 12 13 14 15 H. M. Valett1, M.A. Baker2, J.A. Morrice3, C.S. Crawford, 16 M.C. Molles, Jr., C.N. Dahm, D.L. Moyer4, J.R. Thibault, and Lisa M. Ellis 17 18 19 20 21 22 Department of Biology 23 University of New Mexico 24 Albuquerque, New Mexico 87131 USA 25 26 27 28 29 30 31 present addresses: 32 33 1Department of Biology 2Department of Biology 3U.S. EPA 34 Virginia Tech Utah State University Mid-Continent Ecology Division 35 Blacksburg, Virginia 24061 USA Logan, Utah 84322 USA Duluth, Minnesota 55804 USA 36 540-231-2065, 540-231-9307 fax 37 [email protected] 38 4Water Resources Division 39 United States Geological Survey 40 Richmond, Virginia 23228 USA 41 1 1 Abstract: Flood pulse inundation of riparian forests alters rates of nutrient retention and 2 organic matter processing in the aquatic ecosystems formed in the forest interior. Along the 3 Middle Rio Grande (New Mexico, USA), impoundment and levee construction have created 4 riparian forests that differ in their inter-flood intervals (IFIs) because some floodplains are 5 still regularly inundated by the flood pulse (i.e., connected), while other floodplains remain 6 isolated from flooding (i.e., disconnected). -
Isotopes \&Amp\; Geochemistry: Tools for Geothermal Reservoir
E3S Web of Conferences 98, 08013 (2019) https://doi.org/10.1051/e3sconf/20199808013 WRI-16 Isotopes & Geochemistry: Tools For Geothermal Reservoir Characterization (Kamchatka Examples) Alexey Kiryukhin1,*, Pavel Voronin1, Nikita Zhuravlev1, Andrey Polyakov1, Tatiana Rychkova1, Vasily Lavrushin2, Elena Kartasheva1, Natalia Asaulova3, Larisa Vorozheikina3, and Ivan Chernev4 1Institute of Volcanology & Seismology FEB RAS, Piip 9, Petropavlovsk-Kamch., 683006, Russia 2Geological Institute RAS, Pyzhevsky 7, Moscow 119017, Russia 3Teplo Zemli JSC, Vilyuchinskaya 6, Thermalny, 684000, Russia 4Geotherm JSC, Ac. Koroleva 60, Petropavlovsk-Kamchatsky, 683980, Russia Abstract. The thermal, hydrogeological, and chemical processes affecting Kamchatka geothermal reservoirs were studied by using isotope and geochemistry data: (1) The Geysers Valley hydrothermal reservoirs; (2) The Paratunsky low temperature reservoirs; (3) The North-Koryaksky hydrothermal system; (4) The Mutnovsky high temperature geothermal reservoir; (5) The Pauzhetsky geothermal reservoir. In most cases water isotope in combination with Cl- transient data are found to be useful tool to estimate reservoirs natural and disturbed by exploitation recharge conditions, isotopes of carbon-13 (in CO2) data are pointed either active magmatic recharge took place, while SiO2 and Na-K geothermometers shows opposite time transient trends (Paratunsky, Geysers Valley) suggest that it is necessary to use more complicated geochemical systems of water/mineral equilibria. 1 Introduction Active pore space limitation mass transport velocities are typically greater than heat transport velocities. That is a fundamental reason why changes in the isotope and chemistry parameters of geofluids are faster than changes in the heat properties of producing geothermal reservoirs, which makes them pre-cursors to production parameter changes. In cases of inactive to rock chemical species, they can be used as tracers of fluid flow and boundary condition estimation. -
Invasive Plants in Your Backyard!
Invasive Plants In Your Backyard! A Guide to Their Identification and Control new expanded edition Do you know what plants are growing in your yard? Chances are very good that along with your favorite flowers and shrubs, there are non‐native invasives on your property. Non‐native invasives are aggressive exotic plants introduced intentionally for their ornamental value, or accidentally by hitchhiking with people or products. They thrive in our growing conditions, and with no natural enemies have nothing to check their rapid spread. The environmental costs of invasives are great – they crowd out native vegetation and reduce biological diversity, can change how entire ecosystems function, and pose a threat Invasive Morrow’s honeysuckle (S. Leicht, to endangered species. University of Connecticut, bugwood.org) Several organizations in Connecticut are hard at work preventing the spread of invasives, including the Invasive Plant Council, the Invasive Plant Working Group, and the Invasive Plant Atlas of New England. They maintain an official list of invasive and potentially invasive plants, promote invasives eradication, and have helped establish legislation restricting the sale of invasives. Should I be concerned about invasives on my property? Invasive plants can be a major nuisance right in your own backyard. They can kill your favorite trees, show up in your gardens, and overrun your lawn. And, because it can be costly to remove them, they can even lower the value of your property. What’s more, invasive plants can escape to nearby parks, open spaces and natural areas. What should I do if there are invasives on my property? If you find invasive plants on your property they should be removed before the infestation worsens. -
West Lake Woven Wood Shade Section
West Lake Woven Wood Shade Section Effective April 15, 2014 Save a life: "Install Safety Tension Devices!" Woven Wood Measuring Instructions Measuring Inside Mount (IB) Shades: Measure the exact width (A) and length (B) of the window opening as shown. The factory will deduct ½” overall from the window width for clearance. On all inside mount shades, a small light gap will be visible. Measuring Outside Mount (OB) Shades: Measure the exact width (A) and length (B) of the window opening you wish to cover. The shade should cover the window opening by at least 2” on both the width and length. To cover a window sill, provide a measurement (C) beyond the sill. Outside Mount Inside Mount Measuring Arch Top Valances for Woven Wood Shades: For inside mount shades, measure the exact width and tallest length inside the window opening. For outside mount shades, measure the desired width and tallest length. Make sure to measure the length of outside mount shades at its tallest point. Arch Top woven wood shades must be perfect arches where the length equals ½ the width. For arch top valances, measure dimensions A, X, & Y. For pricing, use the width and tallest length measurement. Make sure to add the arch top shade surcharge. Measuring Angled Shades: It is critical to measure all four sides of the window opening. For inside mount shades, measure the inside of the window opening and for outside mount shades, add the desired overlap. Measure the slope angle with a protractor and provide the angle in degrees. Indicate all measurements on a template to be sent to the factory. -
Hydrogeology of Flowing Artesian Wells in Northwest Ohio
Hydrogeology of Flowing Artesian Wells in Northwest Ohio By Curtis J Coe, CPG and Jim Raab Ohio Department of Natural Resources Division of Water Resources June 2016 Bulletin 48 Table of Contents 1.0 Introduction ........................................................................................................................... 1 1.1 Site Location and Setting .................................................................................................. 1 1.2 ODH Water Well Regulations for Flowing Artesian Wells ............................................. 3 1.3 Purpose and Scope of Work .............................................................................................. 3 2.0 Previous Work ....................................................................................................................... 4 2.1 Bedrock Hydrogeology ..................................................................................................... 4 2.2 Glacial Hydrogeolgy ......................................................................................................... 8 2.2.1 Williams Complex Aquifer ....................................................................................... 8 2.2.2 Williams End Moraine Aquifer ................................................................................. 8 2.2.3 Buried Valley Aquifers ............................................................................................ 13 2.2.4 Lake Maumee Lacustrine Aquifer .......................................................................... -
8040 Introduction to Natural Resources and Ecology Systems
Introduction to Natural Resources and Ecology Systems 8040/36 weeks Table of Contents Acknowledgments ......................................................................................................................................... 1 Course Description ........................................................................................................................................ 2 Task Essentials Table .................................................................................................................................... 2 Curriculum Framework ................................................................................................................................. 6 Exploring Leadership Skills through FFA ................................................................................................... 6 Exploring Leadership Opportunities through FFA ....................................................................................... 7 Understanding Natural Resource Management ............................................................................................ 9 Protecting the Environment ........................................................................................................................ 15 Managing Forest Resources ........................................................................................................................ 25 Managing Wildlife Resources .................................................................................................................... -
Natural Resources Inventory
Natural Resources Inventory Columbia Metropolitan Planning Area Review Draft (10-1-10) NATURAL RESOURCES INVENTORY Review Draft (10-1-10) City of Columbia, Missouri October 1, 2010 - Blank - Preface for Review Document The NRI area covers the Metropolitan Planning Area defined by the Columbia Area Transportation Study Organization (CATSO), which is the local metropolitan planning organization. The information contained in the Natural Resources Inventory document has been compiled from a host of public sources. The primary data focus of the NRI has been on land cover and tree canopy, which are the product of the classification work completed by the University of Missouri Geographic Resource Center using 2007 imagery acquired for this project by the City of Columbia. The NRI uses the area’s watersheds as the geographic basis for the data inventory. Landscape features cataloged include slopes, streams, soils, and vegetation. The impacts of regulations that manage the landscape and natural resources have been cataloged; including the characteristics of the built environment and the relationship to undeveloped property. Planning Level of Detail NRI data is designed to support planning and policy level analysis. Not all the geographic data created for the Natural Resources Inventory can be used for accurate parcel level mapping. The goal is to produce seamless datasets with a spatial quality to support parcel level mapping to apply NRI data to identify the individual property impacts. There are limitations to the data that need to be made clear to avoid misinterpretations. Stormwater Buffers: The buffer data used in the NRI are estimates based upon the stream centerlines, not the high water mark specified in City and County stormwater regulations. -
Do You Drink It? 9-12
DO YOU DRINK IT? 9-12 SUBJECTS: Science (Physical Science, Ecology, Earth Science), Social Studies (Geography) TIME: 2 class periods MATERIALS: 3-liter soda bottles aquarium gravel sand (coarse) pump from liquid dispenser blue, yellow & Red food coloring paper cups straws student sheets droppers scissors or razor blades markers OBJECTIVES The student will do the following: 1. Create an aquifer model. 2. Locate major U.S. aquifers. 3. Explain how a well works. 4. Examine a well’s relationship to the water table. 5. Apply principles of well placement. 6. Explain different ways that groundwater is contaminated. 4-37 BACKGROUND INFORMATION An aquifer is an underground layer of rock or soil that holds the water called groundwater. The word “aquifer” is derived from the Latin “aqua” meaning “water ,”and “ferre” meaning “to bring” or “to yield.” The ability of a geological formation to yield water depends on two factors - porosity and permeability. Porosity is determined by how much water the soil or rock can hold in the spaces between its particles. Permeability means how interconnected the spaces are so that water can flow freely between them. There are two types of aquifers. One is a confined aquifer, in which a water supply is sandwiched between two impermeable layers. These are sometimes called artesian aquifers because, when a well is drilled into this layer, the pressure may be so great that water will spurt to the surface without being pumped. This is an artesian well. The other type of aquifer is the unconfined aquifer, which has an impermeable layer under it but not above it.