Water Facts 3 Using Low-Yielding Wells
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Build an Aquifer
“It All Flows to Me” Lesson 1: Build an Aquifer Objective: To learn about groundwater properties by building your own aquifer and conducting experiments. Background Information Materials: • One, 2 Litter Soda Bottle An aquifer is basically a storage container for groundwater that is made up of • Plastic Cup different sediments. These various sediments can store different amounts of • 1 Cup of each: groundwater within the aquifer. The amount of water that it can hold is depen- soil, gravel, 1” rocks, sand dent on the porosity and the permeability of the sediment. • Pin • Modeling Clay Porosity is the amount of water that a material can hold in the spaces be- • Water tween its pores, while permeability is the material’s ability to pass water • Labels • 1 Bottle of Food Coloring through these pores. Therefore, an aquifer that has high permeability, like • 1 Pair of Scissors sandstone, will be able to hold more water, than materials that have a lower • 1 Ruler porosity and permeability. • One 8 Ounce Cup Directions You will build your own aquifers and investigate which sediments hold more water (rocks or sand). Students in your class will use either sand or rocks to food coloring food coloring build their models. You will use a ruler to measure the height of your water soil table and compare it to the height of water in other sediments. 8oz.food coloring soil ruler 8oz. ruler measuring cup sand measuring cup soil sand pin 8oz. rulerpin gravel scissors Building Directions food coloring measuring cup sandgravel scissors pin 1. Take a pin and use it to make many holes in the bot- scissors 2-liter soilplastic cup gravel tom of a cup. -
Natural Water Retention Measures
Natural Water Retention Measures Issue 32 May 2012 Editorial Contents Page Promoting Natural Water Retention - Wetland management needs a human-centric approach 4 Wetland management should consider human health as well An Ecosystem Approach as biodiversity. By a combination of human activities, the European environment Four-step strategy for wetland restoration 5 has been progressively dehydrated through overexploitation of Scientists call for new approach to multipurpose wetland its water resources. Climate change is likely to place even greater creation or restoration. pressures on these resources, which provide essential ecosystem services to communities throughout Europe, and also lead to an Blocking drainage ditches aids peatland restoration 6 increased risk of extreme events, such as droughts and flooding. Ditch blocking could help restore valuable peatlands but care is needed, study says. This special issue explores potential management measures aimed at enhancing the water storage potential of Europe’s What factors affect run-off from agricultural land? 7 ecosystems and aquifers and safeguarding them against the A study explores ways to reduce environmental impact of effects of climate change and other such human-induced agricultural runoff. pressures. Forests: A positive force for global water availability 8 Of particular concern to policymakers is the protection against Forests should be considered as global public goods, a new flooding that natural ecosystems afford. However, the ability study concludes. of natural features to retain water also delivers other vital ecosystem services including water provision and purification, Soil properties are key factor in flood prevention 9 improvement of soil quality, provision of habitat, cultural services, Scientists investigate the critical role of forest soil conditions air quality, climate regulation and, especially in peat bogs, on rainwater runoff. -
Farming the Ogallala Aquifer: Short and Long-Run Impacts of Groundwater Access
Farming the Ogallala Aquifer: Short and Long-run Impacts of Groundwater Access Richard Hornbeck Harvard University and NBER Pinar Keskin Wesleyan University September 2010 Preliminary and Incomplete Abstract Following World War II, central pivot irrigation technology and decreased pumping costs made groundwater from the Ogallala aquifer available for large-scale irrigated agricultural production on the Great Plains. Comparing counties over the Ogallala with nearby similar counties, empirical estimates quantify the short-run and long-run impacts on irrigation, crop choice, and other agricultural adjustments. From the 1950 to the 1978, irrigation increased and agricultural production adjusted toward water- intensive crops with some delay. Estimated differences in land values capitalize the Ogallala's value at $10 billion in 1950, $29 billion in 1974, and $12 billion in 2002 (CPI-adjusted 2002 dollars). The Ogallala is becoming exhausted in some areas, with potential large returns from changing its current tax treatment. The Ogallala case pro- vides a stark example for other water-scarce settings in which such long-run historical perspective is unavailable. Water scarcity is a critical issue in many areas of the world.1 Water is becoming increas- ingly scarce as the demand for water increases and groundwater sources are exhausted. In some areas, climate change is expected to reduce rainfall and increase dependence on ground- water irrigation. The impacts of water shortages are often exacerbated by the unequal or inefficient allocation of water. The economic value of water for agricultural production is an important component in un- derstanding the optimal management of scarce water resources. Further, as the availability of water changes, little is known about the speed and magnitude of agricultural adjustment. -
Hydrogeologic Characterization and Methods Used in the Investigation of Karst Hydrology
Hydrogeologic Characterization and Methods Used in the Investigation of Karst Hydrology By Charles J. Taylor and Earl A. Greene Chapter 3 of Field Techniques for Estimating Water Fluxes Between Surface Water and Ground Water Edited by Donald O. Rosenberry and James W. LaBaugh Techniques and Methods 4–D2 U.S. Department of the Interior U.S. Geological Survey Contents Introduction...................................................................................................................................................75 Hydrogeologic Characteristics of Karst ..........................................................................................77 Conduits and Springs .........................................................................................................................77 Karst Recharge....................................................................................................................................80 Karst Drainage Basins .......................................................................................................................81 Hydrogeologic Characterization ...............................................................................................................82 Area of the Karst Drainage Basin ....................................................................................................82 Allogenic Recharge and Conduit Carrying Capacity ....................................................................83 Matrix and Fracture System Hydraulic Conductivity ....................................................................83 -
Understanding Aquifers: Demonstration Using a Physical Model
Understanding Aquifers: Demonstration using a Physical Model Part I: Aquifers Explained Geology is the science of planet Earth, its history, and all the processes that act on it. Hydrogeology is the branch of geology which studies how water and rocks interact underground, mainly in aquifers An aquifer is a rock unit that holds enough water to supply water to wells. Aquifers can be found in many types of rocks, such as sandstone, conglomerate, unconsolidated sand and gravel, and fractured rocks composed of limestone or igneous rocks. Here at Barton Springs in Austin, Texas, we are standing on top of the Edward’s Aquifer, composed mostly of fractured limestone. These fractured rocks dissolve overtime and can create large, cave-like systems called Karst aquifers. So when you hear the word Karst, think cave. Some of these caves are big, some of them are small. Karst aquifers are different from sedimentary aquifers, where water flows mostly through the gravel and sand grains similar to a sponge. Hydrogeologists use two terms when investigating aquifers—porosity and permeability. Porosity is all the empty pore space inside a rock given in a percent volume. Porosity represents the volume of water a rock formation can potentially hold. Permeability is how well a fluid can flow within the pore spaces of the rock within the aquifer. For water, we describe this property as hydraulic conductivity. For example, clay and rocks like pumice may have high porosity, but because the pores do not connect with each other, the permeability of these rocks is usually low. Layers of low-permeability material such as clay and shale typically act as barriers to groundwater flow and may often function as an aquitard within a groundwater flow system. -
Stormwater and Water Quality
Contact information: www.engr.uconn.edu/cee 1 We will begin with an overall examination of what is “pollution,” discuss some primary water quality issues. Then, we will move on to some typical impacts that IWC will deal with and address the effectiveness and cost of mitigation measures. 2 Straw poll used to generate discussion on what WAS the state of the environment … then jump to how this has changed. 3 London – early 1850s cholera epidemic surrounding Broad Street Pump Dr. John Snow – broke handle to pump “breaking” the case Pre-1908: filtration used to purify drinking water Boonton Reservoir (NJ) – 1st system in US chlorinated 1908 Safe Drinking Water Act Killer smog – Donora, PA atmospheric inversion layer trapped pollutants near surface in a valley near Pittsburgh, PA – killing several people led to increased atmospheric awareness of air pollution Cuyahoga River (Cleveland) caught fire!!! Yes, water CAN burn! Resulted from garbage and oil on surface Not the only incident involving harbors burning Love Canal, NY – near Buffalo Toxic dumping site in old canal “bathtub” eventually filled with water and seeped into french drains and neighborhood – exposing residents to VERY high levels of pollutants Increased cancer and disease Led to CERCLA (a.k.a. “Superfund”) in 1980 4 Fish kill due to low oxygen in water – likely but not necessarily CSS outfall in West Hartford – YES! -note garbage and toilet paper in reeds in foreground Stormwater filled with sediment – YES! Acid mine drainage (low pH – acid – and high metals) – YES! -orange color -
The Influence of Karst Aquifer Mineralogy And
water Article The Influence of Karst Aquifer Mineralogy and Geochemistry on Groundwater Characteristics: West Bank, Palestine Hassan Jebreen 1,* , Andre Banning 1 , Stefan Wohnlich 1, Andrea Niedermayr 1, Marwan Ghanem 2 and Frank Wisotzky 1 1 Hydrogeology Department, Institute of Geology, Geophysics and Mineralogy, Ruhr University Bochum, Universitätsstr. 150, 44801 Bochum, Germany; [email protected] (A.B.); [email protected] (S.W.); [email protected] (A.N.); [email protected] (F.W.) 2 Department of Geography, Birzeit University, P.O. Box 14, Ramallah, Palestine; [email protected] * Correspondence: [email protected]; Tel.: +49-234-322-5387 Received: 31 October 2018; Accepted: 7 December 2018; Published: 11 December 2018 Abstract: This work reports, for the first time, the mineralogical and geochemical characteristics of karst aquifers in the Central West Bank (CWB) catchment in Palestine. It provides an integrated study approach by correlating the geochemistry of the lithology and hydrochemical data of groundwater samples. Mineralogical analysis showed that all of the samples were dominantly composed of either calcite CaCO3 (5–100 wt. %) or dolomite CaMg(CO3)2 (4–100 wt. %), with minor amounts of quartz and feldspar, which is supported by the inorganic carbon content (9–13 wt. %) and hydrochemical composition of the spring water samples. The whole-rock geochemical data indicated that the samples have low contents of trace elements and transition metals. In contrast, the concentrations of alkaline earth elements (Mg, Ca, Sr, Ba) and Mn were high in the rock and groundwater samples. Generally, the trace elements of rock samples with concentrations >10 ppm included Sr (17–330 ppm), Mn (17–367 ppm), Ba (2–32 ppm), W (5–37 ppm), Cr (3–23 ppm), Zn (1.7–28 ppm), V (4–23 ppm), and Zr (1–22 ppm), while the concentrations of all the other trace elements was below 10 ppm. -
Peak Water Demand Study: Development of Metrics And
The Future of Estimating Peak Water Demand in the Uniform Plumbing Code DAN COLE ACEEE HOT WATER FORUM MARCH, 2018 Estimating Peak Demand for Residential Dwellings Water Demand Calculator Code Provisions Code Provisions PEAK WATER DEMAND CALCULATOR M 101.0 General. M 101.1 Applicability. This appendix provides a method for estimating the demand load for the building water supply and principal branches for single- and multi-family dwellings with water-conserving plumbing fixtures, fixture fittings, and appliances. Code Provisions M 102.0 Demand Load. M 102.1 Water-Conserving Fixtures. Plumbing fixtures, fixture fittings, and appliances shall not exceed the design flow rate in Table M 102.1. Code Provisions M 102.2 Water Demand Calculator. The estimated design flow rate for the building supply and principal branches and risers shall be determined by the IAPMO Water Demand Calculator available for download at www.iapmo.org/WEStand/Pages/WaterDemandCalculator.aspx Code Provisions M 102.3 Meter and Building Supply. To determine the design flow rate for the water meter and building supply, enter the total number of indoor plumbing fixtures and appliances for the building in Column [B] of the Water Demand Calculator and run Calculator. See Table M 102.3 for an example. Code Provisions M 102.4 Fixture Branches and Fixture Supplies. To determine the design flow rate for fixture branches and risers, enter the total number of plumbing fixtures and appliances for the fixture branch or riser in Column [B] of the Water Demand Calculator and run Calculator. The flow rate for one fixture branch and one fixture supply shall be the design flow rate of the fixture according to Table M 102.1. -
Groundwater Movement and Soils
Lesson # 2: Groundwater Movement and Soils Through the activities below, students will learn how different types of soils and soil structure influence groundwater movement. Students will begin to understand how groundwater can become polluted. Activity # 1: “Sand, Gravel & Clay Soils & Groundwater Movement ” Teacher Preparation: Obtain 3 clear plastic containers or cut the tops off of clear plastic pop bottles. Fill one container with sand, the other with gravel and the final container with clay. Allow the students to feel each soil type and look at each container of soil. Have students discuss the differences they see between the 3 soils. Student Discussion Questions: 1. What do you notice about the size of the particles of sand, gravel & clay? Which has the largest particles? The smallest? 2. Ask students what is between the soil particles (spaces). Tell them that the “spaces” between the particles refers to the POROSITY of the soil. Which soil has the largest and smallest spaces? 3. Ask students which soil would allow water to move through the quickest and explain why. Tell them that the term used to describe the rate or speed at which water moves through the soil is called PERMEABILITY. Explain the relationship between porosity and permeability (larger or smaller spaces between the particles of soil results in a faster or slower movement of water through the soil). 4. If you were to construct a well into an aquifer, which of the 3 soils would you choose. Why? (Answer: Gravel. More water can be stored between the large pores and it would be easiest for a well to pump water from a gravel aquifer with large pore spacing.) 5. -
Peak Water: Risks Embedded in Japanese Supply Chains
Peak water: Risks embedded in Japanese supply chains Analysis of how companies in the Nikkei 225 Index are exposed to water risk through suppliers in Asia kpmg.or.jp trucost.com c | Section or Brochure name Contents 1.0 Executive summary 1 2.0 Trade in water risk: Corporate financial exposure in Japan 3 2.1 Study to assess supply chain water risk in the Nikkei 225 Index 3.0 Water use in the Nikkei 225 7 3.1 Supply chain water use varies across sectors 3.2 Variations in the water intensity of companies 3.3 Water scarcity pricing to identify risk 4.0 Mapping water use in supply chains 13 4.1 Water hot spots across the Personal & Household Goods sector 5.0 Corporate water risk in Asia 17 5.1 Creating supplier water risk profiles 5.2 Exposure to water risk in raw materials sourcing 6.0 Conclusions and next steps 21 7.0 Appendix: Trucost methodology 23 Authors: KPMG Director Kazuhiko Saito and Trucost Research Editor Liesel van Ast Acknowledgements: Thanks to Tom Barnett, Jessica Hedley, Steve Bullock, Stefano Dell’Aringa and Aaron Re’em of Trucost for contributing to this study. © 2012 KPMG AZSA Sustainability Co., Ltd., a company established under the Japan Company Law and a member firm of the KPMG network of independent member firms affiliated with KPMG International Cooperative (“KPMG International”), a Swiss entity. All rights reserved. © 2012 Trucost Plc 1 | Peak water: Risks embedded in Japanese supply chains 1.0 Executive summary KPMG AZSA Sustainability Co. has partnered with environmental data and insight experts Trucost to look at supply chain water risk in the Nikkei 225 Index. -
Lesson: Build an Aquifer
LESSON: BUILD AN AQUIFER Grade level: 4ththrough 5thgrade 4-ESSS2-1. Make observations and/or measurements to provide evidence of the effects of weathering or the rate of erosion by water, ice, wind, or vegetation. 5-ESS2-1. Develop a model using an example to describe ways the geosphere, biosphere, hydrosphere, and/or atmosphere interact. Activity Reference: http://www.aquariumofpacific.org/downloads/IAFTM_AquiferLesson.pdf INTRODUCTION Comprehension of the critical role played by water in support of all life on Earth is an essential foundational element of the Inland Empire Resource Conservation District’s (IERCD’s) Water Conservation classroom presentation. This activity is being provided to increase student awareness of water uses and benefits prior to program facilitation, and encourages development of this knowledge in a free form, group exercise. The suite of concepts and vocabulary covered will depend on length of activity facilitated by the participating teacher, but at any length should increase student preparation for IERCD program participation. It would also be suitable for post-program facilitation, to reinforce concepts and vocabulary covered during the program for maximum content retention. OBJECTIVE By engaging in this activity students will: • Obtain, evaluate, and communicate information and experience regarding the operation of an aquifer. • Gain Information about aquifers and the role aquifer’s play in groundwater. BACKGROUND An aquifer is a geologic unit saturated with water that can be used as a drinking supply (potable water). The water in an aquifer can be found in sediments and rock. Some rocks are porous and can hold water in the spaces between the grains. -
The Favorability of Florida's Geology to Sinkhole
Appendix H: Sinkhole Report 2018 State Hazard Mitigation Plan _______________________________________________________________________________________ APPENDIX H: Sinkhole Report _______________________________________________________________________________________ Florida Division of Emergency Management THE FAVORABILITY OF FLORIDA’S GEOLOGY TO SINKHOLE FORMATION Prepared For: The Florida Division of Emergency Management, Mitigation Section Florida Department of Environmental Protection, Florida Geological Survey 3000 Commonwealth Boulevard, Suite 1, Tallahassee, Florida 32303 June 2017 Table of Contents EXECUTIVE SUMMARY ............................................................................................................ 4 INTRODUCTION .......................................................................................................................... 4 Background ................................................................................................................................. 5 Subsidence Incident Report Database ..................................................................................... 6 Purpose and Scope ...................................................................................................................... 7 Sinkhole Development ................................................................................................................ 7 Subsidence Sinkhole Formation .............................................................................................. 8 Collapse Sinkhole