Snake River Plain Aquifer Wells Project, Falls Irrigation District
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Ultimate RV Dump Station Guide
Ultimate RV Dump Station Guide A Complete Compendium Of RV Dump Stations Across The USA Publiished By: Covenant Publishing LLC 1201 N Orange St. Suite 7003 Wilmington, DE 19801 Copyrighted Material Copyright 2010 Covenant Publishing. All rights reserved worldwide. Ultimate RV Dump Station Guide Page 2 Contents New Mexico ............................................................... 87 New York .................................................................... 89 Introduction ................................................................. 3 North Carolina ........................................................... 91 Alabama ........................................................................ 5 North Dakota ............................................................. 93 Alaska ............................................................................ 8 Ohio ............................................................................ 95 Arizona ......................................................................... 9 Oklahoma ................................................................... 98 Arkansas ..................................................................... 13 Oregon ...................................................................... 100 California .................................................................... 15 Pennsylvania ............................................................ 104 Colorado ..................................................................... 23 Rhode Island ........................................................... -
Functional Classification Update Report for the Pocatello/Chubbuck Urbanized Area
Functional Classification Update Report For the Pocatello/Chubbuck Urbanized Area Functional Classification Update Report Introduction The Federal-Aid Highway Act of 1973 required the use of functional highway classification to update and modify the Federal-aid highway systems by July 1, 1976. This legislative requirement is still effective today. Functional classification is the process by which streets and highways are grouped into classes, or systems, according to the character of service they are intended to provide. The functional classification system recognizes that streets cannot be treated as independent, but rather they are intertwined and should be considered as a whole. Each street has a specific purpose or function. This function can be characterized by the level of access to surrounding properties and the length of the trip on that specific roadway. Federal Highway Administration (FHWA) functional classification system for urban areas is divided into urban principal arterials, minor arterial streets, collector streets, and local streets. Principal arterials include interstates, expressways, and principal arterials. Eligibility for Federal Highway Administration funding and to provide design standards and access criteria are two important reasons to classify roadway. The region is served by Interstate 15 (north/South) and Interstate 86 (east/west). While classified within the arterial class, they are designated federally and do not change locally. Interstates will be shown in the functional classification map, but they will not be specifically addressed in this report. Functional Classification Update The Idaho Transportation Department has the primary responsibility for developing and updating a statewide highway functional classification in rural and urban areas to determine the functional usage of the existing roads and streets. -
ITD Board Sets Wish List for Potential Stimulus
ITD board sets wish list for potential stimulus The priorities include six road projects that wouldn't otherwise be done. None are in the Valley. Idaho Statesman, January 8, 2009 By: Cynthia Sewell Idaho transportation leaders want to spend $94 million on six otherwise unfunded road projects if President-elect Barack Obama and the new Congress pass a stimulus package dedicated to infrastructure. The windfall could create between 2,000 and 4,000 Idaho jobs, officials said. None of the six roads are in the Treasure Valley, but the region's section of Interstate 84 has been getting - and is expecting to keep getting - most of the borrowed federal dollars from the Connecting Idaho project. The stimulus projects officials have identified would upgrade treacherous Idaho 95 in North Idaho and jump-start road projects in Pocatello, Twin Falls and East Idaho. The Idaho Transportation Department board picked these projects during a special meeting Wednesday, and officials say they could be under construction by June. Several versions of possible stimulus bills are circulating in Washington, and details are still sketchy. ITD expects Idaho could receive about $100 million for roads. Agency staff had identified $817 million in projects that could be ready for construction within 180 days. The six board members disagreed on two points on how best to spend the $100 million: Whether to put the money toward new projects or use it to repair the state's existing roads. Whether to divide the money equally around the state or give it to the areas with the most need. Jim Coleman, who represents North Idaho, argued that the state should use one-time money to finance key projects it is unlikely to be able to afford under current revenue sources. -
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. -
Section 4: County Profile
SECTION 4: COUNTY PROFILE SECTION 4: COUNTY PROFILE Broome County profile information is presented in the plan and analyzed to develop an understanding of a study area, including the economic, structural, and population assets at risk and the particular concerns that may be present related to hazards analyzed later in this plan (e.g., low lying areas prone to flooding or a high percentage of vulnerable persons in an area). This profile provides general information for Broome County (physical setting, population and demographics, general building stock, and land use and population trends) and critical facilities located within the County. GENERAL INFORMATION Broome County is a rural community located within the south-central part or “Southern Tier” of New York State. The Southern Tier is a geographical term that refers to the counties of New York State that lie west of the Catskill Mountains, along the northern border of Pennsylvania. Broome County lies directly west of Delaware County, 137 miles southwest of Albany and approximately 177 miles northwest of New York City. Broome County occupies approximately 715 square miles and has a population of approximately 199,031 (U.S. Census, 2011). Broome County is one of the 62 counties in New York State and is comprised of one city, sixteen towns, seven villages and many hamlets. The City of Binghamton is the County seat and is located at the confluence of the Susquehanna and Chenango Rivers. The City of Binghamton is part of the “Triple Cities,” which also includes the Villages of Endicott and Johnson City. With two Interstates and a major state route intersecting in the City of Binghamton, the area is the crossroads of the Southern Tier. -
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 -
Federal Register/Vol. 65, No. 233/Monday, December 4, 2000
Federal Register / Vol. 65, No. 233 / Monday, December 4, 2000 / Notices 75771 2 departures. No more than one slot DEPARTMENT OF TRANSPORTATION In notice document 00±29918 exemption time may be selected in any appearing in the issue of Wednesday, hour. In this round each carrier may Federal Aviation Administration November 22, 2000, under select one slot exemption time in each SUPPLEMENTARY INFORMATION, in the first RTCA Future Flight Data Collection hour without regard to whether a slot is column, in the fifteenth line, the date Committee available in that hour. the FAA will approve or disapprove the application, in whole or part, no later d. In the second and third rounds, Pursuant to section 10(a)(2) of the than should read ``March 15, 2001''. only carriers providing service to small Federal Advisory Committee Act (Pub. hub and nonhub airports may L. 92±463, 5 U.S.C., Appendix 2), notice FOR FURTHER INFORMATION CONTACT: participate. Each carrier may select up is hereby given for the Future Flight Patrick Vaught, Program Manager, FAA/ to 2 slot exemption times, one arrival Data Collection Committee meeting to Airports District Office, 100 West Cross and one departure in each round. No be held January 11, 2000, starting at 9 Street, Suite B, Jackson, MS 39208± carrier may select more than 4 a.m. This meeting will be held at RTCA, 2307, 601±664±9885. exemption slot times in rounds 2 and 3. 1140 Connecticut Avenue, NW., Suite Issued in Jackson, Mississippi on 1020, Washington, DC, 20036. November 24, 2000. e. Beginning with the fourth round, The agenda will include: (1) Welcome all eligible carriers may participate. -
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. -
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. -
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. -
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.