Design, Operation, and Maintenance for Sustainable Underground Storage Facilities
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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. -
Data Source: FAO, UN and Water Resources
GROUNDWATER WATER DAY SPECIAL How bad is it already Aquifers under most stress are in poor and populated regions, where alternatives are limited Shrinking source Ganga-Brahmaputra Basin in 145 km3 21 8 India, Nepal and Bangladesh, More than half of the world's major aquifers, The amount of of world's 37 largest aquifer of these 21 aquifer systems North Caucasus Basin in Russia groundwater the systemsÐshaded in redÐlost are overstressed, which and Canning Basin in Australia which store groundwater, are depleting faster world extracts water faster than they could be means they get hardly any have the fastest rate of depletion than they can be replenished every year recharged between 2003 and 2013 natural recharge in the world Aquifer System where groundwater levels are depleting Pechora Basin Tunguss Basin (in millimetres per year) 3.038 1.664 Aquifer System where groundwater levels are increasing Northern Great Ogallala Aquifer Cambro-Ordovician Russian Platform Basin (in millimetres per year) 4.011 Yakut Basin Plains Aquifer (High Plains) Aquifer System 2.888 Map based on data collected by 4.954 0.309 2.449 NASA's Grace satellite between 2003 and 2013 Paris Basin 4.118 Angara-Lena Basin 3.993 West Siberian Basin Californian Central Atlantic and Gulf Coastal 1.978 Valley Aquifer System Plains Aquifer 8.887 5.932 Tarim Basin Song-Liao Basin North Caucasus Basin 0.232 2.4 Northwestern Sahara Aquifer System 16.097 Why aquifers are important 2.805 Nubian Aquifer System 2.906 North China Aquifer System Only three per cent of the world's water -
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 .......................................................................... -
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. -
Water Levels in Major Artesian Aquifers of the New Jersey Coastal Plain, 1988
WATER LEVELS IN MAJOR ARTESIAN AQUIFERS OF THE NEW JERSEY COASTAL PLAIN, 1988 By Robert Rosman, Pierre J. Lacombe, and Donald A. Storck U.S. GEOLOGICAL SURVEY Water-Resources Investigations Report 95-4060 Prepared in cooperation with the NEW JERSEY DEPARTMENT OF ENVIRONMENTAL PROTECTION West Trenton, New Jersey 1995 CONTENTS Page Abstract............................................................. 1 Introduction......................................................... 2 Purpose and scope............................................... 2 Study area...................................................... 2 Previous investigations......................................... 4 Well-numbering system........................................... 4 Methods of data collection...................................... 5 Description of data presented................................... 6 Acknowledgments................................................. 8 Hydrogeology of the Coastal Plain.................................... 8 Description of aquifers and confining units..................... 11 Location of freshwater/saltwater interface...................... 12 Water levels in artesian aquifers of the Coastal Plain............... 13 Cohansey aquifer in Cape May County............................. 13 Water levels............................................... 13 Water-level fluctuations................................... 13 Atlantic City 800-foot sand..................................... 14 Water levels............................................... 14 Water-level -
Causes of Groundwater Depletion
Number 63 Issue Paper February 2019 Aquifer Depletion and Potential Impacts on Long-term Irrigated Agricultural Productivity When developing policies that regulate groundwater systems that are being depleted, the potential consequences of groundwater depletion need to be fully assessed to determine the trade-offs that exist between the undesired impacts of groundwater depletion and whether these impacts outweigh the benefits associated with groundwater use. (Photo from Ed Hennigan/Shutterstock.) is even higher in arid and semi-arid ar- the Mississippi Embayment Aquifer ABSTRACT eas, where the only consistent source of (Mississippi River lowlands bordering Groundwater is the Earth’s most irrigation water is groundwater. In these Arkansas and Mississippi), aquifers in extracted raw material, with almost regions, however, the use of groundwa- southern Arizona, and smaller aquifers 1,000 cubic kilometers per year (800 ter typically far exceeds the rate at which in many western states. million acre-feet per year) of ground- it is naturally replenished, indicating The groundwater resource with the water pumped from aquifers around the that these critical groundwater resources greatest long-term depletion is the High world. Approximately 70% of ground- are being slowly depleted. Within the Plains (Ogallala) aquifer in the Great water withdrawals worldwide are used to United States, groundwater depletion has Plains Region of the United States, support agricultural production systems, occurred in many important agricultural where groundwater levels have declined and within the United States, about 71% production regions, including the Great by more than 50 meters (150 feet) of groundwater withdrawals are used for Plains Region (Nebraska, Colorado, in some areas. -
Supplement of Earth Syst
Supplement of Earth Syst. Dynam., 11, 755–774, 2020 https://doi.org/10.5194/esd-11-755-2020-supplement © Author(s) 2020. This work is distributed under the Creative Commons Attribution 4.0 License. Supplement of Groundwater storage dynamics in the world’s large aquifer systems from GRACE: uncertainty and role of extreme precipitation Mohammad Shamsudduha and Richard G. Taylor Correspondence to: Mohammad Shamsudduha ([email protected]) The copyright of individual parts of the supplement might differ from the CC BY 4.0 License. Supplementary Table S1. Characteristics of the world’s 37 large aquifer systems according to the WHYMAP database including aquifer area, total number of population, proportion of groundwater (GW)-fed irrigation, mean aridity index, mean annual rainfall, variability in rainfall and total terrestrial water mass (ΔTWS), and correlation coefficients between monthly ΔTWS and precipitation with reported lags. ) 2 2) Correlation between between Correlation precipitation TWS and (lag in month) GW irrigation (%) (%) GW irrigation on based zones Climate Aridity indices Mean (2002-16) annual precipitation (mm) Rainfall variability (%) (cm TWS variance WHYMAP aquifer number name Aquifer Continent (million)Population area (km Aquifer Nubian Sandstone Hyper- 1 Africa 86.01 2,176,068 1.6 30 12.1 1.5 0.16 (13) Aquifer System arid Northwestern 2 Sahara Aquifer Africa 5.93 1,007,536 4.4 Arid 69 17.3 1.9 0.19 (8) System Murzuk-Djado Hyper- 3 Africa 0.35 483,817 2.3 8 36.6 1.3 0.20 (-8) Basin arid Taoudeni- Hyper- 4 Africa 0.35 -
Flowing Artesian Wells
Flowing Artesian Wells Water Stewardship Information Series Table of Contents What’s the difference between a flowing artesian well Are there specific actions to avoid when flowing artesian and an artesian well? . 1 conditions are present? . 6 Why do wells flow? . 1 How can flowing artesian well be constructed in bedrock aquifers? . 7 Why is stopping or controlling artesian flow important? . 2 How can flowing artesian well be constructed in How can flowing artesian conditions be determined unconsolidated aquifers? . 7 before drilling? . 2 What should be done if flowing artesian conditions are What are the provincial regulatory requirements for suddenly encountered? . 7 controlling or stopping artesian flow? . 2 What are the key factors in completing and equipping What does it mean to “control” artesian flow from a well? . 3 a flowing artesian well? . 8 Will a flowing artesian well dry up if the flow is stopped How is the pressure or static water level for a flowing or controlled? . 3 artesian well measured? . 8 Are there any water quality concerns with flowing How should flowing artesian wells be closed? . 8 artesian wells? . 3 How is a flowing artesian well disinfected? . 9 Are there any other concerns with flowing artesian wells? . 3 Further Information . 9 What can be done with an existing flowing well? . 4 What if the flow is needed, for example, to increase the baseflow of a creek or stream? . 4 Are there some general guidelines for constructing a flowing artesian well? . 4 What are the key issues to be aware of when drilling a flowing artesian well? . 5 This booklet contains general information on flowing artesian wells for well drillers, groundwater consultants and well owners Hydrostatic head (or confining pressure) is the vertical in British Columbia . -
Innovative Solutions for Water Wars in Israel, Jordan, and The
INNOVATIVE SOLUTIONS FOR WATER WARS IN ISRAEL, JORDAN AND THE PALESTINIAN AUTHORITY J. David Rogers K.F. Hasselmann Chair, Department of Geological Engineering 129 McNutt Hall, 1870 Miner Circle University of Missouri-Rolla, Rolla, MO 65409-0230 [email protected] (573) 341-6198 [voice] (573) 341-6935 [fax] ABSTRACT In the late 1950s Jordan and Israel embarked on a race to collect, convey and disperse the free-flowing waters of the Jordan River below the Sea of Galilee. In 1955 the Johnston Unified Water Plan was adopted by both countries as a treaty of allocation rights. By 1961 the Jordanians completed their 110-km long East Ghor Canal, followed by Israel’s 85-km long National Water Carrier, initially completed in 1964 and extended in 1969. The Johnston allocation plan was successfully implemented for 12 years, until the June 1967 war between Israel and her neighbor Arab states. The Israelis have spearheaded the effort to exploit the region’s limited water resources, using wells, pipelines, canals, recharge basins, drip irrigation, fertigation, wastewater recharge, saline irrigation and, most recently, turning to desalination. In 1977 they began looking at various options to bring sea water to the depleted Dead Sea Basin, followed by similar studies undertaken by the Jordanians a few years later. A new water allocation plan was agreed upon as part of the 1994 Israel-Jordan peace treaty, but it failed to address Palestinian requests for additional allotments, which would necessarily have come from Jordan or Israel. The subject of water allocation has become a non-negotiable agenda for the Palestinian Authority in its ongoing political strife with Israel. -
Groundwater Modeling of the Withdrawal
DOI: 10.7343/as-2018-333 Paper Groundwater modeling of the withdrawal sustainability of Cannara artesian aquifer (Umbria, Italy) Modellazione delle acque sotterranee e prelievo sostenibile dall’acquifero artesiano di Cannara (Umbria) Giovanni Pietro Beretta, Monica Avanzini, Tomaso Marangoni, Marino Burini, Giacomo Schirò, Jacopo Terrenghi, Gaetano Vacca Riassunto: L’acquifero di Cannara (Umbria, Italia) è noto da oltre un Abstract: The Cannara aquifer (Umbria, Italy) has been known for more secolo ed è uno dei principali punti di approvvigionamento di acqua than a century, and is one of the main drinking water supplies in the Umbria potabile nella Regione Umbria. All’inizio veniva utilizzato per scopi Region. In the beginning it was used for irrigation purposes, since this area was irrigui, poiché quest’area era prevalentemente agricola fino agli anni mainly agricultural up to the 1960s. The groundwater—exploited by Umbra ‘60. Le acque sotterranee, sfruttate da Umbra Acque S.p.A. (Società che Acque S.p.A. (a Company supplying drinking water)—is 150 m under ground fornisce l’acqua potabile), sono a 150 m al di sotto il livello del suolo e level and is contained in a porous confined aquifer, which originally had arte- sono contenute in un acquifero poroso confinato, che in origine aveva sian characteristics. Exploitation of 200–300 l/s with nine wells caused a re- caratteristiche artesiane. Lo sfruttamento di 200-300 l/s con nove pozzi duction of piezometric level, maintaining the confined aquifer conditions, except ha causato una riduzione del livello piezometrico, mantenendo le con- for a very short period during which the aquifer was depressurised by drought, dizioni di acquifero confinato, ad eccezione di un periodo molto breve and for increase of emergency withdrawals replacing other water supplies (from durante il quale la falda è stata depressurizzata in seguito alla siccità e springs) for drinking purposes. -
The Secret Life of Groundwater
The Secret Life of Groundwater Presented by Natalie Ballew, Texas Water Development Board Activity by Shae Luther and Josh Sendejar, Texas Water Development Board 1 Groundwater flow according to Athanasius Kircher (Kricher, 1665) Image from www.un-igrac.org/sites/default/files/resources/files/Groundwater_around_world.pdf Groundwater has often been perceived as a complete mystery. Imagination and mythology used to drive perceptions of groundwater flow. This is a depiction of groundwater flow from the 1600s. Back then, people believed that water moved from the sea floor up to mountains through mysterious channels where it emerged as springs. The Texas Supreme Court, in more recent history, has even called groundwater ‘secret, occult, and concealed.’ 2 Now, based on scientific observation, we have the water cycle as we know it today. I’m sure y’all are all familiar with the water cycle, how water moves around the earth and atmosphere. The basics, if you need a refresher, evaporation, condensation and precipitation. The water cycle is so much more than just that. Scientists continue to collect data to understand all parts of the water cycle because it’s essential to life on earth and understanding all parts of it can help us make smart decisions around use and conservation to ensure we have water available for generations to come. 3 Today we’ll focus on the groundwater portion of the water cycle. Groundwater is a very important resource in Texas for things like irrigation, public water supply, and environmental needs; in fact, there is more groundwater use in the state than there is surface water use. -
Strange but True Ction
FOLLOW US: Wednesday, May 6, 2020 thehindu.in facebook.com/thehinduinschool twitter.com/the_hindu CONTACT US [email protected] Printed at . Chennai . Coimbatore . Bengaluru . Hyderabad . Madurai . Noida . Visakhapatnam . Thiruvananthapuram . Kochi . Vijayawada . Mangaluru . Tiruchirapalli . Kolkata . Hubballi . Mohali . Malappuram . Mumbai . Tirupati . lucknow . cuttack . patna Organisms adopt dierent strategies to survive – some of these are Thorny devil so impressive that they may seem like superpowers straight out of The thorny devil is a lizard species adapted Strange but true ction. Read on to discover some of them... to the hot and dry condition of the Australian desert. The upper body of the thorny devil is covered by an intimidating Puersh array of spikes. There are grooves between Zombie ant fungus these spikes which help the lizard absorb The puersh is a slow and clumsy water from the sand that’s wet from the Ophiocordyceps swimmer but to make up for this morning dew or a recent but rare rainfall. unilateralis or shortcoming, the sh has an amazing Essentially, the lizard’s skin works like a zombie ant fungus is ability to inate its elastic stomach several paper towel, soaking up water from the a type of pathogenic times its original size. When threatened, a sand, and channelling it towards the fungus found puersh would expand its stomach and lizard’s mouth. predominantly in quickly gulp large amounts of water, thus tropical forest turning itself into a huge inedible ball. ecosystems. The Some species are known to open up their fungus has a unique hidden spikes as well. As an added way of spreading its protection, their body contains spores for tetrodotoxin, a substance more poisonous reproduction.