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methodology for groundwater resources management of a typical alluvial aquifer systemin Greece

Andreas C. Panagopoulos

methodology for groundwater resources management of a typical alluvial aquifer systemin Greece

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Published by University of Birmingham in Birmingham .
Written in English


Edition Notes

Thesis (Ph.D.)-University of Birmingham, School of Earth Sciences, 1996.

Statementby Andreas C. Panagopoulos.
ID Numbers
Open LibraryOL22215051M

  1. INTRODUCTION. Karst aquifers provide drinkable water for hundreds of millions of people, accounting for 25% of the world and 40% of the US groundwater resources (Ford and Williams ; Quinlan and Ewers ).Karst aquifers have complex characteristics that make them different from other aquifers (Bakalowicz ).They form in soluble rocks, such as dolomite and limestone, Cited by: The hydrogeologic characteristics of the unconsolidated glacial outwash sand and gravel deposits that compose the northeast portion of the alluvial aquifer at Louisville, Kentucky, indicate a prolific water-bearing formation with approximately 7 billion gallons of ground-water storage and an estimated sustainable yield of over million gallons per day. This report describes the construction, calibration, evaluation, and results of a steady-state numerical groundwater flow model of the Great Basin carbonate and alluvial aquifer system that was developed as part of the U.S. Geological Survey National Water Census Initiative to evaluate the nation’s groundwater availability. The study area spans , square miles across five states.


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methodology for groundwater resources management of a typical alluvial aquifer systemin Greece by Andreas C. Panagopoulos Download PDF EPUB FB2

A methodology for groundwater resources management of a typical alluvial aquifer system in Greece Author: Panagopoulos, Andreas C. Panagopoulos A. () A methodology for groundwater resources management of a typical alluvial aquifer system in Greece,The University of Birmingham, U.K Google Scholar Quevauviller Ph () From the groundwater action programme to the groundwater directive-What have we done, what have we learnt, what is the way ahead?Cited by: 1.

Greece. Simulation of the aquifer system in the study area was performed on FEFLOW and the calibrated model was then used for the feasibility assessment of alternative groundwater management strategies based on groundwater artificial recharge.

It was demonstrated that groundwater artificial recharge methodology for groundwater resources management of a typical alluvial aquifer systemin Greece book technically feasible and financially reasonable, thus presents.

Panagopoulos A. (), A methodology for groundwater resources management of a typical alluvial aquifer system in Greece, School of Earth Sciences, Ph.D. Thesis, University of Birmingham, 46p. Tziritis E., Skordas K. and Kelepertsis A. (), The use of hydrogeochemical analyses and multivariate statistics forFile Size: KB.

The DPSIR approach to groundwater management for sustainable development in coastal areas: The case of Nea Peramos aquifer system, Kavala, Greece K.

Mimidis1, P. Andrikakou1, A. Kallioras2 and F. Pliakas1* 1 Engineering Geology Laboratory, Civil Engineering Department, Democritus University of Thrace, Xanthi, Greece. alluvial aquifer, dominantly from sandy gravel sediments. Ljubljansko B. arje is. dominantly agricultural.

Ljubljansko polje aquifer area are. urbanized and agricultural. roundwater is. 4 – 30 m bellow the surface. It is recharg. from precipitation and from Sava river. The present research work uses Residual Kriging to estimate the groundwater level of an unconfined alluvial aquifer, as well as the trend function.

The ground surface elevation is used as auxiliary. WATER RESOURCES AND GROUNDWATER QUALITY the irrigation area has increased between from to 41% (Korinthia) and from to 42% (Achaia).

The aforementioned percentage is one of the higher in Greece. Table 1. Population in the studied area Year/Prefecture Achaia,of the groundwater flow, which takes into account possible variations in the interaction surface-ground water.

Case study The case study, the Petrignano d’Assisi aquifer (approximately 75 km2) is located in the Umbria Region (Central Italy), within the Tiber river basin.

It is part of the Umbra Valley aquifer and is located between the Martani. Panagopoulos A., A methodology for groundwater resources management of a typical alluvial aquifer system in Greece. Panagopoulos Methodology for groundwater resources management of a typical alluvial aquifer systemin Greece book () A methodology for groundwater resources management of a typical alluvial aquifer system in Greece.

Ph.D. thesis, University of Birmingham, Birmingham, p Google Scholar Zampetakis G () Monitoring balance of groundwater and surface waters of Crete, Brackish Aquifers, Volume ΙΙΙ, Almyros Heraklion spring by: 1.

Panagopoulos, A., A methodology for groundwater resources management of a typical alluvial. aquifer system in Greece. Ph.D. thesis, University of Birmingham, Birmingham, pp.

Panagopoulos, A., Karyotis, A., Georgiou, Th., Tsitouras, Al., Groundwater natural backgroundCited by: 1. Dispersion of groundwater age in an alluvial aquifer system Gary S.

Weissmann,1 Y. Zhang, Eric M. LaBolle, and Graham E. Fogg2 Hydrologic Sciences, University of California, Davis, California, USACited by: than 5,2 millions m’ in and the Var delta groundwater exploitation should be raised, The salinisation risks of the alluvial sheet and the coastal aquifer management problems bound to the economic and urban development of the coast [2] [3] led to set up a study of the site to characterize the.

A huge amount of water exists in the ground below your feet, and people all over the world make great use of it. But it is only found in usable quantities in methodology for groundwater resources management of a typical alluvial aquifer systemin Greece book places underground — aquifers.

Read on to understand the concepts of aquifers and how water exists in the ground. A hole dug at the beach is a great way to illustrate the concept. Groundwater circulation and hydrogeochemical evolution in a typical alluvial-lacustrine plain of Qaidam Basin, Northwestern China Mr.

Yong Xiao Use of Boolean Logic in a GIS environment for selecting zones for Artificial Groundwater Recharge in north western Saudi Arabia. Considering the density of freshwater ( g/cm 3 at 20°C) and seawater ( g/cm 3 at 20°C), the equation given by Ghyben-Herzberg simplifies to z = 40 h.

Thus, for every meter of freshwater in an unconfined aquifer above sea level, there will be 40 m of freshwater in the aquifer below sea level (Drabbe and Ghyben, ; Herzberg, ).That is, if the groundwater level declines by a Cited by: 2.

Panagopoulos A.:™™ A methodology for groundwater resources management of a typical alluvial aquifer system in Greece™™ Phd thesis in University of Birmingham, Tsouflidou S., Dimitrakopoulos D. Louloudis G., Terzopoulou E.: flStudy for the protection of Domeniko lignite mine from ground waterfl, PPC, Athens Estimations of the available groundwater resources have been carried out, but in both principal aquifers there are pro­ blems with the application of conventional methods.

In the plateau areas the dambo drainage systems play an important but uncertain role in the movement and storage of groundwater. In the alluvialFile Size: 6MB. Aegean islands' limited groundwater resources set them among the most sensitive water districts of Greece.

Some of the main inhibiting factors affecting groundwater resources are the islands' limited surface areas, complex geological structure, sharp hilly morphology and low storativity combined with low annual rainfall and high average temperatures (Kourmoulis et al. ).Cited by: 2. Integrated Groundwater Resources Management Using the DPSIR Approach in a GIS Environment: A Case Study from the Gallikos River Basin, North Greece Christos Mattas 1, Konstantinos S.

Voudouris 1,* and Andreas Panagopoulos 2 1 Laboratory of Engineering Geology &. An alluvial aquifer can be described as a groundwater system, generally unconfined, that is hosted in laterally discontinuous layers of gravel, sand, silt and clay, deposited by a river in a river channel, banks or flood by: 3.

Groundwater is the most used water resource around the world, but due to population growth and climate change the alluvial lowland aquifers are often polluted and over-exploited. Thus, more and more frequently water managers need to shift their attention to mountain regions to identify groundwater resources for drinking purposes.

A significant portion of water resources comes from groundwater. The DGB starts from the coast with elevations of 0–60 masl and covers an area of 26 km 2, about % of the Comoro watershed area (i.e., km 2) (Figure ).Groundwater is abstracted from a thick intergranular alluvial aquifer dominated by silt clay and an intermittent thin clay layer underlain by a saprolite layer and Cited by: 1.

Ground-Water Models of the Alluvial and Sparta Aquifers: Management Tools for a Sustainable Resource Printed on recycled paper Introduction Arkansas is the fourth largest user of ground water in the United States.

The Mississippi River Valley alluvial aquifer (alluvial aquifer) is a water-bearing assemblage of gravels. Continuing in its forty-year history of providing students and professionals with a thorough grounding in the science and technology of groundwater hydrology, this third edition has been completely updated to reflect the tremendous changes in the field.

A true essential reference, this book provides a unified presentation of groundwater hydrology, treating fundamental principles, methods and. Basic Concepts of Groundwater Hydrology called alluvial basins,ground water fills small, often microscopic pores between the grains of gravel, sand, silt, and clay.

Typical groundwater velocity in a sandy or gravelly aquifer may range from to 50 feet per Size: KB. Reed, T.B.,Recalibration of a ground-water flow model of the Mississippi River Valley alluvial aquifer of northeastern Arkansas,with simulations of water levels caused by projected ground-water withdrawals through U.S.

Geological Survey Water-Resources Investigations Report 03. selected as a case study for the application of FREEWAT platform, to simulate the groundwater flow of the alluvial aquifer layer. The study area is a typical Mediterranean coastal site that is hydraulically connected to the sea, while the groundwater resources are exclusively used for irrigation purposes.

About 20 per cent of all bores in Australia are in alluvial systems and they account for 60 per cent of Australia’s groundwater extraction. Alluvial aquifers are generally shallower than sedimentary and fractured rock aquifers and water levels often fluctuate due to varying recharge and pumping rates.

The primary water source for Emporia and the surrounding areas is the Neosho River and its alluvial aquifer system. To successfully explore and manage our groundwater resources, a detailed knowledge of the spatial distribution of aquifer characteristics such as lithology, thickness and hydraulic properties is essential.

(Park, et. Groundwater Contamination and Aquifer Reclamation at the Rocky Mountain Arsenal, Colorado 6 INTRODUCTION LEONARD F. KONIKOW U.S.

Geological Survey DOUGLAS W. THOMPSON U.S. Army Corps of Engineers AB STRACT Groundwater contamination at the Rocky Mountain Arsenal, Colorado, is related to the disposal of liquid industrial wastes and to industrial.

A large number of Latin American cities are located along the Atlantic, Caribbean, and Pacific coasts, and 30–40 of them rely on groundwater drawn from various types of coastal aquifers, Among them are Mar del Plata, Argentina (taking water from an alluvial aquifer on the shores of the Atlantic); Natal and Recife, Brazil; Santa Marta, Colombia; Havana, Cuba (which gets all its water from a.

the area required to sustain groundwater use and groundwater dependent ecosystem services. GWF represents a water balance between aquifer inflows and outflows, focusing on environmental flow requirements. As the GWF is a tool recently introduced in groundwater assessment and management, only a few studies have been reported in the literature to.

Barlow, P.M., Ahlfeld, D.P., and Granato, G.E.,A simulation-optimization model for evaluation of ground-water development options constrained by minimum streamflow requirements and water-supply demands in Proceedings, MODFLOW and MORE —Managing Ground Water Systems, Eileen Poeter, Mary Hill, Chunmiao Zheng, organizing committee: International Ground Water Modeling.

The structure, status, and processes of the groundwater system, which can only be acquired through scientific research efforts, are critical aspects of water resource management.

Isotope hydrology and hydrogeology is a genuinely interdisciplinary science. It developed from the application of methods evolved in physics (analytical techniques) to problems of Earth and the environmental sciences Cited by: Groundwater Quality Mapping of an Alluvial Aquifer, Eshtehard, Iran Pertanika J.

Sci. & Technol. Vol. 19 (S) 61 MAtErIALS ANd MEthod Groundwater samples were taken directly from 44 sample points in May and October Water quality parameters (chloride, sulfate) were then analyzed in the laboratory of Tehran Regional Water.

Aquifer vulnerability assessment in the Bengal alluvial tract, India, using GIS based DRASTIC model, Modeling Earth Systems and Environment,pp.

Volume 2, Cited by: 4. The Mississippi River Alluvial Aquifer—the aquifer used by farmers, closer to the surface than the source of drinking water—has according to some.

The Ground Water Resources Committee, a subcommittee of the LAAC, produced a map depicting areas of ground water significance at regional scale (,) (see Figure ) to give decision makers the basis for considering ground water as a factor in land acquisition under the Preservation Act (LAAC ).

In developing maps for their. Pdf of groundwater age models for assessing nitrate loading, transport pathways, and management options in a complex aquifer system.

In an aquifer system with complex hydrogeology, mixing of groundwater with different ages could occur associated with various flow pathways.The alluvial aquifers beneath download pdf floodplains of the Mississippi and Missouri rivers are some of Missouri's most valued water resources.

These aquifers are capable of yielding from to more than 2, gallons of water per minute to properly designed and developed wells, and are widely used for municipal water supply and agricultural irrigation.In the current context of climate ebook, improving groundwater monitoring and management is an important issue for human ebook in arid environments.

The exploitation of groundwater resources can trigger land subsidence producing damage in urban structures and infrastructures. Alto Guadalentín aquifer system in SE Spain has been exploited since producing an average piezometric Cited by: 5.