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Published byIngrid Sealy
Modified over 4 years ago
Cyprus Pump Test
Aquifer Study Area
Yeşilkoy Aquifer Area Recharge Area Discharge Area Water Levels in Local Wells 2002 - 2006 2 m drop 5 m drop
Yesilkoy Geology Calcarenite in the Yeşilkoy aquifer Hydraulic Conductivity of Calcarenite
Yesilkoy Aquifer Initial Conceptual Model (Unconfined aquifer)
Yesilkoy Pump Test
Pump Test Results Hand measured Drawdown and Recovery for YK-109 Transducer measured Data for Drawdown and Recovery of YK-109
Pump Test Analysis YK-109 Drawdown Analysis using Theis Method in AquiferTest
Match Point 1/u = 10, W(u) = 1.0 t = 150 min, s = 11 cm
Theis Method Example Match Point 1/u = 10, W(u) = 1.0 t = 150 min, s = 11 cm Q = 0.4359 m3/min
Yeşilköy Aquifer Updated Conceptual Model (Leaky confined aquifer)
Simulation of groundwater response to development: CENTRAL PASSAIC RIVER BASIN, NJ Fatoumata Barry 1,2, Duke Ophori 1, Jeffrey L. Hoffman 2 and Robert.
Groundwater Hydraulics Daene C. McKinney
FMC SPILL SITE July 11, 1996: Tanker truck turned over spilling 6000 gallons (23000L) gasoline 500ft (150m) North from Bear Creek Emergency Response Team.
Chapter 12:Variable-discharge tests and tests in well fields Aquifers may be pumped at variable discharge rates either deliberately or due to characteristics.
Groundwater Flow Equations
Principles of Groundwater Flow
Flow to Wells.
Groundwater Modeling - 1
Chapter 15: Single Well tests
Chapter 14: Well-Performance Tests
Partially Penetrating Wells By: Lauren Cameron. Introduction Partially penetrating wells: aquifer is so thick that a fully penetrating well is impractical.
Well flow & Pumping tests
Aquifer Tests in Unconfined Aquifers Lauren Cameron Spring 2014.
Advanced Hydrogeology Malcolm Reeves Civil and Geological Engineering.
Add Main Topic Here Created by Educational Technology Network
Tripp Winters. Anisotropy is a common feature in water laid sedimentary deposits (fluvial, clastic lake, deltaic and glacial outwash). Water lain.
Chapter 6: Bounded Aquifers Stephanie Fulton January 24, 2014.
ESS 454 Hydrogeology Module 4 Flow to Wells Preliminaries, Radial Flow and Well Function Non-dimensional Variables, Theis “Type” curve, and Cooper-Jacob.
GIS – BASED DRASTIC MODEL FOR ASSESSING
Chapter 4- Leaky Aquifers
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