PPT-Finding groundwater flow

and transport pathways with pattern recognition algorithms Ryan Shaver Where is groundwater Heath RC 1984 Groundwater regions of the United States USGS WSP 2242 p 22. Hydraulic Head. Bernoulli’s Equation. Hydrostatic Pressure. Hydraulic Head. Bernoulli’s Equation. Hydrostatic Pressure. Hydraulic Head. Total Hydraulic Head (drop velocity – why?). . Or. Much of the global H. 2. O, resides below the surface of the Earth in what geologists refer to as . groundwater. . . Although in the subsurface, it has a large impact on society and the features that we see on the surface of the Earth.. LA’s Water Resources. You may be familiar with Spring water… . Aquifer:. A water-bearing. rock. that readily transmits water to wells and springs . Water Bearing Rock??. Let’s investigate!. notes. 2. Groundwater Sampling. Sampling a well with a tennis shoe?. Standards, Directives, Guidelines................... 4. Standards, Directives, Guidelines. Hierarchy:- “more or less a general consensus” EN/AS/NZS=. The Unseen Part of the Water Cycle. Salt Groundwater. Ground Water. Reservoir. . The present-day surface hydrologic cycle. The numbers in parentheses refer to volumes of water in millions of cubic kilometres,. Andrew Austin-Petersen. facebook.com/. negabamonlakeassociation. Overview. Lake Nebagamon . ArcGIS Groundwater Tools. Progress. Issues. Goals. What? Why? Where?. What is a “. Nebgamon. ”?. Chippewa phrase meaning "place to hunt deer by fire on the water.“ . Groundwater Hydraulics. Daene C. McKinney. 1. Course Objectives . Introduction to groundwater, including: . Groundwater in the hydrologic cycle . Characteristics of porous media. Darcy's law of flow in porous media. Daene C. McKinney. 1. Course Objectives . Introduction to groundwater, including: . Groundwater in the hydrologic cycle . Characteristics of porous media. Darcy's law of flow in porous media. Continuity principles. 9.1-9.2). . Groundwater:. . Aquifers and Groundwater flow. Outline of the course. The . Basics. The . global hydrological cycle. Precipitation. Soil water (lab work). Surface energy . fluxes. Evaporation . Ground water occurs when water recharges the subsurface through cracks and pores in soil and rock. Shallow water level is called the water . table. 2. Recharge. Natural. Precipitation. Melting snow. Methods for determining aquifer parameters. In Unit 2 we discussed about various lab and field methods for determining the hydraulic conductivity values for the soil/rocks.. Methods included the use of constant head Permeameter, falling head Permeameter and tracer tests for determining the K.. From Mays, 2011, Ground and Surface Water Hydrology. Effective conductivity . that represents aggregate effect of flow through a layered system. Effective conductivity is . different. parallel to than perpendicular to the layers. For Marcellus Shale Commission. March 10, 2014. Groundwater Flow in Appalachian Plateau. Example community water system source protection area. A confined aquifer with a porosity of 0.18 is 25 m thick. The potentiometric surface elevations at observation wells 800 m apart are 42.8 m and 47.3 m. If the hydraulic conductivity is 15 m/day determine:.