PPT-Sharing Groundwater:

A Robust System for Achieving SGMA Professor Mike Young MikeYoungadelaideeduau Cell 857 928 2519 SGMA 101 Significant unreasonable and undesirable results 1 Depletion of groundwater levels. Use of brackish groundwater could supplement or in some places replace the use of freshwater sources and enhance our Nations water security However a better understanding of the location and charac ter of brackish groundwater is needed to expand dev A DEMONSTRATION THE GROUNDWATER FOUNDATION www.groundwater.org Groundwater is water found underground in the spaces and cracks between rocks, sand, soil and clay. Groundwater is stored in geolo and Management. Kenneth D. Schmidt. Principal. Kenneth D. Schmidt & Associates. Water-Level Hydrographs . for Wells East of Sanger. Water-Level Hydrographs . for Well Southwest of Madera. Water-Level Hydrographs for . 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. 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,. Steve Gaffield – Montgomery Associates. Thomas Hovel – City of Fitchburg, WI. Madeline Gotkowitz – Wisconsin Geological Survey. Topics. Groundwater basics & current issues. Madison’s drinking water issues. Professor Mike Young. Mike.Young@adelaide.edu.au. Cell 857 928 2519. SGMA . 101. Significant unreasonable and undesirable results. (1) Depletion of groundwater levels. (2) Reduction of groundwater storage. 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. Groundwater Sustainability Agency . Governance Formation. REGINA RUBIER. WATER RESOURCES MANAGER. CITY OF STOCKTON - MUNICIPAL UTILITIES DEPARTMENT. JANUARY 26, 2016. Agency Boundary Overlap. SEWD. WID. . G. . . D. S. Floridan Aquifer. Extent. Hydrologic Horizons. Pressure. Tension. θ. pwp. < . θ. < n. θ. fc. < . θ. < n. θ. = n. θ. = n. Geologic Profiles . (Stratigraphy). saturates . pore spaces of . bedrock.. The rate of movement of groundwater is gravity driven, varying between 0.6 inches per day (in sandstones) to several inches per year (in . granites. ). The source of groundwater is rain and melt water infiltrating and percolating through fractures/pores in soil and . . Spokane. . River TMDL Implementation . August 13, . 2014. Llyn Doremus Steve Cox. Dept of Ecology US Geological Survey. Water Quality Program. WA . Water Sciences Center. Objectives and Approach to characterizing phosphorus discharge to Lake Spokane. Secure Alternative Water Sources along with Regulations. Contents. Introduction. Groundwater Use. Water Quality Management. Comprehensive Groundwater Conservation. Lessons Learned. 1. Introduction. Zero Meter Area .