PPT-Groundwater in Indian Water Right Settlements

John E Thorson Ruth Thayer Stanley Pollack Faye Bergan WSWCNARF Indian Water Rights Symposium August 2017 Cases 1963US v Fallbrook Pub Util Dist USDC Cal 1968Tweedy v Texas Co USDC Mont. James . Sorensen. Urban population. By 2050 the urban population of SSA is projected to increase from 40 to nearly 60% and exceed 1.26 billion (UN, 2011).. Natural woman. The rapid growth of many urban areas has overwhelmed the ability of many local authorities to provide basic infrastructure. 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.. Department of Economics. Bapatla. College of Arts & Science. a) Surface Irrigation:. Just flooding water. About 90% of the irrigated areas in the world are by this method.. b) Sprinkler Irrigation:. 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. 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). APPROACH TO INDIAN WATER SETTLEMENTS. . Alan . Mikkelsen. Acting Commissioner of the Bureau of Reclamation and the Chair of the Working Group on Indian Water Rights Settlements. Secretary . Zinke. . 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 . . WSWC/NARF . Symposium. August . 9, 2017. Pamela Williams, Director. Secretary’s Indian Water Rights Office. Indian Water Settlements. History and legal underpinnings. Existing Indian water settlements. 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,. and the fluxes adjacent to the arrows are in millions of cubic kilometres of water per year.. Key points (what your kiddos REALLY need to understand!). We . cannot. consider surface water without thinking about groundwater. Groundwater and surface water do not flow the same way. Interactions between groundwater and surface water may “shift” as a result of other factors. Secure Alternative Water Sources along with Regulations. Contents. Introduction. Groundwater Use. Water Quality Management. Comprehensive Groundwater Conservation. Lessons Learned. 1. Introduction. Zero Meter Area .