PDF-Regional Training Workshop on Integrating Groundwater Management withi

18 January 2019 RCGW KEWI Nairobi KenyaGroundwater Surface Water Interactions Regional Training Workshop on Integrating Groundwater Management within River Basins 1518 January 2019 RCGW KEWI Nairobi. 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 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.. Makes up 23% of Earth’s freshwater.. 12% Shallow (we can reach). 11% Deep (out of our reach). Underground Layers. When precipitation occurs, water often seeps down into the soil and trickles down in between particles of soil and through cracks and spaces in layers of rock. . Alison Parker, . David Nussbaumer, Afua Owusu, Ian Sutton. Understanding . long-term changes in Lusaka’s groundwater levels. Method. Collect long-term data on:. Groundwater levels. Climate. Groundwater abstraction. William L. Cunningham. Acting Chief, USGS Office of Groundwater. Briefing to . ACWI Workgroup . How to Sustain and Enhance High Quality Water Monitoring under Constrained Budgets . January 28, 2013. Monitoring Networks Outline. 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,. CSAC Legislative Conference. May 15, 2014 • Timothy Quinn, ACWA Executive Director. About ACWA. Who We Represent . . .. ACWA members responsible for 90% of the state’s distributed water. Water Sources & Services. sandstone and . Rogersville shale play area, eastern Kentucky. Kentucky . Geological Survey, University of . Kentucky. GSI . Environmental Inc., . Austin. , . TX. Possible Contamination Pathways of Hydraulic Fracturing to Groundwater Aquifers . Water Education Foundation SGMA Tour. October 6, 2016. Overview of Legislation. Recognizes the value of . l. ocal management of water resources. Requires the development . of Groundwater Sustainability . Groundwater Sustainability Agency . Governance Formation. REGINA RUBIER. WATER RESOURCES MANAGER. CITY OF STOCKTON - MUNICIPAL UTILITIES DEPARTMENT. JANUARY 26, 2016. Agency Boundary Overlap. SEWD. WID. 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 . Water Education Foundation SGMA Tour. October 6, 2016. Overview of Legislation. Recognizes the value of . l. ocal management of water resources. Requires the development . of Groundwater Sustainability . Secure Alternative Water Sources along with Regulations. Contents. Introduction. Groundwater Use. Water Quality Management. Comprehensive Groundwater Conservation. Lessons Learned. 1. Introduction. Zero Meter Area .