PPT-Sustainable Groundwater Management in California: A Framewo

Professor Mike Young MikeYoungadelaideeduau Cell 857 928 2519 SGMA 101 Significant unreasonable and undesirable results 1 Depletion of groundwater levels 2 Reduction of groundwater storage. 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. . Chapter 9, Section 2. The Hydrologic Cycle (WATER CYCLE). . Evaporation. Condensation. Precipitation. Runoff. Soil is made up of many small rock and . mineral. fragments.. Holes, . cracks. ,. and crevices exist in the rock underlying the soil.. 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=. Tom M. Marston, U. S. Geological Survey. In cooperation with the . Utah Division of Water Rights. Parowan Valley. Approx. 160 mi. 2. Structural depression between Hurricane fault and the Red Hills. Closed surface-water basin (aside from Winn Gap). 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,. 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 . Sustainable Groundwater Management Act: Engaging with GSAs. OUTLINE. Financing Collaboration & GSA . Formation . Short . Term/ . Immediate. DWR Facilitation Services & Technical . Assistance. 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 . -18 January 2019 RCGW KEWI Nairobi KenyaGroundwater Surface Water Interactions Regional Training Workshop on Integrating Groundwater Management within River Basins 15-18 January 2019 RCGW KEWI Nairobi -18 January 2019 RCGW KEWI Nairobi KenyaIntegration ofGroundwater ManagementintoTransboundary Basin Organizations in AfricaRegional Training Workshop on Integrating Groundwater Management within River Secure Alternative Water Sources along with Regulations. Contents. Introduction. Groundwater Use. Water Quality Management. Comprehensive Groundwater Conservation. Lessons Learned. 1. Introduction. Zero Meter Area . Osaka City and . Saitama Prefecture. No. C3 Ver. 1. Depression caused by land subsidence . https://www.pref.saitama.lg.jp/a0505/901-20091202-17.html. Original. 　. ground elevation. Elevation after land subsidence. SADC Groundwater Conference . 28. th. September 2018. Overview. 2019/01/16. PAGE . 1. TITLE OF DOCUMENT. Project Scope and Deliverables. Objective:. To create an enabling framework for . policy, legal and institutional environment for effective...