PPT-Groundwater-Surface Water Interactions

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. 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.. 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. 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. and. purge techniques. Acquiring . a . representative sample. Your Resources:. ISO Standards (5667). GNS National Protocol. What are we trying to achieve?. 3. Why is this so important?. A REPRESENTATIVE SAMPLE!. 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). W. ater. Chapters 10, 11, & 12. Breaking down rocks by physical means, like . ice, wind, water, gravity, and plants/animals. Ice wedging. occurs when water squeezes into cracks in rocks, freezes, expands, and cracks the rock open. 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 . 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. . 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). 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 . Acknowledgement: This Fact Sheet is one of a series developed by an Interagency Committee with representatives from Saskatchewan Health, Regional Health Authorities, Saskatchewan Watershed Authority, More Information Required No Yes No Yes No Yes No Yes No Yes Yes No Phase 1 Initial GUDI Screening Phase 2a Hydrogeological Review Phase 2b Hydrogeological Investigation Phase 3 (optio -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 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..