PPT-GROUNDWATER GROUNDWATER Groundwater is subsurface water that fully

saturates pore spaces of bedrock The rate of movement of groundwater is gravity driven varying between 06 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 fracturespores in soil and . 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.. 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. Are . you. . prepared. ?. Underground . risks. – . face . them. , . don’t. . hide. . from. . them. !. Who’s. . it. . for. ?. For . you. : the . principal. , the architect, the . real. . Subsurface . Drainage . Water . Using . Constructed Wetlands. Introduction:. Once nitrate (NO. 3. -. ) has . leached into the soil profile, surpassing the root zone, it is considered lost from the . agroecosystem. 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. 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. Air is a fluid (but not a liquid) that behaves similarly to water. We see pressure changes in the subsurface due to barometric pressure and other causes.. We see gas flow in the subsurface due to advection and diffusion due to pressure and concentration gradients, respectively. John E. . Thorson, Ruth Thayer, Stanley Pollack, Faye Bergan. WSWC/NARF Indian Water Rights Symposium (August 2017). Cases. 1963—US v. Fallbrook Pub. Util. Dist. (USDC Cal). 1968—Tweedy v. Texas Co. (USDC Mont). (SUE. ). OVERVIEW. What is Subsurface Utility Engineering (SUE)?. Overview of SUE – Definitions. When to Use SUE. How to Use SUE. Why Use SUE. What is Subsurface Utility Engineering?. SUE. Subsurface Utility Engineering. (SUE. ). OVERVIEW. What is Subsurface Utility Engineering (SUE)?. Overview of SUE – Definitions. When to Use SUE. How to Use SUE. Why Use SUE. What is Subsurface Utility Engineering?. SUE. Subsurface Utility Engineering. Subsurface Trespass and Lateral Rights HBA Oil, Gas & Mineral Law Section May 23, 2019 Monika U. Ehrman Associate Professor of Law Faculty Director, Oil & Gas, Natural Resources, and Energy Center Karen G. Lloyd. C-DEBI network talk July 25, 2013. University of Tennessee, Knoxville. Q: What drives microbial diversity in the vast marine subsurface?. Inagaki et al. 2006, PNAS. Archaea. Bacteria. of runoff. Learning objectives . Be able to describe the processes involved in runoff generation. Be able to distinguish between infiltration excess, saturation excess and subsurface . stormflow. runoff generation mechanisms and identify when and where each is more likely to occur.