Interception on trees, impermeable surfaces Infiltration into soil Interflow downslope along B horizon Overland flow during heavy rain Recharge reaches.

Slides:



Advertisements
Similar presentations
The Drainage Basin System
Advertisements

Water Table and Aquifers
Water Resources.
WATER EVAPORATION: Stage of water cycle when water changes from liquid to vapor (or gas)
28.1 The Hydrologic Cycle Hydrological cycle: natural circulation of water from the oceans to the air, then to the ground, then to the oceans and then.
Precipitation Interception Throughfall Stemflow Evaporation Transpiration Evaporation Ocean Lake Ground water Overland flow Return flow Infiltration Redistribution.
Chapter 9: Water Moving Underground More than 97 percent of all water on Earth is in the ocean as salt water. Glaciers – of the little amount of fresh.
Warm Up Think about where water comes from. Is there more or less water on Earth than there was 1 billion years ago?
Aquifers of the U.S. Fractured RockAquifers of the U.S.
Introduction to Physical and Chemical Hydrogeology (GEO 346C) Instructor: Bayani Cardenas TAs: Travis Swanson and John Nowinski
Chapter 8 Fetter, Applied Hydrology 4 th Edition, 2001 Geology of Groundwater Occurrence.
Water Underground S6E3 Students will recognize the significant role of water in Earth processes. S6E3.a Explain that a large portion of the Earth’s.
Section 1: Water Resources
Warm Up Think about where water comes from. Is there more or less water on Earth than there was 1 billion years ago?
WATER MOVING UNDERGROUND
Water Cycle (Also known as the hydrologic cycle)
Soils, Hydrogeology, and Aquifer Properties
Unit 01 : Advanced Hydrogeology Review of Groundwater Flow Malcolm Reeves Civil and Geological Engineering.
Groundwater and the Hydrologic Cycle
SGES 1302 INTRODUCTION TO EARTH SYSTEM
Water Resources. What is a Watershed ? Area of land that sheds (moves ) water from the highest to the lowest point.
GEO/ENV 315/GEO 514 Hydrogeology Class meets: Time: Mondays: 5:30 pm – 8:30 pm. Location: ESS 183 Office Hours: Wednesdays and Fridays 3:00 – 4:00 pm ESS.
Water Resources A river runs through it…. Water: The Universal Solvent One of the most valuable properties of water is its ability to dissolve. This makes.
Ground Water Write everything in PURPLE!.
By: Victoria Giaccone. Definition: Porosity Porosity and permeability are two of the primary factors that control the movement and storage of fluids.
Water as a Resource Chapter 10. The Global Water Budget Consider water as a resource because it is important for domestic use, agriculture, and industry.
The Drainage Basin System
Aquifers 101 Robert E. Mace Texas Water Development Board Groundwater 101 November 10, 2010.
1 HYDROSPHERE1 INTRODUCTION This unit has three components, The Hydrological cycle and its features. Working with hydrographs and Studying rivers.
DE Envirothon Aquatics Training: Groundwater – Surface Water Connection Chris Brown, Hydrologist Delaware DNREC Tank Management Section.
 Before break, we discussed watersheds and what constitutes a watershed. How do you think water moves through a watershed?
Ground-Water in Virginia George Harlow U.S. Geological Survey 1730 E. Parham Rd Richmond, VA
Water Resources Environmental Science Spring 2011.
How does water underground reach the surface? Freshwater flows underground.
Ogallala Formation (containing High Plains Aquifer): Deposited over 10 million years ago Coarse-grained sand, gravel, fine clay, silt, and sand 174,000.
Groundwater Basics. Water Cycle What is Groundwater? Groundwater is simply water that exists below the earth's surface. Groundwater is often thought.
Groundwater. Where is Earth’s water found? Oceans = 97% Glaciers/ice caps = 2% Groundwater = 0.5% Lakes, rivers, soil, living things, atmosphere, etc.
Water Distribution. The Water Cycle Water is essential to life on Earth. Humans can live for more than month without food, but we can live for only a.
Water Cycle, Groundwater, Aquifers, Caves
6. Drainage basins and runoff mechanisms Drainage basins Drainage basins The vegetation factor The vegetation factor Sources of runoff Sources of runoff.
Water In what ways have you used water today? How much water is used to make a 1KG burger?
Groundwater Water found underground in the cracks and spaces in soil, sand and rock. Question: How does water collect underground? Use the terms permeable.
Label: 1.aquifer 2.water table 3.impermeable layer 4.zone of saturation 5.zone of aeration, 6.recharge area aquifer Water table Impermeable layer (bedrock)
WaterSection 1 Water Resources Water is essential to life on Earth. Humans can live for more than month without food, but we can live for only a few days.
Groundwater Where is groundwater located and how do humans.
Most of the groundwater found in Northern US comes from Canada! That means Canada supplies a portion of the state’s fresh water supply.
Groundwater Geol 1110 Newell guest lecture 3/28/16.
Hydrology. Earth’s Water  Renewable resources can be replenished in a human life span.
Water Chapter 11. Water Resources Section 11.1 Water is essential to life on Earth. Humans can live for more than month without food, but we can live.
WaterSection 1 Section 1: Water Resources Preview Classroom Catalyst Objectives Water Resources The Water Cycle Global Water Distribution Surface Water.
What is the water cycle?.
What are some things that might be in each category?
DO NOW Pick up notes and Review #27. Do you have any labs to turn in?
Groundwater.
Gaining vs. losing streams
Unit 3 The Hydrosphere.
The Water Cycle 5 Processes 1. Evaporation/Transpiration
Water Cycle.
What causes rivers to flood?
Geology of Groundwater Occurrence
What is the water cycle?.
The Hydrologic Cycle Condensation Advection Evaporation
Ground Water Ground Water lies beneath the ground surface, filling pores in sediments and sedimentary rocks and fractures in other rock types Represents.
Groundwater.
When we flush the toilet why should we say “see you later”?
Groundwater.
Water Cycle, Ground Water, and Surface Water
Aim: How can we explain the water cycle?
Groundwater.
DRAINAGE BASIN [GRADE 12 GEOGRAPHY]
Presentation transcript:

Interception on trees, impermeable surfaces Infiltration into soil Interflow downslope along B horizon Overland flow during heavy rain Recharge reaches the water table Groundwater flow from recharge area to stream Water table rises Evaporation removes intercepted water Evapotranspiration (ET) from plants removes water from soil Baseflow to streams depletes water in aquifer Hydrologic Cycle Baseflow and ET continue until next rainfall Rainfall Aquifer Vadose zone Soil B horizon Stream water table Rain stops Overland + Interflow = Stormflow. Stream level rises

Hydrogeologic Regions Geologic controls on –Porosity and hydraulic conductivity –Layering, structure, and aquifer type –Water chemistry –Well yield

Hydro- geology of the Southeast FloridanLimestone Appalachian Sedimentary Rock Limestone Piedmont Crystalline rock Coastal Plain Sand + clay Ground Water Atlas

Fractured crystalline rock

Transition Fractured metamorphic and igneous rock K: m/s T: m 2 /day S: Saprolite: K: m/s S:

Hydrogeologic Conceptual Model R: 0.2 m/yr

Fractured Rock Aquifers in Piedmont K: m/sbulk fractured rock Compare to to m/s for intact samples T: m 2 /day Recharge: m/yr Well Yield: gpm

Atlantic Coastal Plain

Coastal Plain Santee River Delta

Sand and clay

clay Sand Columbia Myrtle Beach Atlantic Coastal Plain

Flowing wells Edwards Aquifer, San Antonio, Texas Roswell Basin, NM, 3600 gpm

Coastal Plain Clastic Aquifers T: ,000 m 2 /day Recharge: m/yr Well Yield: gpm

Floridan Aquifer FloridanLimestone Appalachian Sedimentary Rock Limestone Piedmont Crystalline rock Coastal Plain Sand + clay Ground Water Atlas

Floridan Limestone Aquifer

Dissolution Cave stream

Limestone aquifer

Floridan Aquifer T: ,000 m 2 /day Recharge: m/yr Well Yield: ,000 gpm

Comparison of SE Regions RegionT (m 2 /day)Recharge (m/yr) Qwell (gpm) Piedmont Coastal Plain Clastic , Floridan Limestone 1, , ,000