Groundwater and Groundwater Surface Water Interaction: How Does It Work?

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Transcription:

Napa Valley Groundwater Advisory Committee February 23, 2012 Groundwater and Groundwater Surface Water Interaction: How Does It Work? Thomas Harter University of California, Davis ThHarter@ucdavis.edu http://groundwater.ucdavis.edu Groundwater Resources Association of California

Overview What is groundwater? How much groundwater is there? How fast does groundwater move? How do we measure groundwater? Where does groundwater come from and where does it go? How do Californians use it? Groundwater management and groundwater quality

What is Groundwater? An underground lake? A network of underground rivers? A rectangular network of pipelike water arteries? A giant sponge?

Groundwater = Water completely filling Pores/Fractures

Groundwater in Different Sediments and Rocks

How fast does water flow? water-level drop Sand

How fast does water flow? water-level drop Loam

How fast does water flow? water-level drop Sand Darcy s law: groundwater flow = hydraulic conductivity x pressure gradient

How do we measure hydraulic conductivity? Estimate based on sediment type (gravel, sand, silt, clay, fractured rock): => well logs (geologic logs, geophysical logs) Measure on sediment/rock cores in laboratory Estimate from specific capacity of wells: ratio of pumping rate to well water level drawdown Measure using an aquifer test: 1-day to 7-day well pumping tests Estimate from groundwater models: => matching model results to measured water levels, groundwater flows

Sediments => result of erosion, water, wind, lake deposition, ocean bay deposition fractured bedrock of California s mountain ranges

Unconfined Aquifer Losing stream

What is Groundwater?

Unconfined Aquifer Gaining stream

Springs From: Harter and Rollins, Watersheds, Groundwater, and Drinking Water - A Practical Guide. University of California Agriculture and Natural Resources Publication 3497, 2008; http://anrcatalog.ucdavis.edu/items/3497.aspx

Fall River, NE California Basaltflow Alluvial Basin

Perched Water Table

(Semi-) Confined Aquifer

Artesian Well (Confined Aquifer)

Vernal Pools aka Seasonal Wetlands

Direction of Groundwater Flow?

Map from: http://wwwdpla.water.ca.gov/sjd/groundwater/tle-emap99.html Direction of Regional GW Flow

The Classic Hydrology View From: Jeff Mount California Rivers and Streams Hydrograph storm flow & interflow base flow Time

A Groundwater Well well screen gravel pack

Hydraulic Conductivity from Borehole Logs (Estimated) Courtesy, Claudia Fawn, USGS, 2008

Cone of Depression near a Well from: U.S. Geological Survey, Ground Water and the Rural Homeowner

Local & Regional Groundwater Flow

Gaining Stream

Losing Stream

Disconnected Stream

Dry Stream

Reconnecting Groundwater to Surface Water: Role of Aquifer Heterogeneity Fleckenstein et al., Ground Water 2006

Gaining Stream Stream-Aquifer Connection at the Regional Scale Losing or Disconnected Stream

Well Near a Stream

Well Near a Stream

Well Near a Stream

Well Near a Stream

Well Near a Stream

Well Near a Stream

Well Near a Stream

Well Near a Stream

Well Near a Stream

Well Near a Stream

Well Near a Stream

Well Near a Stream

Well Near a Stream

Well Near a Stream

Groundwater Dependent Ecosystems And the GW SW Interface

Conjunctive Use

Meandering Streams & Paleochannels Boulton and Hancock, Austral J Botany, 2006

The Hyporheic Zone

Losing Gaining Flow Through Woessner, Ground Water 2000

Where does groundwater come from and where does it eventually go? - The Hydrologic Cycle -

Courtesy, Claudia Fawn, USGS, 2008

Space and Time Disconnect between Water Supply and Water Use RAIN WATER USERS

California s Urban Water Users Population (Year 2000): 34 million Water Use: 8-9 MAF MAF = million acre-feet

California s Agricultural Water Users Irrigated Acreage (Year 2000): 9.5 million acres Water Use: 27 35 MAF MAF = million acre-feet

California Water Infrastructure Bridging the Spatial and Temporal Disconnect between SUPPLY and USE California Water Plan, Bulletin 160-2005 Total reservoir storage: 40 MAF

Groundwater Use in California: The Invisible Storage Reservoir From: DWR California Water Plan 2009 (Bulletin 160-2009)

Southern Tulare County Water Budget USE SUPPLY 1990 drought 1977 drought Ruud, Harter et al., 2003, 2004

1977 Tule River Basin: Monthly Water Budgets, Oct-Sep Ruud, Harter et al., 2003, 2004 1980 1998

Irrigation Efficiency

Irrigation Efficiency

Groundwater Management and Groundwater Quality

Integrated Regional Water Management Planning toward Integrated Resource Management Planning Groundwater Surface Water Air Soil quality Energy / Carbon Landuse planning (Courtesy: Sarge Green, CSU Fresno)

Questions?