Groundwater Learning objectives

Slides:



Advertisements
Similar presentations
Yhd Subsurface Hydrology
Advertisements

Physical Properties of Aquifers
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.
STABILITY ANALYSIS IN PRESENCE OF WATER Pore pressures Rainfall Steady state flow and transient flow.
Прикладная Гидрогеология Tomsk Polytechnic University Tomsk, Russian Federation Spring Semester 2014 Yoram Eckstein, Ph.D. Fulbright Professor 2013/2014.
ESS 454 Hydrogeology Module 2 Properties of Materials Basic Physics Darcy’s Law Characteristics of Aquifers Elasticity and Storage Instructor: Michael.
Soil Water ContentSoil Moisture Content Water that may be evaporated from soil by heating at C to a constant weight Gravimetric moisture content.
Week 2 Terminology + Hydraulics review. Terms Porosity Porosity Moisture content Moisture content Saturation Saturation Aquifer Aquifer Aquitard Aquitard.
Groundwater Hydraulics Daene C. McKinney
1 GROUNDWATER HYDROLOGY AND CONTAMINANT TRANSPORT CEVE 518 P.C. de Blanc C.J. Newell 1.Porosity and Density Continued 2.Saturation and Water Content 3.Darcy.
Soil Water Reading: Applied Hydrology Sections 4.1 and 4.2 Topics
Lab 10 - Soil Water Movement Flow Model Experiment 1 –Red dye is added to the waste lagoon and to a well in the unconfined aquifer. –Green dye is added.
Peter Dahlhaus SCGEO 2106 Week 4. PrecipitationEvapotranspirationPond Storage Overland FlowThroughfall InterceptionInterception StorageInfiltrationSoil.
Soil Properties and Soil Water Movement Environmental Hydrology Lecture 4.
Lecture Notes Applied Hydrogeology
Figure (p. 235) (a) Cross-section through an unsaturated porous medium; (b) Control volume for development of the continuity equation in an unsaturated.
Water Movement Below Surface
Surface Water Hydrology: Infiltration – Green and Ampt Method
Lecture 15 Soil Water (2) Soil Water Movement (1) Concept of Hydraulic Head Soil moisture Characteristics Darcy’s Law Infiltration.
1 GROUNDWATER HYDROLOGY AND CONTAMINANT TRANSPORT CEVE 518 P.C. de Blanc C.J. Newell 1.Hydrologic Cycle and Water Distribution 2.Soil Horizons 3.Aquifers.
Infiltration Equations Fundamental Mass Balance Equation: Darcy’s Law (z direction): Where.
Water Resources Assessment Main Resources – Surface water – Groundwater – Unconventional Tools – Flood routing/delineation models – Runoff models – GIS.
Soil Physics David Zumr room: b608 Lecture (and seminar) notes will be available: -
Groundwater Geol 1110 Newell guest lecture 3/28/16.
A.Done Already B.Confident C.Could read text and figure out D.Unsure – need help E.Clueless how to start.
Water: How it moves in the ground and on the surface.
Groundwater movement Objective To be able to calculate the hydraulic conductivity of a sample given measurements from a permeameter To be able to evaluate.
Soil Water Balance Reading: Applied Hydrology Sections 4.3 and 4.4
Radial Flow to an Unconfined Aquifer From Mays, 2011, Ground and Surface Water Hydrology.
Movement & Storage of Groundwater
Properties of Aquifers
Groundwater movement Objective
Groundwater Review Aquifers and Groundwater Porosity
Water in Soil Learning objectives
Surface Water Hydrology Lecture 13: Infiltration
Midterm Review.
Recap Lecture 1 Lecture 2 Volume/Mass balance (by GSL example)
Infiltration and unsaturated flow (Mays p )
Infiltration and unsaturated flow
HYDROLOGY Lecture 6 GROUNDWATER 2
Water in Soil Learning objectives
Infiltration and unsaturated flow
Using the Soil Triangle
Groundwater.
Infiltration and unsaturated flow (Mays p )
Example Estimate the average drawdown over an area where 25 million m3 of water has been pumped through a number of uniformly distributed wells.
Water in Soil Learning objectives
Green and Ampt Infiltration
Steady flow in a confined aquifer
Gaining vs. losing streams
Test 1 Review Chapter 1, Hydrologic cycle and the water balance
Infiltration and unsaturated flow
Confined aquifer storage
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.
Philip B. Bedient Civil and Environmental Engineering Rice University
Aquifer Anisotropy and general flow equations
Permeability By Falling Head Method
Logan Dry Canyon Detention Basin Design Case Study
Groundwater (Part 1) Groundwater as an erosional agent
Determining Hydraulic Conductivity
Where do we get most of our fresh drinking water?
Groundwater vocabulary
Anisotropy – Key ideas Effective conductivity that represents aggregate effect of flow through a layered system Effective conductivity is different parallel.
#26 Groundwater and Aquifers
Groundwater.
Soil moisture, percent organic matter and soil texture calculations
Infiltration and unsaturated flow
Groundwater.
Philip B. Bedient Civil and Environmental Engineering Rice University
Groundwater Flow Example
Presentation transcript:

Groundwater Learning objectives Be able to quantify the properties of water held in and flowing through the subsurface (soil and rock). The properties of interest include porosity, moisture content, pressure, suction, hydraulic conductivity Mays Chapter 2

Schematic cross section illustrating unconfined and confined aquifers From Mays, 2011, Ground and Surface Water Hydrology

Figure 21. Cross section through an unsaturated porous medium (from Chow et al. 1988)

Example 2.2.1 An undisturbed sample of a medium sand weighs 484.68 g. The core is 6 cm in dia and 10.61 cm high. After oven drying the core weighs 447.32 g. Determine the bulk density, void ratio, water content and saturation percentage of the soil.

Well graded silt, sand, gravel mixture Uniformly graded sand Illustrative grain-size distribution curves. The boundaries between size classes designated as clay, silt, sand and gravel are shown as vertical lines.

Soil Texture Triangle From Mays, 2011, Ground and Surface Water Hydrology

Macroscopic and microscopic concepts of a porous medium Macroscopic and microscopic concepts of a porous medium. (from Freeze and Cherry, 1979)