Electrical Resistivity Lab

Slides:



Advertisements
Similar presentations
Water Underground.
Advertisements

Who am I? I am a compound found naturally in Earth I control the Earth’s climate I am necessary for all life I am the universal solvent I am continuously.
RESISTIVITY STUDY SPRING 2010 FIELD EXERCISE APPLIED GEOPHYSICS 492/692 Amie Lamb, Katie Ryan, Justin Skord and Nicole Shivers.
Mini Res by Rob Turner, Bridget Bliss, Scott Briscoe.
Summary Of the Structure of the Milky Way The following graphical data is meant to help you understand WHY astronomers believe they know the structure.
GG 450 February 25, 2008 ELECTRICAL Methods Resistivity.
Problem 7 Time section does not perfectly image depth section Dipping reflectors are incorrectly located Moho displays “velocity pull-down” beneath the.
Electrical Properties of Rocks and Electrical Resistivity Methods
This photo shows the overall lab and electrolytic tank.
Environmental and Exploration Geophysics I tom.h.wilson Department of Geology and Geography West Virginia University Morgantown, WV.
Tom Wilson, Department of Geology and Geography Environmental and Exploration Geophysics I tom.h.wilson Department of Geology and.
- Water beneath the Earth’s surface in sediment and rock formations.
Understanding Labs. Objective/Agenda  Objective: I can record and present experimental data in a neat, clear, organized manner.  Agenda  Go over lab.
Resistivity Method One of the main distinctions between the terrain conductivity and resistivity methods is that the resistivity method employs direct.
SOME NOTES ON MORPHODYNAMIC MODELING OF VENICE LAGOON Gary Parker, Spring, 2004 Venice Lagoon was formed by the action of deposition of mud and sand from.
GG 450 Feb 27, 2008 Resistivity 2. Resistivity: Quantitative Interpretation - Flat interface Recall the angles that the current will take as it hits an.
This screen shows two lines which have exactly one point in common. The common point when substituted into the equation of each line makes that equation.
Movement and Storage of Groundwater SWBAT describe how ground water is stored and moves underground; explain what an aquifer is.
UNDERGROUND CABLE.
Resistivity Results GPH 492 Spring 2013 Schurz, NV.
Aquifer A body of rock or sediment that stores groundwater and allows the flow of groundwater.
Types of resistivity surveys There are several variations on resistivity surveys: 1.A “lateral profile” aims to locate anomalies, along a line or on a.
Environmental and Exploration Geophysics I tom.h.wilson Department of Geology and Geography West Virginia University Morgantown, WV.
Characteristic curves and their responses. The method of Characteristic Curves (Two layer case) Summary of steps Set  1 =  a1 Construct the ratios 
National Geophysical Research Institute (NGRI), a constituent Laboratory of CSIR, was established in 1961 with the mission to carry out research in multidisciplinary.
Basic Review continued tom.h.wilson Department of Geology and Geography West Virginia University Morgantown, WV.
Electrode Spread (Array type)
CHAPTER 3 SUB-SURFACE DRAINAGE THEORY
Respiration continued Part 2.
Hydrosphere Notes Parts 6 - Groundwater. Where is most of Earth’s useable freshwater found? ~97% is Groundwater.
Graphic Communication.  Auxiliary views are additional views that are used in orthographic projection.  Auxiliary views are normally used to view the.
Transparency 4 Click the mouse button or press the Space Bar to display the answers.
ECE 1100: Introduction to Electrical and Computer Engineering
Groundwater Review Aquifers and Groundwater Porosity
Environmental and Exploration Geophysics I
Hussein H. Karim1, Imzahim A. Alwan2, and Fatima Assad Tayeb3
Electrical Resistivity Survey of Yosemite Valley, CA
Soils 5.02: Discuss the soil profile and soil sampling for surface and subsurface layers.
Resistivity modeling.
Lecture 15 Resistivity-GPR
GROUNDWATER.
Sedimentary Rocks.
Resistivity Logs High deep resistivity means:
The Position of Rock Layers
Water Beneath the Surface
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.
FILTRATION III EXAMPLE
Environmental and Exploration Geophysics I
Seismic - Units 10s of Meters Thick
Using Soil Moisture and Matric Potential Observations to Identify Subsurface Convergent Flow Pathways Qing Zhu, Henry Lin, and Xiaobo Zhou Dept . Crop.
Aquifer A body of rock or sediment that stores groundwater and allows the flow of groundwater.
Ocean Circulation based on Density: Temperature and Salinity
Resistivity of the California Wash and Astor Pass
Electro-Resistivity at Perry Canyon for the Burris Mine
Field Recognition of Faults
The Crossley Heath School, Halifax
Electrical Properties
Bellringer Copy down learning log Copy down homework
Chapter 2 - Recall that chapters 1 &2 have been posted on class web page Common relationships between geologic variables. What kind of mathematical model.
ES089 – Working in Three Dimensions
Graphing Systems of Equations.
Groundwater Chapter 10.
Groundwater.
Groundwater.
3.8 Use Inverse Matrices to Solve Linear Systems
C6.1 Wenner array. C6.1 Wenner array C6.1 Wenner array.
How to find these features on a map?
Graphing Systems of Equations.
Groundwater.
Water Underground.
Presentation transcript:

Electrical Resistivity Lab HWR 532 Josh Clemons

The following graphics were generated using “Model 41” consisting of 41 electrodes spaced 1 meter apart with 4 nodes per electrode spacing.

Buried Target Small target, shallow depth

Buried Target Large target, shallow depth

Buried Target Small target, intermediate depth

Buried Target Large target, intermediate depth

Buried Target Small target, deep depth

Buried Target Large target, deep depth

2 Targets, Different r Small, high r target above large, low r target

Note how the following two graphics are almost identical, although the underground situation is different. The small target below the large target is virtually invisible.

2 Targets, Different r Small, high r target below large, low r target

1 Target Large, low r target

1 Target Small, high r target

Values Used for Clay/Sand Slides EC of water = 800 mmho/cm Porosity of sand = 0.4 Porosity of clay = 0.45 Archie equation: ECbulk = (ECwater)(water content)2(porosity)1.2

1 m sand above clay q = 0.05

2 m sand above clay q = 0.05

3 m sand above clay q = 0.05

4 m sand above clay q = 0.05

1 m sand above clay q = 0.15

2 m sand above clay q = 0.15

3 m sand above clay q = 0.15

4 m sand above clay q = 0.15

1 m sand above clay q = 0.25

2 m sand above clay q = 0.25

3 m sand above clay q = 0.25

4 m sand above clay q = 0.25

1 m sand above clay q = 0.35

2 m sand above clay q = 0.35

3 m sand above clay q = 0.35

4 m sand above clay q = 0.35

Notice in the following four slides that it is difficult to tell the difference between various water contents in the same beds.

2 m sand above clay q = 0.05

2 m sand above clay q = 0.15

2 m sand above clay q = 0.25

2 m sand above clay q = 0.35

Inversion Modeling Wenner array, 1 m spacing

Inversion Modeling Wenner array, 1 m spacing RMS error after 3 inversions is 29.7% - not very good. The model indicates a relatively resistive formation or group of formations just below the surface, underlain by less resistive layers.

Inversion Modeling Wenner array, 3 m spacing

Inversion Modeling Wenner array, 3 m spacing RMS after 3 inversions is 35.7% - even worse than for the 1 m spacing. Drawing conclusions from this model would be risky. However, it does appear that there is something relatively resistive just below the surface, underlain by less resistive material.

Inversion Modeling Wenner array, 5 m spacing

Inversion Modeling Wenner array, 5 m spacing RMS after 3 inversions is 64.1% - the worst yet. The RMS has increased with electrode spacing for these models. As with the 3 m spacing, drawing a conclusion is risky. However, the apparent relatively resistive body appears again at right.