Docsity
Docsity

Prepare for your exams
Prepare for your exams

Study with the several resources on Docsity


Earn points to download
Earn points to download

Earn points by helping other students or get them with a premium plan


Guidelines and tips
Guidelines and tips

Current Refraction - Seismology - Lecture Slides, Slides of Geology

Following are the Fundamentals of these Lecture Slides : Current Refraction, Refraction Changes, Distribution of Current, Layered Subsurface, Resistivity, Layered Subsurface, Uniform Subsurface, Apparent Resistivity, Ratio Changes, Electrodes

Typology: Slides

2012/2013

Uploaded on 07/19/2013

saen.chumi
saen.chumi 🇮🇳

4.6

(13)

96 documents

1 / 7

Toggle sidebar

This page cannot be seen from the preview

Don't miss anything!

bg1
Current Refraction
Because refraction changes the distribution of current
in a layered subsurface
The ratio of V/I changes
We can therefore measure changes in resistivity with depth
Uniform subsurface Layered subsurface
12
ρρ
>
Docsity.com
pf3
pf4
pf5

Partial preview of the text

Download Current Refraction - Seismology - Lecture Slides and more Slides Geology in PDF only on Docsity!

Current Refraction

  • Because refraction changes the distribution of current

in a layered subsurface

  • The ratio of V/I changes
  • We can therefore measure changes in resistivity with depth

Uniform subsurface (^) Layered subsurface

ρ 2 > ρ 1

Apparent Resistivity

  • In a VES survey the ratio V/I is measured with increasing

electrode spacing…

  • The ratio changes for two reasons:
    1. Layers of differing resistivity are encountered
    2. The electrodes are now farther apart
      • Causes measured resistance to decrease!
  • To determine #1, we must first correct for #
  • To account for the effects of changes in electrode

spacing, the apparent resistivity is found as:

  • Here, α is a “geometrical factor”
    • equal to a/l for a rod (see previous slides)
    • The geometrical factor varies depending on array configuration / type
      • I’ll show some common array types later
  • For reasons that you will soon see, apparent resistivity

, ρa , is what is typically used

ρ (^) a α

V

I

Apparent Resistivity

Wenner Arrays

  • Pronounced “Venner”. This is the most commonly used in the U.S.
  • All four electrodes are equally spaced. Spacing = a
  • Geometrical correction factor = 2πa
  • Measure resistance (V/I)
  • Calculate apparent resistivity
  • Repeat for a range

of spacings

I

V

ρ a = 2 π a

Wenner VES Survey

  • Results of ρa are plotted as log 10 ρa versus log 10 a
    • Use logs to help accommodate the large range in values For a simple two layer scenario: (multiple layers are more complex)
  • The first few spacings:
    • Electrical current mostly flows in the upper layer
    • so the apparent resistivity is the actual resistivity of the upper layer
  • At spacings that are large compared to layer 1’s thickness:
    • Most of the length that the current travels is in the lower layer
    • So the apparent resistivity is the resistivity of the lower layer How do we determine layer thickness?