Introduction to gpsurya blog

$Dear$ $Friends,$ In this blog you will find around 320 solved Geophysics GATE and CSIR-NET and other competitive exams solutions with a better explanation. Please follow and share if you like it. $Thanks,$ $gpsurya$ and $group$

CSIR-NET 2015 (June)-113

CSIR-NET 2015

113. The following table shows the values of resistance R measured in a Wenner sounding for different electrode spacing, a at a location covered by clay.

a(m)          =        5                      10                 15               20            25
R(ohms)    =       1.0                    0.8                0.6              0.4           0.2

Which of the following conclusions can be made?

A) clay extends to a depth of at least 25m
B) clay is underlain by a thick basement of high resistivity 
C) clay is underlain by water bearing sands overlying a thick basement
D) clay is underlain by water bearing gravel overlying a clay formation

Answer: D

Solution:

In Wenner configuration the current and potential 

electrode pairs have a common mid-point and the

 distance between adjacent electrodes are equal,




apparent resistivity ρa = 2Пa ΔV /I  ---------(1)

  a= electrode spacing


ΔV / I = R , Resistance

therefore ρa = 2ΠaR



1. apparent resistivity at a=5m , R= 1.0 Ω is

ρ1 = 2*3.14*5*1.0

    =31.40 Ωm


2. apparent resistivity at a = 10m R = 0.8Ω is


ρ2 = 2*3.14*10*0.8

    = 50.24Ωm


3. apparant resistivity at a=15m R=0.6Ω is

ρ3 = 2*3.14*15*0.6

    = 94.20 Ωm


4. apparent resistivity at a = 20m R = 0.4Ω is

ρ4 = 2*3.14*20*0.4

    = 50.24 Ωm


5. apparent resistivity at a=25m R=0.2Ω is

ρ5 = 2*3.14*25*0.2

    =31.40Ωm


apparent resistivity values ρ1 < ρ2 < ρ3 > ρ4 > ρ5
Therefore , Clay is presented upper layer and inner 

layer, In between water bearing gravel present ( 

because gravel is high resistivity).





Related Posts

Post a Comment

Subscribe Our Newsletter