THE SMOOTH SOUNDING GRAPH. A Manual for Field Work ... - BGR

THE SMOOTH SOUNDING GRAPH. A Manual for Field Work ... - BGR THE SMOOTH SOUNDING GRAPH. A Manual for Field Work ... - BGR

22.03.2013 Views

11 to get as a contribution from electrode A to the voltage between M and N U ( A) MN = Iρ ⎛ ⎜ 2π ⎜ ⎝ As the arrangement is symmetrical we get the same contribution from electrode B. This results into U MN = U ( A) MN + U ( B) MN = L 2 1 − 2 U For the earth-resistivity ρ we then obtain or a 2 A MN − L 2 = 1 + a 2 ⎞ ⎟ ⎠ Iρ × π ( L 2 ) 2 a − ( a 2 ) 2 (7) 2 2 π ⎡⎛ L ⎞ ⎛ a ⎞ ⎤ U MN ρ = ⎢⎜ ⎟ − ⎜ ⎟ ⎥ (8) a ⎢⎣ ⎝ 2 ⎠ ⎝ 2 ⎠ ⎥⎦ I U ρ = K , I K = 2 2 π ⎡⎛ L ⎞ ⎛ a ⎞ ⎤ ⎢⎜ ⎟ − ⎜ ⎟ ⎥ a ⎢⎣ ⎝ 2 ⎠ ⎝ 2 ⎠ ⎥⎦ i.e. the well-known formula used in calculating the resistivity ρ from the current I between A and B and the voltage U between M and N. K is called "factor of configuration" or "geometric factor". Its dimension is [m]. We now have to study the function of this factor K. As a homogeneous underground is concerned ρ be a constant. Working with a constant cur- rent I - this is technically no problem because I depends after equation (8) only on the quality of grounding the current electrodes A and B (con- tact resistance) and not on their distance - the voltage U decreases by enlarging L. This decrease is compensated by an increasing K. The regu- lating function of K now shall be discussed regarding both electrode con- figurations used nowadays in practical field work.

12 Fig.6 Fig.7 Fig.8

12<br />

Fig.6<br />

Fig.7<br />

Fig.8

Hooray! Your file is uploaded and ready to be published.

Saved successfully!

Ooh no, something went wrong!