logo em-38 inca 2008 international course on archaeogeophysics 20 july-5 august 2008 in İznik,...

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LOGO EM-38 INCA 2008 International Course on ArchaeoGeophysics 20 July-5 August 2008 in İznik, Turkey Ertan Pekşen

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LOGO

EM-38

INCA 2008International Course on ArchaeoGeophysics

20 July-5 August 2008 in İznik, Turkey

Ertan Pekşen

Company Logo www.themegallery.com

Outline

Introduction

Conclusion

EM-38

Data acquisition

Equipment

Interpretation

Theory

Case Study

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Introduction

EM38 has been produced by Geonics. (www.geonics.com)

EM38 is mainly used in agriculture, environmental, archaeology.

EM38 is easy to apply and carry during data acquisitions.

EM-38

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Equipment

EM-38

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Theory

Described by McNeil (1980)

Step 1: An alternating current in the transmitting coil creates a time-varying magnetic field which is sensed by the receiving coil.

Step2: This primary magnetic field (Hp) generates small electric currents in the soil.

Step3: These currents generate a secondary magnetic field (Hs) which is also measured by the receiving coil.

Step 4: The apparent conductivity may be determined from the ratio of the magnetic fields by the relationship.

EM-38

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Data acquisition

44

2211

33

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EM-38 specifications

Frequency= 14.6 kHz

T-R distance=1 m

Horizontal and vertical dipoles

EM-38

h=0.75mh=0.75m h= 1.5mh= 1.5m

Effective depth rangesEffective depth ranges

Measured quantities:Measured quantities:1)1) Apparent conductivities (mS/m)Apparent conductivities (mS/m)2)2) In phase ratio of the secondary to primary In phase ratio of the secondary to primary

magnetic field in parts per thousand (ppt)magnetic field in parts per thousand (ppt)

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EM38 Apparent Conductivity

Fixed frequency: f=14.6 kHz

Fixed coil spacing: s=1 m

Apparent conductivity (B=s/ << 1):

Hp primary field

Hs secondary field

skin depthp

s

0

a H

H

s μ f π

2

EM-38

2

0σω

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Interpretation

EM-38

**Apparent conductivity map since the Apparent conductivity map since the depth range is very shallow.depth range is very shallow.

**Forward and Inverse modeling Forward and Inverse modeling (Hilgendorf, 1997) and (Deidda et (Hilgendorf, 1997) and (Deidda et al., 2003)al., 2003)

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Case Study (Simpson et al 2008)

EM-38

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…continued

EM38

EM38DD provides simultaneous measurement of both (vertical and horizontal) dipoles at

all times.

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Case Study

EM-38

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Conclusion

EM-38

EM38 can be applied to archealogy.

EM38 can quickly be carried out on a field.

EM38 provides information about underground no more than 1.5 m depth .

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