Geomaterial Characterization Using Electrical Properties (EP) EP of - - PowerPoint PPT Presentation

geomaterial characterization using electrical properties
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Geomaterial Characterization Using Electrical Properties (EP) EP of - - PowerPoint PPT Presentation

Geomaterial Characterization Using Electrical Properties (EP) EP of geomaterials are their response to applied electric field Electrical resistivity for a material is Dielectric constant for a material is defined as: k = s / o


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SLIDE 1

EP of geomaterials are their response to applied electric field

Electrical resistivity for a material is ρ Dielectric constant for a material is defined as: k = εs/εo

Geomaterial Characterization Using Electrical Properties (EP)

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SLIDE 2

Geomaterial Characterization Using Electrical Properties

METHODS

  • Low frequency resistivity methods (<100 Hz)
  • High frequency dielectric methods (104 -109 Hz)

Electrical Resistivity () Dielectric constant (k)

ADVANTAGES OVER OTHER METHODS:

  • Non destructive
  • Fast and easy
  • Incorporate response of the micro-structure (of the soil mass)
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SLIDE 3

Parameters influencing Electrical Properties

  • f Geomaterials
  • Porosity and the pore structure
  • Water content
  • Salinity level
  • Cation exchange capacity of the soil
  • Temperature
  • Type and Frequency of the current

Parameters influencing Liquefaction of soils

  • Grain shape and size
  • Porosity & Relative Density
  • Variation of Water table
  • External Forces/Disturbances---shearing
  • Resistivity = f (void ratio)=f (density)
  • Change in resistivity= f (change in the void ratio)

= f (change in the density)

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SLIDE 4

METHODS FOR LABORATORY MEASUREMENT OF SOIL RESISTIVITY Two-electrode method

Power supply SAMPLE Electrode Electrode Voltage Measurement

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SLIDE 5

Four-electrode method

Power supply

SAMPLE

Electrode

~

V

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SLIDE 6

Electrical Resistivity Box (100 mm cube)

Plate electrode Plate electrode

Electrode point

L A I V    L A R  

A= Area of electrodes L= spacing between the electrodes = resistivity R= resistance

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SLIDE 7

ELECTRICAL RESISTIVITY BOX (TWO-ELECTRODE METHOD)

12 cm @ 3 cm 12 cm 12 cm Point Electrodes

It is difficult to determine A

L A R   a . R  

a: shape factor for the electrode

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SLIDE 8

1 2 3 4 16 Ebonite ring 55 mm 25 25 25 95 mm Lock nut Top nut SS pointed tip Copper electrode 32 23 20

ELECTRICAL RESISTIVITY PROBE

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SLIDE 9

Generalized relationship for Determining Soil Electrical Resistivity  = Ae(-(Sr-5)/B) Relationship between Electrical Resistivity and Thermal Resistivity

Log () = CRLog (RT)

CR = A+B.e (-SrC) A, B and C = f (Fine content)

Sr : Degree of saturation

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SLIDE 10

Laboratory Investigations

  • Two-electrode or four-electrode methods
  • Application of :

Surface Network Analyzer (SNA) Impedance analyzer LCR meter

  • Methods based on high frequencies (f>107 Hz) are based on the

wave propagation concept.

  • Methods based on low frequencies (f<106 Hz) are based on

equivalent elements (as the wavelength is much larger than the size of the measurement device).

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SLIDE 11

Field Investigations

Ground Penetrating Radar (GPR) Time Domain Reflectometry (TDR) Capacitance sensor Portable dielectric probe (PDP) Electrical conductivity probe (ECP) Monitoring Slope deformation & Movement

2nd International Symposium and Workshop on Time Domain Reflectometry for Innovative Geotechnical Applications (TDR 2001). www.iti.northwestern.edu/tdr/tdr2001/proceedings/