A634 Induction Conductivity Tool

APPLICATIONS
Conductivity is the inverse of resistivity. Induction logging systems were originally designed to facilitate resistivity measurements in oil-based drilling mud, where there is no conductive medium occurred between the tool and the formation. It is also often used in dry holes or when the borehole fluid is very fresh. The purpose is, as usual, to measure resistivity or conductivity in order to calculate porosity and to interpret lithology. Induction is useful in several types of ground investigation.

Mineral Investigation
The resistivity of rocks depends on several factors. Rocks are usually poor conductors. Rock resistivity is determined, primarily, by porosity and the salinity of the pore fluid.

Clay minerals reduce the resistivity of the formation. Some alteration processes result in the formation of clay minerals, reducing resistivity, while others reduce rock porosity and increase formation resistivity. Decreases in resistivity may be a result of either significant concentration of conductive metal sulphides or oxides. Fracturing increases effective porosity and can, therefore, decrease resistivity.

The complexity of resistivity interpretation means that complementary information from other geophysical measurements or other geological logs is usually required. However, massive sulphide deposits generally consist of conductive ore zones and resistivity logs are often used to delineate these ore zones.

Coal Investigation
Coal usually has high resistivity. This may be reduced according to its porosity, clay, and water content. The porosity of coal varies with rank and so its resistivity increases from lignite to semi-anthracite and then decreases slightly with anthracite. Clay inclusions reduce the resistivity of coal.

Clay-rich lithologies, such as shales, have low resistivity. Clean, relatively dry sandstone has high resistivity. This may be reduced according to porosity, salinity, and clay content.

Resistivity (or conductivity) logs may also indicate oxidation of a coal seam or alteration by an intrusion.

Ground-water Investigation
The Archie equation defines the relationship between porosity and resistivity in reservoir rocks: for more information on this please contact us.

  • A634 - High Sensitivity Range

  • 1 to 300mS/m tool is intended to suit the
    requirements of those concerned with
    relatively low conductivity.

  • A634E- Extended Range

  • 300mS/m to 1000S/m is suited to the
    examination of highly conductive
    metallic minerals and ores. Suitable for
    mineral exploration, mine development
    and planning.

    Available in combination with Nat Gamma or Mag Sus.

    The A634(E)Induction Conductivity tool is designed for measurement of electrical conductivity of rocks in boreholes. High stability and exceptionally wide dynamic range permit precise measurements of conductivity of sand-clay layers and also mineralised water-soaked sands. The tool may be used in water filled, dry and plastic cased boreholes. The response of the probe is practically instantaneous (<0.5 s).

    Specifications

    Tool ParametersA634A634E
    Diameter38 mm38 mm
    Length140 cm160 cm
    Weight5 kg4 kg
    Max. Working Temperature70 degrees C70 degrees C
    Max. Working Pressure10 MPa10 MPa
    Min. no. of Conductors (incl. armour)22
    Supply Voltage Range20 - 45 VDC20 - 45 VDC
    Max. Current Consumption110 mA110 mA
    Nominal Current Consumption80 mA80 mA
    Voltage Polarity in tool Head+ ve on pin 1
    -ve on pin 2 or tool chassis
    + ve on pin 1
    -ve on pin 2 or tool chassis
    Measuring Parameters
    Sensortwo coil systemtwo coil system
    Inter-coil Spacing50 cm30 cm
    Operating Frequency~26 kHz~900 Hz
    Conductivity Range1 - 3000 mS/m300 mS/m - 1000 S/m
    Noise Level<0.5 mS/m
    Accuracy<100 mS/m (5% F.S.)
    100 - 1000 mS/m (3% F.S.)
    1000 - 3000mS/m (10% F.S.)
    <30 S/m (5% F.S.)
    30 - 300 S/m (3% F.S.)
    300 - 1000mS/m (10% F.S.)
    Communication (negative pulse)0 - 20000 cps0 - 20000 cps

    Auslog