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JMZD-2D Sidewall Density Probe

PRODUCT PARAMETERS

  • The motor retracts and extends the borehole arm and monitors the entire retraction and extension process, which is safe and reliable.
  • The method of simultaneous measurement of long and short source distance detectors can compensate for unfavorable factors such as mud cakes.
  • Multi-parameter simultaneous measurement greatly improves work efficiency
Description
FAQ
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Description

JMZD-2D Sidewall Density Probe combines the measurement of focused resistivity parameters (three lateral directions), natural potential parameters, parallel diameter parameters and natural gamma parameters. This instrument can be used in the exploration of oil, coal, gas and other mineral deposits to determine lithology, measure formation porosity, and can also be used to detect the quality of cement cementing outside the casing of production wells.

● Cased

● Bare hole fill with water or mud

● Quantitative calculation of in-situ formation density

● Exploration and quality evaluation of oil, coal, gas and other mineral deposits

● Determine lithology

● Measuring formation porosity

● Testing the cement cementing quality outside the production well casing

● Borehole diameter measurement and correction calculation in conjunction with other well logs

● The motor retracts and extends the borehole arm and monitors the entire retraction and extension process, which is safe and reliable.

● The method of simultaneous measurement of long and short source distance detectors can compensate for unfavorable factors such as mud cakes.

● Multi-parameter simultaneous measurement greatly improves work efficiency

Three lateral electrodesStainless steel electrode, Focusing electrode length: 2L=2×0.6m; Focusing main electrode length:L0=0.06m
Natural potential electrodeLead electrode
 Natural gamma detectorNal crystal, Scattering detector: Nal crystal
Measurement parameters and rangeWell diameter: 60~200mm,5%;
Natural potential: -1200~+1200 mV, 5%;
Focus resistivity: 1.2~1.2×105Ωm, 5%;
Natural gamma: 0~32768cps
Long source distance: 0~32768cps;
Short source distance: 0~32768cps; Density: 1~3 g/ cm³, 3%
Pushing force against wall >10kg
Signal outputBipolar encoding

FAQ

① In SI, it is m·s-2, and one percent of it is the international unit abbreviation g.u.;
② Conversion between SI and CGS: 1g.u.=10-1 mGal

Gravitational field: The space around the earth with gravity is called the gravitational field.
Gravitational potential: The gravitational potential W in the gravitational field is equal to the work done by a particle of unit mass moving from infinity to that point.

① The normal gravity field of the earth: Assuming that the earth is a rotating ellipsoid (reference plane), the surface is glossy, the internal density is uniform, or it is distributed in concentric layers, the density of each layer is uniform, and the deviation of the shape of the ellipsoid from the geoid is very small, then the gravity field generated by the earth is the normal gravity field.
② The normal gravity value is only related to the latitude, the smallest at the equator and the largest at the poles, with a difference of about 50,000 g.u.; the rate of change of the normal gravity value with latitude is the largest at 45° latitude, and zero at the equator and the poles; the normal gravity value decreases with increasing altitude, and its rate of change is -3.086 g.u.. The main feature of the long-term change is the "westward drift" of the geomagnetic elements, both the dipole field and the non-dipole field drift westward, and have a global nature.

The gravitational field strength is equal to the gravitational acceleration in both numerical and dimensional terms, and the two are in the same direction. In gravity exploration, all references to gravity refer to gravitational acceleration. The gravitational field strength at a point in space is equal to the gravitational acceleration at that point.

Gravity exploration is an exploration method that is based on the density difference of rocks and ores. Since density difference will cause local changes in the normal gravity field of the earth (i.e. gravity anomaly), it is used to solve geological problems by observing and studying gravity anomalies.

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