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JFS-2 Probe

PRODUCT PARAMETERS

  • Downhole measurement, signal amplification, and digitization
  • High reliability, high measurement accuracy, and easy to use
Description
FAQ
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Description

JFS-2 Casing Collar Locator & Natural Gamma Probe

JFS-2 Casing Collar Locator & Natural Gamma Probe is composed of a Nal body and a photomultiplier tube to form a natural gamma ray detector, which measures the total amount of natural gamma rays; at the same time, the instrument is also combined with a magnetic positioning detector to detect and locate the distribution of magnetic pipe strings (casing, downhole tools, flower pipes, screens, collars, packers, etc.) at depth. It can also be used in various production wells, cementing, perforating, well repair, casing corrosion monitoring and other occasions.

● Borehole with case

● Bare hole fill with water or mud

● Bare Dry hole

● Casing coupling locator

● Divide stratigraphic interfaces and determine changes in stratigraphic facies

● Determine fine-grained/coarse-grained change sequence

● Determine the location and thickness of aquifers

● Estimate uranium concentration

● Downhole measurement, signal amplification, and digitization

● High reliability, high measurement accuracy, and easy to use

Gamma ray detection sensorNal crystal + photomultiplier tube
Gamma ray detection and counting range0~65000cps, accuracy: 5%F.S
Gamma ray detection energy threshold >0.06MeV
Magnetic positioning sensor65mm electromagnetic sensor
Magnetic positioning measurement range±2500mV
Applicable well diameterΦ50~Φ150mm
Output signalBipolar 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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