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JJY-2D Borehole Geometry Probe
PRODUCT PARAMETERS
- Send instructions from the ground and execute them from the motor.
- Easy to use, high measurement accuracy (well diameter signal has 12-bit resolution), high reliability
Description
Abstract
JJY-2D Borehole Geometry Probe is a mechanical four-arm contact caliper. The four-way dynamic seal piston of the instrument is connected to a zero temperature drift linear sensor, which converts the borehole diameter change into a digital quantity and then transmits it to the ground through encoding. The measurement data in two directions are used to conduct formation information research and formation stress analysis.

Applicable Conditions
● Bare hole fill with water or mud
● Bare Dry hole
Applications
● Locating cracks, caves and casing defects
● Diameter measurement and rock formation stress analysis in two directions
● Rock formation integrity evaluation
● Drilling diameter measurement and correction calculation in conjunction with other well logging
Features
● Send instructions from the ground and execute them from the motor.
● Easy to use, high measurement accuracy (well diameter signal has 12-bit resolution), high reliability
Specifications
| Well diameter measurement method | Four-arm well diameter |
| Well diameter measurement range | Φ60~600 mm |
| Measurement error | 1.5% F.S |
| Well diameter leg opening method | Ground command control, Motor executes retraction and retraction |
| Signal output | Bipolar 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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