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3D Borehole Imaging System — Intelligent High-Definition Panoramic Borehole Camera

PRODUCT PARAMETERS

The intelligent high-definition 3D borehole imaging system integrates an advanced open-lens probe with a combined LED light source and precision motorized hoisting mechanism.
  • 360° Panoramic Imaging
  • Ultra HD + true color
  • Stitching pictures+ video Combination
  • Auto Detection
  • 3D high-definition Sensor
  • Software
Description
FAQ
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Description

Abstract

The intelligent high-definition 3D borehole imaging system integrates an advanced open-lens probe with a combined LED light source and precision motorized hoisting mechanism. This system delivers accurate lithology identification, geological structure investigation, soft mud interlayer detection, fault and fracture zone mapping, and groundwater migration monitoring. In geotechnical engineering, it supports reinforced concrete inspection, concrete quality assessment, auxiliary geotechnical testing, geological hazard monitoring and prediction, underground instrument installation guidance, subsurface pipeline detection, and tunnel excavation reconnaissance.

Working principle

Under visible-light illumination, the borehole camera captures high-resolution images of the casing inner wall and open borehole surface. The probe’s onboard electronics amplify the optical signal and convert it into a frequency-modulated pulse signal. This signal transmits to the surface receiver via single-core or multi-core cable, where it undergoes amplification and digital decoding to reproduce a real-time image identical to the downhole camera’s view.

Applications

Concrete Quality Control

Inspect pouring quality and evaluate grouting treatment effectiveness

Geological Hazard Monitoring

Detect and track landslides, subsidence, and ground instability

Underground Installation Guidance

Direct instrument and sensor placement in boreholes

Pipeline and Tunnel Inspection

Detect subsurface pipelines and perform advance tunnel reconnaissance

Lithology and Structure Mapping

Identify rock types, geological structures, and weak argillaceous interlayers

Fracture Network Characterization

Detect faults, fissures, and broken zones

Hydrogeological Assessment

Observe groundwater activity and support geomechanical testing

Resource Exploration

Support coal seam evaluation, oil well inspection, and mineral deposit assessment

Features

360° Panoramic Imaging

The probe employs a 360° panoramic HD ultra-low-light camera. The front end features an open-design toughened glass hemispherical dome, enabling full circumferential imaging of the borehole wall without blind spots.

Ultra-HD True-Color Imaging

Standard 5-megapixel high-definition lens delivers photorealistic digital color reproduction at 1:1 scale. Images maintain clarity at full magnification with crack resolution down to 0.01 mm.

Seamless Image Stitching + Video Recording

Advanced intelligent image unwrapping algorithms generate seamless cylindrical borehole wall panoramas during probe ascent or descent. The system simultaneously records downhole forward-looking video, with both datasets available for real-time playback and archival storage.

Automated Probe Deployment

A precision stepper motor drives the cable drum at constant speed, eliminating image jitter and depth errors associated with manual hoisting. This ensures consistent data quality across the entire logged interval.

3D High-Precision Attitude Sensor

An integrated high-precision electronic compass and triaxial sensor module achieves ±0.1° angular accuracy. The system supports vertical, inclined, and horizontal borehole orientations with real-time probe attitude indication.

Intelligent Data Management Software

The digital core library replaces physical core samples, eliminating the logistical challenges of core retrieval, transportation, storage, and long-term management. High-definition borehole wall imagery serves as a permanent geological record accessible for reanalysis at any time.

Configuration

Specifications

System Configuration

ComponentDescription
Surface Control UnitIndustrial-grade multimedia processing workstation
User InterfaceTouchscreen display + tactile button controls
Display8.4-inch TFT LCD
Storage128 GB high-speed solid-state drive
Acquisition RateUp to 60 frames per second
Output Resolution>2048 × 2048 pixels
Acquisition ModesReal-time image mosaicking, real-time video recording, or simultaneous image + video capture
Host Dimensions350 × 300 × 150 mm
Host Weight3.5 kg

Probe Specifications

ParameterSpecification
Lens Type360° panoramic lens
Camera HousingOpen-design hemispherical explosion-proof glass dome; tool-free disassembly and replacement
Resolution2–10 megapixels (configurable)
DiameterØ50 mm, Ø63 mm (custom diameters available)
Hoisting MechanismConstant-speed electric drive
Lifting Speed0.5–3.0 m/min (adjustable)
Maximum Cable Length100–1,500 m (customizable)
Depth Encoder Accuracy0.1 mm
IlluminationOpen-design waterproof LED ring array; shadow-free, uniform lighting with no dead angles
3D Attitude SensorReal-time probe orientation for vertical, horizontal, and inclined boreholes
CableCustom lightweight cable; <2 kg per 100 m; tensile strength >200 kg
Measurement AccuracyCrack detection: 0.1 mm; Azimuth: ±0.1°
Battery Endurance8 hours continuous operation

Cases

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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