Seismic Data Acquisition TRIZ Cases

Automated monitoring replaces manual voice broadcasts with digital transmission, reducing arrangement check time.

A marine seismic vibrator generates acoustic waves using magnetic driver systems and spring elements to produce controlled mechanical vibrations.

Passive low frequency seismic system extracts compressional body waves from ambient noise using adaptive filtering and inversion techniques.

A multidimensional mutual coherence map determines optimal source and receiver positions for seismic surveys.

Near-continuous seismic recording with time-based source triggering enhances data acquisition speed.

Hybrid arrays merge cabled, wireless, and nodal readout modes to minimize environmental impact while maintaining high reliability across diverse terrain.

Dithered firing coordinates multiple sources to reduce rig time while maintaining data integrity through cross-correlation processing.

Logging instrument emits acoustic waves that intermodulate in borehole fluid to generate new frequencies for formation imaging.

A phase-weighted nth root stack method computes a product of phase-weighted and nth root stacks to enhance signal-to-noise ratios in seismic data.

Demigration extracts essential source-receiver pairs from prior seismic data, reducing acquisition time while maintaining measurement precision.

A seismic node synchronizes its sampling rate with a GPS timing signal to align data acquisition operations.

A positioning assistance system for vibrator trucks calculates stopping distance and triggers baseplate lowering before arrival.

Frequency filtering removes low-frequency surface waves to create pseudo listen time, eliminating actual wait intervals between sweeps.

A variable-frequency mean filter processes cross-spread azimuth-offset gathers to attenuate random uncompressed cross-talk signals in simultaneous source seismic data.

Creates synthetic well data via random sampling to resolve the contradiction between high-quality training data and costly physical exploration.

Surface acquisition system determines reference and subsequent transit times to synchronize downhole seismic sensing devices.

Combines seismic data and downhole fluid analysis to predict heavy hydrocarbon locations, addressing low velocity contrast detection challenges.

Frequency-diverse source arrays separate coherent wavefields, preventing spatial aliasing and improving subsurface imaging resolution.

Periodic satellite receiver activation synchronizes the acquisition clock while reducing power consumption in cordless seismic recorders.

A computing system selects a pilot sweep with reduced cross-correlation noise to mitigate seismic survey interference.

Decentralized sensor nodes process seismic arrival times locally to refine velocity models, overcoming centralized bandwidth bottlenecks.

A crossed seismic transducer array acquires multi-fold offset data, resolving the contradiction between continuous layer mapping and discrete feature detection.

Active feedback adjusts squeeze piston position to maintain seismic signal frequency despite external perturbations.

Concentrator modules transmit stored data inventories to a central unit for cross-checking against missing data lists.

Segmented source groups with periodic firing maintain signal coherency, enabling effective pre-processing techniques like groundroll removal and denoising.

Azimuth-dip angle gathers separate diffracted waves from reflected waves to resolve interference and improve imaging accuracy.

A seismic sensor network detects surface and subsurface intrusion events using electrical resistivity tomography.

A seismic source array housing integrates a protective structure to restrain suspended sources during marine deployment and recovery operations.

Evaluating geophysical survey acquisition geometry via synthetic data generation to resolve suboptimal subsurface imaging in rugged terrains.

Alternating zero and random dithering times extends the clean record length, resolving clustering issues that limit deblending quality.

Varying phase sequences across towed seismic sources separates energy from multiple emitters during acquisition.

A grid of linear electric motors extends rods into the ground to measure penetration rate and deformation for precise near surface property analysis.

A seismic vibrator system dynamically selects active source groups based on real-time geometrical relationships to optimize energy propagation.

Cross-correlating nearfield hydrophone signals synchronizes acoustic sources to attenuate out-of-band noise and improve seismic data quality.

Independent segment activation directs shear wave amplitude and frequency to resolve low reproducibility in deep seismic surveys.

Segmented architecture calculates epicentral distance from primary waves to predict shear wave acceleration, reducing computing time for instant alarms.

A seismic interface box converts electromagnetic, electrical, gravimetric, and magnetic sensor data into voltage signals compatible with standard recorders.

Virtual trace bins segment seismic traces by offset and azimuthal attributes, resolving numerical instability in full waveform inversion.

Timing alignment method synchronizes borehole and surface micro-seismic waveform data segments using GPS timestamps and linear interpolation.

Deterministic periodic signature variation shifts geophysical wavefields to distinct transformed domain locations, resolving source separation conflicts.

A seismic sensor uses zero-crossing frequency sensing to differentiate vibration types.

A seismic vibrator fixes the coil and moves the magnet to generate controlled waves.

Machine learning classifies seismic data into distinct facies groups, resolving bottlenecks in subsurface characterization accuracy.

Random time separation minimizes coherent energy overlap from simultaneous sources, allowing reliable depth determination and cleaner imaging data.

Fluid-filled flexible membranes maintain acoustic coupling consistency in varying soil conditions, reducing equipment costs and environmental impact.

Digitally controlled grounded inductor simulation circuits replace large spiral inductors with active OP-AMP networks to reduce chip area and loss.

Visibility analysis selects high-visibility traces for targeted prestack migration, reducing processing time while improving imaging quality.

Varying seismic sweep rates shifts harmonic energy to enable suppression via stacking, improving signal-to-noise ratio without impulsive sources.