IMPORTANCE OF GEOPHYSICAL INVESTIGATIONS
Geophysical Engineering is the efficient means of subsurface investigation to evaluate soil properties in applied forced dynamic condition. The merit of application of this low cost aid lies in its ease of deployment and rapidity in providing a reliable knowledge of the underground over a large area, substantiating the requisite Geophysics to evaluation studies thereby.
Technological advancements made in the field of Geophysical Engineering are of portable digital data acquisition instrument systems have increased the versatility in evaluating underground conditions and site characterization.
The state-of-the-art subsurface Geophysical Investigations will be helpful to any large scale projects towards minimizing involvement of the conventional direct exploration methods, aiding in accelerated and economical development of the construction projects.
Honestly say, a particular Geophysical Investigations may not resolve all the problems associated with subsurface investigations. If you consider, seismic refraction test (SRT) may not reveal the low velocity zones under rock interface, which might be present under certain geological conditions. IGS therefore stands in integration of various Geo-Physical Investigations like seismic refraction, resistivity imaging, ReMi, Cross Hole Shear Wave Test (CHST)/downhole/uphole seismic and seismic reflection, to determine various properties of subsurface like bedrock quality and depth, low velocity zones (even under rock interface), fault/fracture/shear zones, water lenses, tunnel route geology etc.
In addition to the geophysical tests state above, we are proud to reveal that Block Vibration Test (BVT) shall be performed as per IS: 5249-1992 for large scale construction projects where Machine Foundations are involved is the best suitable test to avoid assumed values of Es (Modulus of Elasticity of Soil) which will be used in Settlement Calculations and G (Shear Modulus) which is used for Dynamic Spring Constant for attaining Vertical Stiffness factor for any high raised foundation.
Instead of depending the referral values of famous authors, IGS strictly advises to conduct Block Vibration Test to attain accurate value of Young’s Modulus (Es) & Shear Modulus (G) as per the existing site conditions.
Major Advantages of Geophysical Engineering
- Geophysical methods are quick to apply, saving in terms of time and money.
- Light and portable equipment allows access to remotest of sites.
- Provides information on critical geological features like faults/fractures/weak zones/shear zones, not visible from surface information.
- Large areas mapped quickly and inexpensively.
- Researchers can assess site conditions, and target specific locations for detailed investigations by drilling, while avoiding others
- Geophysical methods can quickly produce subsurface geology avoiding delays during execution due to meeting the unexpected.
- Shear wave profiles can be quickly obtained for ascertaining liquefaction potential and earthquake response.
- Buried utilities, pipes and cables, can be detected before drilling/ excavation, avoiding damage to utilities and costly accidents.
- Concrete structures can be quickly scanned to ascertain integrity and detect defects like voids, honeycombing etc.
IGS has highly experienced personnel and advanced instruments to carry out high resolution geophysical surveys for geotechnical investigations. The survey methodology and tools to be used are decided in consultation with the client and depending on site conditions and objectives of survey. A technical report describing our work, including high resolution maps with detailed interpretation is presented to the client upon completion of analysis.
Techniques available to solve a range of subsurface problems for geotechnical investigations
- Bedrock profile, rock quality and depth
- Thickness of overburden
- Fractures and weak zones
- Topography of ground water
- Slope stability studies
- Pipeline route studies
- Electrical Resistivity Imaging
- Bedrock quality and depth measurements
- Excellent 2-dimensional display of ground resistivity.
- Fractures and weak zones
- Delineation of small features like cavity, contamination plumes, weak zones etc.
- Detects soft zones under rock surface (not detected by seismic refraction)
- Possible to conduct across flowing rivers for bedrock depth determination
- ReMi (Refraction Micro-tremor)
- We have another best innovative technique of ReMi (Refraction Micro-tremor) having distinct edge over MASW and SASW in terms of logistics, execution and results.
- ReMi can be performed under the same layout as used for seismic refraction, to obtain excellent shear wave velocity profiles of subsurface.
- The seismic source consists of ambient seismic “noise”, or micro-tremors, which are constantly being generated by cultural and natural noise.
- ReMi can determine shear wave velocities down to a minimum of 40 meters (130 feet) and a maximum of 100 meters (300 feet) depth.
- Critical parameter for earthquake site response and Liquefaction analysis.
- Crosshole/downhole/uphole Seismic Surveys
- Precise determination of P and S wave seismic velocities.
- Determination of Dynamic Elastic Moduli like Poisson’s Ration, Young’s Modulus, Bulk Modulus and Shear Modulus.
- Detects even thin anomalous zones in subsurface.
- Ground Penetrating Radar
- Geological and hydro-geological investigations including mapping of bedrock topography, water levels, solution features, glacial structures, soils and aggregates.
- Engineering investigations to evaluate dams, sea walls, tunnels, pavements, roadbeds, railway embankments, piles, bridge decks, river scour, buildings and monuments.
- Location and evaluation of buried structures including utilities, foundations, reinforcing bars, cavities, tombs, archaeological artifacts, and animal burrows.
- Site investigations: location of buried engineering structures and underground storage tanks.
- Rapid ground coverage- Antenna towed either by hand or from a vehicle.
- High-resolution coverage of the survey area, detecting even small objects.
- On-site interpretation possible due to instant graphic display.
- Micro Gravity Surveys
- Regional geological mapping
- Sediment thickness studies
- Void detection