Applications

We can conduct surveys and provide services which can support a range of research, infrastructure and resource development projects.

Services

We provide Bathymetry/hydrography, Oceanography/hydrology. geophysical/geotechnical, concrete inspection, and land survey services.

Equipment

We have positioning systems, topographic systems, hydrographic systems and much more depending on your needs.

Projects

Take a look at our list of projects from different locations around the Philippines.



RANGE OF SERVICES

  • Bathymetry and Hydrography
  • Oceanography / Hydrology
  • Geophysical / Geotechnical
  • Concrete Ispection
  • Land Survey

SEISMIC SOLUTIONS

Trinav Surveys can now offer Seismic Acquisition and Processing services in the Philippines. With a 24 channel seismograph, Geophones and Processing capabilities we can perform Seismic Refraction, Tomography and MASW (Multichannel Analysis of Surface Waves) studies.

General Configuration for Data Acquisition

Typical applications include:

  • Foundation engineering studies
  • Vs-30 site classification
  • Depth to bedrock
  • Depth to ground water
  • Shallow voids and faults
  • Estimating rippability prior to excavation

The system is “man portable” and can be used in remote areas with no road access.

Surface Wave Data Analysis

Use of 4.5 Hz geophone and a longer record length of 1 to 2 s world have provided more surface wave data, but sill some information can be gleaned from this refraction record. Not surprisingly, the calculated Vs30 is about one-half of the second layer Vp determined through refraction.

Surface Wave Data Analysis

MASW - Applcations

Shear-wave velocity (Vs) information of subsurface materials is directly related to the stiffness property of the materials, which is the key property dealt in all geotechnical engineering projects. In this sense, the MASW method can be applied to any geotechnical engineering project that requires subsurface mapping of the stiffness in 1-D, 2-D, and 3-D formats.

The most common type of application has been the soil-bedrock mapping that delineates topographic boundary between soil and bedrock by an interface of significant velocity (Vs) increase (e.g., from 300 m/sec to 1000 m/sec). It also shows vertical and horizontal variation of soil stiffness by displaying velocity (Vs) variations within the soil range (e.g., 100 m/sec - 300 m/sec). This boundary often shows a gradual change in velocity over a certain depth range rather than a sharply-defined interface, indicating the possible weathered zone on top of the bedrock. More recently, applications to detect subsurface anomalies are merging. These anomalies may include localized low-velocity zones created by various reasons such as existing utility tunnels, void development due to collapse, severely weathered bedrock, loss of cohesiveness in filled materials, etc. In this case, the detection is often facilitated by non-velocity mapping approaches such as back-scattering analysis and common-offset section generation. Another type of application is the performance evaluation that is executed before and after a specific operation is applied. This includes the compaction evaluation for surface and shallow subsurface materials during road and building construction.



Site classification according to EC8 and DIN4149

In order to quantify the design load for buildings due to an earthquake the Eurocode 8 (EC8) and the DIN4149 require the classification of the ground. The dominating or average shear wave velocity in depths down to 30 m is most often used for this classification. Beyond that the standards request certain design features as flexible foundation beams based on the class of the subsoil which are affecting the costs of a building. A seismic survey can often reduce the costs because otherwise necessary safe assumptions concerning the classification are avoided. Surface wave measurements such as MASW are especially suited to determine shear wave velocity profiles at these shallow depths.


Example:

MASW measurements were made in the planning phase of a warehouse to classify the building site and to determine the necessity of flexible foundation beams. The result in the figure to the left shows the calculated shear wave velocity profile, where the velocity depth profile is assigned to the middle of the geophone array. The average shear wave velocities determined at depths of 3 to 20 m is the so called dominating shear wave velocity. This velocity is used to classify the foundation site according to DIN 4149. For this example the site was assigned as subsoil class B with dominating shear wave velocities between 350 and 800 m/s. For class B foundation sites, situated in low risk earthquake zones, the use of flexible foundation beams is not required.

Depth to bedrock

Seismic refraction is well suited for delineating material properties of the subsurface, such as seismic velocities. The obtained seismic velocities indicate the depth to bedrock and the associated bedrock topography variations.

Example:
A seismic refraction survey was conducted at a planned flood control basin. The depth to bedrock and the bedrock topography were delineated to determine the required anchoring depth of the basin. The results enabled a subsurface characterization into three layers of different material properties, based on geological and weathering interfaces.



MAGNETICS

The measurement of the Earth’s Magnetic field is an important Geophysical discipline that has wide applications in various fields

  • Mineral exploration
  • Mining ore body delineation
  • Buried pipelines and other utilities
  • Archeological studies
  • Un-eXploded Ordnance (UXO)
  • Marine ship wrecks
  • Marine anchors, chains and other items
  • Marine cables, pipelines, etc.

Trinav has available Land and Marine Cesium Vapor Magnetometers for Field data acquisition and Proton Precession units for Base Station measurements to allow correction of the data during processing for Diurnal fluctuations.

The Earth’s Magnetic Field in the Philippines is approximately 39,500 nanoTesla with inclination of 0 degrees in the South to 42,500 nanoTesla with inclination of 26 degrees in the North

The Cesium Sensors have a sensitivity of 0.1 nanoTesla and detect small ferrous objects (i.e. UXO) or larger regional trends (mineral exploration)

G-859. A self contained, “Back Pack” configuration that can collect high quality magnetic data at “walking speed”. The integrated GPS enables data collection without the necessity to set-out grid lines prior to the survey

GROUND PENETRATING RADAR

SIR-3000 SYSTEM

TRINAV can now offer an important tool for the non-destructive and non-intrusive mapping and surveying of underground featrures.


The surface intercae radar (S.I.R.), is a ground penetrating radar system that has wide apllications in the inspection, construction and civil engineering fields.



SUB SURFACE MAPPING

A New – Non Destructive Method Of Surveying

WITH OUR GROUND PENETRATING RADAR (G.P.R.) SYSTEMS WE CAN PROVIDE INSPECTION, LOCATION AND MAPPING OF SUB SURFACE FEATURES.

THESE CAN INCLUDE:

  • • CONCRETE THICKNESS
  • • SUB-BASE THICKNESS
  • • EROSION AREAS AND VOIDS
  • • GEOLOGICAL MAPPING
  • • WATER TABLE MAPPING
  • • RE-BAR LOCATION
  • • BURIED UTILITIES (PIPELINES, CABLES. CONDUITS, TUNNELS)


MODEL MLF ANTENNAE SYSTEM


Void/Cavite detection at Mactan Island

MODEL 5103 400 MHz. ANTENNAE SYSTEM

Burned utility survey prior to trenching for cable burial

SURVEY CART WITH 400/900 MHz. ANTENNAE SYSTEM

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Radan 7

The world's most advanced and easy-to-use Ground Penetrating Radar data processing and analysis package New Map Mode with GPS data integration.




3D QuickDraw Module

Surface Wave Data Analysis
  • ● Multiple interactive views of pipes and other targets picked by the user
  • ● Automatic Target and Pipe Recognition Results generated quickly and automatically into the Interactive-3D window
  • ● Edit targets or pipes (size, color, material)
  • ● Link and unlink picks to form pipes and targets
  • ● Ability to add and delete pipes and targets

MAP Mode

New mode allows 2D files collected with GPS data to be viewed in 3D. See the actual spatial view of collected data.


Enhanced and Simplified 3D Viewing

QuickDraw module provides improved 3D viewing options in a single dialog box. Animation from any slice with any other slice. Z width control always available. Stretch, shrink and zoom as desired. Fit a large file into a single view or zoom in on any section.

Geophysics On Marine

Sub Bottom Profilers

Sub-bottom profiling systems identify and measure various marine sediment layers that exist below the sediment/water interface. These acoustic systems use a technique that is similar to single beam echo sounders. A sound source emits an acoustic signal vertically downwards into the water and a receiver monitors the return signal that has been reflected off the sea floor. Some of the acoustic signal will penetrate the seabed and be reflected when it encounters a boundary between two layers that have different acoustic impedance. The system uses this reflected energy to provide information on sediment layers beneath the sediment-water interface.



The Earth’s Magnetic Field in the Philippines is approximately 39,500 nanoTesla with inclination of 0 degrees in the South to 42,500 nanoTesla with inclination of 26 degrees in the North

The Cesium Sensors have a sensitivity of 0.1 nanoTesla and detect small ferrous objects (i.e. UXO) or larger regional trends (mineral exploration)



Trinav G-882

MAGNETICS

The measurement of the Earth’s Magnetic field is an important Geophysical discipline that has wide applications in various fields.

  • ⮚ Mineral exploration
  • ⮚ Mining ore body delineation
  • ⮚ Buried pipelines and other utilities
  • ⮚ Archeological studies
  • ⮚ Un-eXploded Ordnance (UXO)
  • ⮚ Marine ship wrecks
  • ⮚ Marine anchors, chains and other items
  • ⮚ Marine cables, pipelines, etc.

Trinav Geoscience has available Land and Marine Cesium Vapor Magnetometers for Field data acquisition and Proton Precession units for Base Station measurements to allow correction of the data during processing for Diurnal fluctuations.

What is Sub-Bottom Profiling?

Sub-bottom profiling is a non-invasive geophysical technique used to investigate the sediment layers below the seafloor. It helps to identify and analyze geological features, archaeological sites, and environmental conditions beneath the ocean or other water bodies.


Key Features:

  • Accurate imaging of sediment layers
  • Identifying underwater structures and objects
  • Assessing environmental conditions

How Sub-Bottom Profiling Works

Sub-bottom profiling uses specialized equipment called a sub-bottom profiler. This device emits sound waves into the seabed, which bounce back to create a cross-sectional image of the sediment layers and any objects beneath. The data collected helps in creating detailed maps and understanding the composition of the seafloor. It's a non-destructive and eco-friendly technique!

Applications of Sub-Bottom Profiling

Sub-bottom profiling has a wide range of applications:

  • • Environmental Assessment: Monitor underwater habitats and ecosystems.
  • • Archaeological Exploration: Locate shipwrecks, ancient settlements, and artifacts.
  • • Geophysical Surveys: Understand geological formations and natural resources.
  • • Infrastructure Planning: Assess the seabed for safe construction

Other Applications:

  • • Shallow Gas Hazard Surveys
  • • Transition Zone Surveys
  • • Offshore Wind Turbine and Dam Site Surveys
  • • Bedrock Investigation
  • • Cross-River Surveys for Bridge Construction
  • • Pipeline and Construction Surveys
  • • Geotechnical Site Investigation
  • • Coastal Engineering
  • • Ability to correlate seismic data with land based surveys

Advantages of Sub-Bottom Profiling

Non-Invasive: Does not disturb the seafloor or underwater life.

  • Accurate imaging of sediment layers
  • Identifying underwater structures and objects
  • Assessing environmental conditions

Our Expertise in Sub-Bottom Profiling

Trinav Surveys is a team of dedicated experts with 36 years of experience in sub-bottom profiling. Our state-of-the-art HMS Bubble gun, comprehensive data analysis, and commitment to precision ensure that we deliver top-quality results for your project.


Contact us to discuss how we can assist you.

Hydrographic Surveys

Trinav Geoscience has available various systems to measure the water depths and seafloor features.

Single Beam Echo Sounders

These devices take a measurement of the water depth directly below the transducer along pre-determined lines of sounding. By interpolation of adjacent lines of sounding, a contoured depth chart can be produced. The Echo Sounders are interfaced to a computer logging system that is also integrated with GPS Positioning for precise geo-referencing.





Multi Beam Echo Sounders

As the name suggests, these instruments simultaneously measure multiple beams horizontal to the survey Vessel track, thus recording a complete coverage of the seafloor. These multiple beams are calibrated and adjusted by 3 Axis Motion Sensors, Gyro or GPS Compass, Tidal Monitors, and real-time Sound Velocity Profilers.


Multi Beam Softwares



Sea Floor Mapping

Dual Channel Side Scan Sonars are used to map the seafloor features.

Applications:

  • ● Cable & pipeline surveys
  • ● Geological/geophysical surveys
  • ● Mine countermeasures (MCM)
  • ● Geohazard Surveys
  • ● Channel clearance
  • ● Search and recovery
  • ● Archaeological surveys
  • ● Ship Wrecks
  • ● Seafloor debris
  • ● Seafloor classification




Tides

We have Pressure type Tide Gauges to measure the tidal fluctuations at the near shore environment.


Tidal Parameters

  • Generated from Harmonic Constants File: C:\Jobs\job
  • Number of harmonic components: 17 in 10 groups
  • Scan from Friday, 1 January 2010 to Friday, 11 August 2028
  • HAT: 1.290m at 07-Nov-25 6:36:00 pm
  • MHWS: 0.932m
  • MHHW: 0.801m
  • MHW: 0.645m
  • MHWN: 0.262m
  • ML: -0.008m
  • MLWN: -0.282m
  • MLW: -0.665m
  • MLLW: -0.784m
  • MLWS: -0.951m
  • LAT: -1.241m at 29-Apr-25 12:54:00 pm
  • Maximum: 1.290m at 07-Nov-25 6:36:00 pm
  • Minimum: -1.241m at 29-Apr-25 12:54:00 pm
  • Fastest Rate of Rise: 0.587m/hr at 29-Sep-11 3:45:00 pm
  • Fastest Rate of Rall: -0.611m/hr at 29-Apr-25 9:33:00 am
  • Lunitidal (High Water) Interval as inferred from M2 (Hours:Minutes):05:25

Listing of Harmonic Constants

  • #GROUP M2,157.193,0.58230
  • #GROUP K1,232.662,0.15776
  • #GROUP S2,205.920,0.34697
  • #GROUP O1,209.862,0.09818
  • #GROUP P1,267.283,0.03745
  • #GROUP N2,135.760,0.11314
  • #GROUP K2,215.502,0.08059
  • #GROUP Q1,189.378,0.02380
  • #GROUP M4,187.972,0.00181
  • #GROUP MS4,283.170,0.00309

Oceanographic Observations

COASTAL OCEANOGRAPHY

TRINAV provides a range of services and instrumentation for monitoring the Oceans physical parameters.

As many development and infrastructure projects are situated near the coastline, an understanding of the oceans characteristics is essential to the design process to minimize the effects on the project.

Factors that may impact the design include:

  • Coastal erosion
  • Siltation
  • Sediment transport
  • Thermal boundaries
  • Current flow turbulence


Applications that would require monitoring include:

  • Submarine cables & pipelines to evaluate potential for erosion
  • Jetty’s & wharfs for the best orientation to the prevailing wind, currents and waves.
  • Marine outfalls for dispersion modeling
  • Power plant cooling water systems
  • Marinas and moorings
  • Coastal resorts for beach conservation

Parameters to monitor:

  • Ocean currents Velocity and Direction
  • Ocean Waves Significant Height and Period
  • Ocean Waves Direction and Spectral Energy
  • Tidal variations
  • Suspended Sediments
  • Turbidity
  • Conductivity/Salinity/Temperature Water Quality (Temperature, Salinity, Density, P.H., Dissolved Oxygen and O.R.P.)

Instrumentations

We have various instruments to monitor the physical parameters..

  • Sontek Triton: Waves, Tides and Currents
  • Sontek Argonaut: Currents at multi-levels
  • Sontek ADP: Vertical Profiling Current meters
  • Nortek: ADCP Currents and Waves
  • Valeport: Single Point currents and Salinity
  • Horiba: Multi-Parameter Water Quality
  • YSI CTD: Temperature/Salinity
  • Aquatec: Turbidity
  • Aquatec: Suspended Sediment Profiler
  • Bubbler: Tide Gauge
  • RBR: Tide Gauge.

Meteorological Observations

We have Gill Instruments Meteorological stations recording to YSI data loggers to monitor long term weather conditions.

This data can be used for:

  • Power Plants
  • Hydro Plants
  • Agriculture
  • Solar Farms
  • Wind Turbines
  • Coastal oceanography.

Parameters Measured

  • Wind Speed & Direction
  • Air Temperature
  • Air Humidity
  • Barometric Pressure
  • Solar Radiation
  • Rain Fall.

Land Surveying

Using modern instrumentation, we can provide various surveying services:

This data can be used for:

  • Topographic Mapping
  • Bench Mark and Control establishment and checking
  • Boundary Surveys
  • Set-out surveys for Geophysical studies
  • As-built of existing facilities
  • Inter-tidal zone survey
  • Resource monitoring
  • Settlement/Compaction monitoring.