Engineering Survey 2025 MCQ Set-1

Sidescan, single-beam, and multibeam sonar equipment are compact and portable enough for use on small, inflatable boats like Zodiacs. These systems are commonly used in hydrographic surveying for various water depth measurements.

Lidar (light detection and ranging) technology is used in airborne hydrography for shallow-water surveying. It provides accurate depth measurements and shoreline data, often integrated with other sensors for comprehensive surveys. Airborne lidar systems are efficient for covering large shallow water areas.

Hydrographic surveys measure and map underwater features crucial for safe navigation. This includes depths, shorelines, currents, and underwater obstructions. The data supports maritime safety and various marine activities.

The text explicitly lists geological, biological, physical, and chemical oceanography as the major disciplines. These branches study the Earth's structure beneath the ocean, marine life, ocean currents and processes, and the ocean's chemical composition, respectively.

Safe navigation depends on knowing underwater depths, obstacles, and currents. Hydrographic surveys provide this crucial data, preventing accidents and ensuring efficient maritime operations.

Modern hydrographic surveys use advanced sensors (like multibeam sonar and AUVs) to collect high-resolution data. Specialized software processes this data, creating accurate maps of underwater features and improving navigational safety.

Tidal changes affect water depth measurements. Adjusting the soundings (depth measurements) using concurrent tide data ensures accurate water depths are reflected in the final navigation charts. This compensates for the fluctuating water level caused by tides.

Crowd-sourced surveying uses many data points. While individual measurements may be less accurate, the high data density allows algorithms to produce more precise final results than traditional methods. This leads to improved accuracy in the final navigation charts.

Airborne lidar rapidly measures shallow water depths, up to 70 meters. This is faster than traditional methods and allows for comprehensive shallow-water surveys. The dual-frequency laser system measures both surface and bottom reflections to determine depth.

CHARTS and BATS systems integrate multiple airborne sensors (bathymetric lidar, topographic lidar, digital imagery). This allows for simultaneous data collection of water depths, shoreline features, and topography, providing a more comprehensive and detailed hydrographic survey than traditional methods.

Hydrography maps underwater features like depth, currents, and obstructions crucial for safe navigation. This data allows for safe passage, avoiding hazards, and efficient route planning.

Hydrographic surveys map the seafloor and identify submerged hazards. This is crucial for safe maritime navigation by providing data for nautical charts, thus preventing collisions with underwater obstructions.

The system uses acoustic signals to measure distances and calculate the positions of underwater features. This allows for precise mapping of the seabed and identification of any obstacles. It's essential for safe navigation.

Unlike traditional methods, crowd-sourced surveying uses many data points. Algorithms process this high data density to achieve accuracy exceeding individual measurements, despite lower individual measurement precision.

Bathymetry measures the depth of ocean and lake floors. It's essentially underwater topography, providing crucial data for navigation, resource exploration, and understanding underwater landscapes.

Plane surveying treats the Earth as flat, simplifying calculations for smaller areas. It uses plane trigonometry to determine the horizontal and vertical positions of features, ignoring Earth's curvature. This is accurate enough for many engineering projects over limited distances.

Over such short distances, the Earth's curvature is negligible and introduces minimal error in calculations. Using a flat-Earth model simplifies calculations significantly without sacrificing accuracy.

They reflect the precision of a measurement. The number of significant figures indicates the certainty of the measurement; more figures mean higher precision. This is crucial for accuracy in engineering and surveying calculations and results.

It's the vertical distance from the geoid, an equipotential surface approximating mean sea level, to a point. The geoid's undulations reflect variations in Earth's gravity. This differs from ellipsoidal height, which is relative to a mathematical ellipsoid.

It means obtaining the required level of accuracy without unnecessary extra precision, balancing accuracy needs with cost and efficiency. This minimizes resources used while ensuring project requirements are met.

Triangulation uses measured angles and at least one known distance to calculate the positions and distances of other points. This creates a network of precisely located points, crucial for accurate surveying and mapping.

An ellipsoid, formed by rotating an ellipse, closely approximates the geoid's irregular shape. It's a mathematically defined figure used as a reference surface in mapping and surveying. While not a perfect fit, it provides a workable model for calculations.

Traversing is a fundamental plane surveying method. It involves measuring angles and distances along a series of connected lines to determine the coordinates of points. This is a highly efficient method for establishing control points and detailing.

Independent checks act as a quality control mechanism. They help identify and correct errors in data collection and calculations, ultimately ensuring the accuracy and reliability of the survey. This is crucial for preventing costly mistakes.

Absolute precision refers to a defined standard or datum. Relative precision compares a measurement to another measurement. The difference is largely a matter of definition and convenience.

GPS receivers use satellite signals to determine latitude, longitude, and altitude. This 3D positioning is far more precise than traditional methods, significantly improving survey accuracy and efficiency. The data provides not only distance, but also location components in three dimensions.

Data duplication and error prevention are key aspects of safeguarding. Protecting survey data ensures accuracy and prevents costly mistakes or loss of information. Safeguarding maintains data integrity.

It converts raw field measurements into usable information for analysis, design, and construction. This involves computations and transformations using software, enabling creation of maps, plans, and digital terrain models.

Reconnaissance optimizes survey point placement. It ensures clear lines of sight between points, maximizing efficiency and accuracy by considering terrain and existing control points before fieldwork begins.

EDM (Electromagnetic Distance Measurement) technology uses electromagnetic waves to measure distances with millimeter precision, even over several kilometers. It's a key tool for high-accuracy surveying.

In surveying, precision reflects the repeatability of measurements. High precision means repeated measurements yield very similar results, even if those results are systematically off the true value (low accuracy). Accuracy, conversely, refers to how close the measurements are to the true value.

CAD streamlines design processes, improving both precision and efficiency. It allows for easier manipulation and analysis of 3D data, leading to better results.

It's a foundational structure in surveying. Precisely located stations with known coordinates serve as a reference framework for all other measurements, ensuring accuracy and reliability of the survey. These stations are often permanent markers.

It uses 3D mathematical equations to represent landforms and their features within a computer database. This allows for precise coordinate and elevation determination of any point, aiding design and construction.

It represents the Earth's gravity field's equipotential surface. This means it's a surface where the gravitational pull is consistent, approximately matching mean sea level. Surveyors use this to determine accurate elevations.

Duplicating measurements and implementing checks helps identify and correct errors in data collection and processing. This minimizes human error and improves accuracy. Cross-referencing data further enhances reliability.

Random errors create unpredictable variations in measurements. Because these are random, statistical methods (like calculating a mean and standard deviation) can be used to analyze and understand the data's variability and reliability.

Tools like GPS, total stations, and laser scanners improve precision and speed in data acquisition and processing. This leads to more accurate results and faster project completion in engineering surveying.

Weather variations (e.g., temperature, wind) directly affect measurements, introducing natural errors. These are categorized separately from instrumental or personal errors. Understanding these errors is crucial for accurate surveying.

Residuals, the differences between individual measurements and the mean, offer an estimate of accuracy because the true value is unknown. Smaller residuals suggest higher accuracy.

Understanding the measurement process allows for identification and mitigation of errors stemming from equipment limitations, environmental factors, and computational approximations. This ensures more accurate and reliable survey results.

A level surface is perpendicular to the direction of gravity. This means the surface's normal vector points in the vertical direction, aligning with the force of gravity. The geoid, a model of Earth's mean sea level, exemplifies this relationship.

Reliable survey results depend on established principles. This ensures consistent, accurate measurements and prevents errors that could compromise project integrity and safety.

Survey procedures aim to obtain the desired measurements (like distances or coordinates) and determine the reliability (uncertainty) of those measurements. Accuracy assessment is crucial for meaningful results.

Independent checks in surveying are crucial for quality assurance. They help detect and prevent blunders, ensuring the reliability and accuracy of survey results. This is achieved through various techniques, including repeating measurements and using multiple methods to verify data.

These surveys are fundamental in engineering. Control surveys establish a network of precisely located points. Topographic surveys map the Earth's surface features. Setting-out accurately positions construction elements on site.

These errors stem from natural conditions (weather, refraction), instrument imperfections, and human limitations in observation. Understanding these categories is crucial for accurate surveying and error mitigation.

It expresses the error (εx) as a fraction of the measured value (x). This provides a more meaningful comparison of accuracy across different scales of measurement, unlike absolute error. Multiplying by 100 gives the percentage error.

It's the best estimate of the true value from a dataset. Generally calculated as the arithmetic mean, summing all values and dividing by the number of values. For a large dataset, the MPV approaches the true value.