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Related Concept Videos

Pressure Gauges01:20

Pressure Gauges

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Most pressure gauges, like those on scuba tanks, are calibrated to read zero at atmospheric pressure. Readings from such gauges are called the gauge pressure, which is the pressure relative to atmospheric pressure. When the pressure inside the tank exceeds atmospheric pressure, the gauge reports a positive value. Some gauges are designed to measure negative pressure. For example, many physics experiments must take place in a vacuum chamber, a rigid chamber from which some of the air is pumped...
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Measurement of Fluid Pressure01:16

Measurement of Fluid Pressure

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Fluid pressure is commonly measured using devices called manometers, which rely on liquid columns to indicate pressure differences. The height of a liquid column in a manometer reflects the pressure exerted by the fluid, providing a simple yet effective means of measurement. Different types of manometers serve specific purposes based on their configurations and the type of fluids involved.
A basic form of manometer is the piezometer, a vertical tube open at the top and filled with the same...
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Hydrostatic Pressure Force on a Curved Surface01:04

Hydrostatic Pressure Force on a Curved Surface

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Hydrostatic pressure on curved surfaces is a fundamental concept in fluid mechanics with broad applications in the civil engineering field. When fluid is in contact with a curved surface, as in a reservoir, dam, or storage tank, it exerts pressure that varies in magnitude and direction along the curved surface. To assess the total hydrostatic force exerted by the fluid on a curved structure, engineers typically isolate the fluid volume adjacent to the surface and analyze the forces acting on...
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Fluid Pressure01:14

Fluid Pressure

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In mechanical engineering, fluid pressure plays a critical role in designing systems that utilize liquid flow, such as hydraulic systems, pumps, and valves. When designing these systems, engineers must ensure they can withstand the forces created by fluid pressure to avoid damage or failure.
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Variation of Atmospheric Pressure01:18

Variation of Atmospheric Pressure

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Change in atmospheric pressure with height is particularly interesting. The decrease in atmospheric pressure with increasing altitude is due to the decreasing gravitational force per unit area as we move away from the surface of the earth.
Assuming the air temperature is constant at a given altitude and that the ideal gas law of thermodynamics describes the atmosphere to a good approximation, one can find the variation of atmospheric pressure with height.
Let p(y) be the atmospheric pressure at...
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Pressure Variation in a Fluid at Rest01:11

Pressure Variation in a Fluid at Rest

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In a fluid at rest, the pressure at any point beneath the fluid surface depends solely on the depth, not on the container's shape or size. This principle, known as hydrostatic pressure, arises because, in stationary fluids, there is no acceleration, meaning the forces within the fluid balance out. Only vertical forces, caused by the weight of the fluid above, contribute to pressure changes with depth.
When measuring pressure at two different levels within the fluid, the difference in...
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The Measurement of Unsteady Surface Pressure Using a Remote Microphone Probe
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Supersensitive Detector of Hydrosphere Pressure Variations.

Grigory Dolgikh1, Sergey Budrin1, Stanislav Dolgikh1

  • 1V.I. Il'ichev Pacific Oceanological Institute FEB RAS, 690041 Vladivostok, Russia.

Sensors (Basel, Switzerland)
|December 10, 2020
PubMed
Summary

This study introduces a novel instrument for measuring hydrosphere pressure variations. The device achieves high accuracy, offering valuable data for oceanographic and geophysical research.

Keywords:
Michelson interferometerfrequency-stabilized helium-neon laserinfra-gravity waveslaser strainmeterlow-frequency hydroacoustic emittersupersensitive detectorwind wave

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Area of Science:

  • Geophysics
  • Oceanography
  • Instrumentation

Background:

  • Accurate measurement of hydrosphere pressure variations is crucial for understanding oceanic processes and seismic activity.
  • Existing instruments may have limitations in sensitivity, accuracy, or operating range for certain applications.

Purpose of the Study:

  • To present a new instrument for recording hydrosphere pressure variations.
  • To detail the instrument's design, performance, and potential for enhanced capabilities.

Main Methods:

  • Utilizes an equal-arm Michelson interferometer.
  • Employs a frequency-stabilized helium-neon laser for precise measurements.
  • Incorporates a supersensitive detector for infrasonic and sonic frequency ranges.

Main Results:

  • The instrument records hydrosphere pressure variations from 0 to 1000 Hz.
  • Achieves an accuracy of 0.24 mPa at sea depths up to 50 m.
  • Experimental results confirm high performance in infrasonic and sonic ranges.

Conclusions:

  • The developed instrument demonstrates high performance for detecting subtle pressure changes in the hydrosphere.
  • Potential exists for expanding the operating range and enhancing accuracy through system improvements.
  • This technology offers a valuable tool for scientific research in oceanography and geophysics.