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Infrared gas analyzer

From Wikipedia, the free encyclopedia

Kozo Ishida's design for an infrared gas analyzer. See it here
A diagram showing the wavelength at which different atmospheric gases absorb infrared radiation

An infrared gas analyzer measures trace gases by determining the absorption of an emitted infrared light source through a certain air sample. Trace gases found in the Earth's atmosphere become excited under specific wavelengths found in the infrared range. The concept behind the technology can be understood as testing how much of the light is absorbed by the air. Different molecules in the air absorb different frequencies of light. Air with much of a certain gas will absorb more of a certain frequency, allowing the sensor to report a high concentration of the corresponding molecule.

Infrared gas analyzers usually have two chambers, one is a reference chamber while the other chamber is a measurement chamber. Infrared light is emitted from some type of source on one end of the chamber, passes through a series of chambers that contains given quantities of the various gases in question.

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  • How We Measure Photosynthesis
  • PIC | | Infrared Anaylyzer || Oxygen Analyzer || Engineering
  • IE-209 INFRA RED GAS ANALYSER BY KAPIL SHARMA GPC AJMER

Transcription

carbon supports life on earth as we know it in fact we humans are 18 .5 percent carbon our plant friends produce carbon through a process called photosynthesis through photosynthesis plants provide that delicious oxygen that humans and other animals need and love. So, understanding how much photosynthesis is happening, tells us a lot about how healthy the plants are in an ecosystem. Now, we know photosynthesis is happening all around us. we see plants growing and reproducing every day but how do us science minded humans measure how much photosynthesis is happening in plants? in order to grow and produce oxygen. How we measure photosynthesis is the topic of this video. So let's first talk about that carbon generating process called photosynthesis. The "photo" part in photosynthesis relates to light. Plants use energy from light to grow. Now "synthesis" relates the biosynthesis, or the process in which plants syntyhesize light, carbon dioxide or CO2, and water to grow. now to support growth plants absorb co2 from the atmosphere through small pores in their leaves called stomata. using energy from sunlight, co2 and water are synthesized to create sugar. This sugar is then converted into energy that plants need to grow through a process called respiration so the delicious co2 that plants absorbed mixed with some Sun and water creates the perfect cocktail to produce that energy that plants need to grow. And if that's not important enough through photosynthesis, plants also provide clean air for us to breathe. But how do we actually measure photosynthesis? Well one way to measure photosynthesis is to measure how much CO2 plant leaves absorb. Because we know the plant that is actively absorbing CO2 is also performing photosynthesis. but how do we actually measure co2 uptake by a plant? Well let's first place a leaf in a closed chamber that's filled with CO2 rich air. Think about it, if the leaf in the chamber is alive, it will uptake CO2 to produce the energy that it needs to grow. Now one way to measure the CO2 in that chamber is to use a light. The method of using light to measure things in science is called spectroscopy. spectroscopy methods measure how much matter, like CO2, absorbs, reflects and transmits light. Now CO2 loves to absorb infrared light. So if we fill a chamber with a lot of CO2 and we shine infrared light into the chamber a lot of that light will get absorbed. now on the other hand if the chamber doesn't have a lot to CO2 in it only a small amount to that like gets absorbed. Now equip the chamber with a detector that can measure the amount of light that makes it to that end in the chamber. The detector is calibrated which means that it relates the amount of light recorded in the box to a specific amount to CO2. So more light recorded means less CO2 in the chamber and less light recorded means more CO2 in the chamber this chamber system is called an Infrared Gas Analyzer. Infrared gas analyzers are commonly used to measure CO2 uptake. So now that we understand the basics and spectroscopy how do we measure CO2 uptake individual leaf well we can use our infrared gas analyzer chambers system. First add a reference chamber on the left. We'll flow CO2 rich air thorugh this reference chamber and use the infrared light detector to measure how much CO2 is in the air. Next add a second sample chamber on the right. Air flows from the reference chamber to the chamber with a leaf in it and into the sample chamber. The sample chamber uses infrared light detector to measure the amount of co2 in the air after the leaf absorbs what it needs to grow. We can control the volume air moving through the chambers using a flow meter. So we know how much air is in each chamber. Here comes the interesting part... we can calculate the difference in the amount of CO2 measured in our reference chamber compared to the CO2 measured in our sample chamber. the difference between CO2 in the two chambers is the flux. which represents the amount the CO2 taken up by the leaf inside the chamber for photosynthesis. The measurement of the difference in CO2 between the two chambers is called Net Assimilation or ANet. So, the infrared gas analyzer can be used to estimate how much photosynthesis is occurring but if that's not powerful enough it can also be used to measure how temperature and moisture changes in our climate impact carbon uptake. We can also add additional meters to the set up to control things like temperature humidity in the chamber So we can adjust the temperature of the chamber and measure how that affects CO2 uptake of our plant. these measurements can also be combined with other techniques that measure and estimate carbon over large areas For example, the National Ecological Observatory Network or the NEON project uses an infrared gas analyzer installed on its towers across United States. to measure carbon in the atmosphere. NEON will also be combining this atmospheric carbon data with airborne remote sensing to model carbon across entire forests and over larger landscapes. And so, to sum this all up plants use CO2 to perform photosynthesis to grow and provide oxygen. We can measure CO2 uptake with spectroscopy or light measures, using an infrared gas analyzer. these measurements can help us understand both how healthy plants are in an ecosystem and also how changes in climate affect plant growth. And that my friends is how and why we measure photosynthesis.

Principles of Operation

The design from 1975 (pictured above) is a Nondispersive infrared sensor. It is the first improved analyzer that is able to detect more than one component of a sample gas at one time. Earlier analyzers were held back by the fact that a particular gas also has lower absorption bands in the infrared.

The invention of 1975 has as many detectors as the number of gases to be measured. Each detector has two chambers which both have an optically aligned infrared source and detector, and are both filled with one of the gases in the sample of air to be analyzed. Lying in the optical path are two cells with transparent ends. One contains a reference gas and one will contain the gas to be analyzed. Between the infrared source and the cells is a modulator which interrupts the beams of energy.

The output from each detector is combined with the output from any other detector which is measuring a signal opposite to the principal signal of each detector. The amount of signal from other detectors is the amount that will offset the proportion of the total signal that corresponds to the interference. This interference is from gases with a principal lower absorption band that is the same as the principal band of the gas being measured.

For instance, if the analyzer is to measure carbon monoxide and dioxide, the chambers must contain a certain amount of these gases. The infrared light is emitted and passes through the sample gas, a reference gas with a known mixture of the gases in question and then through the "detector" chambers containing the pure forms of the gases in question. When a "detector" chamber absorbs some of the infrared radiation, it heats up and expands. This causes a rise in pressure within the sealed vessel that can be detected either with a pressure transducer or with a similar device. The combination of output voltages from the detector chambers from the sample gas can then be compared to the output voltages from the reference chamber.

The latest Infrared Gas Analyzers

Like earlier infrared gas analyzers, modern analyzers also use nondispersive infrared technology to detect a certain gas by detecting the absorption of infrared wavelengths that is characteristic of that gas. Infrared energy is emitted from a heated filament. By optically filtering the energy, the radiation spectrum is limited to the absorption band of the gas being measured. A detector measures the energy after the infrared energy has passed through the gas to be measured. This is compared to the energy at reference condition of no absorption.

Many analyzers are wall-mounted devices intended for long-term, unattended gas monitoring. There are now analysers that measure a range of gases and are highly portable to be suitable for a wider range of geoscience applications. Fast response high-precision analyzers are widely used to measure gas emissions and ecosystem fluxes using eddy covariance method when used together with fast-response sonic anemometer.

In some analyzers, the reliability of measurements is enhanced by calibrating the analyzer at the reference condition and a known span concentration. If the air would interfere with measurements, the chamber that houses the energy source is filled with a gas that has no detectable concentration of the gas being measured. Depending on the gas being measured, fresh air, chemically stripped air or nitrogen may be used.

See also

References

  • U.S. Patent 5,055,688
  • U.S. Patent 3,898,462
  • Auble, D.L.; Meyers, T.P. (1992). "An open path, fast response infrared absorption gas analyzer for H2O and CO2". Boundary-Layer Meteorology 59(3):243–256. doi:10.1007/BF00119815
This page was last edited on 13 November 2022, at 23:33
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