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An instrument which measures concentrati...

An instrument which measures concentration of `C-14` directly is

A

Accelerator mass spectrometer

B

Spectroscopy

C

Geiger counter

D

All the above.

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The correct Answer is:
To determine the instrument that measures the concentration of Carbon-14 (C-14) directly, we can analyze the options provided: 1. **Understanding Carbon-14 Measurement**: Carbon-14 is a radioactive isotope of carbon used in radiocarbon dating. The measurement of C-14 concentration is crucial in various fields, including archaeology, geology, and environmental science. 2. **Evaluating the Options**: - **Accelerator**: This term is too vague and does not specifically refer to a device that measures C-14. - **Mass Spectrometer**: This is a device that can measure isotopes, including C-14, but it does not do so directly in the context of radiocarbon dating. - **Spectroscopy**: This technique studies the interaction between matter and electromagnetic radiation and is not specifically used for measuring C-14 concentration. - **Giga Counter**: This instrument detects and measures ionizing radiation but is not specifically designed for measuring C-14 concentration. - **Accelerator Mass Spectrometer (AMS)**: This is a specific type of mass spectrometer that accelerates ions to high kinetic energies before mass analysis. AMS is particularly powerful in separating rare isotopes like C-14 from more abundant isotopes. 3. **Conclusion**: The correct instrument for measuring the concentration of C-14 directly is the **Accelerator Mass Spectrometer**. ### Step-by-Step Solution: 1. Identify the need to measure C-14 concentration. 2. Review the options provided. 3. Analyze each option to determine its relevance to measuring C-14. 4. Conclude that the **Accelerator Mass Spectrometer** is the most suitable instrument for this purpose.
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Carbon -14 used to determine the age of organic material. The procedure is absed on the formation of C^(14) by neutron capture iin the upper atmosphere. ._(7)N^(14)+._(0)n^(1) rarr ._(6)C^(14)+._(1)H^(1) C^(14) is absorbed by living organisms during photosynthesis. The C^(14) content is constant in living organism. Once the plant or animal dies, the uptake of carbon dioxide by it ceases and the level of C^(14) in the dead being falls due to the decay, which C^(14) undergoes. ._(6)C^(14)rarr ._(7)N^(14)+beta^(c-) The half - life period of C^(14) is 5770 year. The decay constant (lambda) can be calculated by using the following formuls : lambda=(0.693)/(t_(1//2)) The comparison of the beta^(c-) activity of the dead matter with that of the carbon still in circulation enables measurement of the period of the isolation of the material from the living cycle. The method, however, ceases to be accurate over periods longer than 30000 years. The proportion of C^(14) to C^(12) in living matter is 1:10^(12) . A nuclear explosion has taken place leading to an increase in the concentration of C^(14) in nearby areas. C^(14) concentration is C_(1) in nearby areas and C_(2) in areas far away. If the age of the fossil is determined to be T_(1) and T_(2) at the places , respectively, then

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