Error in measuring rock porosity by Archimedes method

In summary, the standard method for measuring the porosity of a rock involves saturating the pores with water and using Archimedes' principle to determine the volume. After drying the rock, the water weight lost is used to calculate the porosity. However, a major source of error is the need to blot the rock surface dry, as not doing it correctly can result in incorrect measurements. There is a desire for a publication that outlines the expected error from this method, and anyone with information or experience is welcome to share.
  • #1
Peter Persoff
4
0
The standard way to measure porosity of a rock is to get the pores completely saturated with water, then weigh the rock immersed in water and again in air (there are modified balances for this). Using Archimedes' principle, you then can determine the volume of the rock. Then you dry the rock completely and weigh it again (only in air). The water weight lost gives you the pore space in the rock. Divide this into the total volume and you get the porosity.

A major source of error is that when you weigh the rock after taking it out iof the water you have to blot the outside surface dry. Not dry enough and you are weighing some exterior water. Too dry and you will suck some of the water out of the pores and the rock is no longer saturated.

What I am looking for is a textbook or other publication that tells the amount of error to be expected from this source. Anyone with information or experience with this method is welcome to reply.
 
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  • #2
The standard way? What ever happened to mercury porosimeters?
 
  • #3


There are a few potential sources of error in using the Archimedes method to measure rock porosity. One major source, as mentioned in the content, is the potential for not properly drying the exterior surface of the rock. This could result in either over or underestimating the water weight lost and therefore the porosity of the rock.

Another potential source of error is the assumption that all pores are completely filled with water. In reality, some pores may be filled with air or other fluids, leading to an inaccurate measurement of the volume of the rock. Additionally, the method may not work well for rocks with very small or irregularly shaped pores.

As for the amount of error to be expected from these sources, it would likely vary depending on the specific characteristics of the rock being measured and the technique used. It would be best to consult a textbook or published study on the Archimedes method for rock porosity for more specific information. Alternatively, reaching out to experts in the field who have experience with this method may also provide valuable insights.
 

Related to Error in measuring rock porosity by Archimedes method

1. What is the Archimedes method for measuring rock porosity?

The Archimedes method is a technique used to measure the porosity of rocks by determining the volume of space occupied by fluid within the rock's pores. This is done by immersing the rock in a known volume of fluid and measuring the change in volume of the fluid. The difference in volume is equal to the volume of fluid displaced by the rock, which can then be used to calculate the porosity.

2. What are the sources of error in measuring rock porosity by Archimedes method?

Some common sources of error in measuring rock porosity using Archimedes method include: variations in the density of the fluid used, air bubbles trapped within the pores of the rock, and surface tension effects of the fluid. Inaccurate measurements of the rock's dimensions or the volume of fluid can also lead to errors in the porosity calculation.

3. How can we minimize errors when using the Archimedes method to measure rock porosity?

To minimize errors when using the Archimedes method, it is important to use a fluid with a consistent and known density, ensure that the rock is completely immersed in the fluid without any air bubbles, and accurately measure the dimensions of the rock and the volume of fluid. It is also recommended to repeat the measurements multiple times and take an average to reduce the impact of any individual errors.

4. Are there any limitations to using the Archimedes method for measuring rock porosity?

While the Archimedes method is a commonly used technique for measuring rock porosity, it does have some limitations. It may not be suitable for rocks with very small pores or complex pore structures, and it assumes that the fluid used is able to fully penetrate all of the pores in the rock. Additionally, the method may not be accurate for rocks that are highly fractured or contain significant amounts of non-porous material.

5. How can we validate the results obtained from the Archimedes method for measuring rock porosity?

To validate the results obtained from the Archimedes method, it is recommended to compare them with results from other porosity measurement techniques, such as mercury intrusion porosimetry or nuclear magnetic resonance (NMR). It is also important to consider the limitations and potential sources of error when interpreting the results and to repeat the measurements multiple times to ensure consistency.

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