<abstract xmlns="http://www.w3.org/1999/xhtml">

<p>Many characteristics of capillary-porous materials, including limestones and dolomites, depend on the structure of the pore space of a given material, so the article attempts to accurately determine the geometric characteristics of pores and their ability to transport water. Much information on the pore structure of carbonate rocks can be obtained from literature studies. There is a lack of information on the use of full hysteresis dilatometric thermoporometry methods for this purpose, as well as the fusion of differential analysis of volumetric strain (DAVS) results with mercury intrusion porosimetry (MIP) results.</p>
<p>The subject of the research presented in this article is the analysis of pore structure in carbonate rocks using the method of differential analysis of volumetric strain and mercury intrusion porosimetry. Based on the measurements made, the pore size, pore volume, content of empty pores and pores containing water incapable of phase transformation were analyzed. The geometry of mesopores of rock samples examined by differential analysis of volumetric strain and mercury intrusion porosimetry was compared. A fusion of the distribution of mesopores from the DAVS study with a part of the distribution of meso- and macropores obtained by the MIP study was performer.</p>
</abstract>

Many characteristics of capillary-porous materials, including limestones and dolomites, depend on the structure of the pore space of a given material, so the article attempts to accurately determine the geometric characteristics of pores and their ability to transport water. Much information on the pore structure of carbonate rocks can be obtained from literature studies. There is a lack of information on the use of full hysteresis dilatometric thermoporometry methods for this purpose, as well as the fusion of differential analysis of volumetric strain (DAVS) results with mercury intrusion porosimetry (MIP) results.
The subject of the research presented in this article is the analysis of pore structure in carbonate rocks using the method of differential analysis of volumetric strain and mercury intrusion porosimetry. Based on the measurements made, the pore size, pore volume, content of empty pores and pores containing water incapable of phase transformation were analyzed. The geometry of mesopores of rock samples examined by differential analysis of volumetric strain and mercury intrusion porosimetry was compared. A fusion of the distribution of mesopores from the DAVS study with a part of the distribution of meso- and macropores obtained by the MIP study was performer.

Fusion of Differential Analysis of Volumetric Strain Method (Dilatometric Thermoporometry) and Mercury Intrusion Porosimetry Method for Pore Space Characterization in Carbonate Rocks

Structure and Environment

This work is licensed under the Creative Commons Attribution 3.0 Public License.

Many characteristics of capillary-porous materials, including limestones and dolomites, depend on the structure of the pore space of a given material, so the...

Fusion of Differential Analysis of Volumetric Strain Method (Dilatometric Thermoporometry) and Mercury Intrusion Porosimetry Method for Pore Space Characterization in Carbonate Rocks

Publié en ligne: 26 juil. 2023

Pages: 90 - 98

DOI: https://doi.org/10.30540/sae-2023-009

Mots clés
differential analysis of volumetric strain method, mercury intrusion porosimetry, carbonate rocks, pore space

© 2023 Karol Skowera, published by Sciendo

This work is licensed under the Creative Commons Attribution 3.0 Public License.

Fusion of Differential Analysis of Volumetric Strain Method (Dilatometric Thermoporometry) and Mercury Intrusion Porosimetry Method for Pore Space Characterization in Carbonate Rocks

Publié en ligne: 26 juil. 2023

Pages: 90 - 98

DOI: https://doi.org/10.30540/sae-2023-009

Mots clésdifferential analysis of volumetric strain method, mercury intrusion porosimetry, carbonate rocks, pore space

© 2023 Karol Skowera, published by Sciendo

This work is licensed under the Creative Commons Attribution 3.0 Public License.

Mots clés
differential analysis of volumetric strain method, mercury intrusion porosimetry, carbonate rocks, pore space