Thermal Effects on Physical Properties of Materials

2017 ◽  
pp. 123-128
Author(s):  
Mario Di Giovanni
Keyword(s):  
Physical Properties ◽  
Thermal Effects ◽  
Properties Of Materials

Experimental charge-density analysis towards predictive materials science

2021 ◽  
Vol 4 (03) ◽  
pp. 50-71
Author(s):  
Leonardo Dos Santos ◽  
Bernardo L. Rodrigues ◽  
Camila B. Pinto
Keyword(s):  
Physical Properties ◽  
Charge Density ◽  
Materials Science ◽  
New Materials ◽  
Wide Applicability ◽  
Density Analysis ◽  
Properties Of Materials ◽  
A Charge ◽  
Experimental Charge Density

The ongoing increase in the number of experimental charge-density studies can be related to both the technological advancements and the wide applicability of the method. Regarding materials science, the understanding of bonding features and their relation to the physical properties of materials can not only provide means to optimize such properties, but also to predict and design new materials with the desired ones. In this tutorial, we describe the steps for a charge-density analysis, emphasizing the most relevant features and briefly discussing the applications of the method.

Physical properties of materials derived from diamondoid molecules

2014 ◽  
Vol 78 (1) ◽  
pp. 016501 ◽  
Author(s):  
W A Clay ◽  
J E P Dahl ◽  
R M K Carlson ◽  
N A Melosh ◽  
Z-X Shen
Keyword(s):  
Physical Properties ◽  
Properties Of Materials

Thermal effects on the physical properties of limestone from the Yucatan Peninsula

2014 ◽  
Vol 1611 ◽  
pp. 171-176
Author(s):  
W.S. Gónzalez-Gómez ◽  
J. May-Crespo ◽  
P. Quintana ◽  
A. May-Pat ◽  
F. Avilés ◽  
...  
Keyword(s):  
Physical Properties ◽  
Thermal Effects ◽  
Yucatan Peninsula ◽  
Industrial Applications ◽  
Thermal Treatments ◽  
Matrix Cracks ◽  
Compression Strain ◽  
Yucatán Peninsula ◽  
Limestone Rock ◽  
Loss Of Mass

ABSTRACTRocks are composed of minerals, bounding matrix, cracks and pores. The study of changes in the physical properties of rocks as a function of heat treatment is relevant to various engineering and industrial applications. The effect of thermal damage on the compression, strength, ultimate compression strain, color and loss of mass of two different limestones extracted from the Yucatan Peninsula is studied. Different thermal treatments are applied by heating the sample from room temperature up to 600°C, with steps of 100°C. The results show a high correlation between the heat transport characteristics, mechanical properties, content of organic matter and the presence of carbonates and iron oxides in each type of limestone rock.

scholarly journals Transient Thermal Effects in Sedimentary Basins with Normal Faults and Magmatic Sill Intrusions—A Sensitivity Study

Geosciences ◽  
2019 ◽  
Vol 9 (4) ◽  
pp. 160 ◽  
Author(s):  
Magnhild Sydnes ◽  
Willy Fjeldskaar ◽  
Ivar Grunnaleite ◽  
Ingrid Fjeldskaar Løtveit ◽  
Rolf Mjelde
Keyword(s):  
Physical Properties ◽  
Thermal Effects ◽  
Sedimentary Basins ◽  
Sensitivity Study ◽  
Fault Slip ◽  
Structural Development ◽  
Potential Source Rock ◽  
Magmatic Intrusions ◽  
Transient Thermal ◽  
Magmatic Sill

Magmatic intrusions affect the basin temperature in their vicinity. Faulting and physical properties of the basin may influence the magnitudes of their thermal effects and the potential source rock maturation. We present results from a sensitivity study of the most important factors affecting the thermal history in structurally complex sedimentary basins with magmatic sill intrusions. These factors are related to faulting, physical properties, and restoration methods: (1) fault displacement, (2) time span of faulting and deposition, (3) fault angle, (4) thermal conductivity and specific heat capacity, (5) basal heat flow and (6) restoration method. All modeling is performed on the same constructed clastic sedimentary profile containing one normal listric fault with one faulting event. Sills are modeled to intrude into either side of the fault zone with a temperature of 1000 °C. The results show that transient thermal effects may last up to several million years after fault slip. Thermal differences up to 40 °C could occur for sills intruding at time of fault slip, to sills intruding 10 million years later. We have shown that omitting the transient thermal effects of structural development in basins with magmatic intrusions may lead to over- or underestimation of the thermal effects of magmatic intrusions and ultimately the estimated maturation.

scholarly journals Esterases affect the physical properties of materials used to seal the endodontic space

2019 ◽  
Vol 35 (8) ◽  
pp. 1065-1072
Author(s):  
M.Q. Marashdeh ◽  
S. Friedman ◽  
C. Lévesque ◽  
Y. Finer
Keyword(s):  
Physical Properties ◽  
Properties Of Materials ◽  
Materials Used
Sign in / Sign up

Export Citation Format

Share Document