DLB-X7
Materials
- Nov 23, 2021
- 3
Hi Everyone,
I am hoping someone can help me understand the below - metallurgically and on a nanoscience stand point -
Material 1020 - ASTM A105
Normalized from the "as forged condition"
Normalize Temperature 1650F
Surface contact Thermocouple - 45 Minutes at temperature.
Preheated furnace - Furnace with ramp 100 F per hour from 1600F to 1650F (Below 1600F no ramp)
Cooling, Enclosed air chamber with fan for controlled atmosphere cooling
Furnace certified AMS2750 Latest revision Class 5
Furnace Atmosphere Nitrogen
ASTM - A370,E23 V-Notch Impact Testing
@-50F
Test 1 Ft/lbs 54,20,10 Lateral (in.) .053, .025, .014 Shear% 70, 90, 100
Test 2 180 deg from 1st Test, around 30" in dia. Ft/lbs 49,66,16 Lateral (in.) .049, .063, .018 Shear% 80, 70, 100
As you can see the values are anything but consistent
Standard size Tensile ASTM E8 - Tensile 71.7 KSI, Yield 44.0 KSI, Elong% 38, RA% 67
Material is machined to size - Thickest cross section 1.5 inches with no odd geometry.
Normally I conduct thermal processing at 1 hour per inch of thickness. Material is usually oversized to allow for oxidation and decarburization then machined after thermal processing. I have reduced soak time to minimize the depth of decarburization on the material surface.
Being 1.5 inches - Surface temperature of the material at 1650 F for 45 minutes - I am not really comprehending how the core is not at least at or above the critical A3 temperature for this material. Homogeneous Austenite for low carbon steel should take a short amount of minutes for the final disappearance of Carbon concentration Gradients around 1550 F and above that temperature within seconds "with composition in consideration". Prior microstructure is pearlite with fairly fine but, mixed grain size being that the material was in the "as forged condition" still air cooled to ambient.
We all understand how grains are formed during heating and how the FCC structure of "austenite" is formed - A1 and A3 and what there roll is in the carbon phase diagram and how grains are formed during a still air cooling along with the formation of pearlite, Fe-Fe3C and Ferrite microstructure.
I have studied steels in an atomic level perspective, with many studies on theories of pearlite, in-depth martensite transformations along with lattice structures and crystal defects for many years along with the heat treatment of many variety of steels each there own thermal processing. I deal with ASTM, API and critical 20E, 20F specifications. I am looking for a scientific theory along with hopefully a referenced, thesis, theory, book or law that would shed some light on why this anomaly in the impact testing is occurring.
The remedy for my situation is hopefully just increase soak time and test again however, what I am looking for is an in-depth perspective on what exactly may be happening or direction to literature that may be relevant. I can not visualize what is happening "I am probably just missing something simple that I am not thinking of however, I have not had any luck on finding in-depth information on what might be happening within the material and during the fracture.
If Soak was not long enough for full Austenitization
Microstructure was Pearlite and ferrite
Partial Austenitization
Inter-critical Spheroidlizing
Austenitizing grains cooled to form pearlite
I am thinking associated microstructures should show relatively high absorption of energy before fracture. Both Impact test specimens are taken at the same depth in the material.
Equalization of surface and core temperature is not really the information I am trying to find, it is what we want and need for the quality of the product however, nucleation and the growth of grains whithin a material does not happen at any one exact set temperature. Atomic movement happens throughout the entire range of temperatures - Composition matters, Temperature and Time matters.
The material processed and question is strictly academic and not for Production.
Thanks in advance for any input on this topic.
I am hoping someone can help me understand the below - metallurgically and on a nanoscience stand point -
Material 1020 - ASTM A105
Normalized from the "as forged condition"
Normalize Temperature 1650F
Surface contact Thermocouple - 45 Minutes at temperature.
Preheated furnace - Furnace with ramp 100 F per hour from 1600F to 1650F (Below 1600F no ramp)
Cooling, Enclosed air chamber with fan for controlled atmosphere cooling
Furnace certified AMS2750 Latest revision Class 5
Furnace Atmosphere Nitrogen
ASTM - A370,E23 V-Notch Impact Testing
@-50F
Test 1 Ft/lbs 54,20,10 Lateral (in.) .053, .025, .014 Shear% 70, 90, 100
Test 2 180 deg from 1st Test, around 30" in dia. Ft/lbs 49,66,16 Lateral (in.) .049, .063, .018 Shear% 80, 70, 100
As you can see the values are anything but consistent
Standard size Tensile ASTM E8 - Tensile 71.7 KSI, Yield 44.0 KSI, Elong% 38, RA% 67
Material is machined to size - Thickest cross section 1.5 inches with no odd geometry.
Normally I conduct thermal processing at 1 hour per inch of thickness. Material is usually oversized to allow for oxidation and decarburization then machined after thermal processing. I have reduced soak time to minimize the depth of decarburization on the material surface.
Being 1.5 inches - Surface temperature of the material at 1650 F for 45 minutes - I am not really comprehending how the core is not at least at or above the critical A3 temperature for this material. Homogeneous Austenite for low carbon steel should take a short amount of minutes for the final disappearance of Carbon concentration Gradients around 1550 F and above that temperature within seconds "with composition in consideration". Prior microstructure is pearlite with fairly fine but, mixed grain size being that the material was in the "as forged condition" still air cooled to ambient.
We all understand how grains are formed during heating and how the FCC structure of "austenite" is formed - A1 and A3 and what there roll is in the carbon phase diagram and how grains are formed during a still air cooling along with the formation of pearlite, Fe-Fe3C and Ferrite microstructure.
I have studied steels in an atomic level perspective, with many studies on theories of pearlite, in-depth martensite transformations along with lattice structures and crystal defects for many years along with the heat treatment of many variety of steels each there own thermal processing. I deal with ASTM, API and critical 20E, 20F specifications. I am looking for a scientific theory along with hopefully a referenced, thesis, theory, book or law that would shed some light on why this anomaly in the impact testing is occurring.
The remedy for my situation is hopefully just increase soak time and test again however, what I am looking for is an in-depth perspective on what exactly may be happening or direction to literature that may be relevant. I can not visualize what is happening "I am probably just missing something simple that I am not thinking of however, I have not had any luck on finding in-depth information on what might be happening within the material and during the fracture.
If Soak was not long enough for full Austenitization
Microstructure was Pearlite and ferrite
Partial Austenitization
Inter-critical Spheroidlizing
Austenitizing grains cooled to form pearlite
I am thinking associated microstructures should show relatively high absorption of energy before fracture. Both Impact test specimens are taken at the same depth in the material.
Equalization of surface and core temperature is not really the information I am trying to find, it is what we want and need for the quality of the product however, nucleation and the growth of grains whithin a material does not happen at any one exact set temperature. Atomic movement happens throughout the entire range of temperatures - Composition matters, Temperature and Time matters.
The material processed and question is strictly academic and not for Production.
Thanks in advance for any input on this topic.