Re: [meteorite-list] What is and isn't a Widmanstatten Pattern was Cooling rates

2009-09-21 Thread Jeff Grossman

I think there are some misconceptions here, although this is not my
specialty.  Most of the metallic minerals in iron meteorites are
described as "alloys" in that they are composed of various metals
combined together.  These alloys have specific structures, e.g., the
metal atoms in kamacite are arranged in a body-centered cubic structure
and those in taenite are face-centered cubic.  The minerals Kamacite and
taenite are solid solutions of mainly Fe and Ni which can have a range
of compositions without altering the basic structure.  Tetrataenite is
another alloy, but this time with a fixed composition (FeNi) and an
ordered structure.

Formation of the Widmanstatten structure is pretty well understood.  It
does not happen as the metal cools from the liquid state and
solidifies.  That process leads to the formation of just taenite.  Only
when the alloy cools to much lower temperature, after it is completely
solid, can the Widmanstatten pattern form.   High pressures are not
involved. Goldstein and coworkers have shown that the process is
controlled by the Fe-Ni-P phase diagram.  Depending on the exact
composition of the alloy, a variety of phase transformations take place
over a range of temperatures, ultimately leading to the formation of
kamacite and taenite. Composition and cooling rate play roles in
determining in the structures we now observe.  You can read about it in:
http://articles.adsabs.harvard.edu/full/2005M%26PS...40..239Y

jeff

Mr EMan wrote:

We had a metallurgist on the list a few years back that insisted Widmanstatten patterns were found 
everywhere and posted some micrographs supporting his assertion.  As I recall he got very ill with 
us when we pointed out why, what he had photos of, weren't Widmanstatten patterns. It was focused 
on a physical "casual" similarity not "causal" chemistry.

Once again Widmanstatten patterns aren't stress fractures nor alloy specific 
patterns. I further assert that metal in meteorites is NOT an alloy in that the 
nickel is in a specific locus within a molecule. It is therefore not a mixture 
but a compound, chemically speaking.

Widmanstatten patterns are a cross-sectional view of crystal latices that 
result from the migration of nickel atoms over eons into two distinct unusual, 
zoned, crystalline arrangements. Bandwidth is actually plate thickness. The 
migration is chemically driven while the metal is molten and only occurs in a 
specific range of temperatures. This is a subtle but distinct difference. This 
migration may even be a molecule by molecule transfer of nickel atoms which 
takes millions of years to clear out a 3mm band. This is to say a nickel atom 
may move in one side of a molecule and forces the central nickel atom to the 
face and lacking stability is ejected out the other side--maybe not, as the 
actual displacement/sorting is still an enigma.  The nickel iron content may 
assemble from a single form as it accretes and represent a move to homogeneity 
interupted when the mass ran out of thermal energy.  It may all start out as 
taenite and part of it converts to
 kamacite or vice versa. Who really knows? 

I fully believe collisions would impede if not stop the process-- not speed it up.  It is easy and natural to try to infer a similar pattern might be from a similar process but the only similarity is in low contrast photographs when the scale is ignored.  


Elton

--- On Sun, 9/6/09, E.P. Grondine  wrote:

  

From: E.P. Grondine 
Subject: Re: [meteorite-list] Cooling rates
To: meteorite-list@meteoritecentral.com, "Steve Dunklee" 

Date: Sunday, September 6, 2009, 1:47 PM
Hi Steve, all - 

I don't think they're due to repeated collisions. 


Suppose that we have molten iron/nickle under incredible
compression, which is then almost instantaneously released.



  

250 parent bodies seems like a lot. Perhaps instead there
was more differentiation within fewer parent bodies.

Ed


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Re: [meteorite-list] What is and isn't a Widmanstatten Pattern was Cooling rates

2009-09-21 Thread Jeff Grossman
I'd like to correct what I said two weeks back about alloys.  I've 
talked with a specialist (Joe Goldstein) and he clarified the 
terminology for me as material scientists would use it.


An "alloy" refers to a batch of metal containing more than one element 
(only one of which needs to be a metallic element).  The term carries no 
implications about how the mixture formed or what its structure is. 

The term "alloy" should not be used to refer to a specific phase that 
crystallizes from an alloy or is present in the alloy.  Taenite and 
kamacite are not alloys.  They are phases (minerals). Therefore, 
hundreds of websites (including some professional ones) use the term 
incorrectly.  An iron meteorite IS an alloy, even if it only contains 
one phase like taenite. Alloys can and often are composed of crystalline 
phases.


Jeff

Mr EMan wrote:

--- On Mon, 9/7/09, Jeff Grossman  wrote:
 <"alloys" in that they are composed of various metals combined together.>> 


I understood the distinction was that the Fe Ni formed a "chemical compound" 
not merely a mixture like copper and tin to make brass but even brass can form 
crystalline plates so that may be a bad example. It was my understanding that were it not 
for the mineral structure The Fe-Ni would be called an alloy.  Agreed that it is 
frequently discussed in terms of alloy.

 <>

I stand corrected, 30 years is a lot of facts to keep in just one's head. I did 
recall correctly that there is a temperature range and below which all 
translocation stops. Seems off the top of my head it is 800°C.

<>. 


I have long suspected that phosphorus was a key component in the 
process--likely as a catalyst.  The Schreibersite seems to exist largely at the 
boundaries in thin laminae even surrounding trolite nodules.  I look forward to 
reading Goldstein's paper.

Thanks again,
Elton

  



--
Dr. Jeffrey N. Grossman   phone: (703) 648-6184
US Geological Survey  fax:   (703) 648-6383
954 National Center
Reston, VA 20192, USA


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Re: [meteorite-list] What is and isn't a Widmanstatten Pattern was Cooling rates

2009-09-08 Thread Mr EMan
I guess once again as with CCDs my education is outdated.  I see that any metal 
compound or mixture can be called an alloy. OR it has come into such common use 
the distinction between mixture and compound is obsolete when talking about 
metals.

Elton

--- On Tue, 9/8/09, Mr EMan  wrote:

> From: Mr EMan 
> Subject: Re: [meteorite-list] What is and isn't a Widmanstatten Pattern was 
> Cooling rates
> To: "Meteorite-list" , "Jeff Grossman" 
> 
> Date: Tuesday, September 8, 2009, 6:38 PM
> --- On Mon, 9/7/09, Jeff Grossman
> 
> wrote:
>  < are described as
> "alloys" in that they are composed of various metals
> combined together.>> 
> 
> I understood the distinction was that the Fe Ni formed a
> "chemical compound" not merely a mixture like copper and tin
> to make brass but even brass can form crystalline plates so
> that may be a bad example. It was my understanding that were
> it not for the mineral structure The Fe-Ni would be called
> an alloy.  Agreed that it is frequently discussed in
> terms of alloy.
> 
>  < liquid state and solidifies.>>
> 
> I stand corrected, 30 years is a lot of facts to keep in
> just one's head. I did recall correctly that there is a
> temperature range and below which all translocation stops.
> Seems off the top of my head it is 800°C.
> 
> < is controlled by the Fe-Ni-P phase diagram>>. 
> 
> I have long suspected that phosphorus was a key component
> in the process--likely as a catalyst.  The
> Schreibersite seems to exist largely at the boundaries in
> thin laminae even surrounding trolite nodules.  I look
> forward to reading Goldstein's paper.
> 
> Thanks again,
> Elton
> __
> http://www.meteoritecentral.com
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Re: [meteorite-list] What is and isn't a Widmanstatten Pattern was Cooling rates

2009-09-08 Thread Mr EMan
--- On Mon, 9/7/09, Jeff Grossman  wrote:
 <> 

I understood the distinction was that the Fe Ni formed a "chemical compound" 
not merely a mixture like copper and tin to make brass but even brass can form 
crystalline plates so that may be a bad example. It was my understanding that 
were it not for the mineral structure The Fe-Ni would be called an alloy.  
Agreed that it is frequently discussed in terms of alloy.

 <>

I stand corrected, 30 years is a lot of facts to keep in just one's head. I did 
recall correctly that there is a temperature range and below which all 
translocation stops. Seems off the top of my head it is 800°C.

<>. 

I have long suspected that phosphorus was a key component in the 
process--likely as a catalyst.  The Schreibersite seems to exist largely at the 
boundaries in thin laminae even surrounding trolite nodules.  I look forward to 
reading Goldstein's paper.

Thanks again,
Elton
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Re: [meteorite-list] What is and isn't a Widmanstatten Pattern was Cooling rates

2009-09-07 Thread Tom Randall (KB2SMS)


Excellent article and info! Thank you Jeff!

Tom

---
"I don't like country music, but I don't mean to denigrate those who  
do. And for the people who like country music, denigrate means 'put  
down.'"  -- Bob Newhart


http://home.roadrunner.com/~kb2sms/

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Re: [meteorite-list] What is and isn't a Widmanstatten Pattern was Cooling rates

2009-09-07 Thread Jeff Grossman
I think there are some misconceptions here, although this is not my 
specialty.  Most of the metallic minerals in iron meteorites are 
described as "alloys" in that they are composed of various metals 
combined together.  These alloys have specific structures, e.g., the 
metal atoms in kamacite are arranged in a body-centered cubic structure 
and those in taenite are face-centered cubic.  The minerals Kamacite and 
taenite are solid solutions of mainly Fe and Ni which can have a range 
of compositions without altering the basic structure.  Tetrataenite is 
another alloy, but this time with a fixed composition (FeNi) and an 
ordered structure.


Formation of the Widmanstatten structure is pretty well understood.  It 
does not happen as the metal cools from the liquid state and 
solidifies.  That process leads to the formation of just taenite.  Only 
when the alloy cools to much lower temperature, after it is completely 
solid, can the Widmanstatten pattern form.   High pressures are not 
involved. Goldstein and coworkers have shown that the process is 
controlled by the Fe-Ni-P phase diagram.  Depending on the exact 
composition of the alloy, a variety of phase transformations take place 
over a range of temperatures, ultimately leading to the formation of 
kamacite and taenite. Composition and cooling rate play roles in 
determining in the structures we now observe.  You can read about it in: 
http://articles.adsabs.harvard.edu/full/2005M%26PS...40..239Y


jeff

Mr EMan wrote:

We had a metallurgist on the list a few years back that insisted Widmanstatten patterns were found 
everywhere and posted some micrographs supporting his assertion.  As I recall he got very ill with 
us when we pointed out why, what he had photos of, weren't Widmanstatten patterns. It was focused 
on a physical "casual" similarity not "causal" chemistry.

Once again Widmanstatten patterns aren't stress fractures nor alloy specific 
patterns. I further assert that metal in meteorites is NOT an alloy in that the 
nickel is in a specific locus within a molecule. It is therefore not a mixture 
but a compound, chemically speaking.

Widmanstatten patterns are a cross-sectional view of crystal latices that 
result from the migration of nickel atoms over eons into two distinct unusual, 
zoned, crystalline arrangements. Bandwidth is actually plate thickness. The 
migration is chemically driven while the metal is molten and only occurs in a 
specific range of temperatures. This is a subtle but distinct difference. This 
migration may even be a molecule by molecule transfer of nickel atoms which 
takes millions of years to clear out a 3mm band. This is to say a nickel atom 
may move in one side of a molecule and forces the central nickel atom to the 
face and lacking stability is ejected out the other side--maybe not, as the 
actual displacement/sorting is still an enigma.  The nickel iron content may 
assemble from a single form as it accretes and represent a move to homogeneity 
interupted when the mass ran out of thermal energy.  It may all start out as 
taenite and part of it converts to
 kamacite or vice versa. Who really knows? 

I fully believe collisions would impede if not stop the process-- not speed it up.  It is easy and natural to try to infer a similar pattern might be from a similar process but the only similarity is in low contrast photographs when the scale is ignored.  


Elton

--- On Sun, 9/6/09, E.P. Grondine  wrote:

  

From: E.P. Grondine 
Subject: Re: [meteorite-list] Cooling rates
To: meteorite-list@meteoritecentral.com, "Steve Dunklee" 

Date: Sunday, September 6, 2009, 1:47 PM
Hi Steve, all - 

I don't think they're due to repeated collisions. 


Suppose that we have molten iron/nickle under incredible
compression, which is then almost instantaneously released.



  

250 parent bodies seems like a lot. Perhaps instead there
was more differentiation within fewer parent bodies.

Ed


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US Geological Survey  fax:   (703) 648-6383
954 National Center
Reston, VA 20192, USA



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Re: [meteorite-list] What is and isn't a Widmanstatten Pattern was Cooling rates

2009-09-06 Thread Mr EMan
We had a metallurgist on the list a few years back that insisted Widmanstatten 
patterns were found everywhere and posted some micrographs supporting his 
assertion.  As I recall he got very ill with us when we pointed out why, what 
he had photos of, weren't Widmanstatten patterns. It was focused on a physical 
"casual" similarity not "causal" chemistry.

Once again Widmanstatten patterns aren't stress fractures nor alloy specific 
patterns. I further assert that metal in meteorites is NOT an alloy in that the 
nickel is in a specific locus within a molecule. It is therefore not a mixture 
but a compound, chemically speaking.

Widmanstatten patterns are a cross-sectional view of crystal latices that 
result from the migration of nickel atoms over eons into two distinct unusual, 
zoned, crystalline arrangements. Bandwidth is actually plate thickness. The 
migration is chemically driven while the metal is molten and only occurs in a 
specific range of temperatures. This is a subtle but distinct difference. This 
migration may even be a molecule by molecule transfer of nickel atoms which 
takes millions of years to clear out a 3mm band. This is to say a nickel atom 
may move in one side of a molecule and forces the central nickel atom to the 
face and lacking stability is ejected out the other side--maybe not, as the 
actual displacement/sorting is still an enigma.  The nickel iron content may 
assemble from a single form as it accretes and represent a move to homogeneity 
interupted when the mass ran out of thermal energy.  It may all start out as 
taenite and part of it converts to
 kamacite or vice versa. Who really knows? 

I fully believe collisions would impede if not stop the process-- not speed it 
up.  It is easy and natural to try to infer a similar pattern might be from a 
similar process but the only similarity is in low contrast photographs when the 
scale is ignored.  

Elton

--- On Sun, 9/6/09, E.P. Grondine  wrote:

> From: E.P. Grondine 
> Subject: Re: [meteorite-list] Cooling rates
> To: meteorite-list@meteoritecentral.com, "Steve Dunklee" 
> 
> Date: Sunday, September 6, 2009, 1:47 PM
> Hi Steve, all - 
> 
> I don't think they're due to repeated collisions. 
> 
> Suppose that we have molten iron/nickle under incredible
> compression, which is then almost instantaneously released.

> 250 parent bodies seems like a lot. Perhaps instead there
> was more differentiation within fewer parent bodies.
> 
> Ed
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