![]() |
|
![]() |
#1 |
Member
Join Date: May 2006
Posts: 7,048
|
![]()
Quite frankly BSM, I don`t want to do it at all.
I believe I can mostly identify meteoritic material by recognising the origin, method of construction, and probable maker of a blade, and then using the "touch test"---the stuff does feel a little bit different to other materials used as pamor. I`ve been posing the question all these years because I`ve sometimes thought it might be a good academic exercise to put together a sampling of blades that recognised Javanese experts considered contained meteoritic material, and seeing just how good the indicators that have been used were. The mix is not at all homogenous. Its layers upon layers upon layers. You could probably test 20 different spots before you struck a square 1/8 inch that actually had meteoritic material in it. On the types of blades that I know contain meteoritic material I could not imagine any keris fancier approving the polish of even one section of 1/8 by 1/8 inch.You probably could ID a section of material that waslikely to contain meteoritic material though. That would probably reduce the number of tests needed. A normal Javanese keris blade is going to run about 16 inches, including the tang. But tell me this:- those trace elements that you would be looking for:- are they still going to be there after the material has gone through many, many weld heats? |
![]() |
![]() |
![]() |
#2 | |
Member
Join Date: Nov 2005
Posts: 189
|
![]() Quote:
Iron meteorites are full of the non-volatile stuff that didn't burn off during the birth of the solar system, and was too heavy to float away from the center of the new-born planets/asteriods - I bet a few minutes at 2300 F would have little effect. Thanks for that very good synopsis of the ebay auction copy, BSMStar! I'm curious about what levels of these trace elements are in commercial steel, now...time to do some research... ![]() |
|
![]() |
![]() |
![]() |
#3 |
Member
Join Date: Nov 2005
Posts: 189
|
![]()
Perhaps a better way -
Take a couple months going through the various reference material standards for steels on the web, pulling out the info on the few for which there is trace element data. Do the same for iron meteorites. Pick a couple trace elements that aren't typically manipulated in steel production, say Ag, Au, As, Ge, Ta, Zr, Hf, La; the earth steels should plot in one area (or along a single line) when comparing two elements, meteoric metal in one or more areas outside or overlapping - the 'right' pair of elements should allow good discrimination. You might be able to get the same result by comparing Ni to Co, or P to S; but since those are manipulated elements they might not graph well. Get a keris tested, it should fall between the two areas, if it's a mix of the two metals - and you've only paid for one lab test! You'll have to put in some hours with the Excel program's chart function, though ![]() Bonus, you could publish an article in a scientific journal or popular magazine once you're done! http://www.nist.gov/srm |
![]() |
![]() |
![]() |
#4 |
Member
Join Date: Dec 2004
Location: Europe
Posts: 2,718
|
![]()
Hi Jeff,
For one who knows something about what you describe, it sounds plausible that the way you describe it will work very well – I don’t know anything about it ![]() |
![]() |
![]() |
![]() |
#5 |
Member
Join Date: Nov 2005
Posts: 189
|
![]()
You'd have to sample carefully, but since we are limiting the discussion to non-destructive techniques, I think EMP or XRF (X-ray flourescence) are the only options. Both of those techniques can be aimed, so you could (with EMP, at least) get measurements of the different layers in the pamor. I'm not sure how small an area XRF samples, but they use it on artifacts in museums, so it's very non-destructive. The trace elements are uniformly distributed through the metals, so you'd only have to take into account the mix of the two metals in the folding process, and sample accordingly...
...or so I think! ![]() ![]() INAA (or EMP or XRF) would be good if you could take some filings off the end of a tang, but then you couldn't be sure the tang was the same metal as the pamor, and you'd have potential issues. |
![]() |
![]() |
![]() |
#6 | |||
Member
Join Date: Jan 2005
Location: Kansas City, MO USA
Posts: 312
|
![]() Quote:
Quote:
Quote:
Jens... I hope I addressed your question too. Last edited by BSMStar; 5th August 2006 at 06:38 PM. |
|||
![]() |
![]() |
![]() |
#7 |
Member
Join Date: Jan 2005
Location: Kansas City, MO USA
Posts: 312
|
![]()
I you are hard core on trace... try this link.
![]() http://www.metbase.de/description/an...tsinirons.html |
![]() |
![]() |
![]() |
#8 |
Member
Join Date: May 2006
Posts: 7,048
|
![]()
As I write this I am looking at a keris that I made the pamor material for. It was made from meteoritic material from Arizona, and the concentration of this material is pretty rich. About the largest area of this pamor that I could definitely identify as solid, uninterrupted meteoritic material, is approx. 1.5 mm. That`s near enough to the 1/8 inch we were talking about, so if the size of the keris itself doesn`t rule it out, and taking into account the other factors that have been addressed, it would seem to be physically possible to analyse a keris blade and determine if meteoritic material had been used in its manufacture.
The "what can I make from it" factor is not a part of this discussion. As I have already stated, my interest in this purely academic, as has been my continuing interest since 1988 in the metallurgical analysis of old and archaic keris in order to determine composition and techniques used in manufacture. The market value of any keris, even those at the top of the market, would not be sufficiently increased by a positive ID of meteoritic material to come anywhere near covering what would appear to be the cost of testing. The whole thing is simply an interesting question that has grown out of a folk belief, or perhaps we should say "item of faith" that has entered the Javanese keris belief system since the Prambanan meteorite was used in the manufacture of keris in Central Jawa, in the early 1800's. This was addressed by Bronson in his 1987 paper:- "Terrestrial and Meteoritic Nickel in the Indonesian Keris". However, technology has moved along a bit in the last 20 years, and it seems that we now have the means that Bronson did not have to be able to provide definite ID . Now all we need is somebody with access to equipment, interest, funding, and of course, access to samples. Bring all these things together, and somebody could produce a landmark paper. Actually, Haryono Arumbinang carried out an analysis on some old keris, in Jogja, in , I think, 1983. I do not have the results of this analysis to hand, but I have got them around somewhere. Regretably the interpretation of his analysis has been badly distorted by people not equipped to interpret it. |
![]() |
![]() |
![]() |
|
|