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#1 |
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Hi Jeff and all,
Sorry I'm late to the discussion, but I'm not convinced that a microprobe would give a good answer to the percent of meteoric iron in a keris, especially an old one. The unobvious problem is that keris blades are occasionally cleaned with an arsenic (As) solution, so the researcher has to factor in the accumulation (if any) from cleaning. Since it's not pure arsenic in the Indonesian cleaning solutions, this would take some experimentation. The obvious problem is that the terrestrial iron isn't pure iron, nor is the carbon to make the steel pure carbon. There's going to be a mix of other trace elements that will have to be factored in. In old blades, the iron will not be to an industrial spec, but may have been smelted from ore in the village where the blade was made, or beaten together from recycled sources. Similarly,the carbon source can affect the trace element signature of the steel. For instance, coal picks up various heavy metals (such as mercury, the bane of the midwest US), and trees that are used to make charcoal typically accumulate some cesium (a byproduct of potassium metabolism), and some plants deliberately accumulate metals. As another example, one tree species in New Caledonia naturally accumulates so much nickel (as a chemical defense against herbivores) that the sap could be mined, if it was more common. Given that, in Indonesia, we're talking about one of the richest rainforest areas on the planet (i.e. lots of tree species), the tree species used into charcoal could affect the chemistry of the charcoal used to make the steel, affecting the chemical fingerprint of the resulting keris. Complex? Yup. The only solution I've come up with so far is to get two blades from the smith, one a tool with no meteoric iron, the other a keris with some putative meteoric iron, both forged at roughly the same time, so they have the same source materials, aside from the meteoritic component. Then you can factor out the terrestrial sources. After that, you have to determine how cleaning the keris with the arsenic solution affects that blade's chemistry. Once you've done that, you can actually say how much of the keris is meteoric. Bottom line, it will be difficult to predict or determine the trace element chemistry of the terrestrial component of keris, and without that information, it would be very, very difficult to detect the extraterrestrial material in a trace element analysis. The "good" news is that an old keris is in many ways the worst case scenario. A blade forged with modern, industrial steel, made in the northern hemisphere from materials of known or knowable chemistry, would be much simpler to study F |
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#2 |
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Hi Fearn,
This is most interesting, the only thing I can see which could make a difference is the greater pollution in the air to day than some hundred years ago – would this make a difference? Jens |
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#3 | ||
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#4 |
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I agree BSMStar, so long as we're talking about ID'ing meteorite samples.
When we're trying to ID the meteoric component in a knife made of mixed terrestrial and meteoric materials, it's a bit more complex. The blade is made of: 1) the meteoric material (with a readily identifiable asteroidal fingerprint?) 2) iron from a terrestrial source, with either a known or unknown chemical fingerprint depending on age and source, and 3) carbon (for steel) from a terrestrial source, that probably contains traces of contaminants such as cesium, mercury, or whatever, depending on the source of the carbon (charcoal, coal, etc). I'll submit that this mixture can be deciphered if 2) and 3) are known--basically, in an industrial setting, especially where the steel is purchased and contains 2 and 3 already. In a non-industrial setting, such as with a century-plus old keris from somewhere in Java, it will be extraordinarily difficult to decipher all three, since we have little idea about the source any of the ingredients. F |
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#5 | |
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Also, keep in mind that meteorites are older than earth rocks. We are not looking at Rubidium/Strontium ratios (good age indicators), but are not the trace indicators we are looking for (not looking specifically for isotopes, we are looking at elemental abundance - unless something has changed in the pass thirty some years). Also, (let me add) in the field of Tektites, LDG (Libyan Desert Glass) has a very small amount of a meteoritic component, that is traceable back to a chondritic impactor. LDG is believed to be earth rock impactites (as are all true Tektites), created during an “impact” event. Talk about an unknown mix and meteoritic dilution… but the fingerprint is still there. Fearn, you have the last word. Last edited by BSMStar; 7th August 2006 at 03:23 PM. |
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#6 |
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I think the amount of Iridium in typical (not the meteorite impact ones)mineralized (ore-bearing) Earth rocks is measured in a couple ppb (part per billion), down to parts per trillion; the two iron meteorite info sheets on the previously posted Metbase link were a couple ppm (parts per million) - it seems like even after taking into account the concentrating effects of smelting and the diluting effects of mixing meteoric metal and earth metal, there's room for a noticeable difference.
But it's all speculation until we get some data to crunch. ![]() |
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#7 | |
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#8 |
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nechesh, as earlier stated, testing your collection may not be desirable. I would not take a valuable Pusaka and test it (any why would you want to). But I believe I have made the point that testing old blades which are not deemed “valuable,” to see what percentage of the population may contain meteoritic material, may have some worth. My gut feel is that it well be far fewer than people think. It may let us know if there is indeed a look (a pamor affect) and feel (tactile response) to the blades that contain meteorite. Therefore, there will be some benefit for the research effort that could be applied to blades in our collections (or we may find out you can only tell by testing).
I think the rub is talking someone to doing the research… and giving up the samples. |
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#9 |
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Great information on testing for trace elements. Obvious to me we have some heavy hitters at bat here
![]() I have some knowledge of Neutron Activation Analysis testing from my Georgia Tech days. I wonder if anyone has tried or has any knowledge of it? For anyone interested, this is a Link to some information about it, I found it using Google search. one side effect is that the item is now radioactive and depending on the isotope half life it may be a while before it decays down. ![]() http://www.missouri.edu/~glascock/naa_over.htm Gene |
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#10 |
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See what happens when you use the words 'meteorite' and 'dagger' in a thread title, Gene?
![]() It had occured to me that pre-industrial iron would have a different (and more variable) chemical signature; I suspect it would not cause too much noise to obscure the extra-terrestrial signature over all the potential elements...there might be archaeological papers that have previous analyses on old keris, one could check them against modern steel & look for differences. ![]() ![]() |
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#11 |
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You're certainly right about that, Jeff. To be honest, I only read the thread because I'd just finished reading about the "Arctic Iron Age"--where the Inuit and Dorset peoples before them made tool blades out of meteoric iron for, I don't know, a thousand years or so. Another story.
Anyway, I think it'd be a great subject for a metallurgy/archeology PhD--looking at Indonesian blade making, and determining how much of the steel's chemical composition/isotopic signature depends on the metal source, how much depends on the carbon and fuel sources, and how much depends on the arsenic staining (at least in the keris blades). It would be interesting to know if there is enough information to determine things like blade origin (or origin of materials) or blade age through a test. Not something I'd want to do, although I'd be happy to help analyze the data for patterns. Oh well, something to dream about. F |
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