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Here is an excerpt from an article I found to be rather interesting:
The ICR (Institute for Creation Research) recently spent eight years on a project known as RATE (Radioisotopes and the Age of The Earth). The RATE team claims the results have yielded convincing and irrefutable scientific evidence of a young earth.
Diamond
Diamond is difficult to combust. The RATE samples apparently required modifications to the normal procedure [1], presumably higher combustion temperatures and longer combustion times, likely increasing the sample chemistry contamination. The samples were reportedly pitted and may have been subjected to previous analyses and to unknown contamination. Nevertheless, RATE’s five deep-mine diamond samples had radiocarbon levels only slightly above background (0.01 to 0.07 pMC after background subtraction), while the seven alluvial samples ranged from 0.03 to 0.31 pMC after background subtraction.
Subsequently, the RATE team inserted diamond directly into an ion source, eliminating the sample chemistry, and measured much lower radiocarbon values, “between 0.008 and 0.022 pMC, with a mean value of 0.014 pMC,” apparently with no background subtraction [6]. This much lower value for unprocessed diamond provides strong evidence that their processed diamond samples had been contaminated, most likely by the modified sample chemistry.
Taylor and Southon have also measured unprocessed diamond, finding a similar range of 0.005 to 0.03 pMC without background subtraction. They interpret this result as their instrument background, primarily due to ion source memory. Their ion source current varied, unintentionally, over about a factor of two, perhaps due to crystal face orientation or to conductivity differences between samples. “The oldest 14C age equivalents were measured on natural diamonds which exhibited the highest current yields” [4]. This important observation provides evidence about the source of the radiocarbon.
If the radiocarbon were intrinsic to the sample, there would be no change in the radiocarbon ratio with sample current. The 14C, 13C, and 12C would change in unison. However, if the radiocarbon were coming from ion source memory or elsewhere in the accelerator, it should give a count rate independent of ion source current. Normalizing the radiocarbon count rate to the ion source current, which is predominantly 12C, would result in higher radiocarbon content for lower source currents, as observed. This data provides clear evidence that at least a significant fraction of the radiocarbon detected by Taylor and Southon in diamond measurements did not come from the diamonds themselves and thus could not be “intrinsic radiocarbon.”
The lower values for unprocessed diamond and the current-dependent behavior find no explanation in Baumgardner’s “intrinsic radiocarbon” model. But these results fit well with the Taylor and Southon evidence that instrument background (specifically ion source memory) is material-dependent, with diamond exhibiting significantly less ion source memory than graphite. The radiocarbon detected in natural, unprocessed diamond measurements seems to be nothing more than instrument background.
Read the complete article: RATE’s Radiocarbon: Intrinsic or Contamination?
The ICR (Institute for Creation Research) recently spent eight years on a project known as RATE (Radioisotopes and the Age of The Earth). The RATE team claims the results have yielded convincing and irrefutable scientific evidence of a young earth.
Diamond
Diamond is difficult to combust. The RATE samples apparently required modifications to the normal procedure [1], presumably higher combustion temperatures and longer combustion times, likely increasing the sample chemistry contamination. The samples were reportedly pitted and may have been subjected to previous analyses and to unknown contamination. Nevertheless, RATE’s five deep-mine diamond samples had radiocarbon levels only slightly above background (0.01 to 0.07 pMC after background subtraction), while the seven alluvial samples ranged from 0.03 to 0.31 pMC after background subtraction.
Subsequently, the RATE team inserted diamond directly into an ion source, eliminating the sample chemistry, and measured much lower radiocarbon values, “between 0.008 and 0.022 pMC, with a mean value of 0.014 pMC,” apparently with no background subtraction [6]. This much lower value for unprocessed diamond provides strong evidence that their processed diamond samples had been contaminated, most likely by the modified sample chemistry.
Taylor and Southon have also measured unprocessed diamond, finding a similar range of 0.005 to 0.03 pMC without background subtraction. They interpret this result as their instrument background, primarily due to ion source memory. Their ion source current varied, unintentionally, over about a factor of two, perhaps due to crystal face orientation or to conductivity differences between samples. “The oldest 14C age equivalents were measured on natural diamonds which exhibited the highest current yields” [4]. This important observation provides evidence about the source of the radiocarbon.
If the radiocarbon were intrinsic to the sample, there would be no change in the radiocarbon ratio with sample current. The 14C, 13C, and 12C would change in unison. However, if the radiocarbon were coming from ion source memory or elsewhere in the accelerator, it should give a count rate independent of ion source current. Normalizing the radiocarbon count rate to the ion source current, which is predominantly 12C, would result in higher radiocarbon content for lower source currents, as observed. This data provides clear evidence that at least a significant fraction of the radiocarbon detected by Taylor and Southon in diamond measurements did not come from the diamonds themselves and thus could not be “intrinsic radiocarbon.”
The lower values for unprocessed diamond and the current-dependent behavior find no explanation in Baumgardner’s “intrinsic radiocarbon” model. But these results fit well with the Taylor and Southon evidence that instrument background (specifically ion source memory) is material-dependent, with diamond exhibiting significantly less ion source memory than graphite. The radiocarbon detected in natural, unprocessed diamond measurements seems to be nothing more than instrument background.
Read the complete article: RATE’s Radiocarbon: Intrinsic or Contamination?