Basic research of shock reaction on organic materials and its implication for cosmochemistry
Basic research of shock reaction on organic materials and its implication for cosmochemistry
批准号:
16340172
负责人:
MIMURA Koichi
金额:
$10.82万
依托单位:
依托单位国家:
日本
项目类别:
Grant-in-Aid for Scientific Research (B)
财政年份:
2004
资助国家:
日本
项目状态:
已结题
起止时间:
2004 至 2006
中文摘要
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英文摘要
Polycyclic aromatic hydrocarbons (PAHs) were impacted to study the behavior of PAHs against shock. We applied these results to estimate the survival degree of organic matter delivery by carbonaceous asteroids against their impacts pressures at the accretion stage of early Earth. The estimation suggests that a large quantity of prebiotic organic materials leading to life should have been delivered to the early Earth by the asteroids.Shock recovery experiments on PAHs were carried out. In the experiments, we examined the shock-induced dehydrogenation of PAHs and δD vales and discussed the hydrogen amounts supplied to the Earth's atmosphere and interior during its formation. Then, we show that the cumulative amount of hydrogen in the Earth's interior at that point and its δD value were comparable to those already established for the Earth's interior.Shock recovery experiments on Murchison meteorite samples were performed. δD values of the shocked Murchison showed an initial increase from +10.6%0 to +59.1%0 before declining to-87.6%0, as the dehydrogenation progressed. The behavior of δ^<13>C simply decreased from-15%0 to-7.65%0. The plot of those isotope data collected along devolatilization shows a variation curve that suggests the evolution of those isotopes in the meteorites. Shock is one of the processes effectively controlling the isotope features of the solar system.We performed shock-recovery experiments on insoluble organic matter (IOM) purified from the Murchison meteorite. The shock selectively released D and ^<13>C from the IOM. The selective release of heavier isotopes from IOM would be due to its structure, in which D and ^<13>C-enriched parts are present as an inhomogeneity and are weakly attached to the main network. This effective release of D is probably an inherent result of shock. Thus, shock would effectively control the hydrogen isotope behavior of extraterrestrial organic matter during the evolution of the solar nebula.
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DOI:
10.1111/j.1945-5100.2007.tb00238.x
发表时间:
2007-03-01
期刊:
METEORITICS & PLANETARY SCIENCE
影响因子:
2.2
作者:
[Mimura, Koichi, Okamoto, Michioki, Hashimoto, Shigemasa]
通讯作者:
Hashimoto, Shigemasa
Shock-induced isotope evolution of hudrogen and carbon in meteorites
冲击引起的陨石中氢和碳的同位素演化
DOI:
--
发表时间:
2005
期刊:
Geophysical Research Letters 32
影响因子:
--
作者:
[Mimura K., Okamoto M., Nakatsuka T., Sugitani K., Abe O.]
通讯作者:
Abe O.
Shock-induced dehydrogenation of polycyclic aromatic hydrocarbons with or without serpentine : Implications for nlanetary accretion
有或没有蛇纹石的多环芳烃的冲击诱导脱氢:对行星吸积的影响
DOI:
--
发表时间:
2005
期刊:
Earth and Planetary Science Letters 232
影响因子:
--
作者:
[Mimura K., Toyama S., Sugitani K.]
通讯作者:
Sugitani K.
DOI:
10.1016/j.gca.2004.06.020
发表时间:
2005-01-01
期刊:
GEOCHIMICA ET COSMOCHIMICA ACTA
影响因子:
5
作者:
[Mimura, K, Toyama, S]
通讯作者:
Toyama, S
Shock-induced dehydrogenation of polycyclic aromatic hydrocarbons with or without serpentine : implications for planetary accretion.
有或没有蛇纹石的多环芳烃的冲击引起的脱氢:对行星吸积的影响。
DOI:
--
发表时间:
2005
期刊:
Earth Planet.Sci.Lett. 232
影响因子:
--
作者:
[Mimura K., Toyama S., Sugitani K., Mimura et al.]
通讯作者:
Mimura et al.
共 8 条
Chemical evolution of organic materials derived by meteorite impacts on the early Earth
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批准号:21340164
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项目类别:Grant-in-Aid for Scientific Research (B)
-
资助金额:$12.15万
-
财政年份:2009
-
负责人:MIMURA Koichi
-
依托单位:
国内基金
海外基金
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