On the stellar sources of presolar graphite

نویسندگان

  • Ernst Zinner
  • Sachiko Amari
  • Manavi Jadhav
چکیده

Primitive meteorites contain graphite spherules whose anomalous isotopic compositions indicate a stellar origin. The isolation of presolar graphite grains is difficult and they have been less well studied than presolar silicon carbide grains. While previous isotopic measurements have been made on graphite from the Murchison meteorite and mostly on low-density grains, a new separation of graphite from the Orgueil meteorite and the application of a new ion microprobe, the NanoSIMS, have provided a wealth of C, N, O, Al, and Si isotopic data on grains with a range of densities. These data confirm that low-density grains come from supernovae. These grains are characterized by 15 N, 18 O, 28 Si and 49 Ti excesses, high inferred 26 Al/ 27 Al ratios, as well as evidence for the initial presence of the short-lived radionuclides 22 Na, 41 Ca, and 44 Ti. All these signatures point to an origin in Type II supernovae. The Ne-E(L) component, almost pure 22 Ne, is characteristic of presolar graphite and led to its discovery. In SN grains it is due to the decay of short-lived (T1/2 = 2.6 yr) 22 Na, which apparently was implanted into the grains. Many high-density grains have high 12 C/ 13 C ratios (>300) and large excesses in 30 Si and smaller excesses in 29 Si. These signatures are best explained by an origin in low-metallicity AGB stars. In these stars the enrichments of the envelope in the heavy Si isotopes and in 12 C, products of nucleosynthesis in the He shell, are much larger than those expected for solar-metallicity parent stars. The high 12 C/ 13 C ratios imply also high C/O ratios, which probably caused the preferential condensation of graphite grains over SiC grains. An AGB origin of high-density grains is compatible with the presence of internal sub-grains with high concentrations of the s-process elements Zr, Mo, and Ru, reflecting the high abundances of these elements in the envelope of such stars. The stellar source of high-density grains with 12 C/ 13 C ratios around 10 remains elusive.

برای دانلود رایگان متن کامل این مقاله و بیش از 32 میلیون مقاله دیگر ابتدا ثبت نام کنید

ثبت نام

اگر عضو سایت هستید لطفا وارد حساب کاربری خود شوید

منابع مشابه

Presolar graphite grains and their stellar origins: A review

Presolar grains are sub-micron to micron-sized stardust grains that are found in very primitive solar system materials. Laboratory measurements of presolar grains allow cosmochemists to understand the chemical and physical conditions in circumstellar environments, where the grains condensed. They provide important constraints for models of stellar nucleosynthesis and Galactic chemical evolution...

متن کامل

Nanosims Studies of Presolar Graphite Grains: Are C-isotopic Ratios Grain-size- Dependent?

Introduction: After silicon carbide (SiC), graphite is the best studied presolar mineral. A wealth of information exists on the isotopic compositions of C and of many minor/trace elements in micrometer-sized grains [e.g., 1-5]. Presolar graphite grains exhibit large C-isotopic anomalies with C/C ratios between 2 and 7000. Although this range is compatible with what is observed for SiC [6, 7], t...

متن کامل

Extreme O Isotopic Anomalies in Presolar Oxides from the Murray Cm2 Chondrite

Introduction: O-rich stardust grains found in primitive meteorites provide information about a wide range of astrophysical environments. Based on their O isotopic ratios, these grains can be placed into discrete groups, thought to reflect distinct stellar sources [1], such as low-mass AGB stars and supernovae (SNe). However, measurements of sub-μm presolar oxides have revealed sub-populations w...

متن کامل

New Stellar Sources for High-density, Presolar Graphite Grains

We present C, N, O, Si, Al-Mg, K, Ca, and Ti isotopic analyses of seven high-density (ORG1f, 2:02 2:04 g cm ) graphite grains from Orgueil with C/C ratios smaller than 20. The presence of 44Ti in three of these grains indicates an origin in Type II supernovae (SNe). The C excesses in these SNe grains, however, remain enigmatic. The remaining grains have extremely large Ca and Ti isotopic anomal...

متن کامل

Presolar Grains from Novae

We report the discovery of five SiC grains and one graphite grain isolated from the Murchison carbonaceous meteorite whose major-element isotopic compositions indicate an origin in nova explosions. The grains are characterized by low C/C (4-9) and N/N (5-20) ratios, large excesses in Si (Si/Si ratios range to 2.1 times solar) and high Al/Al ratios. These isotopic signatures are theoretically pr...

متن کامل

ذخیره در منابع من


  با ذخیره ی این منبع در منابع من، دسترسی به آن را برای استفاده های بعدی آسان تر کنید

عنوان ژورنال:

دوره   شماره 

صفحات  -

تاریخ انتشار 2006