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2017 | 8 | 110-122

Article title

Średni ciężar atomowy chondrytu Ensisheim (LL6)

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Content

Title variants

EN
Mean atomic weight of Ensisheim LL6 chondrite

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PL

Abstracts

EN
Mean atomic weight Amean of Ensisheim (LL6, fall 1492) ordinary chondrite has been determined using literature data on chemical composition of the meteorite and using relationships: between mean atomic weight and Fe/Si atomic ratio, between Amean and grain density, and between Amean and magnetic susceptibility (Szurgot 2015a–f, 2016a, b, d, e). It was shown that Ensisheim’s Amean = 23.32, and 23.06 for composition without water, and with H2O, respectively. These values are close to the mean atomic weight of LL chondrite falls (Amean = 23.36, and 23.03), and are close to Amean values of LL6 chondrite falls (Amean = 23.30, and 23.06, Szurgot 2016b). Ensisheim’s Fe/Si atomic ratio (0.509) leads to Amean = 23.16±0.12 which is close to the values determined by bulk composition. This means that Ensisheim belongs to LL6 chondrites, as previously classified (Jarosewich i Dodd 1985). Using dependence between mean atomic weight and grain density (Szurgot 2015a–c, 2016d) leads to Amean = 23.70±0.54 (dgr = 3.52±0.04 g/cm3, Macke 2010), and using dependence between Amean and magnetic susceptibility (Szurgot 2016a, d) gives Ameanc = 22.78±0.24 (logc = 4.15±0.09, Macke 2010). Arithmetic mean Amean (dgr) and Amean (logc) gives 23.24±0.65, and arithmetic mean of Amean (dgr), Amean (logc), and Amean(Fe/Si), gives 23.21±0.46 values close each other, and close to Amean(bulk composition) determined using compositional data. Mean atomic number Zmean, and Amean/Zmean ratio of the meteorite have been also determined. Ensisheim’s Zmean = 11.51 for composition without H2O, and 11.40 for composition with H2O. Amean/Zmean ratios are: 2.026 and 2.023, for composition without water, and with H2O, respectively. Ensisheim’s silicates shown values: Amean = 22.19, Zmean = 10.97, Amean/Z mean = 2.022, Fe/Si = 0.355, Amean(Fe/Si) = 22.28, and Fe, Ni metal values: Amean = 57.26, Zmean = 26.96, and Amean/Z mean = 2.124.

Discipline

Year

Volume

8

Pages

110-122

Physical description

Contributors

  • Centrum Nauczania Matematyki i Fizyki Politechniki Łódzkiej

References

  • Anderson D.L., 1989, Theory of the Earth, Blackwell, London.
  • Anderson D.L., Kovach R. L., 1967, The composition of the terrestrial planets, Earth Planet. Sci. Lett., 3, s. 19–24.
  • Anderson D.L., Jordan T., 1970, The composition of lower mantle, Phys. Earth Planet. Interior, 3, s. 23–35.
  • Birch F., 1961, Composition of the Earth’s Mantle, Geophys. J. Int., 4, s. 295–311.
  • Consolmagno G.J., Britt D.T., Macke R.J., 2008, The significance of meteorite density and porosity. Chemie der Erde 68, s. 1–29.
  • Hutchison R., 2004, Meteorites – A petrologic, chemical and isotopic synthesis, Cambridge.
  • Jarosewich E., 1990, Chemical analyses of meteorites: A compilation of stony and iron meteorite analyses, Meteoritics, 35, s. 323–337.
  • Jarosewich E., Dodd, R.T., 1985, Chemical variations among L-chondrites-IV. Analyses, with petrographic notes, of 13 L-group, and 3 LL-group chondrites, Meteoritics, 20, s. 23–36.
  • Macke R.J., 2010, Survey of meteorite physical properties: density, porosity and magnetic susceptibility, Ph.D. Thesis, University of Central Florida, Orlando.
  • Maj S., 1998, Phonon thermal conductivity of geomaterials: Relationship to the density and mean atomic weight, Acta Geophys. Pol. 46, s. 415-425.
  • Marvin U., 1992, The meteorite of Ensisheim: 1492 to 1992, Meteoritics, 27, s. 28–72.
  • McSween, H.Y., Bennett III M.E., 1991, The Mineralogy of Ordinary Chondrites and Implications for Asteroid Spectrophotometry, Icarus, 90, s. 107–116.
  • Ringwood A.E., 1966, Chemical evolution of the terrestrial planets, Geochim. Cosmochim. Acta, 30, s. 41–104.
  • Rochette P., Sagnotti L., Bourot-Denise M., Consolmagno G., Folco L., Gattacceca J., Osete L.M., Pesonen L., 2003, Magnetic classification of stony meteorites: 1. Ordinary chondrites, Meteoritics & Planet. Sci., 38, s. 251–268.
  • Rochette P., Gattacceca J., Bonal L., Bourot-Denise M., Chevrier V., Clerc J.P., Consolmagno G., Folco L., Gounnelle M., Kohout T., Lauri Pesonen L., Eric Quirico E., Sagnotti L., Skripnik A., 2008, Magnetic classification of stony meteorites: 2. Non-ordinary chondrites, Meteoritics & Planet. Sci., 43, s. 959–980.
  • Rochette P., Gattacceca J., Lewandowski M., 2012, Magnetic classification of meteorites and application to the Sołtmany fall, Meteorites, 2, s. 67–71.
  • Rowland I.D., 1990, A Contemporary Account of the Ensisheim Meteorite, 1492, Meteoritics, 25, s. 19–22.
  • Szurgot M., 2015a, Mean atomic weight of Earth, Moon, Venus, Mercury and Mars. Effect of mass of cores and density of planets, Lunar and Planetary Science Conference XXXXVI. #1536.pdf
  • Szurgot M., 2015b, Core mass fraction and mean atomic weight of terrestrial planets, moon, and protoplanet Vesta, Comparative Tectonics and Geodynamics of Venus, Earth, and Rocky Exoplanets Workshop. #5001.pdf
  • Szurgot M., 2015c, Średni ciężar atomowy chondrytu Sołtmany, chondrytów L6 i minerałów pozaziemskich, Acta Societatis Metheoriticae Polonorum, 6, s. 107–128.
  • Szurgot M., 2015d, Mean atomic weight of Chelyabinsk and Olivenza LL5 chondrites, Meteoritics & Planetary Science, 50 Suppl. S1. #5008.pdf
  • Szurgot M., 2015e, Mean atomic weight of Pułtusk meteorite and H chondrites, Meteoritics & Planetary Science, 50 Suppl. S1. #5013.pdf
  • Szurgot M., 2015f, Mean atomic number of Chelyabinsk, Sołtmany and Pułtusk meteorites, 57 Konwersatorium Krystalograficzne, Wrocław, Streszczenia komunikatów, s. 172–173.
  • Szurgot M., 2015g, Średni ciężar atomowy minerałów pozaziemskich, 57 Konwersatorium Krystalograficzne, Wrocław, Streszczenia komunikatów, s. 174–175.
  • Szurgot M., 2016a, Mean atomic weight of L/LL and H/L intermediate ordinary chondrites. Lunar Planet. Sci. Conf., 47th: Abstract #2180.
  • Szurgot M., 2016b, Mean atomic weight of ordinary chondrites. Effect of petrologic type, Meteoritics & Planetary Science, 51, Suppl. S1, #6021.pdf.
  • Szurgot M., 2016c, Mean atomic weight of Białystok eucrite, Łowicz mesosiderite, and Baszkówka chondrite, Meteoritics & Planetary Science, 51, Suppl. S1, #6005.pdf.
  • Szurgot M., 2016d, Średni ciężar atomowy chondrytówLL5: Siena, Hautes Fagnes i NWA 7915, Acta Societatis Metheoriticae Polonorum, 7, s. 133–143.
  • Szurgot M., 2016e, Mean atomic weight and mean atomic number of Košice and Pułtusk H4-5 chondrites, 58 Konwersatorium Krystalograficzne, Wrocław, Streszczenia komunikatów, s. 173–174.
  • Szurgot M., 2017a, Mean atomic weight of Earth and enstatite chondrites. Lunar Planet. Sci. Conf., 48th: Abstract #1130.
  • Szurgot M., 2017b, Mean atomic weight of chondrules and matrices in Semarkona, Allende and Sharps meteorites, LPI Contrib. No. 1963, Workshop on Chondrules and Protoplanetary Disk, Abstract #2002.

Document Type

article

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YADDA identifier

bwmeta1.element.psjd-583ebbb6-bcdf-4fb5-96ca-5901c89947bb
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