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@ARTICLE{Edmund:616207,
      author       = {Edmund, Eric and Chuvashova, Irina and Konôpková, Zuzana
                      and Husband, Rachel and Strohm, Cornelius and Appel, Karen
                      and Bähtz, Carsten and Ball, Orianna and Bouffetier,
                      Victorien and Brugman, Kara and Buakor, Khachiwan and
                      Chantel, Julien and Chariton, Stella and Duff, Matthew and
                      Dwivedi, Anand and Glazyrin, Konstantin and Hosseini-Saber,
                      S. M. A. and Jaisle, Nicolas and Laurus, Torsten and Li,
                      Xiang and Masani, Bernhard and McHardy, James and McMahon,
                      Malcolm and Merkel, Sébastien and Mohrbach, Katharina and
                      Mondal, Anshuman and Morard, Guillaume and Prakapenka,
                      Vitali B. and Prescher, Clemens and Ryu, Young-Jay and
                      Schwinkendorf, Jan-Patrick and Tang, Minxue and Younes, Zena
                      and Sanchez-Valle, Carmen and Liermann, Hanns-Peter and
                      Badro, James and Lin, Jung-Fu and McWilliams, R. Stewart and
                      Goncharov, Alexander F.},
      title        = {{T}he {T}hermal {C}onductivity of {B}ridgmanite at {L}ower
                      {M}antle {C}onditions {U}sing a {M}ulti‐{T}echnique
                      {A}pproach},
      journal      = {JGR / Solid earth},
      volume       = {129},
      number       = {6},
      issn         = {2169-9313},
      address      = {Hoboken, NJ},
      publisher    = {Wiley},
      reportid     = {PUBDB-2024-06367},
      pages        = {e2024JB028823},
      year         = {2024},
      note         = {ISSN 2169-9356 not unique: **2 hits**. Waiting for
                      fulltext},
      abstract     = {The thermal conductivity of bridgmanite, the primary
                      constituent of the Earth's lower mantle, has been
                      investigated using diamond anvil cells at pressures up to 85
                      GPa and temperatures up to 3,100 K. We report the results of
                      time-domain optical laser flash heating and X-ray Free
                      Electron Laser heating experiments from a variety of
                      bridgmanite samples with different Al and Fe contents. The
                      results demonstrate that Fe or Fe,Al incorporation in
                      bridgmanite reduces thermal conductivity by about $50\%$ in
                      comparison to end-member MgSiO$_3$ at the
                      pressure-temperature conditions of Earth's lower mantle. The
                      effect of temperature on the thermal conductivity at 28–60
                      GPa is moderate, well described as $k = k_{300}(300/T)^a$,
                      where a is 0.2–0.5. The results yield thermal conductivity
                      of 7.5–15 W/(m × K) in the thermal boundary layer of the
                      lowermost mantle composed of Fe,Al-bearing bridgmanite.},
      cin          = {FS-PETRA-D / FS-HIBEF / DOOR ; HAS-User / $XFEL_E1_HED$},
      ddc          = {550},
      cid          = {I:(DE-H253)FS-PETRA-D-20210408 /
                      I:(DE-H253)FS-HIBEF-20240110 / I:(DE-H253)HAS-User-20120731
                      / $I:(DE-H253)XFEL_E1_HED-20210408$},
      pnm          = {631 - Matter – Dynamics, Mechanisms and Control
                      (POF4-631) / 6G3 - PETRA III (DESY) (POF4-6G3) / SEPtiM -
                      Solidification of Earth's Primitive Mantle (101019965)},
      pid          = {G:(DE-HGF)POF4-631 / G:(DE-HGF)POF4-6G3 /
                      G:(EU-Grant)101019965},
      experiment   = {EXP:(DE-H253)P-P02.2-20150101},
      typ          = {PUB:(DE-HGF)16},
      UT           = {WOS:001243670900001},
      doi          = {10.1029/2024JB028823},
      url          = {https://bib-pubdb1.desy.de/record/616207},
}