TY - JOUR

T1 - Natural occurrence of pure nano-polycrystalline diamond from impact crater

AU - Ohfuji, Hiroaki

AU - Irifune, Tetsuo

AU - Litasov, Konstantin D.

AU - Yamashita, Tomoharu

AU - Isobe, Futoshi

AU - Afanasiev, Valentin P.

AU - Pokhilenko, Nikolai P.

PY - 2015/10/1

Y1 - 2015/10/1

N2 - Consolidated bodies of polycrystalline diamond with grain sizes less than 100 nm, nanopolycrystalline diamond (NPD), has been experimentally produced by direct conversion of graphite at high pressure and high temperature. NPD has superior hardness, toughness and wear resistance to single-crystalline diamonds because of its peculiar nano-textures, and has been successfully used for industrial and scientific applications. Such sintered nanodiamonds have, however, not been found in natural mantle diamonds. Here we identified natural pure NPD, which was produced by a large meteoritic impact about 35 Ma ago in Russia. The impact diamonds consist of well-sintered equigranular nanocrystals (5-50 nm), similar to synthetic NPD, but with distinct [111] preferred orientation. They formed through the martensitic transformation from single-crystal graphite. Stressinduced local fragmentation of the source graphite and subsequent rapid transformation to diamond in the limited time scale result in multiple diamond nucleation and suppression of the overall grain growth, producing the unique nanocrystalline texture of natural NPD. A huge amount of natural NPD is expected to be present in the Popigai crater, which is potentially important for applications as novel ultra-hard material.

AB - Consolidated bodies of polycrystalline diamond with grain sizes less than 100 nm, nanopolycrystalline diamond (NPD), has been experimentally produced by direct conversion of graphite at high pressure and high temperature. NPD has superior hardness, toughness and wear resistance to single-crystalline diamonds because of its peculiar nano-textures, and has been successfully used for industrial and scientific applications. Such sintered nanodiamonds have, however, not been found in natural mantle diamonds. Here we identified natural pure NPD, which was produced by a large meteoritic impact about 35 Ma ago in Russia. The impact diamonds consist of well-sintered equigranular nanocrystals (5-50 nm), similar to synthetic NPD, but with distinct [111] preferred orientation. They formed through the martensitic transformation from single-crystal graphite. Stressinduced local fragmentation of the source graphite and subsequent rapid transformation to diamond in the limited time scale result in multiple diamond nucleation and suppression of the overall grain growth, producing the unique nanocrystalline texture of natural NPD. A huge amount of natural NPD is expected to be present in the Popigai crater, which is potentially important for applications as novel ultra-hard material.

UR - http://www.scopus.com/inward/record.url?scp=84943181309&partnerID=8YFLogxK

U2 - 10.1038/srep14702

DO - 10.1038/srep14702

M3 - Article

AN - SCOPUS:84943181309

VL - 5

JO - Scientific Reports

JF - Scientific Reports

SN - 2045-2322

M1 - 14702

ER -