欢迎登录材料期刊网

材料期刊网

高级检索

研究了退火对磁场诱导下高定向热解石墨(HOPG)输运特性的影响.结果表明,退火后HOPG的R-T曲线明显变得光滑,且退火后电阻率增大了近50%,相应温度下的磁电阻效应均减小约40%.分析认为,这是由于HOPG内部存在层错与所含杂质缺陷引起的.磁场下电阻率随温度的变化表明,外加磁场对低温下的金属导电行为存在抑制作用,随着外加磁场的增加,低温下的金属导电行为受到抑制,在H=5.57×104A/m时,低温下的绝缘体-金属转变(I-M)被完全抑制,呈半导体性质.随着磁场的继续增加,在磁场高于H=9.24×105A/m时再次出现绝缘体-金属转变,即再入型金属导电行为,且退火对这一转变过程没有影响,表明这种绝缘体-金属转变是由外加磁场诱导产生的.

参考文献

[1] Foley G M T;Zeller C;Falardeau E R et al.[J].Solid St Commun,1977,24:371.
[2] Hannay N B;Geballe T H;Matthias B T et al.[J].Physical Review Letters,1965,14:225.
[3] Kopelevich Y;Esquinazi P;Torres J H S et al.[J].Journal of Low Temperature Physics,2000,119:691.
[4] Esquinazi P;Setzer A;Hohne R et al.[J].Physical Review B:Condensed Matter,2002,66:024429.
[5] Kempa H;Esquinazi P;Kopelevich Y .[J].Physical Review B:Condensed Matter,2002,65:24110(R).
[6] Kempa H.;Mrowka F.;Setzer A.;Torres JHS.;Hohne R. Esquinazi P.;Kopelevich Y. .Magnetic-field-driven superconductor-insulator-type transition in graphite[J].Solid State Communications,2000(10):539-542.
[7] Sercheli MS.;Kopelevich Y.;da Silva RR.;Torres JHS.;Rettori C. .Evidence for internal field in graphite: a conduction electron spin-resonance study[J].Solid State Communications,2002(9/10):579-583.
[8] Kopelevich Y;Lemanov V V;Moehlecke S et al.[J].Physics of the Solid State,1999,41:1959.
[9] Lukyanchuk I A;Kopelevich Y .[J].Physical Review Letters,2006,97:256801.
[10] Khveshehenko D V .[J].Physical Review Letters,2003,87:206401.
[11] Khveshchenko D V .[J].Phya Rev Lett,2003,87:246802.
[12] Gorbar E V;Gusynin V P;Miransky V A et al.[J].Physical Review B,2002,66:045108.
[13] Kopelevich Y;Torres J H S;da Silva R R et al.[J].Physical Review Letters,2003,90:15.
[14] Woollam J A .[J].Phya Rev Lett,1970,25:810.
[15] Uji S.;Iye Y.;Brooks JS. .Field-induced phase transition in Kish graphite[J].Physica, B. Condensed Matter,1998(0):299-302.
[16] 都有为;王志明;倪刚 等.[J].物理学报,2004,53:4.
[17] Guaynin V P;Miransky V A;Shovkovy I A .[J].Physical Review Letters,1994,73:3499.
上一张 下一张
上一张 下一张
计量
  • 下载量()
  • 访问量()
文章评分
  • 您的评分:
  • 1
    0%
  • 2
    0%
  • 3
    0%
  • 4
    0%
  • 5
    0%