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Anelastic Relaxation at 400K in Pr_(1-x)Ca_xMnO_3 Manganite

机译:Pr_(1-x)Ca_xMnO_3锰矿中400K的弹性弛豫

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We have performed anelastic measurements in the hertz and kilohertz frequency range of the ceramic Pr_(1-x)Ca_xMnO_3 manganite with x = 0.35 and 0.50 in the temperature range 100-500 K. In both samples there were several internal friction peaks which move in temperature and stabilize after the second cycle of temperature. At x = 0.35 we can see the effects, according to the phase diagram of Y. Tomioka et al.[1], related to the antiferromagnetic transition T_N approx= 165 K, the charge order transition at T_(CO) approx= 230 K and a large relaxation at T_R = 317 K (5.1 KHz). There are also several non identified small peaks at 120 K, 200 K, 260 K and 396 K. At x = 0.50 we can distinghish the charge order transition (T_(CO) = 238 K) and a large relaxation IF peak at T_R = 411 K (1Hz). There is no evidence of the antiferromagnetic transition which takes place normally at T_N = 175 K for this concentration. In both ranges of frequencies we have obtained similar results. The activation energy calculated from the T_R dependence on the low frequency data were for x = 0.50 H(0.50) approx= 4.8 ± 0.5 eV and H(0.35) approx= 4.3 ± 0.2 eV. We are not able till present to explain the microscopic origin of this relaxation, but some efforts are described.
机译:我们在100-500 K的温度范围内,在x = 0.35和0.50的陶瓷Pr_(1-x)Ca_xMnO_3锰矿的赫兹和千赫兹频率范围内进行了无弹性测量。在两个样品中都有几个内部摩擦峰在温度并在第二个温度循环后稳定下来。根据Y. Tomioka等人[1]的相图,在x = 0.35处,我们可以看到与反铁磁跃迁T_N约= 165 K有关,在T_(CO)时的电荷序跃迁约= 230 K的影响。在T_R = 317 K(5.1 KHz)时有很大的弛豫。在120 K,200 K,260 K和396 K处还有几个未识别的小峰。在x = 0.50时,我们可以区分出电荷序跃迁(T_(CO)= 238 K)和在T_R =处的大弛豫IF峰。 411 K(1Hz)。没有证据表明反铁磁转变通常在该浓度下在T_N = 175 K时发生。在这两个频率范围内,我们都获得了相似的结果。由T_R对低频数据的依赖性计算出的激活能为:x = 0.50 H(0.50)大约= 4.8±0.5 eV,H(0.35)大约= 4.3±0.2 eV。直到现在我们还不能解释这种松弛现象的微观原因,但是将描述一些努力。

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