La2/3(Ca,Ba)1/3MnO3系统的顺磁共振研究

报道了对La2/3Ca1/3MnO3和La2/3Ba1/3MnO3 同温度下的电子顺磁共振（EPR）实验研究，当温度高于某一特征温度Tmin时，共振线宽随温度降低而线性变窄；当温度低于Tmin时，共振线宽表现出反常展宽。基于“瓶颈（bottleneck)”自旋－晶格弛豫模型我们对这种行为进行了讨论，并且指出A位离子平均半径强烈影响着自旋－晶格交换作用和自旋－自旋相互作用的强弱。     

La2/3(Ca,Ba)1/3MnO3系统的顺磁共振研究

报道了对La_2/3Ca_1/3MnO₃和La_2/3Ba_1/3MnO₃系统不同温度下的电子顺磁共振(EPR)实验研究,当温度高于某一特征温度Tmin时,共振线宽随温度降低而线性变窄;当温度低于Tmin时,共振线宽表现出反常展宽.基于“瓶颈(bottleneck)”自旋-晶格弛豫模型我们对这种行为进行了讨论,并且指出A位离子平均半径强烈影响着自旋-晶格交换作用和自旋-自旋相互作用的强弱.     

ELECTRON SPIN RESONANCE DATING FOR THE AGE OF PEKING-MAN, LOC.1, ZHOUKOUDIAN, BEIJING

In this paper, we used ESR dating method to measure the accumulative dose of the fossil teeth samples, which are contemporaneous with the Peking-Man. The internal annual dose rate of samples are got by neutron activation analysis and the environmental annual dose rate by highly sensitive TL dosimeters to be embedded in cave deposits in the site. The results of ESR dating are corresponded with the dating results obtained by U-series, FT, TL and paleomagnetic stratigraphical methods on the 3rd, 4th, 7th and 10th layers. Calculation of using different models, the close-equilibrium model, the linear uranium accumulation model and radon loss-linear uranium accumulation model, for travertine, deer teeth and rhinoceros tooth, we obtained the age of the First Peking- Man in the nth layer is 578 ka and gave ages of other layers, from the 1st to the 13th layer in Peking- Man site.