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Critical exponents of the second-order manganite Nd_(0.5)Sr_(0.25)Ca_(0.25)MnO_3 determined from magnetic entropy change measurements

机译:由磁熵变测量确定的二阶锰矿Nd_(0.5)Sr_(0.25)Ca_(0.25)MnO_3的临界指数

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摘要

The critical exponents of second-order phase transition were deduced from magnetic entropy change. Using the magnetic field dependence of entropy change and the Widom scaling relation, some relevant critical exponents can be calculated directly from them. Based on critical exponents, a corresponding Arrott plot can be established as an initial model. Through a limited nonlinear fitting, we can obtain the final critical exponents. This method eliminates the drawbacks of the routine method which relies on the subjective selection of an initial model and involves the multi-step nonlinear fitting process. It was applied to the manganite Nd_(0:5)Sr_(0:25)Ca_(0:25)MnO_3 to verify its utility and feasibility. The spontaneous magnetization obtained using the final critical exponents is consistent with that deduced from the isothermal magnetization measurements, indicating that the utilization of the magnetic field dependence of magnetic entropy change to determine critical exponents is a valid method.
机译:从磁熵变推导了二阶相变的临界指数。利用熵变的磁场依赖性和Widom比例关系,可以直接从中计算出一些相关的临界指数。基于关键指数,可以建立相应的Arrott图作为初始模型。通过有限的非线性拟合,我们可以获得最终的临界指数。该方法消除了常规方法的缺点,该常规方法依赖于初始模型的主观选择,并且涉及多步非线性拟合过程。将其应用于锰矿Nd_(0:5)Sr_(0:25)Ca_(0:25)MnO_3,以验证其实用性和可行性。使用最终临界指数获得的自发磁化强度与从等温磁化强度测量得出的自发磁化强度相一致,表明利用磁熵变的磁场依赖性确定临界指数是一种有效方法。

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