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钙钛矿型DyFe_xMn_(1-x)O_3(0≤x≤1)的水热组成调变合成及磁性表征 被引量:1
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作者 董忠平 张胤 《稀土》 EI CAS CSCD 北大核心 2012年第4期49-53,共5页
通过环境友好的水热法对DyFexMn1-xO3(0≤x≤1)系列化合物进行组成调变合成,同时借助于ICP元素分析、XRD、扫描电镜SEM以及磁强计对其进行了表征。研究结果显示,该系列化合物随Fe掺杂量的增加,磁性发生明显的变化,由反铁磁向弱铁磁转变。
关键词 水热法 组成调变 磁性
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Improvement of Computation Method of Fault Motion Coordination Ratio and Analysis of Earthquake Cases
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作者 Li Ruisha Zhang Xi +1 位作者 Jia Xiaodong Tang Hongtao 《Earthquake Research in China》 2014年第1期54-61,共8页
According to the concept of the fault motion coordination ratio( FCR),this paper discusses the effect of the starting point on the result of FCR calculation and puts forward the calculation method for FCR using the sl... According to the concept of the fault motion coordination ratio( FCR),this paper discusses the effect of the starting point on the result of FCR calculation and puts forward the calculation method for FCR using the sliding window and the index for evaluating the dispersion. Earthquake cases analysis shows that at the Lijiang site across the fault: the FCR value varied greatly and its distribution was dispersive before the MS7. 0 Lijiang earthquake,while the value was stable and less dispersive after the earthquake,which reflects the strain accumulation of the fault during the seismogenic process and the poor movement coordination between the motion of the three components. After the earthquake,the fault was in a free activity state,the accumulated strain energy released, and the movement of the three components was coordinated mutually. At present,FCR dispersion of Lijiang is at a low value,and fault strain accumulation is at a low level. 展开更多
关键词 Lijiang earthquake Fault motion coordination ratio (FCR) Cross-faultmeasurement DISPERSION
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