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Atomic-scale images of charge ordering in a mixed-valence manganite   总被引:3,自引:0,他引:3  
Renner Ch  Aeppli G  Kim BG  Soh YA  Cheong SW 《Nature》2002,416(6880):518-521
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Summary By reacting dopa, -methyl- and -ethyldopa and the corresponding esters with aldehydes geminate amino-carbinols of the general formula I can be prepared. The acetylation of the adduct of -methyldopa-methylester with acetaldehyde and benzaldehyde and the resolution of the latter compound withd-tartaric acid is described.  相似文献   
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Kummamuru RK  Soh YA 《Nature》2008,452(7189):859-863
The role of magnetic domains (and the walls between domains) in determining the electrical properties of ferromagnetic materials has been investigated in great detail for many years, not least because control over domains offers a means of manipulating electron spin to control charge transport in 'spintronic' devices. In contrast, much less attention has been paid to the effects of domains and domain walls on the electrical properties of antiferromagnets: antiferromagnetic domains show no net external magnetic moment, and so are difficult to manipulate or probe. Here we describe electrical measurements on chromium--a simple metal and quintessential spin density wave antiferromagnet--that show behaviour directly related to spin density wave formation and the presence of antiferromagnetic domains. Two types of thermal hysteresis are seen in both longitudinal and Hall resistivity: the first can be explained by the quantization of spin density waves due to the finite film thickness (confirmed by X-ray diffraction measurements) and the second by domain-wall scattering of electrons. We also observe the striking influence of the electrical lead configuration (a mesoscopic effect) on the resistivity of macroscopic samples in the spin density wave state. Our results are potentially of practical importance, in that they reveal tunable electrical effects of film thickness and domain walls that are as large as the highest seen for ferromagnets.  相似文献   
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Ma KF  Tanaka H  Song SR  Wang CY  Hung JH  Tsai YB  Mori J  Song YF  Yeh EC  Soh W  Sone H  Kuo LW  Wu HY 《Nature》2006,444(7118):473-476
Determining the seismic fracture energy during an earthquake and understanding the associated creation and development of a fault zone requires a combination of both seismological and geological field data. The actual thickness of the zone that slips during the rupture of a large earthquake is not known and is a key seismological parameter in understanding energy dissipation, rupture processes and seismic efficiency. The 1999 magnitude-7.7 earthquake in Chi-Chi, Taiwan, produced large slip (8 to 10 metres) at or near the surface, which is accessible to borehole drilling and provides a rare opportunity to sample a fault that had large slip in a recent earthquake. Here we present the retrieved cores from the Taiwan Chelungpu-fault Drilling Project and identify the main slip zone associated with the Chi-Chi earthquake. The surface fracture energy estimated from grain sizes in the gouge zone of the fault sample was directly compared to the seismic fracture energy determined from near-field seismic data. From the comparison, the contribution of gouge surface energy to the earthquake breakdown work is quantified to be 6 per cent.  相似文献   
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一类非线性系统的稳定性   总被引:3,自引:0,他引:3  
研究了一类非线性系统的输入输出稳定性问题,这类系统的特点是其模型为系统输出的线性拟函数。对非线性稳定性系统,利用稳定性的线性等价原理,提出了这一类非线性系统的稳定性判据;对非线性随机系统,给出了m阶均值意义下的稳定性定义,提出了一种二阶均值下的输入输出稳定性条件,给出了几个示例说明。  相似文献   
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