利用反预报方法从截面预言近滴线丰质子核的结合能

在Origin等数据处理软件中,当实验数据较少时,自由参数的不同初始化设置会导致较大的结果差异,这为物理结果的确定带来较大不确定性.通过最小二乘法分析了345MeV/u ~(78) Kr+~9Be反应中产生的丰质子同位素的截面和结合能,并得到线性回归方程.通过回归方程,利用结合能预报部分丰质子核素的截面,以及通过实验截面对近质子滴线核素的结合能进行反预报测量.这对于近质子滴线的丰质子核素实验测量具有较好的借鉴意义.     

任意实矩阵的优势特征值

对任意实矩阵本文证明了利用位移技术，在不涉及复运算的前提下，可以求得一个或一对优势特征值。并探讨上述结果的数值实现途径．     

磁控式异步电动机软起动器的开发与应用

详细介绍了将传统磁放大器用于异步电机降压起动、实现软起动功能的原理以及实际实现线路，是异步电机减压软起动技术领域的一项创新。     

螺恶嗪化合物在有机溶液中的酸致变色研究

合成了四种螺恶嗪光致变色化合物,并对它们在有机溶剂中所表现的酸致变色现象进行了研究。发现它们与盐酸在室温下形成的复合物(SP.HCl),随溶液极性的增加,其吸光强度增大,吸收光谱发生蓝移。     

关于严格循环权位移的一个问题

给出了一个内射单侧权位移,其权序列空间H~2(β)≠H~∞(β),但对任意φ(z)属于H~∝(β),其部分和序列按算子范数收敛于φ(z).从而否定回答了Shields在文献[1]中的第12问题.     

氧同位素标准样品的研制

使用高纯同位素物质精确配制同位素混合物,作为标准物,确定质谱仪器的系统误差。本工作用天然丰度水定量稀释高浓重氧水,制取从0.1982至96.92原子％~(18)O的氧同位素标准水样,用来校准质谱仪器。 实验采用BrF_5将水样转化成O_2。用质谱峰高法测定(18)~O和(17)~O丰度。比较质谱测定值和计算得到的丰度值C,求出质谱仪固有偏差校正系数K、并得到K与C的线性相关关系。 共得到16个具有准确丰度值的氧同位素标准水样。     

A model for carbon isotope distribution of methane during diagenesis

The evolution of methane carbon isotope with depth has been discussed based on diagenetic reaction kinetics and isotopic Rayleigh fractionational theory. A mathematical model to describe data of methane carbon isotope for the Liaohe oil field has been established.     

A continuous 200-ka palaeoclimatic record from stalagmite in Tangshan Cave, Nanjing

An oxygen isotope temperature record from 381 to 166 kaB. P. (²³⁰Th/²³⁴U dating and tuned ages) has been obtained by combining data on the isotopic composition of calcites with that of fluid inclusions trapped in a stalagmite from a limestone cave in which a fossil cranium deposited. Several laminae in microsequence of the stalagmite represent climatic events or shifts. The Nanjing man fossil was older than 381 kaB. P.     

Osmium isotope determination on mantle-derived peridotite xenoliths from Panshishan with N-TIMS

The¹⁸⁷Os/¹⁸⁸Os ratios of spinel lherzolite xenoliths from Panshishan determined with N-TIMS are lower than that of the primitive mantle, which shows depleted mantle characteristics. Their positive correlation with Al₂O₃/MgO suggests that the geochemical behavior of trace elements Re and Os is similar to that of Al₂O₃ and MgO respectively during the magmatic evolution and Re-Os isotopic system is largely immune to mantle metasomatism. A model age of 2.8–3.4 Ga obtained by¹⁸⁷Os/¹⁸⁸Os-Al₂O₃/ MgO correlation might represent the homogeneous age of the mantle lithosphere beneath the area.     

The neodymium isotopic characteristic and geological significance of Kuokesu plagioclase amphibolites from the Kuruktag, Xinjiang, China

The plagioclase amphibolites from Kuokesu area, Kuruktag, Xinjiang occur as enclaves embedded in the granodioritic gneiss. In the light of major elements and REE data, the parent rocks of the plagioclase amphibolites belong to weak_alkaline basalts. Their Nd model ages mainly range from 2 832 to 3 075 Ma. The seven plagioclase amphibolites yield a reasonable good isochron age of (828±86) Ma(2σ) with I Nd =0.510 981±82, ε Nd ( t )=-11.5±1.6. Such a case shows the existence of great proportion of the Archaean mafic crustal basement on the Kuokesu area. The strong tectonic_thermal event at about 820 Ma made the Sm_Nd isotope of the metamorphic rocks homogenization. This event would be associated with the Tarim Movement.