Profile of the composition fractions in neutron stars

The composition fractions of β-stable neutron stars and their radial distributions are investigated based on Skyrme-Hartree-Fock theory and Tolman-Oppenheimer-Volkoff (TOV) equation. It is found that a pure neutron interior with a radius of 3.5 km can exist in the neutron stars. When the radius is greater than 3.5 km, the fractions of the proton, electron and μ⁻ appear and increase with the increment of the radius, then decrease after reaching their maximum at the radius of 8 km. These results make it possible to further study the thermal evolution and magnetic properties of the neutron stars.     

Hf isotopic compositions of the standard zircons for U-Pb dating

Zircon, a common accessory mineral in various kindsof rocks, is an important subject for U-Pb isotopic dating.With requirements for high spatial resolution with highprecision and accuracy, SHRIMP (Sensitive High Resolu-tion Ion Micro Probe) and LA-ICPMS (Laser AblationInductively Coupled Plasma Mass Spectrometry) nowserve as the important tools in zircon U-Pb dating. Sinceboth methods need standard zircon for external age cali-bration, an ideal standard zircon is critical for obtai…     

Hf isotopes of the 3.8 Ga zircons in eastern Hebei Province, China： Implications for early crustal evolution of the North China Craton

Zircon U-Pb dating indicates that the fuchsite quartzite in eastern Hebei Province was derived from weathering and erosion of the 3.6-3.8 Ga granitic rocks. In-situ zircon Hf analyses show that the Lu-Hf isotopic system remained closed during later thermal disturbances. Zircons with concordant ages have Hf isotopic model ages of about 3.8 Ga, suggesting a recycling of this ancient crust. The -3.8 Ga zircons have similar Hf isotopic compositions to those of chondrite, indicating that their source rocks （granitic rocks） were derived from partial melting of the juvenile crust which originated from a mantle without significant crust-mantle differentiation. Therefore, it is proposed that there was no large-scale crustal growth before -3.8 Ga in eastern Hebei Province. Considering zircon Hf isotopic data from other areas, it is concluded that the most ancient crust in the North China Craton probably formed at about 4.0 Ga, and the possibility to find crust older than 4.0 Ga is very limited.     

ISOSPIN EQUILIBRIUM AND NONEQUILIBRIUM IN INTERMEDIATE ENERGY HIC

采用同位旋相关的ＱＭＤ模型探讨了同位旋的平衡与非平衡．此ＱＭＤ模型包含了同位旋相关的对称能、库仑能、Ｎ－Ｎ截面和Ｐａｕｌｉ阻塞．观察到随着入射能量超过某一阀能存在着同位旋由平衡到非平衡的跃迁，发现这种现象是由不同反应机制的共存与竞争所导致的，即当ＩＣＦ（非完全熔合）分量占主导时同位旋平衡能够达到，而当碎裂分量占主导时同位旋平衡受到破坏．     

小型引力波天线隔振装置研究

本文对三级隔振装置进行了研究,该隔振装置是为23kg小型引力波捧状天线而设计制造的。分析表明,该隔振装置的透过率在5000Hz处为10~(-18)量级,满足引力波天线的隔振要求。     

AM/DMDAAC共聚水凝胶的电场敏感性能

 为研究阳离子性DMDAAC共聚物水凝胶的电场敏感性能,以丙烯酰胺(AM)和二甲基二烯丙基氯化铵(DMDAAC)为单体,N,N'-亚甲基双丙烯酰胺为交联剂,过硫酸铵和亚硫酸氢钠为氧化还原引发剂,采用水溶液聚合法制备了AM/DMDAAC共聚物水凝胶,考查样品水凝胶在外加直流电场刺激下的消溶胀动力学和弯曲行为。研究表明,DMDAAC单体含量、施加电压的时间和施加电压大小以及所在溶液的离子强度对水凝胶的电敏感性能有着显著影响,有望使其在化学阀、仿生驱动器方面得到应用。在低浓度NaCl溶液中向正极弯曲,随着NaCl质量分数的增加,向正极弯曲角度逐渐减小,并进一步向负极弯曲。影响凝胶弯曲角度转变的临界NaCl质量分数为0.3%—0.4%,不同的单体配比,其临界NaCl质量分数也不一样。     

Petrogenesis of the Neoproterozoic bimodal volcanic rocks along the western margin of the Yangtze Block： New constraints from Hf isotopes and Fe/Mn ratios

High-precision major element and Hf isotope data are reported for the Neoproterozoic Suxiong volcanic rocks along the western margin of the Yangtze Block. These volcanic rocks have variable εHf（T） values and Fe/Mn ratios. The relatively primitive basalts have high Fe/Mn ratios and high Hf-Nd isotopic compositions, indicating that they were generated by partial melting of garnet clinopyroxene in mantle plume at high pressure. Thus, the Suxiong basalts are genetically related to the proposed Neoproterozoic superplume. On the contrary, a few differentiated basalts have low Fe/Mn ratios and low Hf-Nd isotopic compositions. They are likely to experience assimilation-fractional crystallization process. The Suxiong rhyolites have consistent Hf and Nd model ages of 1.3-1.4 Ga. They are likely generated by shallow dehydration melting of pre-existing young arc igneous rocks associated with the basaltic underplating/intrusion in a continental rift.     

Hf isotopes of zircon megacrysts from the Cenozoic basalts in eastern China

Cenozoic basalts are widely distributed in eastern China, and some of them contain zircon megacrysts which are considered to be constituent mineral of the subcontinental lithospheric mantle （SCLM） and petrogenetically related to mantle metasomatism induced by addition of crustal materials. Using the Laser Ablation Multiple Collector Inductively Coupled Plasma Mass Spectrometry （LA-MC-ICPMS）, zircon megacrysts from the Cenozoic basalts at Changle in Shandong, Mingxi in Fujian, and Penglai in Hainan provinces have been used for Hf isotopic analyses. The data indicate that there is no significant deviation for the different zircon grains in each locale, except those from Penglai. The obtained ^176Hf /^177Hf ratios are 0.28302- 0.28308 for Changle, 0.28297-0.28300 for Mingxi, and 0.28288-0.28293 for Penglai, with corresponding ear values of 8.7-10.8, 7.0-7.9, and 3.9-5.7, respectively. These data display that there existed some regional heterogeneity, but the Hf model ages clustere in the Phanerozoic. Therefore, it is inferred that metasomatism of the lithospheric mantle beneath eastern China took place in the Phanerozoic, most probably in the Mesozoic-Cenozoic. However, the formation time of the iithospheric mantle is not clearly constrained based on the present Hf isotopic data.     

AMPS/DMAEMA共聚水凝胶合成与性能

以AMPS和DMAEMA为共聚单体,N,N'-亚甲基双丙烯酰胺为交联剂,采用静置水溶液聚合法合成AMPS/DMAEMA共聚物水凝胶。在反应温度30℃,经正交实验研究了合成反应的工艺条件:交联剂用量4.0wt%,引发剂用量0.5wt%,单体总浓度0.2g/mL,AMPS:DMAEMA=3:7(质量比)。该凝胶对离子强度、pH值均表现出了显著的体积突变现象,体积相变发生在离子强度I和pH值分别为0.1和4左右,但随温度变化的体积突变不明显。