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.     

选择性催化氧化H2S的催化剂研究

在考察了几种单组分氧化物把硫化氢催化氧化为单质硫的基础上，采用共沉淀法合成了3种复合氧化物催化剂A，B，C，并考察了它们的催化活性和选择性．结果表明，在一定条件下，催化剂B的转化率和选择性分别在90％和97％以上，在40h的催化性能稳定性测试中，其转化率和选择性均能保持稳定，具有良好的催化性能．     

冶炼工业废气中SO_2的脱除研究

研究用软锰矿的水悬浮液脱除冶炼工业废气中SO_2的工艺可行性,提出抑制副产物MnS_2O_6生成的途径。     

CoCl（CNPh）2（pph3）2的制备,结构和性质

由ＣｏＣｌ（ＰＰｈ３）３与过量ＰｈＮＣＳ在苯溶液中的反应制备出一种流的Ｃｏ（Ｉ）的五配位配合物．根据红外，１Ｈ核磁共振、快原子轰击质谱、ｘ电子能谱及元素分析结果确定其分子式为ＣｏＣｌ（ＣＮＰｈ）２（ＰＰｈ３）２与类似的配合物比较，推断该配合物具有三角双锥结构，其中两个大体积的叔膦基成轴间配位．从ｄ－ｐ户反馈π键度讨论了ＩＲ及１ＨＮＭＲ．此外，也对该回合物的溶解性、热稳定性以及对Ｏ２的稳定性加以了描述．     

六氟化硫气体特性及安全运行管理

着重从六氟化硫气体自身特性出发,结合引黄工程使用六氟化硫气体组合开关的实际情况,探讨了六氟化硫气体在引黄工程中的安全运行管理问题.     

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.