基于最小矩阵距离准则的一种群体决策方法

在分析了基于层次分析法的群体决策方法的类型、评价准则后,提出了一种基于最小矩阵距离准则的群体决策方法。该方法应用一个矩阵空间上的距离公式,将求群体判断矩阵的问题看成为求与各个体判断矩阵的距离之和为最小的矩阵的问题,然后又进一步等价为目标规划问题。该方法比较直观可信,因而容易说服各评判者接受由该方法得到的群体判断矩阵。     

WC—Co硬质合金刀片热丝法金刚石薄膜涂层附着力

用热丝法研究了ＷＣ－６％Ｃｏ硬质合金刀片金刚石薄膜涂层附着力。结果表明：采用温度为８０℃,（ＨＣｌ：ＨＮＯ３：Ｈ２Ｏ）（体积比）为１∶１∶１溶液对硬质合金刀片表面去Ｃｏ１５ｍｉｎ后,经４０ｕｍ金刚石粉及１．５ｕｍ金刚石加２０ｕｍＴａＣ混合粉进行超声预处理,结果表明,沉积的金刚石薄膜与硬质合金刀片基底具有良好的附着力,而经４０ｕｍ金刚石粉处理的薄膜涂层组织与附着力要好一些。     

ZrO2-ZiCrAl系功能梯度热障涂层界面残余热应力研究

研究用等离子喷涂方法制备Ｚｒｏ２－ＮｉＣｒＡｌ系功能梯度热障涂层的不同梯度过渡层之间,以及与基体之间界面的残余热应力和功能梯度热障涂层厚度、组分对残余热应力的影响．方法来用热弹性有限元方法．结果所设计的功能梯度热障涂层的界面残余热应力得到有效缓和．结论对于所要保护的基体,可用有限元数值分析结果选择适当的功能梯度材料体系．     

功能梯度材料的基体与颗粒界面热应力研究

研究金属－陶瓷功能梯主材料的基体与颗粒的界面热应力。方法给出功能制备的有限元计算优化设计方案,针对所制备的梯度材料的结构特点,采用双层嵌套模型研究基体与颗粒的界面热应力与两相材料体积分数的变化关系。     

土法造纸木素降解之探索Ⅲ.嫩毛竹自然发酵过程中的细菌分离鉴定与嫩竹软化菌的筛选

试验证实,嫩毛竹自然发酵过程中的微生物主要是细菌。分离出并纯化了１００株细菌,其中６０株是芽胞杆菌。将分离出的１００株细菌分别接入石灰预处理过的嫩竹,从中筛选出能使嫩竹进一步软化的菌株３株,也均为芽胞杆菌。对这６０株芽胞杆菌进行了形态学及其生理生化特征的鉴定,按Ｐｒｉｅｓｔ氏等（１９８８年）的数值分类系统分类到组,将３株（３０８,３０９,３１０）对嫩竹软化有明显作用的芽胞杆菌的１株（３０８）鉴定到种,认为是短小芽胞杆菌（Ｂ．ｐｕｍｉｌｕｓ）。另外４０株非芽胞杆菌参阅《伯杰氏系统细菌学手册》第１卷和第２卷,鉴定到科或属,有微球菌、葡萄球菌、李氏杆菌、不动杆菌、肠杆菌科等。     

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.     

Leakage of mantle helium from the Liaodong Peninsula, China

The isotopic cumpositions of helium have been investigated in hot spring gases sampled from the Liaodong Peninsula. China. The³He/⁴He ratios range from 0.14 Ra (0.14 times the atmospheric³He/⁴He ratio of 1.40 × 10^-6 to 0.72 Ra.³He/⁴He versus⁴He/²⁰Ne ratios and He contents suggest that a small amount of mantle-derived helium reaches the earth’s surface. Helium iwtope ratios of the hot spring gases show a distribution pattern similar to the regional heat flow values, indicating that the positive thermal anomaly occurring in the rtrea is closely associated with the presence of mantle-derived helium. The observations described above provide some significant evidence that the molten magma originating from partial melting of the upper mantle may have intruded into the continental crust along the activity fault. The coupling of the presence of mantle He and heat flow anomalies to seismic activity in studied region seem to imply that there is an internal relationship between mantle degassing and seismic activity.