煤与瓦斯突出预报的模糊聚类关联分析法

首先采用模糊聚类分析对煤与瓦斯突出的样本集合进行分类，建立不同突出程度的模糊模式。然后用关联分析确定待预报样本与模式的关联程度，以此预测预报样本的煤与瓦斯突出危险程度。这种预报方法相对于模糊聚类分类后，将模式与待预报样本组成新的样本集合，再进行聚类分析，以此分类结果进行预报法。不仅可靠程度高，而且能定量描述待报样本与模式的亲和程度。     

25%灰克中速克灵的气相色谱分析

利用气相色谱对速克灵进行定量分析,方法线性相关系数为0.9999,变异系数小于0.8%,平均回收率为100.3%.     

瓦斯隧道煤窑采空区处理施工技术

黄陵二号煤矿铁路专用线白石隧道是一座瓦斯隧道，涧身通过地段有大面积小煤窑采空区分布。从钻孔、灌浆、安全措施、质量保证措施、质量检查等方面阐述了隧道煤窑采空区的处理方法，以供类似工程参考。     

老屋基矿防治煤与瓦斯突出问题的分析和探讨

介绍了老屋基矿采、掘工作面防突措施情况，总结了老屋基矿防治煤与瓦斯突出措施取得的效果。     

柴油机排气呈白色故障排除及分析

以红岩6-250ZCD柴油机故障为例,发现并分析了柴油机排气呈白色的特殊原因,有利于今后故障的快速确诊.     

电增压促进废气再循环对发动机性能的影响

在一台1.5 L带废气涡轮增压的直喷汽油机上进行了电动增压和废气再循环（exhaust gas recirculation, EGR）协同对发动机动力性和经济性的影响规律试验研究。结果表明：全负荷下电动增压促进最高废气再循环率随转速的上升而下降,在4个试验转速下分别提升了17.7%、15.2%、13.84%和0;部分负荷下电动增压促进最高废气再循环率随负荷的提高与转速下降,在6个试验工况下最高废气再循环率分别被提高了23.63%、30.31%、0、14.09%、19.74%和0。全负荷与较低的3个转速下电动增压介入后有效燃油消耗率（brake specific fuel consumption, BSFC）降低近10%,最高转速下废气涡轮增压完全取代电动增压;部分负荷下的两组工况内,电动增压介入后,最高BSFC降低了10.8%和8.4%。结论表明合理应用电增压促进最高废气再循环率可以提升发动机的燃油经济性并保持较高的动力性。     

紫苏微量元素的测定

利用火焰原子吸收涨研究了紫苏根、茎、叶中８种微量元素的含量,并通过实验拟定了各待测元素的最佳分析条件,呼元素的回收率在９６－１０５％之间,相对偏差小于６％,方法快速、准确、实用性强、同时,对紫苏的药理作用进行了探讨,为办的开发提供实验依据。     

High-precision timing of the Quaternary standard samples with thermal ionization mass spectrometry (TIMS) U-series method

Two national stalagmite standard (GBW04412, GBW04413) and one international coral standard (RKM_4) have been determined by using thermal ionization mass spectrometry (TIMS) method. The values of ( 234 U/ 238 U) act , ( 230 Th/ 234 U) act and age are all consistent in error range with the standard values obtained by using α spectrometry.     

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.     

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.