熵增大原理的论证

本文以理想气体的行为为手段引出熵函数,并以热力学第一定律为基础,论证了熵增大原理.这种论证为学生理解这一原理打下坚实的基础.     

氨水法在烧结烟气脱硫中的应用

文章介绍了一种用稀氨水吸收炼钢厂烧结烟气的脱硫工艺，并对其工艺流程、工艺特点及其优势进行了详细论述。     

低气压气体放电电子束机理的探讨

本文在实验研究的基础上，对气体放电电子束的形成机理和物理模型提出了的见解，并以此为依据对电子束的能谱进行了模拟，实验结果与理论符合很好。     

焦炉集气管压力优化控制策略

以唐山钢铁(集团)有限公司炼焦制气厂1号、2号焦炉集气管工艺过程为例，介绍了一种普遍适合于钢铁企业焦炉集气管压力调节的控制策略。     

煤气共采、综合开发探讨

对煤气共采、综合开发作了初步探讨，指出综合开发是山西煤层气开发的首选之路。     

论非理想费米气体的低温排斥作用

用腰势法讨论低温下非理想费米气体的排斥势占优势时的配分函数、基态压强等，并研究气体的磁化率与温度的关系，从而定量地解释了非理想费米气体具有较强磁化率的原因。     

速克灵与百菌清混合制剂的分析方法研究

论述了在同一气相色谱条件下测定速克灵、百菌清混合制剂中有效成分含量的方法。该法简单、快速、准确。速克灵(pmcymibone)、百菌清(chlorothanil)变异系数分别为2．1，0．66，回收率分别为98．0％～100．6％和99．3％～100．8％，线性相关系数分别为0．9500和0．9987。     

Dating formation of natural gas pools using fluid inclusion data from reservoirs

A method has been suggested which is based on the homogenization temperatures and other data of fluid inclusions from a reservoir rock, with the combination of burial and geothermal history of the hosted rock, to date the gas reservoir formation. On the basis of this, a case study of the Carboniferous-Permiangas pools in the Ordos Basin has been conducted. The results have shown that the reservoir sandstones of the gas pool were filled by gases during 125-150 Ma, earlier in the southern area and later in the northern area, which is consistentwith the basin's geological and geochemical background under which the gas pools formed.     

电子束照射法治理燃煤发电厂废气技术研究

在阐明电子束照射法脱硫脱氮技术的机理、流程、特点的基础上，探讨了该工艺在应用于燃烧发电厂废气治理过程中存在的主要经济、技术问题.     

Geochemical characteristics and formation process of natural gas in Kela 2 gas field

 On the basis of a large amount of natural gascomponents and the carbon isotope as well as some otheranalysis data in Kela 2 gas field, the geochemical character-istics, source, origin, and formation process of natural gashave been discussed. The components of gas in the field tendto be "dry", and the drying coefficient is close to 1.0. Thecarbon isotope tends to be heavier, for instance, the averageof δ¹³C₁ is -27.36‰ and that ofδ¹³C₂ is -18.5‰. Compre-hensive analysis shows that humic natural gas in the Kuqapetroleum system comes mainly from Triassic and Jurassicsource rocks, and the contribution of Jurassic source rocks tothe pool maybe is more than that of Triassic rocks. The maincause that the gas tends to be dry and bears heavier isotopecomposition lies in the fact that Kela 2 natural gas is the ac-cumulation of late production of humic source rocks, and itis affected by the abnormal high pressure as well. Consider-ing the hydrocarbon generating and structural history, wecan regard the gas pool formation processes as twice fillingand twice adjusting (destroying), that is, the filling anddestroying process in the early Himalayan movement and thefilling and adjusting in the late Himalayan movement.