1) Acid-Rock Reaction
酸-岩反应
1.
The oil in Ordovician carbonate reservoirs experienced intense degradation,but the followed acid-rock reaction consumed almost all the early organic acids and depressed the oil acidity.
奥陶系碳酸盐岩油藏原油曾经历严重降解,但产生的大量有机酸在随后的酸-岩反应中被消耗,呈高降解低酸值特征,侏罗系、三叠系、石炭系原油酸值的形成主要与地层水活动造成的晚期降解有关。
2.
The Study on Rheological Properties of Visco-Elastic Surfactant Diverting Acid and the Kinetics of Its Acid-Rock Reaction;
但是,该体系的流变性能及其影响因素的系统研究和酸-岩反应动力学研究还没有见到文献报道,从而制约了VES转向酸体系性能的更好发挥和新型VES体系的开发以及施工的优化设计。
2) acid/rock reaction
酸岩反应
1.
The experimental methods of acid/rock reactions were presented briefly and the expressions for parameters of acid/rock reaction kinetics were discussed.
简述了酸岩反应实验方法,讨论了酸岩反应动力学参数的表达式。
3) thermochemical sulphate reduction(TSR)
硫酸盐岩热化学反应(TSR)
4) water-rock reaction
水岩反应
1.
The development of super-viscous oil with steam stimulation is greatly effected by water-rock reaction under high temperature.
高温水岩反应对超稠油的蒸汽吞吐开发影响很大,为了提高超稠油的开发效果,从油藏地质条件和开采方法及效果分析入手,对现场取得的岩心进行了X射线衍射分析,对地层水、蒸汽冷凝水进行离子分析。
2.
The factors of influencing reservoir properties include water-rock reaction,water-liquid reaction,petroleum composition variation and asphalt deposition when steam and hot water migrate in heavy oil formation.
利用高温高压物理模拟实验,研究了河南油田稠油储层注蒸汽过程中的水岩反应、水液反应、原油组分变化和沥青沉积等因素引起的储层物性变化。
6) water-rock interaction
水-岩反应
1.
Chemical compositions of surface and ground waters of Guiyang city: discussion of water-rock interaction and contamination in karstic hydrological system;
贵阳市地表水地下水化学组成:喀斯特水文系统水-岩反应及污染特征
2.
On the basis of geological and geochemical characteristics of the Yinshan polymetallic deposit, Jiangxi province, and from the view point of water-rock interaction and related isotope exchange, the present paper queries the validity of the conclusion that magmatic water was the main origin of ore-forming fluid in Yinshan deposit, which was proposed by some previous studies.
本文以银山矿床的地质地球化学特征为依据，以水－岩反应及其同位素交换为出发点，对前人关于该矿床成矿流体主要来自岩浆水的结论提出质疑。
3.
The geochemical behaviors of oxygen and hydrogen isotopes in water-rock interaction are discussed.
论证了开放体系单阶段和二阶段水-岩反应中氧同位素行为接近于封闭体系氧同位素交换演变轨迹，具有成因指示意义，但不具定量意义。
补充资料：二十二烷酸与硬脂酸和四聚乙二胺的反应产物
CAS：68442-88-6
分子式：C22H44O2·C18H36O2·C8H23N5
中文名称：二十二烷酸与硬脂酸和四聚乙二胺的反应产物
英文名称：Behenic acid, stearic acid, tetraethylene pentamide docosanoic acid, reaction products with stearic acidand
分子式：C22H44O2·C18H36O2·C8H23N5
中文名称：二十二烷酸与硬脂酸和四聚乙二胺的反应产物
英文名称：Behenic acid, stearic acid, tetraethylene pentamide docosanoic acid, reaction products with stearic acidand
说明：补充资料仅用于学习参考，请勿用于其它任何用途。
参考词条