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1)  terpanes and steranes
甾烷和藿烷
1.
The preliminary results show that samples of both categories contained plasticizers,n-alkanes,polycyclic aromatic hydrocarbons(PAHs),oxy-PAHs,and minor amounts of terpanes and steranes.
比较了2006年春季沙尘天气和非沙尘天气吸附到TSP样品中增塑剂、正构烷烃、多环芳烃(PAHs)、甾烷和藿烷类等有机污染组分特征。
2)  hopane
藿烷
1.
The molecular carbon isotope composition (δ13Cmole) of n-alkanes, isoprenoid hydrocarbons, isoalkanes, anti-isoalkanes and hopanes in the oils and source rocks from the West Liaohe Depression are systematically studied.
以辽河西部凹陷潜山带原油及其源岩为例,系统研究了正构烷烃、异戊二烯烷烃、异构与反异构及藿烷系列化合物的碳同位素组成与分布特征,探讨了其相互关系及生源-环境因素的影响。
2.
By using biomarker GC, GC—MS analysis techniques, the geochemical characters of steranes and hopanes from crude oils of Tahe oil field were investigated in this paper.
运用生物标志物色谱质谱技术,对比研究了塔河油田各油区原油生物标志化合物中甾、藿烷系列化合物特征。
3)  sterane
甾烷
1.
Distribution and sources of steranes and pentacyclic triterpanes in surface soils and bottom sediments from Tianjin;
天津地区表层土壤和河流沉积物中甾烷与五环三萜烷的分布特征及污染源分析
2.
Direct evidence of sterane and 4-methyl-sterane originating from plant pollens in organic deposit;
沉积有机质中甾烷、4-甲基甾烷植物花粉来源的直接证据
3.
The biodegradation of regular sterane and rearranged sterane in crude oil was studied on the basis of simulated biodegradation experiment to the crude oil.
通过喜氧细菌对原油的模拟生物降解实验,以及对模拟产物的饱和烃色谱—质谱分析,对原油饱和烃中规则甾烷和重排甾烷的降解作用进行了研究。
4)  steranes
甾烷
1.
Study on steranes as a indicator of oil spills;
甾烷作为溢油指示物(或指标)的研究
2.
Study on Steranes as Indicators of Spilled Oi1s by Fuzzy Clustering Analysis;
甾烷作为溢油指示物的模糊聚类分析研究
3.
The results of pyrolysis experiments, performed in confined system (gold capsule) demonstrate that maturation behaviors of hopanes (hopenes) and steranes released from kerogen change substantially with the variation of water amount and mineral nature.
C3122S/(22R+22S)升藿烷和C2920S/(20R+20S)和C29αββ/(ααα+αββ)甾烷比值都先从240℃至280℃降低,然后从280℃至320℃升高。
5)  ββ hopenes
ββ藿烷
1.
Compound specific isotopic analysis (CSIA) in combination with conventional organic geochemical investigation of ββ hopenes from 8 immature samples (6 peat samples, 1 source rock sample and 1 shale sample) representing various kerogen types, depositional environments were conducted.
应用单烃碳稳定同位素分析(CSIA) 技术,研究南方泥炭等8 个样品溶剂可抽提部分中的ββ藿烷化合物的成因联系- 结果表明,ββ藿烷是细菌藿多醇特别是藿四醇在成岩作用极早期经细菌改造的产物- 改造过程中,侧链的断裂会导致同位素分馏,通常会导致藿类环系相对富集13C
6)  bishomohopane
双高藿烷
补充资料:藿烷

藿烷hopane

五环三萜类中分布较广泛的生物标志物,藿烷类化合物主要反映原核微生物(细菌)的输入.南极湖泊样品超临界流体萃取物中检测到丰富的藿烷类化合物.有三降藿烷,降藿烷,藿烷,升藿烷,二升藿烷,三升藿烷等,还检测到了丰度较低的伽玛蜡烷.

这类化合物是石油和煤中常见的生物标志物。藿烷不是由生物体直接合成的,而是由死亡生物体经地球化学过程演化而来的.在早期成岩作用过程中形成的饱和烃类藿烷在构型上均以生物构型(r型)为主.在成岩过程中藿烷类化合物由生物构型逐渐转变为地质构型(s型),最后达到s型与r型的平衡状态[s/(s+r)=0.6].在水样中检出藿烷,而且22s/(22s+22r)17琢(h)21茁(h)构型升藿烷比值大于0.5,可以推断饮用水源水体已受到化石燃料的污染.

原核生物与真核生物的最大区别就是其细胞膜中一般不含胆固醇,而是含有hopanoid(藿烷类化合物 )。

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