deomethyl hopane

简明释义

脱甲基藿烷;

英英释义

Deomethyl hopane is a type of triterpenoid hydrocarbon, specifically a derivative of hopane, characterized by the absence of a methyl group at a specific position in its molecular structure.

去甲基霍潘是一种三萜烃,特指霍潘的衍生物,其分子结构在特定位置缺少一个甲基团。

例句

1.Researchers found that deomethyl hopane levels can help in oil exploration.

研究人员发现,去甲基霍潘水平可以帮助石油勘探。

2.The identification of deomethyl hopane in rock samples can reveal past environmental conditions.

在岩石样本中识别出去甲基霍潘可以揭示过去的环境条件。

3.The presence of deomethyl hopane indicates a specific type of geological formation.

存在去甲基霍潘表明一种特定类型的地质构造。

4.In the sediment samples, the concentration of deomethyl hopane was significantly high.

在沉积物样本中,去甲基霍潘的浓度显著较高。

5.Geochemists often analyze deomethyl hopane to understand the maturation of organic matter.

地球化学家经常分析去甲基霍潘以了解有机物的成熟过程。

作文

In the field of organic geochemistry, the term deomethyl hopane refers to a specific type of hopane compound that has been subjected to demethylation. Hopanes are pentacyclic triterpenoids that are commonly found in sedimentary rocks and are often used as biomarkers for the geological age of sediments and the thermal maturity of organic matter. The process of demethylation involves the removal of methyl groups from the molecule, which can significantly alter its chemical properties and biological significance. Understanding deomethyl hopane is crucial for geologists and paleontologists alike, as it can provide insights into ancient environments and the biological processes that occurred millions of years ago.The significance of deomethyl hopane lies in its ability to serve as a reliable indicator of the depositional environment of organic matter. For instance, the presence of deomethyl hopane in a rock sample may suggest that the organic material underwent specific diagenetic processes, which can be linked to certain types of depositional environments, such as marine or freshwater settings. This information is invaluable for reconstructing past climates and understanding the evolution of life on Earth.Moreover, the study of deomethyl hopane can aid in the exploration of petroleum resources. As hydrocarbons are formed from organic matter over geological time, the presence of specific hopanes, including deomethyl hopane, can indicate the potential for oil and gas reserves in a given area. By analyzing the concentration and distribution of these compounds, geologists can make informed predictions about where to drill for fossil fuels.In addition to its geological implications, deomethyl hopane also plays a role in environmental science. The analysis of hopanes in sediment cores can help researchers understand the impact of human activities on ecosystems. For example, increased levels of deomethyl hopane in sediment layers may correlate with industrial pollution or oil spills, providing a historical record of environmental changes over time.Furthermore, the study of deomethyl hopane contributes to our understanding of microbial activity in ancient environments. Certain microorganisms are known to produce hopanes as part of their metabolic processes, and the presence of deomethyl hopane can indicate the types of microbial communities that existed in the past. This knowledge enriches our comprehension of the evolution of life and the complex interactions between organisms and their environments throughout Earth’s history.In conclusion, the term deomethyl hopane encapsulates a wealth of information relevant to various scientific disciplines, including geology, paleontology, and environmental science. Its significance as a biomarker for ancient organic matter, an indicator of petroleum potential, and a record of environmental change underscores the importance of studying this compound. As research continues to evolve, the insights gained from deomethyl hopane will undoubtedly enhance our understanding of Earth’s past and inform our approaches to managing natural resources and protecting the environment in the future.

在有机地球化学领域,术语deomethyl hopane指的是一种特定类型的霍潘化合物,该化合物经历了去甲基化过程。霍潘是一种常见于沉积岩中的五环三萜类化合物,通常用作沉积物地质年龄和有机物热成熟度的生物标志物。去甲基化过程涉及从分子中去除甲基基团,这可以显著改变其化学性质和生物学意义。理解deomethyl hopane对地质学家和古生物学家来说至关重要,因为它可以提供关于数百万年前古代环境和生物过程的见解。deomethyl hopane的重要性在于它能够作为有机物沉积环境的可靠指标。例如,岩石样本中deomethyl hopane的存在可能表明有机物经历了特定的成岩过程,这可以与某些类型的沉积环境(如海洋或淡水环境)相关联。这些信息对于重建过去的气候和理解地球上生命的演变是无价的。此外,deomethyl hopane的研究可以帮助探索石油资源。随着烃类物质在地质时间内由有机物形成,特定霍潘的存在,包括deomethyl hopane,可以指示某一地区潜在的油气储量。通过分析这些化合物的浓度和分布,地质学家可以对钻探化石燃料的地点做出明智的预测。除了其地质意义外,deomethyl hopane在环境科学中也发挥着作用。沉积物核心中霍潘的分析可以帮助研究人员理解人类活动对生态系统的影响。例如,沉积层中deomethyl hopane水平的增加可能与工业污染或石油泄漏相关,为历史环境变化提供了记录。此外,deomethyl hopane的研究有助于我们理解古代环境中的微生物活动。某些微生物已知会在其代谢过程中产生霍潘,而deomethyl hopane的存在可以指示过去存在的微生物群落类型。这些知识丰富了我们对生命演化及其与地球历史上复杂的生物与环境相互作用的理解。总之,术语deomethyl hopane蕴含着与多个科学学科相关的大量信息,包括地质学、古生物学和环境科学。作为古代有机物的生物标志物、石油潜力的指示器以及环境变化的记录,其重要性凸显了研究这一化合物的必要性。随着研究的不断发展,从deomethyl hopane中获得的见解无疑将增强我们对地球过去的理解,并为未来管理自然资源和保护环境提供指导。