metamict state

简明释义

异变态

英英释义

A metamict state refers to a condition in which a crystalline material, typically a mineral, becomes amorphous due to the damage caused by radiation, leading to a loss of its original structure.

变质状态是指一种晶体材料(通常是矿物)由于辐射造成的损伤而变得无定形,从而失去其原有结构的状态。

例句

1.The metamict state of certain minerals can affect their optical properties significantly.

某些矿物的变质状态会显著影响其光学特性。

2.The mineral underwent a transformation into a metamict state due to prolonged radiation exposure.

该矿物因长期辐射暴露而转变为变质状态

3.The stability of the crystal structure is lost when a material enters a metamict state.

当材料进入变质状态时,其晶体结构的稳定性会丧失。

4.When analyzing the sample, we discovered it was in a metamict state, complicating our findings.

在分析样本时,我们发现它处于变质状态,这使我们的发现变得复杂。

5.Researchers are studying the properties of zircon in its metamict state to understand its geological history.

研究人员正在研究锆石在其变质状态下的特性,以了解其地质历史。

作文

The study of materials and their properties has always been a fascinating aspect of science. One particularly interesting phenomenon is the metamict state, which refers to the disordered state of certain minerals, particularly those containing uranium or thorium, that have undergone radiation damage over time. In essence, the metamict state represents a transition from a crystalline to an amorphous structure due to the effects of radioactive decay. This transformation can significantly alter the physical and chemical properties of the material, making it an important subject of study in geology and materials science.When minerals like zircon or monazite contain radioactive elements, they gradually accumulate damage from emitted particles, leading to the metamict state. This state is characterized by a loss of long-range order within the crystal lattice, resulting in a material that is less stable and more susceptible to environmental changes. Understanding the metamict state is crucial for geologists, as it can provide insights into the history of the Earth and the processes that have shaped its crust.Moreover, the implications of the metamict state extend beyond geology; they also impact fields such as nuclear waste management and materials engineering. For example, when considering the disposal of nuclear waste, scientists must account for the potential for materials to enter a metamict state over time. This knowledge helps in predicting the longevity and safety of containment strategies, ensuring that hazardous materials do not pose a risk to the environment.In addition, the metamict state can influence the performance of materials used in various applications. For instance, zircon, often used in ceramics and electronics, may exhibit altered properties when it transitions to a metamict state. This change can affect its durability, thermal stability, and overall functionality. Thus, researchers are keen to understand how to mitigate these effects and maintain the integrity of materials subjected to radiation.Furthermore, the study of the metamict state opens up new avenues for research into the synthesis of novel materials. By mimicking the conditions that lead to this state, scientists can potentially create new compounds with desirable properties for use in technology and industry. This innovative approach highlights the importance of understanding the fundamental processes that govern material behavior at the atomic level.In conclusion, the metamict state is a complex and multifaceted phenomenon that holds significant implications across various scientific disciplines. From providing insights into geological processes to influencing the safety and performance of materials in engineering applications, the study of the metamict state is essential for advancing our knowledge and capabilities in both natural and applied sciences. As research continues to evolve, we can expect to uncover even more about this intriguing state of matter, further solidifying its importance in the scientific community.

材料及其性质的研究一直是科学中一个引人入胜的方面。一个特别有趣的现象是变质状态,它指的是某些矿物(特别是那些含有铀或钍的矿物)由于时间的辐射损伤而发生的无序状态。本质上,变质状态代表了由于放射性衰变的影响,从晶体结构转变为无定形结构的过程。这种转变可以显著改变材料的物理和化学性质,使其成为地质学和材料科学中重要的研究对象。当锆石或独居石等矿物含有放射性元素时,它们会逐渐积累来自发射粒子的损伤,导致进入变质状态。这种状态的特征是晶格内长程有序性的丧失,导致材料不再稳定,更容易受到环境变化的影响。理解变质状态对地质学家至关重要,因为它可以提供有关地球历史及其地壳形成过程的见解。此外,变质状态的影响超越了地质学;它们还影响核废料管理和材料工程等领域。例如,在考虑核废料处置时,科学家必须考虑材料随着时间的推移可能进入变质状态的潜力。这一知识有助于预测封存策略的持久性和安全性,确保有害材料不会对环境构成风险。此外,变质状态还可以影响用于各种应用的材料的性能。例如,锆石通常用于陶瓷和电子产品,当它过渡到变质状态时,其性质可能会发生变化。这种变化可能影响其耐久性、热稳定性和整体功能。因此,研究人员非常希望了解如何减轻这些影响,并保持受辐射材料的完整性。此外,变质状态的研究为合成新材料开辟了新的研究途径。通过模拟导致这种状态的条件,科学家们有可能创造出具有所需特性的新的化合物,用于技术和工业。这种创新方法突显了理解支配材料行为的基本过程在原子水平上的重要性。总之,变质状态是一个复杂而多面的现象,对各个科学学科都有重要的影响。从为地质过程提供见解到影响工程应用中材料的安全性和性能,研究变质状态对于推动我们在自然科学和应用科学中的知识和能力至关重要。随着研究的不断发展,我们可以期待揭示更多关于这一引人入胜的物质状态的内容,进一步巩固其在科学界的重要性。