phyllosilicate

简明释义

英[ˌfɪləʊˈsɪlɪkeɪt]美[fɪləˈsɪlɪkeɪt]

n. [矿物] 页硅酸盐，[土壤] 层状硅酸盐

英英释义

单词用法

同义词

反义词

例句

1.Based on the Numbers of layer charge of phyllosilicate with expansive layers (PSEL), expansive layers are classified as montmorillonite layers and vermiculite layers.

依据含膨胀性晶层层状硅酸盐矿物(PSEL)层电荷的大小把膨胀性晶层分为蒙皂石晶层和蛭石晶层两类。

2.Based on the Numbers of layer charge of phyllosilicate with expansive layers (PSEL), expansive layers are classified as montmorillonite layers and vermiculite layers.

依据含膨胀性晶层层状硅酸盐矿物(PSEL)层电荷的大小把膨胀性晶层分为蒙皂石晶层和蛭石晶层两类。

3.The invention provides a biodegradable material composition, which contains polylactic acid, organic phyllosilicate and natural fiber containing coupling agent.

本发明提供了一种可生物降解材料组合物，该组合物含有聚乳酸、有机层状硅酸盐和含有偶联剂的天然纤维。

4.The mineral composition of the rock includes a significant amount of phyllosilicate 层硅酸盐, which contributes to its unique properties.

这块岩石的矿物成分包含了大量的phyllosilicate 层硅酸盐，这使其具有独特的性质。

5.In soil science, the presence of phyllosilicate 层硅酸盐 minerals can influence the soil's ability to retain water.

在土壤科学中，phyllosilicate 层硅酸盐 矿物的存在会影响土壤保持水分的能力。

6.Geologists often study phyllosilicate 层硅酸盐 structures to understand the metamorphic processes of rocks.

地质学家经常研究phyllosilicate 层硅酸盐 结构，以了解岩石的变质过程。

7.The clay minerals in the sample are primarily phyllosilicate 层硅酸盐 types, such as kaolinite and montmorillonite.

样品中的粘土矿物主要是phyllosilicate 层硅酸盐 类型，例如高岭土和蒙脱石。

8.Researchers are exploring the role of phyllosilicate 层硅酸盐 in the formation of certain types of clay deposits.

研究人员正在探讨phyllosilicate 层硅酸盐 在某些类型粘土沉积物形成中的作用。

作文

Phyllosilicates are a fascinating group of minerals that play a crucial role in various geological and environmental processes. These minerals, characterized by their layered structure, are primarily composed of silicate tetrahedra and octahedra. The term phyllosilicate (层状硅酸盐) refers to their unique arrangement, where sheets of these tetrahedra and octahedra are stacked together, resulting in a two-dimensional framework. This structure not only gives them distinctive physical properties but also influences their chemical behavior. One of the most well-known examples of phyllosilicate (层状硅酸盐) minerals is mica, which is commonly found in igneous and metamorphic rocks. Mica exhibits perfect cleavage, allowing it to be easily split into thin sheets. This property is due to the weak van der Waals forces that hold the layers together, making it an excellent material for various applications, including electronics and cosmetics. Another important phyllosilicate (层状硅酸盐) mineral is clay, which is ubiquitous in sedimentary environments. Clays are essential for soil formation and provide vital nutrients to plants. Their ability to retain water and nutrients makes them a key component of fertile soils. The study of phyllosilicate (层状硅酸盐) minerals is not only important for understanding the Earth's crust but also has significant implications for environmental science. For instance, the interactions between phyllosilicate (层状硅酸盐) minerals and pollutants can influence the mobility and bioavailability of heavy metals in soils and water bodies. This knowledge is crucial for developing strategies to remediate contaminated sites and protect ecosystems. Furthermore, phyllosilicate (层状硅酸盐) minerals are also involved in the carbon cycle. Certain types of clays can capture carbon dioxide, thereby playing a role in mitigating climate change. The ability of these minerals to sequester carbon highlights their importance in sustainable practices and environmental management. In addition to their environmental significance, phyllosilicate (层状硅酸盐) minerals have various industrial applications. They are used in the manufacture of ceramics, rubber, and paints due to their unique properties such as plasticity, thermal stability, and chemical resistance. The versatility of phyllosilicate (层状硅酸盐) minerals makes them invaluable in many industries, contributing to technological advancements and economic development. In conclusion, the study of phyllosilicate (层状硅酸盐) minerals provides insights into fundamental geological processes and offers practical solutions to environmental challenges. Their layered structure and unique properties make them essential components of the Earth's system and valuable resources for human society. As we continue to explore and understand these remarkable minerals, we uncover new opportunities for sustainable development and environmental stewardship.

层状硅酸盐是一组迷人的矿物，它们在各种地质和环境过程中发挥着至关重要的作用。这些矿物以其层状结构为特征，主要由硅酸盐四面体和八面体组成。术语phyllosilicate（层状硅酸盐）指的是它们独特的排列方式，其中这些四面体和八面体的片层相互叠加，形成二维框架。这种结构不仅赋予它们独特的物理特性，还影响它们的化学行为。 最著名的phyllosilicate（层状硅酸盐）矿物之一是云母，它通常存在于火成岩和变质岩中。云母表现出完美的解理，使其易于分裂成薄片。这一特性源于保持层之间的弱范德华力，使其成为电子和化妆品等各种应用的优良材料。另一种重要的phyllosilicate（层状硅酸盐）矿物是粘土，它在沉积环境中普遍存在。粘土对土壤形成至关重要，并为植物提供重要营养。它们保持水分和营养的能力使其成为肥沃土壤的关键组成部分。 对phyllosilicate（层状硅酸盐）矿物的研究不仅对理解地壳有重要意义，而且对环境科学也具有重大影响。例如，phyllosilicate（层状硅酸盐）矿物与污染物之间的相互作用可以影响重金属在土壤和水体中的迁移和生物可利用性。这一知识对于制定修复受污染地点和保护生态系统的策略至关重要。 此外，phyllosilicate（层状硅酸盐）矿物还参与碳循环。某些类型的粘土可以捕获二氧化碳，从而在减缓气候变化方面发挥作用。这些矿物捕获碳的能力突显了它们在可持续实践和环境管理中的重要性。 除了环境意义外，phyllosilicate（层状硅酸盐）矿物还有各种工业应用。由于其独特的塑性、热稳定性和化学抗性，它们被广泛用于陶瓷、橡胶和涂料的制造。phyllosilicate（层状硅酸盐）矿物的多功能性使其在许多行业中不可或缺，为技术进步和经济发展做出了贡献。 总之，对phyllosilicate（层状硅酸盐）矿物的研究为我们提供了对基本地质过程的深入了解，并为解决环境挑战提供了实际解决方案。它们的层状结构和独特属性使其成为地球系统的重要组成部分，也是人类社会宝贵的资源。随着我们不断探索和理解这些非凡的矿物，我们发现了可持续发展和环境管理的新机会。