kieserite

简明释义

[ˈkiːzəraɪt][ˈkizəˌraɪt]

n. 硫酸镁石

英英释义

Kieserite is a mineral consisting of hydrated magnesium sulfate, commonly found in evaporite deposits and used as a fertilizer.

Kieserite是一种矿物,主要成分是水合硫酸镁,通常在蒸发岩沉积物中发现,并用作肥料。

单词用法

kieserite mineral

Kieserite 矿物

kieserite formation

Kieserite 形成

kieserite deposits

Kieserite 沉积

kieserite content

Kieserite 含量

同义词

magnesium sulfate

硫酸镁

Kieserite is often used as a magnesium fertilizer in agriculture.

Kieserite通常用作农业中的镁肥料。

epsomite

硫酸镁矿

Epsomite is commonly found in evaporite deposits and can be harvested for various industrial applications.

硫酸镁矿常见于蒸发岩沉积物中,可用于各种工业应用。

反义词

calcite

方解石

Calcite is commonly used in the construction industry.

方解石常用于建筑行业。

dolomite

白云石

Dolomite is often used as a soil conditioner.

白云石常用作土壤改良剂。

例句

1.The boric acid did not crystallized with kieserite at same time when concentration of boric acid is lower than 4 %.

当硼酸的浓度小于4%时,硼酸不与一水硫酸镁共结晶。

2.The boric acid did not crystallized with kieserite at same time when concentration of boric acid is lower than 4 %.

当硼酸的浓度小于4%时,硼酸不与一水硫酸镁共结晶。

3.The mineral kieserite is often used in the production of fertilizers.

矿物kieserite常用于肥料的生产。

4.The presence of kieserite can indicate specific environmental conditions.

kieserite的存在可以指示特定的环境条件。

5.In agriculture, kieserite is valued for its magnesium content.

在农业中,kieserite因其镁含量而受到重视。

6.Geologists study kieserite to understand the formation of evaporite deposits.

地质学家研究kieserite以了解蒸发岩沉积物的形成。

7.Some industrial processes utilize kieserite as a source of magnesium sulfate.

一些工业过程利用kieserite作为硫酸镁的来源。

作文

Kieserite, a mineral composed primarily of magnesium sulfate, plays a significant role in various geological and industrial processes. Found commonly in evaporite deposits, kieserite is often associated with other minerals such as halite and gypsum. Its formation typically occurs through the evaporation of saline waters, leading to the crystallization of this unique compound. The presence of kieserite in sedimentary environments indicates a history of arid conditions where water bodies have dried up, leaving behind concentrated minerals.

In terms of its physical properties, kieserite usually appears as white or colorless crystals, although impurities can give it a yellow or brown hue. It has a relatively low hardness on the Mohs scale, making it easy to identify and differentiate from other minerals. The solubility of kieserite in water is an important characteristic, as it can dissolve and re-form under varying environmental conditions. This property is particularly relevant in agricultural practices, where kieserite is used as a magnesium fertilizer, providing essential nutrients to crops.

The industrial applications of kieserite extend beyond agriculture. It is utilized in the production of magnesium oxide, which is a key ingredient in refractory materials. These materials are crucial in high-temperature applications, such as steelmaking and glass production. Additionally, kieserite is employed in the chemical industry for the synthesis of various magnesium compounds, showcasing its versatility and importance in modern manufacturing processes.

Geologists and mineralogists often study kieserite to understand past climatic conditions and the evolution of sedimentary basins. By analyzing the distribution and composition of kieserite deposits, researchers can infer changes in sea levels, salinity, and temperature over geological time scales. This information is invaluable for reconstructing Earth's environmental history and predicting future climatic shifts.

In summary, kieserite is much more than just a mineral; it is a vital component of various natural processes and industrial applications. Its significance in agriculture, industry, and geology underscores the interconnectedness of these fields and highlights the importance of understanding minerals like kieserite in our world. As we continue to explore and utilize the resources provided by nature, the study of kieserite remains essential for sustainable development and environmental stewardship.

凯泽石,一种主要由硫酸镁组成的矿物,在各种地质和工业过程中发挥着重要作用。它通常在蒸发岩沉积物中发现,凯泽石常与其他矿物如岩盐和石膏相关联。它的形成通常发生在盐水的蒸发过程中,导致这种独特化合物的结晶。凯泽石在沉积环境中的存在表明曾经存在干旱条件,水体已经干涸,留下了浓缩的矿物。

在其物理特性方面,凯泽石通常呈现为白色或无色的晶体,尽管杂质可能使其呈现黄色或棕色。它在莫氏硬度表上的硬度相对较低,使其易于识别并与其他矿物区分开来。凯泽石在水中的溶解性是一个重要特征,因为它可以在不同的环境条件下溶解和重新形成。这一特性在农业实践中尤其相关,凯泽石作为一种镁肥料,提供作物所需的基本营养。

凯泽石的工业应用超越了农业。它被用于生产氧化镁,而氧化镁是耐火材料的关键成分。这些材料在高温应用中至关重要,例如钢铁制造和玻璃生产。此外,凯泽石还在化学工业中用于合成各种镁化合物,展示了其多功能性和在现代制造过程中的重要性。

地质学家和矿物学家经常研究凯泽石以了解过去的气候条件和沉积盆地的演变。通过分析凯泽石沉积物的分布和成分,研究人员可以推断海平面、盐度和温度在地质时间尺度上的变化。这些信息对于重建地球的环境历史和预测未来气候变化至关重要。

总之,凯泽石不仅仅是一种矿物;它是各种自然过程和工业应用的重要组成部分。它在农业、工业和地质学中的重要性突显了这些领域之间的相互联系,并强调了理解像凯泽石这样的矿物在我们世界中的重要性。随着我们继续探索和利用自然提供的资源,对凯泽石的研究仍然是可持续发展和环境保护的关键。