概括
酸盐矿物质很快将二氧化释放到海水中. 这项研究表明,即使是常见的矿物质也会快速反应,这挑战了以前关于海洋化学系统中缓慢地质速率的假设.
科学领域:
- 地质化学 地质化学
- 海洋化学 海洋化学
- 矿物学是什么?矿物学是什么?
背景情况:
- 酸盐矿物质在海洋环境中非常丰富.
- 以前的理解表明,酸盐矿物质和海水之间的反应速度很慢.
- 离子交换被认为是主要的相互作用机制.
研究的目的:
- 为了研究各种矿物质释放到海水中的二氧化的速度.
- 挑战地质上缓慢的矿物和海水反应的假设.
- 评估海洋化学系统对破碎酸盐的反应能力.
主要方法:
- 精细颗粒矿物质样本 (1克) 在人造海水 (200毫升) 中进行化.
- 在6个月的时间内测量了水中的度.
- 测试的特定矿物包括高酸盐,酸盐,酸盐,酸盐,酸盐和两种类型的蒙特莫里隆石.
主要成果:
- 在10天和6个月内,从所有测试的矿物中观察到显著的二氧化释放.
- 蒙莫里隆石样本显示了最高的二氧化度 (例如,蒙莫里隆石B:10 ppm在10天,21 ppm在6个月).
- 考利尼特的释放量最低 (0.6 ppm 在10天,2.2 ppm 在6个月).
结论:
- 酸盐矿物质与海水迅速反应,释放大量的二氧化.
- 海洋应该被视为一种化学系统,对添加的微粒酸盐产生快速反应.
- 观察到的速度与海洋环境中矿物质溶解在地质上缓慢的假设相矛盾.
更多相关视频
11:50Metal-silicate Partitioning at High Pressure and Temperature: Experimental Methods and a Protocol to Suppress Highly Siderophile Element Inclusions
Published on: June 13, 2015
09:39Proof-of-Concept for Gas-Entrapping Membranes Derived from Water-Loving SiO2/Si/SiO2 Wafers for Green Desalination
Published on: March 1, 2020
相关概念视频
Effect of Sea Water on Concrete
Concrete exposed to seawater can undergo degradation like the dissolution of ettringite and gypsum, increasing the material's porosity and decreasing its strength. In contrast, the crystallization of salts within the concrete's pores can cause expansion, particularly above the waterline where evaporation occurs. Nonetheless, this expansion only happens when seawater, enabled by the concrete's permeability, manages to infiltrate the structure.
Concrete in areas between tide marks, which undergo...
Concrete in areas between tide marks, which undergo...
Alkali Aggregate Reaction in Concrete
The alkali-aggregate reaction in concrete involves natural siliceous minerals in aggregates reacting with alkaline hydroxides derived from cement alkalis. This reaction forms an alkali-silica gel that absorbs water, swells, and increases in volume, which is confined by the surrounding cement paste, creating internal pressures that crack and disrupt the concrete. The extent of expansion and damage can be partly attributed to the alkali-silica reaction's osmotic hydraulic pressure and the...
Alkali Metals
Group 1 elements are soft and shiny metallic solids. They are malleable, ductile, and good conductors of heat and electricity. The melting points of the alkali metals are unusually low for metals and decrease going down the group, while the density increases going down the group with the exception of potassium (Table 1).
Table 1: Properties of the alkali metals
Table 1: Properties of the alkali metals
Precipitation Reactions
In a precipitation reaction, aqueous solutions of soluble salts react to give an insoluble ionic compound – the precipitate. The reaction occurs when oppositely charged ions in solution overcome their attraction for water and bind to each other, forming a precipitate that separates out from the solution. Since such reactions involve the exchange of ions between ionic compounds in aqueous solution, they are also referred to as double displacement, double replacement, exchange reactions, or...
Preparation and Reactions of Sulfides
Sulfides are the sulfur analog of ethers, just as thiols are the sulfur analog of alcohol. Like ethers, sulfides also consist of two hydrocarbon groups bonded to the central sulfur atom. Depending upon the type of groups present, sulfides can be symmetrical or asymmetrical. Symmetrical sulfides can be prepared via an SN2 reaction between 2 equivalents of an alkyl halide and one equivalent of sodium sulfide.
Halogens
Group 17 elements, known as halogens, are nonmetals. At room temperature, fluorine and chlorine are gases, bromine is a liquid, and iodine a solid. Astatine is a highly unstable radioactive element, so currently, most of its properties are unknown due to its short half-life. Tennessine is a synthetic element also predicted to be in this group.
