Does Mongolia have lithium?

This electrochemical behavior makes lithium ideal for energy storage applications in batteries. In comparison to Mongolia's main minerals such as copper, coal, iron ore, and feldspar, lithium has been relatively under-studied. Mongolia has around 15-16 occurrences of lithium, with 5 deposits identified thus far.

Where are lithium deposits located in Mongolia?

Referring to the 1908 map of the Bogd Khanate of Mongolia, there is a cluster of lithium deposits known as Tastig in the region between Zavkhan and Khuvsgul aimags. Mongolia is encircled by lithium deposits situated to the south of Lake Baikal. Geological research in China has achieved a high level of development and is advancing rapidly.

Where is lithium found in China?

In the Altai city of the Altai region, there is a cluster of lithium deposits known as Khukhtogoo in Mongolian. This area is regarded as China's primary lithium region. The Altai region was once part of Mongolia during the Bogd Khanate of Mongolia. Therefore, a century ago, Mongolia possessed significant lithium deposits.

Why is lithium a good energy storage material?

With a single electron in its outer shell, it readily loses and gains electrons. This electrochemical behavior makes lithium ideal for energy storage applications in batteries. In comparison to Mongolia's main minerals such as copper, coal, iron ore, and feldspar, lithium has been relatively under-studied.

How has lithium changed the world?

There has been a significant shift in global lithium consumption trends. Historically, lithium was primarily utilized in oil refining, fuel processing, and the porcelain industry. However, over the past two decades, its use in rechargeable battery production has increased tenfold.

Where does lithium come from?

In contrast, salt or brine lithium deposits are more common in hot and dry regions with significant evaporation. Argentina, Chile, and Bolivia, known as the "golden triangle" of lithium in South America, primarily extract lithium from salt deposits.