通常对有着巨大科学和实际意义的含盐建造和游离(分子)氮矿床的形成问题是分别加以研究的,但是有根据认为含盐层的形成和氮矿床往往是互相联系的。 盐中微量成分和气体组成的性状是使研究者们认为层间盐水参与了含盐建造的形成的最主要根据。氮就是这样的组分之一,它在天然盐矿中是分布最广泛的气体成分。它的大量存在早被许多研究者所查明。 The formation of salt-bearing and free (molecular) nitrogen deposits, which are of great scientific and practical significance, are usually studied separately, but it is believed that the formation of salt layers and the nitrogen deposits are often interlinked. The trace elements in the salt and the composition of the gas make the researchers believe that interlayer brine is the most important basis for salt formation. Nitrogen is one such component, which is the most widely distributed gas component in natural salt ores. Its massive presence has long been identified by many researchers.