大气化学法的依据,就是利用金属矿床从其形成时开始到其完全被破坏为止所存在的天然作用,即“呼吸作用”。由于这种作用,在裸露矿、盲矿、埋藏矿和隐伏-埋藏矿之上的超覆岩石中、底层土壤和土壤的空气中以及近地表的大气圈层中,都会形成气体分散晕。这些气体分散晕虽然少数可与矿床同时形成,但多数是由矿体和矿床中后来出现的物理-化学作用和生物作用形成的。它们是一种由化学元素无机化合物、有机化合物和有机元素化合物等组成的复杂的、多组分的动力体系,然而,有关这些化合物在气体分 The basis of the atmospheric chemistry method is the use of the natural role of the metal deposit from its formation until its complete destruction, ie, “respiration.” Because of this effect, gas dispersal haloes are formed in the air of the underlying soils and soils and in the near-surface atmosphere in the overburden rocks of bare, blind, buried and buried-burial mines. Although the minority can be formed simultaneously with the deposits, most of these gas-dispersion haloes are mostly formed by the subsequent physico-chemical and biological effects in the ore bodies and deposits. They are complex, multi-component kinetic systems consisting of chemical elements such as inorganic compounds, organic compounds and organic-element compounds. However,