论文部分内容阅读
Б.И.维尔纳 茨基把碘作为在天然条件下以微观分散状态为主要存在形式的典型代表元素:“在地壳深处我们发现碘只呈微量分散状态——在与其化学成分没有任何明显关系的变质或火成矿物或岩石中……。碘的分散是彻底的。它可以在毫无例外的所有矿物中找到。呈微量分散状态是碘在地壳中最特征的和最常见的存在形式。”同时根据微观分散观点还可得出
Vernautsky uses iodine as a typical representative element that is predominately in microscopic dispersion under natural conditions: “In the depths of the crust we find that iodine is only slightly dispersed - no noticeable difference from its chemical composition Relationship metamorphism or igneous mineral or rock .... The dispersal of iodine is complete, it can be found in all minerals without exception, in the form of microdispersion, the most characteristic and most common form of iodine in the earth’s crust ”At the same time, we can draw from the viewpoint of micro dispersion