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据苏联文摘1986年2(?)242条报道,M.巴兰尼和H.格尔仲在第30届国际地球物理会议上发表了“氡迁移的新观点及其在普查铀矿床的应用”的论文。论文中对氡作长距离的迁移没有作解释。这个观点的实质是以物理和地质作用为基础来解释氡的迁移的。作者认为,在铀矿体中形成的氡,一般以微气泡的形式同其它气体一起能很快地迁移到潜水面附近,后来的迁移主要是基于扩散作用。在这个新观点的基础上,作者提出了一套深部爱曼测量的方法和技术,并列出了若干应用实
According to the Soviet Union Digest 1986 2 (?) 242 reports, M. Barrani and H. Geerzhong in the 30th International Geophysical Conference delivered a “new viewpoint of radon migration and its application in the census uranium deposit” Thesis. The paper does not explain the long-distance migration of radon. The essence of this view is to explain radon migration based on physical and geological functions. The author believes that the radon formed in uranium ore body, usually in the form of microbubbles, can quickly migrate to the vicinity of the surface along with other gases, and the subsequent migration is mainly based on diffusion. On the basis of this new viewpoint, the author proposes a set of methods and techniques of deepmanman measurement, and lists some practical applications