A COMPARISON OF FEATURES CHARACTERISTIC OF NUCLEAR EXPLOSION CRATERS AND ASTROBLEMES *
A COMPARISON OF FEATURES CHARACTERISTIC OF NUCLEAR EXPLOSION CRATERS AND ASTROBLEMES *
复制标题
核爆炸弹坑和天体问题的特征比较*
DOI:
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发表时间:
1965
期刊:
影响因子:
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通讯作者:
N. Short
中科院分区:
文献类型:
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作者:
N. Short
Lawrence Radiation Laboratory, Universi ty of California Livermore, Cal i f . INTRODUCTION When Hutton stated tha t “The present is the key to the past,” he certainly didn’t have in mind the topic which forms the subject of this paper. But, actually there may be no more dramatic examples of this aphorism than a comparison of nuclear cratering, a case where men have direct control over initiating, executing, and recording the event, with impact cratering, a process that with few exceptions has not happened during human history, yet most probably has recurred frequently in the geologic past. The points to be developed are these: (1) tha t a terrestrial impact crater, or astrobleme, is a unique structure produced in a fraction of a minute by a singular combination of forces which generate intense overpressures or shocks, of magnitudes and characteristic actions not produced by any other natural process on ear th ; (2) that underground nuclear explosions at shallow depths in many respects simulate the mechanisms by which impact craters a re formed, and under appropriate conditions can lead to end results bearing a strong resemblance to the astroblemes; (3) tha t there are, however, notable differences in the processes and mechanisms of development of these two types of craters; and ( 4 ) tha t a detailed study of nuclear explosion craters is a proper approach to understanding the genesis of impact craters. Nuclear cratering as a technique for large-scale earth moving is a major part of the AEC’s Plowshare program for peaceful uses of the atom. Since 1957, intensive experimentation in the application of nuclear explosives to digging canals and harbors, to stripping overburden, and to building dams and catchment basins, has led to a new technology now considered to hold practical promise for the future. Many chemical and several nuclear cratering explosives have been detonated under carefully controlled and instrumented conditions. The characteristics of these craters have been rigorously documented by extensive mapping, excavating, and drilling. The outcome of these studies has been a vastly improved, more sophisticated understanding of the physics and engineering aspects of cratering, much of which can be directly extrapolated to impact craters. The objective of