Moment Tensor Source-Type Analysis for the Democratic People's Republic of Korea-Declared Nuclear Explosions (2006-2017) and 3 September 2017 Collapse Event

被引:36
作者
Chiang, Andrea [1 ]
Ichinose, Gene A. [1 ]
Ford, Sean R. [1 ]
Matzel, Eric M. [1 ]
Myers, Steve C. [1 ]
Walter, W. R. [1 ]
Dreger, Doug S. [2 ]
机构
[1] Lawrence Livermore Natl Lab, 7000 East Ave,MC 043,MC 046, Livermore, CA 94550 USA
[2] Berkeley Seismol Lab, 307 McCone Hall, Berkeley, CA 94720 USA
基金
美国国家科学基金会;
关键词
HIGH-PRECISION LOCATION; MOUNT ST-HELENS; SINGLE-FORCE; UNDERGROUND EXPLOSIONS; SURFACE-WAVES; INVERSION; EARTHQUAKE; ERUPTION; RELEASE; YIELD;
D O I
10.1785/0220180130
中图分类号
P3 [地球物理学]; P59 [地球化学];
学科分类号
0708 ; 070902 ;
摘要
The Democratic People's Republic of Korea (DPRK) conducted its sixth announced nuclear test on 3 September 2017 03: 30 UTC (m(b) 6.1). There was an aftershock 8.5 min later (m(b) 4.1). Such aftershocks were noteworthy and often associated with post-nuclear explosion collapses. We performed moment tensor (MT) and network sensitivity solution (NSS) analysis using regional long-period surface-wave and first-motion (FM) polarities. We also extended this analysis to the previous five DPRK nuclear tests. The NSS results, which include MT solution uncertainties, show large isotropic components for the events and are within the population of other U.S. nuclear and collapse events on the fundamental lune. The FM data improved the NNS source-type resolution. The agreement between MT seismic moments and independent coda-envelope amplitudes indicated no biases with the Earth model error or poorly constrained seismic moment for shallow seismic sources. The MT for the collapse is not a pure implosion and consistent with an equivalent tensional closing crack mechanism and two-sided vertical point force. The DPRK aftershock has similar circumstances to the collapse 21 min after the 5 August 1982 Atrisco nuclear test. We calculated a range of volume reduction of 1.06 x 10(5) -4.23 x 10(5) m(3) due to 2.68 x 10(15) -1.07 x 10(16) N . m seismic moment range based on diorite rock properties and a closing tensile crack model. In comparison, the cavity radius-yield scaling relation resulted in 2.84 x 10(5) -1.14 x 10(6) m(3) volume range. The overlap in the volume range suggests that the aftershock can be explained by collapse of the explosion cavity. A less likely tunnel-collapse scenario requires a 3-to 13-km-long tunnel to match an equivalent volume change (assuming a 30 m(2) cross-sectional area) and would possibly resulted in secondary sources and mechanism asymmetries detectable by MT methods.
引用
收藏
页码:2152 / 2165
页数:14
相关论文
共 65 条
[41]  
Myers SC, 2007, GEOPHYS J INT, V171, P1049, DOI [10.1111/j.1365-246X.2007.03555.x, 10.1111/J.1365-246X.2007.03555.x]
[42]   Absolute Locations of the North Korean Nuclear Tests Based on Differential Seismic Arrival Times and InSAR [J].
Myers, Stephen C. ;
Ford, Sean R. ;
Mellors, Robert J. ;
Ichinose, G. ;
Baker, Scott .
SEISMOLOGICAL RESEARCH LETTERS, 2018, 89 (06) :2049-2058
[43]   Source-Type-Specific Inversion of Moment Tensors [J].
Nayak, Avinash ;
Dreger, Douglas S. .
BULLETIN OF THE SEISMOLOGICAL SOCIETY OF AMERICA, 2015, 105 (06) :2987-3000
[44]  
Nguyen B., 1994, EOS T AGU S, V75
[45]   The Coupled Location/Depth/Yield Problem for North Korea's Declared Nuclear Tests [J].
Pasyanos, Michael E. ;
Myers, Stephen C. .
SEISMOLOGICAL RESEARCH LETTERS, 2018, 89 (06) :2059-2067
[46]   Equivalent volume sources for explosions at depth: Theory and observations [J].
Richards, PG ;
Kim, WY .
BULLETIN OF THE SEISMOLOGICAL SOCIETY OF AMERICA, 2005, 95 (02) :401-407
[47]   SEISMIC YIELD DETERMINATION OF SOVIET UNDERGROUND NUCLEAR-EXPLOSIONS AT THE SHAGAN RIVER TEST SITE [J].
RINGDAL, F ;
MARSHALL, PD ;
ALEWINE, RW .
GEOPHYSICAL JOURNAL INTERNATIONAL, 1992, 109 (01) :65-77
[48]   Time-domain source function (TDSF) for nuclear and chemical explosions-analysis around Nevada National Security Site (NNSS) [J].
Saikia, Chandan K. .
GEOPHYSICAL JOURNAL INTERNATIONAL, 2017, 209 (02) :1048-1063
[49]  
Shin JS, 2010, GEOPHYS J INT, V180, P243, DOI [10.1111/J.1365-246X.2009.04422.x, 10.1111/j.1365-246X.2009.04422.x]
[50]   VELOCITY OF SHEAR WAVES IN ROCKS TO 10 KILOBARS [J].
SIMMONS, G .
JOURNAL OF GEOPHYSICAL RESEARCH, 1964, 69 (06) :1123-+