SUMMARY
Detonating a 150 Kiloton nuclear bomb 77 meters underground generates a Source Region EMP (SREMP) effect, which is powerful but limited in range, typically extending one to two kilometers. Unlike High-altitude EMP (HEMP), which has long-range effects, underground detonations do not produce HEMP. The type of soil, such as rock or granite, can influence the SREMP's intensity and range. Glasstone's "The Effects Of Nuclear Weapons" serves as a definitive resource for understanding these effects.
PREREQUISITES
- Understanding of nuclear weapon effects
- Familiarity with EMP types: HEMP and SREMP
- Knowledge of geological impacts on explosive detonations
- Access to Glasstone's "The Effects Of Nuclear Weapons"
NEXT STEPS
- Research the differences between HEMP and SREMP effects
- Study the impact of various soil types on explosive detonations
- Examine case studies of underground nuclear tests
- Review Glasstone's "The Effects Of Nuclear Weapons" for detailed EMP data
USEFUL FOR
Researchers, military strategists, and anyone interested in the effects of nuclear detonations on the environment and infrastructure.