Abstract

The study investigated the dynamic soil properties of States in Niger Delta region of Nigeria as a function of seismic activities. The down-hole seismic test was used to determine the response of the soils. The results of soil samples collected up to 30m depth, showed that the average young modulus increases with increase in depth, which ranged from 115.77±1.74 to 3231.17±1.01 kPa across the States. Also, shear wave velocity generally increases with increase in depth. The average shear wave velocity across the States ranged from 126.00±1.86 to 288.00±2.63m/s. Also, the average P-wave velocity increases with depth, with values across the States ranging from 310.60±3.51 to 656.00±3.69m/s. On the other hand, the void ratio was observed to be constant at certain range of depth, and in most with values across the States ranging from 0.651±.093 to 0.860±.067. Unlike void ratio, Poisson’s ratio fluctuates with depth, with values across the States ranging from 0.23±2.27 to 0.36±1.18. Based on the results, the Niger Delta region may be resistant to earthquake, but as an oil hub of Nigeria, it is also susceptible to earthquake that could be triggered by stress due to heavy load and seismic activities.

Highlights

  • Natural disasters have become a great challenge to humans

  • The seismic down-hole dynamic soil properties of the various locations in Niger Delta region of Nigeria was studied based on young modulus, shear wave velocity, p-wave velocity, void ratio and Poisson’s ratio

  • From analysis, the numerical values of the average young modulus obtained from sites located in Rivers State ranged from 156.96±2.18-3231.17±1.01 kPa, while others ranged from 118.17±3.37-2809.21±2.51 kPa for Bayelsa State, 119.81±1.132769.53±0.46 kPa for Akwa Ibom State and 115.77±1.74-2900.25±2.09 kPa for Delta State

Read more

Summary

Introduction

Natural disasters have become a great challenge to humans These disasters ranged from the failures of embankments, natural slopes, earth structures and foundations; and they have been attributed to the liquefaction of sands, landslides and slope instability (Ige et al, 2016). These natural disasters are a result of seismic effects and only occur in a geographical area with distinct characteristics. The wave generated due to earthquakes developed vibrations in the ground and create severe natural disasters which are functions of regional seismicity, nature of the source of mechanism, geology, and local soil conditions. Its activities result from accumulated stresses within the outer 700 Km shell of the earth (Osagie, 2008)

Methods
Results
Conclusion
Full Text
Published version (Free)

Talk to us

Join us for a 30 min session where you can share your feedback and ask us any queries you have

Schedule a call