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Books > Earth & environment > Earth sciences > Structure & properties of the Earth
Earthquakes pose myriad dangers to heritage collections worldwide.
This book provides an accessible introduction to these dangers and
to the methodologies developed at the Getty and other museums
internationally for mitigating seismic vulnerability. Conceived as
a primer and reference, this abundantly illustrated volume begins
with an engaging overview of explanations for earthquakes from
antiquity to the nineteenth century. A series of chapters then
addresses our modern understanding of seismic events and approaches
for mitigating the damage they cause to heritage collections,
covering such subjects as earthquake measurement, hazard analysis,
the response of buildings and collections to seismic events, mount
making, and risk assessment; short sections by specialists in
seismic engineering complement the main text throughout. Readers
will find a range of effective seismic mitigation measures, from
simple low-cost approaches to complex base-isolation techniques. In
bridging the gap between seismologists and seismic engineers, on
the one hand, and collections care professionals, on the other,
this volume will be of interest to conservators, registrars,
designers, mount makers, and others involved in the management and
care of collections in museums and other cultural institutions. "
Understanding and specification of the higher altitudes of the
atmosphere with global coverage over all local times is hampered by
the challenges of obtaining direct measurements in the upper
atmosphere. Methods to measure the properties of the atmosphere
above the stratopause is an active area of scientific research. In
this thesis, we revisit the use of infrasound as a passive remote
sensing technique for the upper atmosphere. Signals from the
Tungurahua volcano in Ecuador are used to investigate the behavior
of the upper atmosphere. Depending on the atmospheric conditions,
stratospheric, mesospheric and thermospheric arrivals are observed
during intervals of explosive volcanic activity. It is found that
the travel times and dominant frequencies of the thermospheric
arrivals exhibit a coherent variability with periods equal to those
of the tidal harmonics. Theoretical predictions using atmospheric
specifications show that the stratospheric arrivals are predicted
within 1 percent of the observed value. For thermospheric arrivals,
this error can be as high as 10 percent. The error in thermospheric
celerities is found to be in accord with the typical uncertainty in
upper atmospheric winds. Given the observed response of the
infrasound celerities to upper atmospheric tidal variability, it is
suggested that infrasound observations may be used as an additional
source of information to constrain the atmospheric specifications
in the upper atmosphere. We present corrected wind profiles that
have been obtained by minimizing misfits in traveltime and source
location using a Bayesian statistics grid search algorithm.
Additionally, a new numerical method has been developed to solve
the problem of infrasound propagation in a stratified medium with
background flow, based on a modal expansion.
In recent years, a number of disasters caused by earthquakes have
demonstrated the vulnerability of both the developing and the
developed world. This book provides new research on earthquakes.
Chapter One focuses on the behavior of a simple spring-block model
from the viewpoint of nonlinear dynamics and seismology. Chapter
Two employs a new technique based on Extreme Learning Machine (ELM)
for determination of liquefaction susceptibility of soil based on
Standard Penetration Test (SPT) and Cone Penetration Test (CPT)
from the Chi-Chi earthquake. Chapter Three presents a review of
earthquake phenomenon in Nigeria, the occurrence and available
data. Chapter Four describes the behavior and failure mechanisms of
unreinforced masonry buildings and different rehabilitation and
strengthening techniques. Chapter Five presents the results related
to the preferred sources of information related to Risk, Hazard and
Natural disaster. Chapter Six presents results regarding urban and
semi-rural schoolchildren's seismic risk perception, awareness and
preparedness of a highly seismic region, in the state of Oaxaca,
Mexico. Chapter Seven reviews the anomalous decrease in groundwater
radon before the Taiwan large earthquakes.
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Etna
(Paperback)
G. F. Rodwell
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Volcanoes around the world have their own legends, and many have
wrought terrible devastation, but none has caught the imagination
like Vesuvius. We now know that immense eruptions destroyed Bronze
Age settlements around Vesuvius, but the Romans knew nothing of
those disasters and were lulled into complacency-much as we are
today-by its long period of inactivity. None of the nearly thirty
eruptions since AD 79 has matched the infamous cataclysm that
destroyed Pompeii and Herculaneum within hours. Nearly two thousand
years later, the allure of the volcano remains-as evidenced by its
popularity as a tourist attraction, from Shelley and the Romantics
to modern-day visitors. Vesuvius has loomed large throughout
history, both feared and celebrated. Gillian Darley unveils the
human responses to Vesuvius from a cast of characters as far-flung
as Pliny the Younger and Andy Warhol, revealing shifts over time.
This cultural and scientific meditation on a powerful natural
wonder touches on pagan religious beliefs, vulcanology, and travel
writing. Sifting through the ashes of Vesuvius, Darley exposes how
changes in our relationship to the volcano mirror changes in our
understanding of our cultural and natural environments.
Ash produced as a consequence of explosive volcanic eruptions can
cause multiple hazards both close to the volcano and at great
distances. Explosive volcano eruptions often release volcanic
plumes into the atmosphere, which consist of tephra
(submillimeter-sized rock particles), water vapor and other gases
such as carbon dioxide (CO2), sulfur dioxide (SO2) and hydrogen
sulfide (H2S). Particles from volcano eruptions are transported by
wind to thousands of kilometers away, or even over 10,000 km from
their source for some fine particles. This book discusses the
environmental impact and health risks volcanic ash poses as well as
its chemical composition.
Microseismic Imaging of Hydraulic Fracturing: Improved Engineering
of Unconventional Shale Reservoirs (SEG Distinguished Instructor
Series No. 17) covers the use of microseismic data to enhance
engineering design of hydraulic fracturing and well completion. The
book, which accompanies the 2014 SEG Distinguished Instructor Short
Course, describes the design, acquisition, processing, and
interpretation of an effective microseismic project. The text
includes a tutorial of the basics of hydraulic fracturing,
including the geologic and geomechanical factors that control
fracture growth. In addition to practical issues associated with
collecting and interpreting microseismic data, potential pitfalls
and quality-control steps are discussed. Actual case studies are
used to demonstrate engineering benefits and improved production
through the use of microseismic monitoring. Providing a practical
user guide for survey design, quality control, interpretation, and
application of microseismic hydraulic fracture monitoring, this
book will be of interest to geoscientists and engineers involved in
development of unconventional reservoirs.
This book introduces the theory that the Sun is getting hotter, and
that is why the Earth is experiencing Global Warming.
Metamorphism generates electrical and magnetic phenomena, and is
influenced by these forces. Information fundamental to their
combined study is presented, including examples from
microtectonics, crystal physics, geophysics, seismology, mineralogy
and materials science. Applications for earthquake prediction,
planetary science research, alternative energy and science
education are included. Work on reported seismic electric signals
is analyzed and summarized. Ten hypotheses related to earthquake
mechanisms and prediction are presented, as well as eighteen
recommendations for further study. Eight microtectonic deformation
mechanisms are explored. Two hundred seventeen descriptions of
minerals exhibiting ferroelectricity, pyroelectricity or
piezoelectricity are presented, with quantitative data where known.
Fifty-three of these are centrosymmetric, and explanations are
given for their apparent violations of crystal theory. A
comprehensive list of thirty-two mechanisms that generate telluric
currents is also presented, as are some novel or inexpensive
experimental techniques in crystal physics.
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