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ISSN: 1998-4499
All
papers of the journal were peer reviewed by two independent
reviewers. Acceptance was granted when both reviewers'
recommendations were positive.
Main
Page
Paper
Title, Authors, Abstract (Issue 1, Volume 1, 2007) |
Pages |
The importance of crustal shear wave velocity profile for ground motion modelling
Hing-Ho Tsang, Nelson T. K. Lam, S. H. Lo
Abstract: The potential seismic amplification and attenuation
properties of an area are well correlated with the shear wave velocity
(SWV) profile of crustal rock. When local strong motion records are
lacking, the attenuation behaviour of future earthquakes can be
inferred from a crustal SWV model that is representative of the area of
interest. Details of the SWV profile close to the earth surface (1-2 km
depth) are particularly critical. Unfortunately, such details cannot be
obtained by conventional seismic reflection/refraction surveys. This
study demonstrates the use of information from a combination of
sources to produce a set of composite SWV profiles for four principal
geological formations that are prevalent in Hong Kong. Their
respective local upper crustal modification factors have been
computed and the significant differences have been highlighted.
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1-5 |
Site-dependent response spectral attenuation
modelling: a case study of long distance
earthquakes affecting Singapore
Hing-Ho Tsang, Nelson T. K. Lam, S. H. Lo
Abstract: A site-dependent response spectral attenuation model
is an important element in a site-dependent seismic hazard assessment.
Seismic attenuation behaviour is controlled by a large number of wave
modification mechanisms, some of which have characteristics specific
to a local area or a particular site, whilst others can be generalised to
the entire seismic region. Factors representing these mechanisms are
often not resolved. An attenuation modelling approach is
demonstrated in this paper, to evaluate individual regional and local
wave modification factors. The upper-crust amplification factor
computed from the modelled rock shear wave velocity profile was then
combined with predicted attenuation parameters to determine the
upper-crust modification filter function associated with Singaporean
geological formations. Stochastic simulations of the seismological
model for the magnitude 9.3 Aceh earthquake (Indonesia) on the 26th
of December in 2004, were performed and compared with the response
spectra recorded on a rock site in Singapore.
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6-10 |
Paper
Title, Authors, Abstract (Issue 2, Volume 1, 2007) |
Pages |
Tectonic activities and deformation in South
Korea constrained by GPS observations
Shuanggen Jin and Pil-Ho Park
Abstract: High precision GPS observations provide crucial
insights into understanding the pattern and physical process of
tectonic activities. In this paper, GPS data for the period from March
2000 to February 2004 were analyzed to quantitatively investigate
the crustal deformation patterns and distributions in the southern
Korean Peninsula. The high maximum shear strain rates are
concentrated in the middle part of South Korea, which remarkably
agrees with the shear trends in the Okcheon Belt and the Honam
Shear Zone (HSZ) with a direction NE-SW. In addition, South Korea
is dominated by both ENE-WSW compression and NNW-SSE
extension, which is nearly consistent with earthquake focal
mechanism solution (Mw ≥ 4.0, 1936-2004), indicating that the
seismicity can be used to improve GPS-derived deformation style
and orientation. Furthermore, it reflects that the occurrence of
shallow earthquakes in South Korea is closely related with the
horizontal strain.
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11-15 |
Generation of the Moon and Some Other Celestial Bodies due to
Explosion in Planet Interiors
D.V.Voronin
Abstract: It is difficult to explain an origin of all celestial bodies of the Solar system due to smooth evolution
of the protoplanet cloud. An alternative to the evolutionary one is the hypothesis of their explosive origin. It is
supposed, that on the solid inner core of a planet the active layer is formed from particles of uranium and
thorium oxides, weighed in liquid iron of the outer core of the planet. The explosion in such a layer might occur
as a result of collision of the planet with an asteroid. Collision of the protoplanet with an asteroid, the
subsequent explosion in an active layer and fragmentation of the planet in conditions of gravitation is
numerically simulated. for two-dimensional non-stationary motion of the compressible medium on the basis of
laws of conservation of mass, pulse and energy. The hypothesis that some bodies of the Solar system may be
formed as a result of nuclear explosions in the protoplanet core is numerically confirmed in the paper. If the
initial velocity of protoplanet rotation is small enough, the structure and composition of fragments may be
determined by the cumulative jet going from a planetary core to its surface. The origin of Io may be so
explained, for example. For the great enough velocity of rotation the nuclear explosion in the planet interiors
breaks the balance between the centrifugal forces and the gravitation. That results in the separation of the
great mass of the stone-silicate shell of the planet and the generation of satellites like the Moon.
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16-21 |
Using geostatistical analysis and spectral
signature for identifying shale distribution and
type in El-Salhia project, Ismaillia, Egypt
El Nahry A.H.
Abstract: The current work aimed at recognizing shale distribution
and its type in El Salhia project where it represents a serious
limiting factor that preclude the agricultural development in that
project. Shale is a fine-grained sedimentary rock whose original
constituents were clays or muds. It is characterized by thin laminae
breaking with an irregular curving fracture, often splintery and
usually parallel to the often-indistinguishable bedding plane. Shale
formation are typically as a result of deposition in very slow
moving water and are often found in lake and lagoonal deposits, in
river deltas, on floodplains and offshore of beach sands.Two main
landforms affecting shale distribution were recognized in the
project i.e. I-The Nile river terraces.II-The deltaic stage of the river
terraces. Geostatistical analysis was performed to identify shale
spatial distribution.
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22-26 |
Paper
Title, Authors, Abstract (Issue 3, Volume 1, 2007) |
Pages |
Degradation of Indus Delta Mangroves in
Pakistan
Amjad, A. Shah., Kasawani, I., and Kamaruzaman, J
Abstract: A largely arid/semi-arid country, Pakistan has a diverse
landscape, with high mountain ranges, fragile watersheds, alluvial
plains, sandy deserts and coastal mangroves. Indus, the major river of
Pakistan, falls into the Arabian Sea in the Sindh coast forming a fanshaped
delta interspersed with 17 major and numerous minor creeks
and mudflats. Indus delta mangroves are unique in being the
largest area of arid climate mangroves and the 7th largest block in the
world. They are dominated by Avicennia marina (locally known as
Timmer), which occupies about 90% of total mangroves in the delta.
Reduction in inflow of freshwater from Indus on account of diversion
of water for other purposes, inflow of pollutants from industries,
navigational activities and intermix of industrial effluent, and human
and livestock population pressure for fuelwood and fodder collection
have exposed this complex ecosystem to severe environmental and
social stresses in the form of loss of habitat and biodiversity, decline
in fish productivity and social problems for coastal communities. The
paper provides an overview of Pakistan's Indus delta mangroves, lists
the manifold causes threatening their existence, and suggests
corrective measures for preserving/developing this important
ecosystem of the world.
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27-34 |
Geostatistical analysis for estimation of mean
rainfalls in Andhra Pradesh, India
Krishna Murthy B R and G Abbaiah
Abstract: Rainfall is a hydrological phenomenon that varies in magnitude in space as well as in time and requires suitable tools to predict mean values in space and time. Estimation of rainfall data is necessary in many natural resources and water resource studies. There are several methods to estimate rainfall among which interpolation is very useful approach. In this research, geostatistical interpolation methods are used to estimate monthly (June-December), seasonal (South-West and North-East Monsoon seasons) and annual rainfalls in Andhra Pradesh, India. Monthly rainfall data from a network of 23 meteorological stations for the period 1970-2003 has been in the study. The main objectives of this work are: (1) to analyze and model the spatial variability of rainfall, (2) to interpolate kriging maps for different months as well as seasons, (3) to analyze and model the structural cross correlation of rainfall with elevation for different seasons, (4) to investigate whether co-kriging would improve the accuracy of rainfall estimates by including elevation as a secondary variable, and (5) to compare prediction errors and prediction variances with those of kriging and cokriging methods for different seasons. Rainfall surfaces have been predicted using ordinary kriging method for these analyses. Co-kriging analysis has been done to improve the accuracy of prediction, by including the elevation as a co-variate. It has not resulted in significant improvement in the prediction. It was observed that the rainfall data is skewed and Box-cox transformation has been used for converting the skewed data to normal.
It is observed that the trend is present in all the cases, and is constant for November, North-East monsoon. The first order polynomial fits well for June, August, Sept, October, December, Annual period and South -West monsoon. The second order polynomial fits best for July. It has been observed that the directional effects are predominant in October, November, South-West Monsoon and Annual rainfall. Spherical model fits well for June, July, November, South-West and North-East monsoons, where as the Gaussian model fits well for August, September, October, December and annual rainfalls. Nugget effect is zero for June, November, and North-East monsoon. The cross-validation error statistics of OCK presented in terms of coefficient of determination (R2), kriged root mean square error (KRMSE), and kriged average error (KAE) are within the acceptable limits (KAE close to zero, R2 close to one, and KRMSE from 0.98 to 1.341). The exploratory data analysis, variogram model fitting, and generation of prediction map through kriging were accomplished by using ESRI’S ArcGIS and geostatistical analyst extension.
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35-51 |
3D Heat Generation and Transfer in Gravity
Dam on Rock Foundation using Galerkin Finite
Volume Solver on Tetrahedral Mesh
S.R. Sabbagh-Yazdi and N.E. Mastorakis
Abstract: In order to solve temperature field in a typical gravity
concrete dam and its natural foundation, the three-dimensional
temperature diffusion equation is chosen as the mathematical model.
The finite volume formulation is derived using Galerkin approach for
the mesh of tetrahedral elements. This method facilitates solving
temperature problems with complicated geometries. The algorithm
not only is able to handle the essential boundary conditions but also
the natural boundary conditions using a novel technique. Accuracy
and efficiency of the algorithm is assessed by comparison of the
numerical results for a bench mark problem of heat generation and
transfer in a block with its analytical solution. Finally the developed
model is applied to compute temperature field in a three dimensional
gravity concrete dam on rock foundation.
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52-60 |
Application of Seismic Tomography
Techniques in Dam Site
Kambiz Teimoornegad, Neda poroohan
Abstract: In this paper seismic data obtained from several
boreholes located at Nimroud dam site in the east part of Tehran, was
used to model 2D tomography of the subsurface model. To increase
the accuracy in the modeling procedure , back projection , damped
least squares and smoothest function method were used and their
results were compared. The back projection method is an
approximation weighted solution , while the second method is based
on the damped least squares operator. The third method is more
stable for estimation of the model parameter than the two previous
mentioned methods. Analysis of the model sensitivity showed that ,
variation of the final residual time with respect to the obtained
velocity values diagrams from four boreholes at dam axis differs
from the other diagrams. These differences are between – 25 to + 10
percentage greater values. The geological information , sample core
from the boreholes as well as the velocity values abnormality
obtained at the study area were attributed to a hidden fault at the dam
site area.
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61-69 |
Analysis of the Landslide
Movements
Ancuta Rotaru, Daniel Oajdea, Paulica Raileanu
Abstract: Understanding the causes of
slope development, particularly the initiation of
movement, requires knowledge of a set of factors,
usually associated with groundwater, that are often
difficult to determine. Landslides commonly occur as
a result of: heavy rainfall, rapid snowmelt, wet
winter and spring particularly if previous years
were also wet, the removing of the material from the
base, loads material at the top, earthquakes,
erosion, poor forest management, addition of water
to a slope from irrigation, roof downspouts, poor
drainage, septic-tank effluent, canal leakage, or
broken water. Most landslides in Romania occur as a
result of a combination of poor forest management
and intense rainfall. A continuous recording of
landslide displacements is often required in order
to better understand the complex relationship
between the triggering factors and the dynamics of
the movement. In recent years structural geology has
been used as a tool to investigate the development
and evolution of potential rockslides. The
recognition of the processes that triggered the
movement is of primary importance to understand the
landslide mechanisms. The paper analyses the
movement of the landslides from the point of view of
different stages of landslide activity: pre-failure
stage, failure sage, post-failure stage and
reactivation stage.
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70-79 |
Numerical Model of Generating
of the Surface that Borders a Hidden Volume
Nicolae Dobritoiu
Abstract: In the practical activity,
especially in the knowledge activity of a deposit,
one encounters the situation of determination of the
form of the surface that borders a reserve unit of
useful mineral substances. The knowledge of the form
of a surface that borders a reserve unit allows its
geometric parameters determination and the
calculation of the volume of reserve unit. These
informations are used in the decision process of
mine working of the deposits of the useful mineral
substances.
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80-87 |
Paper
Title, Authors, Abstract (Issue 4, Volume 1, 2007) |
Pages |
Clustering Analysis Method
based on Fuzzy C-Means Algorithm of PSO and PPSO
with Application in Real Data
Jeng-Ming Yih, Yuan-Horng Lin, Hsiang-Chuan Liu
Abstract: The popular fuzzy c-means
algorithm (FCM) converges to a local minimum of the
objective function. Hence, different initializations
may lead to different results. The important issue
is how to avoid getting a bad local minimum value to
improve the cluster accuracy. The particle swarm
optimization (PSO) is a popular and robust strategy
for optimization problems. But the main difficulty
in applying PSO to realworld applications is that
PSO usually need a large number of fitness
evaluations before a satisfying result can be
obtained. In this paper, the improved new algorithm,
“Fuzzy C-Mean based on Picard iteration and PSO (PPSO-FCM)”,
is proposed. Three real data sets were applied to
prove that the performance of the PPSO-FCM algorithm
is better than the conventional FCM algorithm and
the PSO-FCM algorithm.
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89-98 |
New Magnetosphere for the
Earth In Future
Tara Ahmadi
Abstract: All of us know the earth
magnetic field come to be less and this problem can
be a serious problem in future but now we find other
problems that can destroy our planet life or in
minimum state can damage it such as FTE theory ,
solar activities , reversing magnetic poles,
increasing speed of reversing that last reverse,
reducing magnetic strength ,finding leaks in
magnetosphere ,etc. some of these reasons will be
factors for increasing the solar energy that hit to
the Earth and perhaps changing in our life and
conditions of the Earth. In this paper , I try to
show a way to against to these problems and reduce
their damages to the Earth perhaps The Earth will
repair himself but this repair need many time that
humans could not be wait. In the past time magnetic
field was reversed but now we are against to the
other problems that can increase the influence of
reversing magnetic field for the Earth and all these
events can be a separated problem for us, these
problem may be can not destroyed humans life but can
be cause of several problems that occur for our
healthy and our technology in space. This way is
building a system that produce a new magnetic field
that will be in one way with old magnetic field this
system will construe by superconductors and a metal
that is not dipole. This paper explain all the
problems in addition to the way of repair their
damages on the Earth and show the suitable shape of
system that can help us for future programs.
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99-107 |
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