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دانلود کتاب Fundamentals of Finite Element Analysis

McGraw-Hill, Jun 25, 2003 – 494 pages This new text, intended for the senior undergraduate finite element course in mechanical, civil and aerospace engineering departments, gives students a solid, practical understanding of the principles of the finite element method within a variety of engineering applications.  Hutton discusses basic theory of the finite element method while avoiding variational calculus, instead focusing upon the engineering mechanics and mathematical background that may be expected of senior engineering students. The text relies upon basic equilibrium principles, introduction of the principle of minimum potential energy, and the Galerkin finite element method, which readily allows application of finite element analysis to nonstructural problems.  The text is software-independent, making it flexible enough for use in a wide variety of programs, and offers a good selection of homework problems and examples.  A Book Website is also included, with book illustrations for class presentation; complete problem solutions (password protected); the FEPC 2-D finite element program for student use; instructions on FEPC and its use with the text; and links to commercial FEA sites.

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دانلود کتاب – Fundamentals of Finite Element Analysis -David V

منبع : scribd.com

دانلود کتاب – Fundamentals of Finite Element Analysis -David V- Hutton

Fundamentals of Finite Element Analysis, David V. Hutton

McGraw-Hill, Jun 25,
2003 – 494 pages This new text, intended for the senior undergraduate
finite element course in mechanical, civil and aerospace engineering
departments, gives students a solid, practical understanding of the
principles of the finite element method within a variety of engineering
applications.  Hutton discusses basic theory of the finite element
method while avoiding variational calculus, instead focusing upon the
engineering mechanics and mathematical background that may be expected
of senior engineering students. The text relies upon basic equilibrium
principles, introduction of the principle of minimum potential energy,
and the Galerkin finite element method, which readily allows application
of finite element analysis to nonstructural problems.  The text is
software-independent, making it flexible enough for use in a wide
variety of programs, and offers a good selection of homework problems
and examples.  A Book Website is also included, with book illustrations
for class presentation; complete problem solutions (password protected);
the FEPC 2-D finite element program for student use; instructions on
FEPC and its use with the text; and links to commercial FEA sites.


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برای دانلود اینجا کلیک کنید…

http://www.scribd.com/mobile/documents/74563079

بازگشت به صفحه اصلی وبلاگ مهندسی عمران راه و ساختمان(مهندس حسن فراهانی)

برچسب‌ها: دانلود کتاب, Fundamentals of Finite Element Analysis, David V, Hutton, مهندس حسن فراهانی

منبع: http://hfarahani48.blogfa.com/post-9218.aspx

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قطب نماهای ناوبری (Compass navigation) و نیاز آن برای نقشه های دریایی (مهندس حسن فراهانی)

منبع : حمل و نقل دریایی

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Marine compass

In China compasses have been in use since the Han dynasty (2nd century BCE
to 2nd century CE) when they were referred to as “south-pointers”.
However at first these magnets were only used for geomancy much like in
the art of Feng Shui.

Eventually, during the Sung dynasty (1000 CE) many
trading ships were then able to sail as far as Saudi Arabia using
compasses for marine navigation. Between 1405 and 1433, Emperor Chu Ti’s
Treasure Fleet of the Dragon Throne ruled the entire South Pacific and
the Indian Ocean, a territory that ranges from Korea and Japan to the
Eastern coast of Africa.

At this time Western mariners were still rather ignorant of the navigational use of the magnet. Petrus Perigrinus van Maricourt
wrote a first treatise on the magnet itself: “De Magnete” (۱۲۶۹). And
though its nautical use was already mentioned in 1187 by the English
monk Alexander Neckham, the use onboard only came about around the 13th
and 14th century in the Mediterranean Sea.

Much later, in 1545, Pedro de Medina (Sevilla 1493-1567)
wrote the Spanish standard work “Arte de Navegar” on marine compass
navigation. This masterpiece was first translated in Dutch (1580) and
was -O Irony- used by Jacob van Heemskerk
when the Dutch destroyed the Spanish fleet near Gibraltar in 1607. The
drawback was of course Van Heemskerk’s own death during this victory.

Magnetic Variation

In the fin-de-siècle of the sixteenth century mariners
believed that the magnetic north pole coincided with the geographic
north pole. Any suggestion otherwise had been denied by Pedro de Medina.

Magnetic observations made by explorers in subsequent
decades showed however that these suggestions were true. But it took
until the early nineteenth century, to pinpoint the magnetic north pole
somewhere in Arctic Canada (78° N , 104° W). From then on the angle
between the true North and the Magnetic North could be precisely corrected for. This correction angle is called magnetic variation or declination.

It is believed that the Earth’s magnetic field is
produced by electrical currents that originate in the hot, liquid, outer
core of the rotating Earth. The flow of electric currents in this core
is continually changing, so the magnetic field produced by those
currents also changes. This means that at the surface of the Earth, both
the strength and direction of the magnetic field will vary over the
years. This gradual change is called the secular variation
of the magnetic field. Therefore, variation changes not only with the
location of a vessel on the earth but also varies in time.

The correction for magnetic variation for your location is shown on the nearest! nautical chart’s compass rose.
In this example we find a variation of 4° ۱۵′ W in 2009, with an
indicated annual correction of 0° ۰۸′ E. Hence, in 2011 this variation
is estimated to be 3° ۵۹′, almost 4° West. This means that if we sail
90° on the chart (the true course), the compass would read 94°.

Another example: let’s say the compass rose gives a
variation of 2° ۵۰′ E in 2007, with a correction of 0° ۰۴′ E per year.
In 2009 this variation is estimated to be 2° ۵۸′, almost 3° East. Now,
if we sail 90° on the chart, the compass would read 87°.

Correcting for variation

Difference between true course and magnetic course
These overlayed compass roses show the difference between true north
and magnetic north when the magnetic variation is 10° West.

From the image we find: tc = cc + var
in which “cc” and “tc” stand for “compass course” and “true course”, respectively.

To convert a true course into a compass course
we need first assign a “-” to a Western and a “+” to a Eastern
variation. Note that this makes sense! because of the clockwise
direction of the compass rose. Here, the inner circle is turned 10°
anticlockwise, hence -10°.
Now, use the same but re-written equation:
cc = tc – var
235° = ۲۲۵° – (-۱۰°)
So, to sail a true course of 225°, the helmsman has to steer a compass course of 235°.

To convert a compass course into a true course
we can use the original equation. If we have steered a compass course
of 200°, we have to plot a true course of 203° in the chart if the
variation is 3° East or a true course of 190° if the variation is 10° West.

Magnetic deviation

Magnetic deviation is the second correctable error. The
deviation error is caused by magnetic forces within your particular
boat. Pieces of metal, such as an engine or an anchor, can cause
magnetic forces. And also stereo and other electric equipment or wiring,
if too close to the compass, introduce errors in compass heading.

Furthermore, the deviation changes with the ship’s
heading, resulting in a deviation table as shown below. The vertical
axis states the correction in degrees West or East, where East is again
positive.

Deviation table: For each heading a different deviation correction is needed.

The horizontal axis states the ship’s heading in
degrees divided by ten. Thus, when you sail a compass course of 220°,
the deviation is 4° W. (Note, that on most modern sailing yachts the
deviation is usually not larger than 3°).

When a compass is newly installed it often shows larger
deviations than this and needs compensation by carefully placing small
magnets around the compass. It is the remaining error that is shown in
your deviation table.
You can check your table every now and then by placing your boat in the line of a pair of leading lights and turning her 360 degrees.

Correcting for both deviation and variation

Converting a compass course into a true course, we can still use our equation but we need to add the correction for deviation:
cc + var + dev = tc

Example 1: The compass course is 330°, the deviation is +3° (table) and the variation is +3° (chart);
330° cc + 3° var + 3° dev = ?° tc
giving a true course of 336° which we can plot in our chart

Example 2: The compass course is 220°, the deviation is -4° (table) and the variation is still +3° (chart).
220° cc + 3° var + -4° dev = ?° tc
giving a true course of 219°.

Example 3: The compass course is still 220°, therefore the deviation is still -4° (table) but let’s use a variation of -10° this time.
220° cc + -10° var + -4° dev = ?° tc
giving a true course of 206°.

Converting a true course into a compass course is a little less straight forward, but it is still done with the same equation.

Example 4: The true course from the chart is 305° and the variation is +3° (chart), yet we don’t know the deviation;
?° cc + 3° var + ?° dev = 305° tc
Luckily, we can rewrite this so this reads:
cc + dev = 305° tc – + 3° var = 302°
In
plain English: the difference between the true course and the variation
(305 – + 3) = 302 should also be the summation of the compass course
and the deviation. So, we can tell our helms person to steer 300°, since
with a cc of 300° we have a deviation of +2° (As can be deduced from
the deviation table above).

Example 5: The true course
from the chart is 150° and we have a Western variation of 7 degrees
(-7°). We will use the rewritten equation to get:
150° tc – - 7° var = cc + dev = 157°
From the deviation table we find a compass course of 160° with a deviation of -3°.
Voilà!

Magnetic course

The magnetic course (mc) is
the heading after magnetic variation has been considered, but without
compensation for magnetic deviation. This means that we are dealing with
the rewritten equation from above:
tc – var = cc + dev = mc.

Magnetic courses are used for three reasons:Three types of North - compass, magnetic, true

To convert a true course into a compass course like we saw in the last paragraph.

On vessels with more than one steering compass, also
more deviation tables are in use; hence only a magnetic or true course
is plotted in the chart.

Bearings taken with a handheld compass often don’t
require a correction for deviation, and are therefore useful to plot in
the chart as magnetic courses.

Note, that the actual course lines the
navigator draws in the chart are always true courses! These can
subsequently be labeled with the true course or the corresponding
magnetic or compass course if appropriate. In the next chapter we will be plotting courses in the chart.

To summarise, we have three types of “north” (true,
magnetic and compass north) like we have three types of courses: tc, mc
and cc. All these are related by deviation and variation.

Glossary

Maps with isogonic lines:
World – overview 2000
World – detailed 2000
World – detailed 2005
World – animated in time
Variation: The angle between the magnetic north pole and the geographic north pole. Also called the magnetic declination.

Secular variation: The change of magnetic declination in time with respect to both strength and direction of its magnetic field.

West (-) , East (+):
Western variations or deviations are designated with a negative sign by
convention due to the compass card’s clockwise direction.

Deviation: The error in compass heading caused by electric magnetic currents and or metal objects.

Deviation table: A table containing deviations in degrees versus the ship’s heading (compass course) in degrees. Usually plotted in a graph.

True course: Course plotted in the chart i.e. course over the ground or “course made good”. The course corrected for compass errors.

Compass course: The course (ship’s heading) without the correction for compass errors.

cc + var + dev = tc: This
equation shows the connection between the compass course, its errors and
the true course. It can also be read as: tc – var = cc + dev

بازگشت به صفحه اصلی وبلاگ مهندسی عمران راه و ساختمان(مهندس حسن فراهانی)

برچسب‌ها: قصب نماهای ناوبری, Compass navigation, نقشه های دریایی, مهندس حسن فراهانی

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آّشنایی با جزر و مد (Tides) (مهندس حسن فراهانی)

منبع : حمل و نقل دریایی

آّشنایی با جزر و مد (Tides)

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Tidal movements

The tide is the vertical
rise and fall of the sea level surface caused primarily by the change in
gravitational attraction of the moon, and to a lesser extent the sun.
As
the earth spins on its axis the centrifugal force results in slightly
deeper water near the equator as opposed to shallower water at the
poles. In fact it causes a flow from the poles to the equator.
The
earth is also in orbit around the sun (one revolution in one year)
creating not only another centrifugal force but also a gravitational
interaction. These two yield a bulge on the night site (centrifugal) and
a bulge on the day site (gravitational) both of them moving as the
world turns. Therefore, a certain place on this world will experience
two high and two low tides each day.
With these forces alone, we would not have spring tides and neap tides.
Spring tides have higher high tides and lower low tides whereas neap
tides have lower high tides and higher low tides. Hence, the range (difference in water level between high and low tide) is much larger in a spring tide than in a low tide.

This animation shows how the tide changes during the lunar cycle. When the sun, moon and earth are aligned : spring tide.
When at right angles the forces are not aligned:
neap tide.
The time between spring and neap is approximately 7 days.

These differences in range can be explained if we
include the moon into our earth-sun system. The moon and the earth orbit
each other around a point (called the barycenter or baricenter) 2000
odd kilometres inside the earth, creating a centrifugal
and a gravitational bulge. Moreover, despite the sun’s immensely larger
mass, the moon exerts a 2.25 times larger gravi­tatio­nal attraction,
since the moon is much closer to our earth.
It is the combined effect
of the sun and moon that creates spring and neap tides. In the
animation the gravitational forces of both the sun and the moon are
taken into account. When aligned with the earth they combine their
attraction and otherwise they counteract their attraction. The sun is
located in the corner right below, far outside this picture (note the
eclipse) while the moon is revolving round the earth. One full circle
corresponds to one lunar cycle (about 28 days).

The
figure below shows the ideal sinusoids of both spring and neap tides.
Vertically the water height is shown versus horizontally the time.
Ideally, the time between a low and a successive high is somewhat more
than 6 hours.
The sinoidal curve of the Tide
The time difference between spring tide and neap tide is normally 7 days and is in accordance with the phases of the moon.
Yet, water has mass and therefore momentum. Moreover, it is a viscous
fluid that generates friction if moved. Therefore, the actual spring
tide lags a day or so behind a full moon or new moon occurrence.

So, tidal movements are intrinsically periodical, resulting in a Tidal day of 24 hours and 50 minutes containing one tidal cycle,
namely two highs and two lows. This basic pattern may be distorted by
the effects of landmasses, constrained waterways, friction, the Coriolis
effect, or other factors. Hence, predictions are possible and we expect
the the next day’s high tide to come about 50 minutes later.
However,
a closer look at the orbit of the moon reveals that the moon is not
always in the equatorial plane, resulting in three types of tides:

Semi-diurnal tide: Featuring
two highs and two lows each day, with minimal variation in the height
of successive high or low waters. This type is more likely to occur when
the moon is over the equator.

Diurnal tide: Only
a single high and a single low during each tidal day; successive high
and low waters do not vary by a great deal. This tends to occur in
certain areas when the moon is at its furthest from the equator.

Mixed tide: Characterized by
wide variations in heights of successive high and low waters, and by
longer tidal cycles than those of the semi-diurnal cycle. These tides
also tend to occur as the moon moves furthest north or south of the
equator.

Chart Datums

The depths and heights in the chart need a plane of
reference: the Chart Datum (see interactive figure below). Depths are
usually described with respect to low water reference planes (yielding
lower charted depths, which are safer) and heights are shown with
respect to high water reference planes (again, yielding lower vertical
clearances on the chart, which are safer). As such, the chance that the observed depth or vertical clearance beneath a bridge is smaller than the charted depth or height is rather small.

In this example the Charted Depths are related to LAT.
The Observed Depth or Drying Height is a combination of Tidal Height Charted Depth.

 
This
example shows the various spring and neap tides around mean water
level. Note that spring low water is the lowest. Both ranges are
indicated.

 
In
this example the light elevation is reduced to high water. Also a
clearance under a bridge is charted in that way. The ‘height’ refers to
the building itself. On land yet another CD can be in use.

Some Chart Datums and their abbreviations:

MHWS : Mean High Water Spring

HW : High Water

MHWN : Mean High Water Neap

ML : Mean Level

MLWN : Mean Low Water Neap

MLWS : Mean Low Water Spring

LAT : Low Astronomical Tide

 

Overview

Tide: The vertical rise and
fall of the surface of a body of water caused primarily by the
differences in gravitational attraction of the moon, and to a lesser
extent the sun, upon different parts of the earth when the positions of
the moon and sun change with respect to the earth.

Spring Tide: The tidal
effect of the sun and the moon acting in concert twice a month, when the
sun, earth and moon are all in a straight line (full moon or new moon).
The range of tide is larger than average.

Neap Tide: This opposite
effect occurs when the moon is at right angles to the earth-sun line
(first or last quarter). The range of tide is smaller than average.

Range: The vertical difference between the high and low tide water levels during one tidal cycle.

Tidal Day: 24 hours and 50
minutes. The moon orbits the earth every month, and the earth rotates
(in the same direction as the moon’s orbit) on its axis once every 24
hours.

Tidal Cycle: One high tide plus a successive low tide.

Semi-diurnal Tide: The most
common tidal pattern, featuring two highs and two lows each day, with
minimal variation in the height of successive high or low waters.

Diurnal Tide: Only a single
high and a single low during each tidal day; successive high and low
waters do not vary by a great deal. Such tides occur, for example, in
the Gulf of Mexico, Java Sea and in the Tonkin Gulf.

Mixed Tide: Characterized by
wide variation in heights of successive high and low waters, and by
longer tide cycles than those of the semidiurnal cycle. Such tides
occur, for example, in the U.S. Pacific coast and many Pacific islands.

Chart Datum or Tidal reference planes: These fictitious planes are used as the sounding datum for the tidal heights.

Drying Height: Clearance in meters (or feet in old charts) above the chart datum.

Charted Depth: Clearance in meters (or feet in old charts) below the chart datum.

Observed Depth: Height of tide + charted depth: the actual depth in meters.

Height of light: The height of light above the bottom of its structure.

Elevation: The height of the light above the chart datum.

Rule of Twelve: Assuming a
tidal curve to be a perfect sinusoid with a period of 12 hours. The
height changes over the full range in the six hours between HW and LW
with the following fractions during each respective hour: 1/12  ۲/۱۲ 
۳/۱۲  ۳/۱۲  ۲/۱۲  ۱/۱۲٫

Rule of Seven: The change
from spring range to neap range can be assumed linear, each day the
range changes with 1/7th of difference between the spring and neap
ranges. Hence, the daily change in range = (spring range – neap
range)/7.

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۱ – Information from the chart

Position of tabulated tidal levels data with designation 'a' - chart symbol
Most often the chart presents succinct tide tables for certain
positions. These positions are marked with the “square”. The table below
shows us an example for two different positions. The first refers to
Cowes (UK), the second to a position south of Cowes.

 Position
Heights above LATMean HW
Mean LWSpring
Neap
Spring
Neap Cowes
1,7 m
1,5 m
0,2 m
0,4 mPosition of tabulated tidal levels data with designation 'a' - chart symbol
5,2 m
4,3 m
0,4 m
1,2 m

This data only provides us with average high and low
waters heights. Moreover, it is merely valid at spring or neap tides. To
use it we need to first find out how many hours we are from high water.
Secondly, we need to know if it is spring or neap or sometime in
between at that particular moment. We shall use this table to solve two
types of problems. Finding height of tide at a particular location at a
particular time:

To get over a shoal.

To pass under a bridge.

Almanacs and many other nautical publications contain
predictions of the times of high and low tides at many major standard
ports. Also listed are differences in times of tides from these ports for additional secondary ports. To work with this succinct data we need two extra tools:

Rule of twelve To interpolate between high and low water heights we use the Rule of Twelve.
We assume the tidal curve to be a perfect sinusoid with a period of 12
hours. The height changes over the full range in the six hours between
HW and LW.

Hence, two hours after the HW the water has fallen 3/12 of the full range.

To interpolate between spring and neap tides we use the Rule of Seven.
Since the change from spring range to neap range can be assumed linear
(instead of sinusoid), each day the range changes with 1/7th of
difference between the spring and neap ranges.
Hence, the daily change in range is (spring range – neap range)/7.

Shoal problem:
Our shoal near Cowes has a
charted depth of 1 meter and we would like to cross it at about 15:00
hours with our yacht (draft 1,5 m).

From any nautical almanac we find that HW occurs at 03:18 15:53 and LW occurs at 09:45 22:03
at a standard port nearby. We also find that at our location HW occurs
one hour later and that spring tide is due in two days. Hence, we have a
HW around 17:00.

Via the rule of seven we find out that today the range is:
spring range – 2 x ( (spring range – neap range)/7 )
4,8 – 2 x ( ( 4,8 – 3,1)/7 ) 4,8 – 2 x 0,25 = 4,3 m.

We also need today’s HW height:
which is Spring HW – 2 days x ( (5,2 -4,3)/7 ) = 5,0 m.

Via the rule of twelve we find out that at two hours before high water the height is:
5,0 – 3/12 x 4,3 = height at 15:00 hours = 3,9 m.

So, after three interpolations we derive the water
height at 1500 hours. Considering the charted depth leads to an observed
depth of 4,9 meters, enough for our draft of 1,5 meters.

Bridge problem:
An overhanging rock, power
lines or bridges have their clearances charted with respect to another
chart datum than LAT. Normally, ‘high water’ or ‘MHW spring’ are used as
reference planes.

An example:
Above our shoal hangs the ‘Cowes bridge’.
At 15:00 hours we would like to pass this bridge, which has a charted
height of 20 meters to HW. Our mast is 23 meters high. In the example
above we found that the water height was 1,1 meters below HW level at
that time. Obviously, we will have to wait!
So, at what time will we be able to pass under this bridge?
The
water height must be 3 meters lower than HW level (5,0 m). That is
almost 9/12 of the range (4,3 m) indicating four hours after HW. Conclusion, we will have to wait at least six hours in total.

2 – Information from tide tables

Instead of mere averages, a tide tableDetailed Tide Table.
provides us each day with the times of high and low water for a
particular place. Basically, it is same table like the one we found in
the chart, but is extended for every day in a year. By using this method
we get more accurate water heights since it involves less
interpolation. The example shows us a part of a very detailed tide
table, which even includes heights for every hour.

3 – Information from tidal curves

In most tables the tides can also be characterized by a
tidal curve. This method substitutes the rule of twelve providing more
accurate heights. The left side contains the water height information
with the lowest heights to the left where also the chart datum is
indicated. The low water height will be marked at the bottom and the
high water height will be marked at the top.
Tidal Curve.
The area under the curve will be marked with the time information.
To find the water height at a specific time we need to know first how many hours before or after the HW this is. Then

Tidal Curve:Finding Heights.

Tidal Curve:Finding Time with Height.
Often this is done when the curve is not sinusoid and the rule of twelve is rendered useless.

 

Overview

Tide: The vertical rise and
fall of the surface of a body of water caused primarily by the
differences in gravitational attraction of the moon, and to a lesser
extent the sun, upon different parts of the earth when the positions of
the moon and sun change with respect to the earth.

Spring Tide: The tidal
effect of the sun and the moon acting in concert twice a month, when the
sun, earth and moon are all in a straight line (full moon or new moon).
The range of tide is larger than average.

Neap Tide: This opposite
effect occurs when the moon is at right angles to the earth-sun line
(first or last quarter). The range of tide is smaller than average.

Range: The vertical difference between the high and low tide water levels during one tidal cycle.

Tidal Day: 24 hours and 50
minutes. The moon orbits the earth once earth month, and the earth
rotates (in the same direction as the moon’s orbit) on its axis once
every 24 hours.

Tidal Cycle: A successive high and low tide.

Semi-diurnal Tide: The most
common tidal pattern, featuring two highs and two lows each day, with
minimal variation in the height of successive high or low waters.

Diurnal Tide: Only a single
high and a single low during each tidal day; successive high and low
waters do not vary by a great deal. Gulf of Mexico, Java Sea and in the
Tonkin Gulf.

Mixed Tide: Characterized by
wide variation in heights of successive high and low waters, and by
longer tide cycles than those of the semidiurnal cycle. U.S. Pacific
coast and many Pacific islands.

Chart Datum or Tidal reference planes: These fictitious planes are used as the sounding datum for the tidal heights.

Drying Height: Clearance in meters (or feet in old charts) above the chart datum.

Charted Depth: Clearance in meters (or feet in old charts) below the chart datum.

Observed Depth: Height of tide + charted depth: the actual depth in meters.

Height of light: The height of light above the bottom of its structure.

Elevation: The height of the light above the chart datum.

Rule of Twelve: Assuming a
tidal curve to be a perfect sinusoid with a period of 12 hours. The
height changes over the full range in the six hours between HW and LW
with the following fractions during each respective hour: 1/12  ۲/۱۲ 
۳/۱۲  ۳/۱۲  ۲/۱۲  ۱/۱۲٫

Rule of Seven: The change
from spring range to neap range can be assumed linear, each day the
range changes with 1/7th of difference between the spring and neap
ranges. Hence, the daily change in range = (spring range – neap
range)/7.

بازگشت به صفحه اصلی وبلاگ مهندسی عمران راه و ساختمان(مهندس حسن فراهانی)

برچسب‌ها: آّشنایی با جزر و مد, Tides, neap tides, spring tides, LAT, مهندس حسن فراهانی

منبع: http://hfarahani48.blogfa.com/post-9191.aspx

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قصب نماهای ناوبری (Compass navigation) و نیاز آن برای نقشه های دریایی (مهندس حسن فراهانی)

منبع : حمل و نقل دریایی

Home Nav. course Sailing Greece Turkish Coasts Yacht charter Gulets                

Marine compass

In China compasses have been in use since the Han dynasty (2nd century BCE
to 2nd century CE) when they were referred to as “south-pointers”.
However at first these magnets were only used for geomancy much like in
the art of Feng Shui.

Eventually, during the Sung dynasty (1000 CE) many
trading ships were then able to sail as far as Saudi Arabia using
compasses for marine navigation. Between 1405 and 1433, Emperor Chu Ti’s
Treasure Fleet of the Dragon Throne ruled the entire South Pacific and
the Indian Ocean, a territory that ranges from Korea and Japan to the
Eastern coast of Africa.

At this time Western mariners were still rather ignorant of the navigational use of the magnet. Petrus Perigrinus van Maricourt
wrote a first treatise on the magnet itself: “De Magnete” (۱۲۶۹). And
though its nautical use was already mentioned in 1187 by the English
monk Alexander Neckham, the use onboard only came about around the 13th
and 14th century in the Mediterranean Sea.

Much later, in 1545, Pedro de Medina (Sevilla 1493-1567)
wrote the Spanish standard work “Arte de Navegar” on marine compass
navigation. This masterpiece was first translated in Dutch (1580) and
was -O Irony- used by Jacob van Heemskerk
when the Dutch destroyed the Spanish fleet near Gibraltar in 1607. The
drawback was of course Van Heemskerk’s own death during this victory.

Magnetic Variation

In the fin-de-siècle of the sixteenth century mariners
believed that the magnetic north pole coincided with the geographic
north pole. Any suggestion otherwise had been denied by Pedro de Medina.

Magnetic observations made by explorers in subsequent
decades showed however that these suggestions were true. But it took
until the early nineteenth century, to pinpoint the magnetic north pole
somewhere in Arctic Canada (78° N , 104° W). From then on the angle
between the true North and the Magnetic North could be precisely corrected for. This correction angle is called magnetic variation or declination.

It is believed that the Earth’s magnetic field is
produced by electrical currents that originate in the hot, liquid, outer
core of the rotating Earth. The flow of electric currents in this core
is continually changing, so the magnetic field produced by those
currents also changes. This means that at the surface of the Earth, both
the strength and direction of the magnetic field will vary over the
years. This gradual change is called the secular variation
of the magnetic field. Therefore, variation changes not only with the
location of a vessel on the earth but also varies in time.

The correction for magnetic variation for your location is shown on the nearest! nautical chart’s compass rose.
In this example we find a variation of 4° ۱۵′ W in 2009, with an
indicated annual correction of 0° ۰۸′ E. Hence, in 2011 this variation
is estimated to be 3° ۵۹′, almost 4° West. This means that if we sail
90° on the chart (the true course), the compass would read 94°.

Another example: let’s say the compass rose gives a
variation of 2° ۵۰′ E in 2007, with a correction of 0° ۰۴′ E per year.
In 2009 this variation is estimated to be 2° ۵۸′, almost 3° East. Now,
if we sail 90° on the chart, the compass would read 87°.

Correcting for variation

Difference between true course and magnetic course
These overlayed compass roses show the difference between true north
and magnetic north when the magnetic variation is 10° West.

From the image we find: tc = cc + var
in which “cc” and “tc” stand for “compass course” and “true course”, respectively.

To convert a true course into a compass course
we need first assign a “-” to a Western and a “+” to a Eastern
variation. Note that this makes sense! because of the clockwise
direction of the compass rose. Here, the inner circle is turned 10°
anticlockwise, hence -10°.
Now, use the same but re-written equation:
cc = tc – var
235° = ۲۲۵° – (-۱۰°)
So, to sail a true course of 225°, the helmsman has to steer a compass course of 235°.

To convert a compass course into a true course
we can use the original equation. If we have steered a compass course
of 200°, we have to plot a true course of 203° in the chart if the
variation is 3° East or a true course of 190° if the variation is 10° West.

Magnetic deviation

Magnetic deviation is the second correctable error. The
deviation error is caused by magnetic forces within your particular
boat. Pieces of metal, such as an engine or an anchor, can cause
magnetic forces. And also stereo and other electric equipment or wiring,
if too close to the compass, introduce errors in compass heading.

Furthermore, the deviation changes with the ship’s
heading, resulting in a deviation table as shown below. The vertical
axis states the correction in degrees West or East, where East is again
positive.

Deviation table: For each heading a different deviation correction is needed.

The horizontal axis states the ship’s heading in
degrees divided by ten. Thus, when you sail a compass course of 220°,
the deviation is 4° W. (Note, that on most modern sailing yachts the
deviation is usually not larger than 3°).

When a compass is newly installed it often shows larger
deviations than this and needs compensation by carefully placing small
magnets around the compass. It is the remaining error that is shown in
your deviation table.
You can check your table every now and then by placing your boat in the line of a pair of leading lights and turning her 360 degrees.

Correcting for both deviation and variation

Converting a compass course into a true course, we can still use our equation but we need to add the correction for deviation:
cc + var + dev = tc

Example 1: The compass course is 330°, the deviation is +3° (table) and the variation is +3° (chart);
330° cc + 3° var + 3° dev = ?° tc
giving a true course of 336° which we can plot in our chart

Example 2: The compass course is 220°, the deviation is -4° (table) and the variation is still +3° (chart).
220° cc + 3° var + -4° dev = ?° tc
giving a true course of 219°.

Example 3: The compass course is still 220°, therefore the deviation is still -4° (table) but let’s use a variation of -10° this time.
220° cc + -10° var + -4° dev = ?° tc
giving a true course of 206°.

Converting a true course into a compass course is a little less straight forward, but it is still done with the same equation.

Example 4: The true course from the chart is 305° and the variation is +3° (chart), yet we don’t know the deviation;
?° cc + 3° var + ?° dev = 305° tc
Luckily, we can rewrite this so this reads:
cc + dev = 305° tc – + 3° var = 302°
In
plain English: the difference between the true course and the variation
(305 – + 3) = 302 should also be the summation of the compass course
and the deviation. So, we can tell our helms person to steer 300°, since
with a cc of 300° we have a deviation of +2° (As can be deduced from
the deviation table above).

Example 5: The true course
from the chart is 150° and we have a Western variation of 7 degrees
(-7°). We will use the rewritten equation to get:
150° tc – - 7° var = cc + dev = 157°
From the deviation table we find a compass course of 160° with a deviation of -3°.
Voilà!

Magnetic course

The magnetic course (mc) is
the heading after magnetic variation has been considered, but without
compensation for magnetic deviation. This means that we are dealing with
the rewritten equation from above:
tc – var = cc + dev = mc.

Magnetic courses are used for three reasons:Three types of North - compass, magnetic, true

To convert a true course into a compass course like we saw in the last paragraph.

On vessels with more than one steering compass, also
more deviation tables are in use; hence only a magnetic or true course
is plotted in the chart.

Bearings taken with a handheld compass often don’t
require a correction for deviation, and are therefore useful to plot in
the chart as magnetic courses.

Note, that the actual course lines the
navigator draws in the chart are always true courses! These can
subsequently be labeled with the true course or the corresponding
magnetic or compass course if appropriate. In the next chapter we will be plotting courses in the chart.

To summarise, we have three types of “north” (true,
magnetic and compass north) like we have three types of courses: tc, mc
and cc. All these are related by deviation and variation.

Glossary

Maps with isogonic lines:
World – overview 2000
World – detailed 2000
World – detailed 2005
World – animated in time
Variation: The angle between the magnetic north pole and the geographic north pole. Also called the magnetic declination.

Secular variation: The change of magnetic declination in time with respect to both strength and direction of its magnetic field.

West (-) , East (+):
Western variations or deviations are designated with a negative sign by
convention due to the compass card’s clockwise direction.

Deviation: The error in compass heading caused by electric magnetic currents and or metal objects.

Deviation table: A table containing deviations in degrees versus the ship’s heading (compass course) in degrees. Usually plotted in a graph.

True course: Course plotted in the chart i.e. course over the ground or “course made good”. The course corrected for compass errors.

Compass course: The course (ship’s heading) without the correction for compass errors.

cc + var + dev = tc: This
equation shows the connection between the compass course, its errors and
the true course. It can also be read as: tc – var = cc + dev

بازگشت به صفحه اصلی وبلاگ مهندسی عمران راه و ساختمان(مهندس حسن فراهانی)

برچسب‌ها: قصب نماهای ناوبری, Compass navigation, نقشه های دریایی, مهندس حسن فراهانی

منبع: http://hfarahani48.blogfa.com/post-9188.aspx

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بازگشت به صفحه اصلی وبلاگ مهندسی عمران راه و ساختمان(مهندس حسن فراهانی)

برچسب‌ها: دانلود, دستورالعمل, نرم افزار, طراحی بتن آسفالت, میخ پرچ, DowelCAD 2, 0, مهندس حسن فراهانی

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معرفی ۵۰ منبع اصلی در مدیریت بحران (مهندس حسن فراهانی)

۲٫ Benjamin, Daniel, and Steven Simon. The Age of Sacred Terror. New York: Random House, 2002.

3. Brower, David J. and Charles C. Bohl. Principles and Practice of Hazards Mitigation. Emmitsburg, MD: FEMA Emergency Management Higher Education Project College Course, April 2000. At:

4. Bullock, Jane, George Haddow, Damon Coppola, Erdem Ergin, Lisa Westerman, and Sarp Yeletaysi. Introduction to Homeland Security. Amsterdam and other cities: Elsevier, Butterworth Heinemann: 2005.

5. Burby, Raymond J., et al. Building Disaster Resilient Communities. Emmitsburg, MD: FEMA Emergency Management Higher Education Project College Course, May 2002. Accessed at:

6. Burby, Raymond. Cooperating with Nature: Confronting Natural Hazards with Land-Use Planning for Sustainable Communities. Washington, DC: Joseph Henry Press, 1998.

7. Canton, Lucien G. Emergency Management: Concepts and Strategies for Effective Programs. Hoboken NJ: Wiley Inter-Science, 2007.

8. Cutter, Susan L. (Ed.). American Hazardscapes: The Regionalization of Hazards Disasters. Wash DC: Joseph Henry Press, 2001.

9. Department of Homeland Security. National Response Plan. Washington, DC: DHS, May 25, 2006 Revision.

10. Drabek, Thomas E. and Gerard J. Hoetmer (eds.). Emergency Management: Principles and Practice for Local Government. DC: International City Managers Association, 1991.

11. Drabek, Thomas E. Strategies for Coordinating Disaster Responses. Boulder, CO: Program on Environment and Behavior, Monograph 61, University of Colorado, 2003.

12. Drabek, Thomas E. Social Dimensions of Disaster, 2nd Edition.
Emmitsburg, MD: FEMA Emergency Management Higher Education Project College Course, April 2004. Accessed at:

13. EMAP Standards (Emergency Management Accreditation Program). NEMA

14. Enarson, Elaine, et al. A Social Vulnerability Approach to Disasters. Emmitsburg MD: FEMA Emergency Management Higher Education Project College Course, May 2003. Accessed at:
http://training.fema.gov/EMIWeb/edu/completeCourses.asp

15. FEMA. Guide For All-Hazard Emergency Operations Planning (State and Local Guide (SLG) 101). Washington DC: FEMA, September 1996.

16. FEMA Independent Study IS-1, Emergency Manager: An Orientation to the Position.

17. FEMA. Multi Hazard Identification and Risk Assessment – A Cornerstone of the National Mitigation Strategy. Washington, DC: FEMA. 1997. Accessed at:

18. Flynn, Stephen. The Edge of Disaster: Rebuilding A Resilient Nation. NY: Random House, 2007.

19. Godschalk, David R., with the Assistance of David Salvesen. Breaking the Disaster Life Cycle: Future Directions in Natural Hazard Mitigation. FEMA Emergency Management Higher Education Project College Course, March 2004. Accessed at

20. Godschalk, David R., Timothy Beatley, Philip Berke, David Brower, and Edward Kaiser. Natural Hazard Mitigation: Recasting Disaster Policy Planning. Island Press. 1999.

21. Haddow, George D. and Jane A. Bullock. Introduction to Emergency Management (2nd Ed.). Burlington, MA: Elsevier Butterworth-Heinemann, 2006.

22. Kincaid, J. Peter. Research and Analysis Methods in Emergency Management. Emmitsburg, MD: FEMA Emergency Management Higher Education Project College Course, December 1998. Accessed at:

23. Laws, Ordinances, Regulations, Plans Establishing, Affecting Guiding EM

24. Lindell, Michael K., Carla Prater, Ronald W. Perry. Fundamentals of Emergency Management. Emmitsburg MD: FEMA Emergency Management Hi-Ed Project, 2006.

25. Lustic, Ian S. Trapped in the War on Terror. Philadelphia: University of Pennsylvania Press, 2006.

26. May, Peter J, et al. Environmental Management and Governance: Intergovernmental Approaches to Hazards and Sustainability. London NY: Routledge, 1996.

27. McEntire, David A. Disaster Response Operations and Management. Emmitsburg, MD: FEMA Emergency Management Higher Education Project College Course, September 2005. Accessed at:

28. Mileti, Denis. Disasters by Design: A Reassessment of Natural Hazards in the U.S. Washington, DC: Josephy Henry Press, 1999.

29. Mueller, John. Overblown: How Politicians and the Terrorism Industry Inflate National Security Threats, and Why We Believe Them. Free Press, 2006.

30. National Commission on Terrorist Attacks Upon the United States. The 9/11 Commission Report (Final Report of the National Commission on Terrorist Attacks Upon the United States; Authorized Edition). New York: W.W. Norton Co., 2004.

31. National Research Council. Facing Hazards and Disasters: Understanding Human Dimensions. Washington, DC: National Academies Press, 2006.

32. National Fire Protection Association. NFPA 1600: Standard on Disaster/Emergency Management and Business Continuinty Programs, 2007 Edition. Quincy, MA: NFPA, 2007. At:

33. National Incident Management System (NIMS) materials, including FEMA IS-700.

34. Noji, Eric K. (Ed.). The Public Health Consequences of Disasters. New York and Oxford: Oxford University Press, 1997.

35. Perrow, Charles. 1999. Normal Accidents: Living With High-Risk Technology. Princeton, NJ: Princeton University Press.

36. Pine, John. Hazard Mapping and Modeling. Emmitsburg MD: FEMA Emergency Management Higher Education Project College Course, November 2006. Accessed at:

37. Pine, John C. Technology and Emergency Management. Emmitsburg MD: FEMA Emergency Management Higher Education Project College Course, February 1999. Accessed at:

38. Platt, Rutherford H. Disasters and Democracy: The Politics of Extreme Natural Events. Washington, DC: Island Press, 1999.

39. Quarantelli, E.L. (ed.) What is a Disaster – Perspectives on the Question. London and New York: Routledge, 1998.

40. Rodrigeuz, Havidan, Enrico L. Quarantelli, and Russell R. Dynes. Handbook of Disaster Research. Springer, 2006.

41. Rottman, Steven J. Individual and Community Disaster Education Course. Emmitsburg, MD: FEMA Emergency Management Higher Education Project College Course, March 2000. Accessed at:

42. Shaw, Greg. Business and Industry Crisis Management, Disaster Recovery, and Organizational Contiuity. Emmitsburg MD: FEMA Emergency Management Higher Education Project College Course, November 1999. Accessed at:

43. Shaw, Gregory. Hazards Risk Management. Emmitsburg, MD: FEMA Emergency Management Higher Education Project College Course, January 2004. Accessed at:

44. Smith, Gavin. Holistic Disaster Recovery: Creating a More Sustainable Future. Emmitsburg MD: FEMA Emergency Management Higher Education Project College Course, September 2004. Accessible at:

45. Sylves, Richard T., and William L. Waugh, Jr. Disaster Management In The U.S. and Canada – The Politics, Policymaking, Administration and Analysis of Emergency Management (2nd ed.).
Springfield, IL: Charles C. Thomas, 1996.

46. Tierney, Kathleen J, Michael K. Lindell and Ronald W. Perry. Facing the Unexpected: Disaster Preparedness and Response in the United States. Joseph Henry Press, 2001.

47. Tobin, Graham A. and Burrell E. Montz. Natural Hazards: Explanation and Integration. New York and London: The Guilford Press, 1997.

48. Waugh, William L. Living With Hazards/Dealing With Disasters-An Introduction To Emergency Management. Armonk, NY: M.E. Sharpe, Inc., 2000.

49. Waugh, William L. Jr. Terrorism and Emergency Management. Emmitsburg, MD: FEMA Emergency Management Higher Education Project College Course, September 2000. Accessed at:

50. Wisner, Ben, Piers Blaikie, Terry Cannon, and Ian Davis. At Risk: Natural Hazards, People’s Vulnerability and Disasters (2nd Ed.). London and New York: Routledge, 2004.

منبع: http://hfarahani48.blogfa.com/post-8930.aspx

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بازگشت به صفحه اصلی وبلاگ مهندسی عمران راه و ساختمان(مهندس حسن فراهانی)

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برنامه پروکن prokon 2.5.17 SP1 + کرک پروکن Kgen.PROKON.2012 (مهندس حسن فراهانی)

منبع : ایران سازه

برنامه پروکن prokon 2.5.17 SP1

PROKON Structural Analysis and Design 2.5.17 SP1

PROKON Structural Analysis and Design 2.5.17 SP1 | 200.3 MB

Fileserve Filesonic

PROKON Structural Analysis and Design software trusted by structural engineers worldwide teveloped by Engineers, for Engineers.

Company History

PROKON Software Consultants was founded by Karl Eschberger and Jacques
Pienaar in 1989. Working as young structural engineers in a large
consulting firm, they recognised the immense potential of software in
structural analysis and design (it was still early days for the PC).
During their time consulting, they wrote small individual programs for
the hand-held calculators like the Hewlett-Packard HP-35 Scientific
Calculator. As word spread around, many of their colleagues started
using the programs for their daily work.

About PROKON Structural Analysis and Design

PROKON Structural Analysis and Design is a suite of over thirty
structural analysis, design and detailing programs. The first PROKON
programs were developed in 1989, and today PROKON is used worldwide in
over eighty countries. The suite is modular in nature, but its true
power lies in the tight integration between analysis, design and
detailing programs.

By Engineers, for Engineers

PROKON Structural Analysis and Design is developed by a team of
professional engineers and aimed for use by structural engineers and
technicians. The software provides quick and reliable answers to
everyday structural and geotechnical engineering problems:

- Frame and finite element analysis

- Steel member design

- Steel connection design

- Reinforced and prestressed concrete design

- CAD and reinforced concrete detailing

- Timber member design

- Masonry design

- Other structural applications such as section properties calculation and section database


Download


http://www.filesonic.com/file/4096979534


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لینک مستقیم


http://sv01.p
remium.irleech.com/dl/203381/pssaade2517s1.rar

برنامه کرک پروکن Kgen.PROKON.2012

http://hfarahani48.blogfa.com

به حجم ۷۶ کیلوبایت

در فرمت فشرده (rar)

بازگشت به صفحه اصلی وبلاگ مهندسی عمران راه و ساختمان(مهندس حسن فراهانی)

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