3-Newton`s law of gravity قانون نيوتن للثقالة
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Transcript 3-Newton`s law of gravity قانون نيوتن للثقالة
3- Newton's law of gravity
قانون نيوتن للثقالة
Galileo Galilei
(1564-1641)
Using a telescope he
made, Galileo
observed:
Moons of Jupiter.
Phases of Venus.
His findings supported
a Copernican model.
He spent the end of
his life under “house
arrest” for his beliefs.
Johannes Kepler
German astronomer (1571–1630)
Kepler has try to
deduce a
mathematical
model for the
motion of the
planets.
Isaac Newton (1642-1727).
• " Every particle in the Universe
attracts every other particle with a
force that is directly proportional
to the product of their masses and
inversely proportional to the
square of the distance between
them ".
• أي جسيم في الكون يجذب أي جسيم
آخر بقوة تتناسب طرديا ً مع
مضروب كتلتيهما وتتناسب عكسيا
مع مربع المسافة فيما بينهما.
If the particles have
masses m1 and m2 and
are separated by a
distance r, the
magnitude of this
Fg
gravitational force is:
m2 وm1 إذا كانت كتلة الجسيمان
فإن، r وكان يفصالهما مسافة
:مقدار قوة التثاقل يكون
G
m1 m2
r
2
• where G is a universal constant called the
universal gravitational constant which
has been measured experimentally.
• The value of G depends on the system of
units used, its value in SI units is:
.ً ثابت عام يسمى ثابت التثاقل العام وهو مقاس معملياGحيث
على نظام الوحدات المستخدمة وقيمته فيGتعتمد قيمة
:النظام الدولي
G = 6.672 x 10-11 N. m2 / kg2
• The force law is an:
inverse-square law
قانون التربيع العكسي
because the magnitude of the
force varies as the inverse square
of the separation of the particles.
• We can express this force in
vector form شكل اتجاهيby
defining a unit vector
r12 متجه الوحدة
• Because this unit vector is in the
direction of the displacement vector
r12 directed from m1 to m2, the force
exerted on m2, by m1 is :
F21 = - (G ( m1 m2 ) / r122 ) r12
• Likewise, by Newton's third law
the force exerted on m1 by m2,
designated F12, is equal in
magnitude to F21 and in the
opposite direction.
• That is these forces form an actionreaction pair زوج من قوى الفعل ورد الفعل
F12 = F21
• the gravitational force exerted by a
finite-size, spherically symmetric
mass distribution on a particle
outside the sphere is the same as
if the entire mass of the sphere
were concentrated at its center
• تعمل القوى كما لو أن كتلة الكرة
. مركزة في مركزها
• For example, the force exerted by the
Earth on a particle of mass m at the
Earth's surface has the magnitude
Fg = G ( mE m ) / RE2
mE is the Earth's mass كتلة األرضand
RE is the Earth's radius نصف قطر األرض
• This force is directed toward the
center of the Earth
موجهة نحو مركز األرض
• At points inside the earth:
We would find that the force
decreases as we approach the
center.
Exactly at the center the
gravitational force on a body
would be zero.
4-Measurement of the gravitational constant
قياس ثابت التثاقل العام
The universal gravitational constant, G, was
measured by Henry Cavendish in 1798
5- Weight and gravitational force
الوزن وقوة التثاقل
If g is the magnitude of the free-fall
acceleration, and since the force on a
freely falling body of mass m near the
surface of the Earth is given by
F = m g, we can equate
m g = G ( mE m / RE2 )
g
G mE
2
RE
Using the facts that g = 9.80 m/s2 at
the Earth's surface and RE = 6.38 x
10)6( m, we find that
mE = 5.98 x 10)24( kg.
• From this result, the average density
of the Earth is calculated to be :
• ρE = mE / VE = mE / ( 4/3 π RE3 )
•
= 5.98 x 10 24
/
( 4/3 π 6.38 x 106 m
)3
= 5500 kg/m3 = 5.5 g/cm3
• Since this value is higher than
the density of most rocks at the
Earth's surface (density of
granite =
3 g/cm3),
• we conclude that the inner core
of the Earth has a density much
higher than the average value.
• بما أن تلك الكثافة قيمتها أعلى من كثافة
معظم المواد الصخرية على األرض فإننا
نستنتج من ذلك أن القلب الداخلي لألرض له
كثافة أعلى من القيمة المتوسطة لكثافة
.األرض
• The magnitude of the gravitational
force acting on this mass is:
• Fg = G ( ME m / r2 )
= G ( ME m / ( RE + h )2 )
• If the body is in free-fall, then
Fg = mg' and we see that g', the freefall acceleration experienced by an
object at the altitude h, is
g' = G mE / r2
= G mE / ( RE + h ) 2
• Thus, it follows that g' decreases with
increasing altitude تقل عجلة الجاذبية كلما
ارتفعنا عن سطح األرض.
• Since the true weight of an object is
mg , we see that as r →∞, the true
weight approaches zero.
6- The Gravitational Field مجال
التثاقل
• When a particle of mass m is
placed at a point where the
field is the vector g, the
particle experiences a force
Fg = m g.
• the gravitational field is defined
by:
g = Fg / m
• consider an object of mass m
near the Earth's surface.
The gravitational force on the
object is directed toward the
center of the Earth and has a
magnitude (m g).
• Since the gravitational force on
the object has a magnitude :
(G mE m) / r2
field g is
g
Fg
m
G mE
r
2
where r is a unit vector pointing
radially outward from the Earth, and
the minus sign indicates that the field
points toward the center of the Earth
and is always opposite to r
r
• We have used the same symbol
نفس الرمزg for gravitational field
magnitude that we used earlier for
the acceleration of free fall.
The units of the two quantities are
the same الكميتان لهما نفس الوحدات.
Example
• A ring-shaped body with radius a
has total mass M. Find the
gravitational field at point p, at a
distance x from the center of the
ring, along the line through the
center and perpendicular to the
plane of the ring.
• We imagine the ring as being
divided into small segments Δs,
each with mass ΔM. At point P
each segment produces a
gravitational field Δg with
magnitude.
• Δg = )G ΔM( / r2 = )G ΔM( / )x2 + a2)
• The component of this field along the xaxis is given by : Δgx = - Δg cosφ =
• - G ΔM .
x
• x2 + a2
(x2 + a2) ½
•
•
= - G ΔM x
(x2 + a2)3/2
• we simply sum all the ΔM 's.
This sum is equal to the total
mass M.
gx
GM x
(x a )
2
2
3
2
7-Gravitatiuonal Potential
energyطاقة الوضع للجاذبية
• we know that the earth's
gravitational force on a body of
mass m, at any point outside
the earth, is given by
• w = fg = (G m mE ) / r2
We compute the work Wgrav done by the
gravitational force when r changes
from r1 to r2
r2
W grav
r1
Fr dr
Thus Wgrav is given by:
r2
W grav
G m mE
dr
r
r1
2
G m mE
r2
G m mE
r1
• Wgrav = U1 - U2 where U1 and U2
are the potential energies of
positions 1 and 2 . So Comparing
this with the eq. of Wgrav gives:
U
G m mE
r
8- Kepler's laws قوانين كبلر
•The complete analysis is
summarized in three statements,
known as Kepler's laws:
• l. All planets move in elliptical orbits with
the Sun at one of the focal
points.
كل الكواكب تتحرك في مدارات
.على شكل قطع ناقص تقع الشمس في إحدى بؤرتيه
• 2. The radius vector drawn from the Sun
to a planet sweeps out equal areas in
equal time intervals.
• المتجه القطري المخطوط ما بين الشمس و كوكب ما يمسح
. مساحات متساوية في أزمنة متساوية
• 3. The square of the orbital period of any
planet is proportional the cube of the semi
major axis of the elliptical orbit.
ربع الزمن الدوري ألي كوكب يتناسب مع مكعب
•
. المحور األفقي للمدار الذي على شكل قطع ناقص