Thứ Hai, 30 tháng 1, 2017

Waching daily Jan 30 2017

For Some Likes

After 2 hours

After 20 minutes

For more infomation >> Για Λίγα Likes (For some Likes) - Duration: 1:14.

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Farming Simulator 17 SEEDS AND FERTILIZER #4 - Duration: 18:04.

HI GUYS !!!! Welcome to Farming Simulator 17 Mods Channel This is the fourth episode of the series SEEDS AND FERTILIZER. In this video I show you some new mods you can use to plant and fertilize your fields.

JOHN DEERE 8030 SERIES Front Attacher 5 Engine Setup 3 Wheel Setup 4 Design Setup

IC CONTROL SPACE Illuminated Dash

Amazone EDX 6000 TC 6m Working Width Crops: maize, sugar beet, soya beans, sunflower

Vss Front Cultivator 5m Working Width Colorable

Seed Express 1260 Semi Trailer Fillable only with seeds, fertilizer and potatos. 45,000l Capacity Colorable

Upgraded Seed and fertilizer storage Placeable Silos

Changelog: Removing grass improves when placing, Fertilizer bearing bug fixes Shovel triggered with seed Fill particles New silo for better removal

Seed Express 1260 Semi Trailer Open Cover And Ladders X KEY Pipe Out O KEY

This is game stock KVERNELAND OPTIMA V Sowing Machine is not compatible :p

I made some mistakes in this video but I decided to share it with you to give you some advice what to AVOID

1) Most of the time game stock tools are not compatible with modded tools.

2) If you adapt more than one implement on your tractor the option HIRE WORKER It is likely to malfunction

3) If you decide to combine Front cultivator and sowing machine try to have the same working width or if you can not find the same working width Sowing Machine must be wider.

My first thought to combine Vss Front Cultivator and Amazone EDX 6000 TC ...

But my the calculations were wrong and I made the wrong choice to use game stock KVERNELAND OPTIMA V Sowing Machine

So the Front Cultivator it was wider and a part of the field stay unplanted

To overload the sowing machine , must be stop and folded

the worker confused

If you enjoy watching my videos... Give thumb up SUBSCRIBE FOR MORE And for any question ( or just for say HI!!) LET comment I will be happy to answer you...... bb

For more infomation >> Farming Simulator 17 SEEDS AND FERTILIZER #4 - Duration: 18:04.

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Amazing Street Wall Painting Art Competition In Lahore Held By Master Paints - Duration: 11:58.

Amazing Street Wall Painting Art Competition In Lahore

Sponser By Master Paints

Along Maulana Shaukat Ali Road University Side Wall

More Then 100 Paintings By More Then 500 Artist

Watch Full Video To Give Balanced Review Through Comment Box

For more infomation >> Amazing Street Wall Painting Art Competition In Lahore Held By Master Paints - Duration: 11:58.

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EOS s2: Tag Team PVP BG!~ - Duration: 3:12.

Welcome! ʕ•ᴥ•ʔ

♥Lucystar + RenGasai Tag Team ♥

Save yourself Lucy!! ◉_◉

Time for a ninja kill!

Ninja kill 2! ☠

Double sided tag team ftw!

Thank you for watching! ❤

For more infomation >> EOS s2: Tag Team PVP BG!~ - Duration: 3:12.

-------------------------------------------

CSGO-Funny Moments #1 Russian Team - Duration: 3:14.

For more infomation >> CSGO-Funny Moments #1 Russian Team - Duration: 3:14.

-------------------------------------------

19. Physics | MOD | Graphical Analysis of Motion | by Ashish Arora (GA) - Duration: 17:11.

Dear students, now we are going to use graphical analysis of motion. as we are studying rectilinear

motion, in rectilinear motion 3 types of graph are used in motion analysis. we'll see that

these graphs are quite helpful, in solving various kind of problems of , rectilinear

motion also. these three types of graph are . displacement versus time graph. second is,

velocity versus time graph . and the third is, acceleration versus time graph. we also

discuss the variant of displacement time graph as, distance time graph . we'll also discuss

distance versus time graph. we'll also discuss speed versus time graph, because , some particular

type of problems are also asked on distance and speed versus time graphs. but we don't

need to spend much time on these at, slight variations of displacement and velocity time

curves. lets discuss these one by one. now if we talk about displacement versus time

graphs . these are also known as , position versus time graphs. there is no difference

between position versus time and displacement versus time graphs. say for a given rectilinear

motion, we, draw the displacement time curve, like this. so this is the curve, according

to which, the position of a particle varies with time. so its function is given as x=

f of t. in this situation at any instant of time, (t) we can directly get the position

of particle by using, this curve, or by substituting the value of time in this function. say if

this point is p, we draw a tangent , of this curve at this point p, and say it makes an

angle theta with the time axis so we can simply state. the slope of the curve. at point p

can be written as, d x by d t, which is = tan theta . and we all know that d x by d t, can

be directly written as, instantaneous velocity of the particle at this position p. so by,

displacement time graph , at any point if we want to calculate , or we want to evaluate

the instantaneous velocity of the particle, we just need to find out the slope of the

curve, at that point and the slope will be directly give us the, instantaneous velocity

of the particle at that point. so in this situation we can see that, this tangent makes

an acute angle, with the, time axis, here we can simply state the velocity v p which

is tan theta , will be a positive , quantity. if we talk about the decreasing part of the

curve at a point q, if we consider a tangent, you can state, this angle theta dash will

be an obtuse angle. so at point q, the instantaneous velocity can be written as tan theta dash.

and tangent of the obtuse angle can be written as, a negative physical quantity. so in the

decreasing part of curve we can say with time the displacement is coming down , or displacement

is decreasing. or, as if we talk about the position of particle it is moving towards

origin. so we can state vector ally the velocity will be, negative. we can also talk about

various situations, like, for a practical situation . if say, a particle moves, in such

a way, that, first it accelerates, than it moves uniformly, and then say it retards . initially

say it was at rest, and finally also say it'll come to rest . so first it accelerates its

velocity increases, than it moves uniformly , and then finally, it comes to rest. now

in such situations, if particle is accelerating we can simply state the slope will first increase.

and then it moves uniformly that mean its slope remains constant, because you can see

the slope is giving as the instantaneous velocity. and if it it retards, that mean the slope

decreases and finally it becomes zero. so if we draw, the displacement time graph, of

such a motion, we can state first slope is increasing, the curve goes like this you can

see , continual sly the angle which , tangent makes with the time axis increasing. and then

say, for a time t 1 it is, accelerating, and from time t 1 to t 2 or you can say for a

duration t 2 , it moves uniformly so we can draw a straight line. so here, the whole slope,

for the duration t 2 remains constant, then it retards , so you can simply draw a curve

like this. which for another duration say t 3. now in this situation finally you can

see the slope become zero and earlier also slope was zero. this is the curve , which

is representing a motion where particle first accelerate, then moves uniformly and then,

retards . similar to this if we just, consider an experimental

situation like, say this positive direction of x axis. from origin a particle starts.

it moves with a velocity v. it goes up to a particular position in a time t 1. then

for a time t 2 it remains at rest over there , and then it comes back to origin, with the

same velocity v. in a time t 3. so from zero to t 1, it was moving uniformly , up to, this

position, say we write maximum displacement x m. for a duration t 2 it remains at rest,

and then , for at time t 2 it'll start, moving in opposite direction, and time t 3 it comes

back. now if we draw, the , position versus time graph, for this motion. you can simply

state it t = 0 particle starts, with an uniform velocity, uniform velocity means the slope

remains constant here we can write tan theta = v. this was the time t 1 for which the particle

was moving uniformly. then you can state up to time t 2 , or for the duration t 2 minus

t 1 it remains at rest. so its position remains constant i.e. at, x m. and then, it'll start

coming back so the velocity, is in opposite direction or we can say, when it was moving

toward (right) velocity was positive and now velocity is negative. so it comes down and

at a time t 3 it'll reach the, original position back. so, you can simple state again x becomes

zero. and say this angle is theta dash, so we can again write tan theta dash is equals

to v. now this angle will be , 180 minus theta, and we can state the, tangent of obtuse angle

is negative . so this angle theta dash can be directly taken as the angle by which we

can directly calculate the negative slope . so this is the, curve which is drawn , for

uniform motion then rest for some duration , and then again uniform motion in opposite

direction . now if similar , this is the curve which we call as position time curve or position

time graph . if similar graph is drawn for distance time .

let us draw distance time graph for the same, motion of particle when it is moving then

rest , taking rest and then coming back. so you can simply state , if we talk about displacement

, it first increases to x m then decreases to zero. but when we talk about distance , we

can state distance is continually increasing, because from here to here the distance is

x m, and when it comes back , the total distance travelled by the particle will become 2 x

m. now only difference in position time and distance time graph, can be taken, that, distance

time graph , if this is taken as distance, distance time graph will never come down.

say it'll first increase to a position, of x m, for a time t 1, than, it remains, at

rest , up to a time t 2, and then again it returns back, but if we talk about, position

it is coming down, but if we talk about distance it is still increasing, so the same graph

can be, drawn in reverse direction. so up to a time t 3, it will be able to cover a

distance of 2 x m. this is the distance time graph for the same motion, you can simply

state if we are having a displacement time graph, then for those portions of displacement

time graph, where the curves is coming down, you can draw the mirror image with respect

to time axis in upward direction, that will become, distance time graph.

if we talk about velocity time graphs. these are the graphs relating velocity with time.

say we draw, graph in, velocity and time, for motion of particle, this graph is drawn,

for the function of velocity how it varies with time. at, any position of this graph,

similar to, that of displacement time graph. here if you draw tangent , and you find out

the slope, of this graph, say at point x, we can simply state this point is relating

time with, velocity. and here the slope can be written as d v by d t or it can be written

as tan theta. and here the slope is giving us, the acceleration of particle at the position

x. so always remember that the slope of velocity time graph gives us the , instantaneous acceleration.

and, if a slope is positive like, here you can see acceleration at point x, it is

tan theta and theta is acute angle this can be taken as , positive acceleration . positive

acceleration means the velocity, and acceleration have same direction and you can simply state,

the, speed of particle is increasing or the magnitude of velocity is increasing in this

case. when we talk about the decreasing part of the curve , at any position if we draw

tangent, you can see the angle theta dash is obtuse. so this the point y, so we can

say acceleration at point y it'll be tan theta dash , which is an negative quantity. so here

you can see the velocity is decreasing so acceleration we considered to be negative.

so be careful about, the situation, where we have finding the slope of velocity time

curve as, acceleration. along with this we are already studied, in calculus, that area

under a curve can be given by, for between, two, coordinates on time axis, say t 1 and

t 2. if we find out the area of this curve. so area under the curve can be given as,

integration of v d-t from t 1 to t 2 . here you can see, this integration of v d-t, will

be given as displacement only. because, if we talk about v into d-t, it is the displacement

covered by the particle during the time d-t. so if we calculate the total displacement

of particle, from point t 1 to time t 2, it can directly be given as, integration of v

d-t from t 1 to t 2, it'll give us the displacement of particle. from t =, t 1 to, t 2. this

is another advantage of using velocity time graph, that from velocity time graph using

slope we can find out the instantaneous acceleration of particle, and finding out the area under

the curve, like say if we find out this area by using integration, this area under the

curve gives us the, displacement of particle, between two given time instants, in the

given situation.

if we just have a look on motion situation, as shown in the velocity time graph. a particle

moves in such a way that, t= 0 its initial velocity was zero, first velocity increases

that means it was accelerating, and then after some time it'll decreases and again

it become zero at time t 1. than velocity becomes negative, you can say, this is the

negative direction of velocity, and velocity becomes negative that means particle as returned

in opposite direction, and at time t 2 (again) its velocity become zero. so in such situation

you can say from time 0 to t 1. the area between the curve and the time axis, above the time

axis this, positive. and from time t 1 to t 2 you can see, that this area is below the

time axis, so this is written as negative. say, this total area is s1 and this total

area is s 2. so we can state, total displacement. of particle. from t = 0 to t 2. is, total

displacement can be written as s 1 minus s 2. but when we talk about distance travelled.

you can always write distance travelled= s 1 + s 2. because s 1 is the distance travelled,

in positive direction and s 2 is the distance travelled in, opposite direction. so displacement

will be s 1 minus s 2, but when we talk about distance travelled it will be s 1 + s 2, so

be careful about such situations, while drawing velocity time curves. similar to this we can

also talk about, acceleration time graphs. but there is nothing much to discuss about

acceleration time graphs. like if we draw acceleration time graph, for a given motion,

you can simply state in acceleration time graph if we find out the slope. that a slope

will give us the (rate) with which will the acceleration is varying. which is not of much

import ants, in, our limitations, or, in the syllabus we are analyzing the things, but

when we talk about the, (area) under the acceleration time curve or area between the acceleration

time curve and time axis, say between to instants t 1 and t 2, so when it is of, quite importance

like, if we find out this area. this area is say (a) so this (a) can be written as integration

of (a) d-t from time t 1 to t 2. this (a) d-t will give us, net change. in velocity,

of particle. from, t 1 to t 2. there is something which is important for us to keep in mind,

integration of (a) d-t from t1 to t 2 gives us the net change in velocity of particle

in going from, time t 1 to, time t 2. this, you should always keep in mind

For more infomation >> 19. Physics | MOD | Graphical Analysis of Motion | by Ashish Arora (GA) - Duration: 17:11.

-------------------------------------------

Video: Cold, seasonal day ahead - Duration: 2:41.

CINDY: THIS IS A GENTLE SLAP

FROM MOTHER NATURE.

IT'S NUTS.

TAKE A LOOK AT THE CALENDAR.

15 DAYS IN A ROW ABOVE AVERAGE.

THINGS ARE CHANGING A LITTLE

BIT.

HERE WE GO THIS WEEK.

THE JET STREAM TO OUR SOUTH.

THAT IS GOING TO BRING IN COLDER

AIR TO NEW ENGLAND.

TEMPERATURES WILL TREND NEAR OR

BELOW AVERAGE AT TIMES THE NEXT

COUPLE OF DAYS.

AVERAGE HIGH IS 36.

NO 40'S OR 50'S THIS WEEK.

WE'RE GOING TO KEEP TEMPERATURES

IN THE 30'S.

FEELING MORE SEASONAL IN THE

DAYS AHEAD.

COLD START OUT THE DOOR.

TEENS SHOWING UP NORTH AND WEST

OF TOWN.

BEDFORD 19.

17 ORANGE.

14 JAFFREY.

WORCESTER 24 DEGREES RIGHT NOW.

WE HAVE PARTLY CLOUDY SKIES.

YOU CAN SEE HOW THE CLOUDS

INCREASE THIS AFTERNOON.

YOUR TEMPERATURES MAY HOVER NEAR

OR BELOW THE FREEZING MARK

THROUGH WORCESTER COUNTY.

30 IN BOSTON, UPPER 20'S IN THE

CAPE.

TEMPERATURES WILL TOP OUT IN THE

MID 30'S FROM BOSTON DOWN

THROUGH THE SOUTH SHORE AND CAPE

AND LOWER 30'S BACK TO THE

WORCESTER HILLS.

INCREASING CLOUDS.

NOT A LOT HAPPENING NOW.

WHEN YOU LOOK TO THE SOUTH,

THERE'S A LITTLE BIT OF SNOW IN

THE D.C. AREA.

THIS IS GOING TO TRACK JUST

SOUTH OF OUR REGION.

MOST OF US AREN'T GOING TO SEE

MORE THAN CLOUD COVER.

THIS MAY GRAZE NANTUCKET WITH

LIGHT RAIN AND SNOW AS WE GET

DEEPER IN THE AFTERNOON.

THE BRIGHTER SKIES WILL BE PAST

LUNCHTIME.

CLOUDS WILL INCREASE A LITTLE

BIT.

ON THE CAPE, VINEYARD AND

NANTUCKET, COULD BE A PERIOD OF

LIGHT RAIN OR SNOW.

BY ABOUT 5:00, 6:00 THIS

AFTERNOON INTO THIS EVENING, IT

PULLS AWAY QUICKLY OVERNIGHT,

AND SKIES CLEAR OUT.

THAT WILL ALLOW TEMPERATURES TO

DROP WAY DOWN.

THIS TIME TOMORROW, HEADING OUT

THE DOOR, MANY OF US IN THE

TEENS.

THE WINDS WON'T BE STRONG.

WE'LL HAVE COLD AIR IN PLACE

TOMORROW MORNING, BUT IT'S A

QUIET START ON TUESDAY.

ANOTHER SYSTEM IS GOING TO RACE

TOWARD US.

THIS ONE IS STARVED FOR

MOISTURE.

DURING THE AFTERNOON AND EVENING

HOURS, IT WILL BE COLD ENOUGH

FOR LIGHT SNOW TO BREAK OUT.

AS THIS SITS IN THE WATERS, IT'S

GOING TO PULL IN EXTRA MOISTURE.

THAT MAY KEEP SNOW SHOWERS GOING

INTO WEDNESDAY MORNING AS WELL.

A LIGHT SNOW EVENT COMING LATER

TUESDAY INTO WEDNESDAY MORNING,

COATING TO AN INCH SOUTH OF

BOSTON, ONE TO TWO BOSTON TO

WORCESTER, AND SOUTHERN NEW

HAMPSHIRE, THE ROUTE 2 CORRIDOR,

COULD SEE LOCALIZED TWO TO THREE

INCHES OF SNOW.

HERE'S THE TIMELINE.

THE MORNING HOURS ARE QUIET.

AS WE GET TOWARD THE AFTERNOON,

5:00, 6:00, DURING AND AFTER THE

EVENING COMMUTE, LIGHT SNOW

CONTINUES INTO THE OVERNIGHT.

WE WILL WAKE UP TO IT WEDNESDAY.

WE'LL DRY THINGS OUT IN THE

AFTERNOON.

For more infomation >> Video: Cold, seasonal day ahead - Duration: 2:41.

-------------------------------------------

19. Physics | MOD | Graphical Analysis of Motion | by Ashish Arora - Duration: 17:11.

Dear students, now we are going to use graphical analysis of motion. as we are studying rectilinear

motion, in rectilinear motion 3 types of graph are used in motion analysis. we'll see that

these graphs are quite helpful, in solving various kind of problems of, rectilinear

motion also. these three types of graph are. displacement versus time graph. second is,

velocity versus time graph. and the third is, acceleration versus time graph. we also

discuss the variant of displacement time graph as, distance time graph. we'll also discuss

distance versus time graph. we'll also discuss speed versus time graph, because, some particular

type of problems are also asked on distance and speed versus time graphs. but we don't

need to spend much time on these at, slight variations of displacement and velocity time

curves. lets discuss these one by one. now if we talk about displacement versus time

graphs. these are also known as, position versus time graphs. there is no difference

between position versus time and displacement versus time graphs. say for a given rectilinear

motion, we, draw the displacement time curve, like this. so this is the curve, according

to which, the position of a particle varies with time. so its function is given as x=f

of t. in this situation at any instant of time, (t) we can directly get the position

of particle by using, this curve, or by substituting the value of time in this function. say if

this point is p, we draw a tangent , of this curve at this point p, and say it makes an

angle theta with the time axis so we can simply state. the slope of the curve. at point p

can be written as, d x by d t, which is = tan theta. and we all know that d x by d t, can

be directly written as, instantaneous velocity of the particle at this position p. so by,

displacement time graph, at any point if we want to calculate, or we want to evaluate

the instantaneous velocity of the particle, we just need to find out the slope of the

curve, at that point and the slope will be directly give us the, instantaneous velocity

of the particle at that point. so in this situation we can see that, this tangent makes

an acute angle, with the, time axis, here we can simply state the velocity v p which

is tan theta, will be a positive, quantity. if we talk about the decreasing part of the

curve at a point q, if we consider a tangent, you can state, this angle theta dash will

be an obtuse angle. so at point q, the instantaneous velocity can be written as tan theta dash.

and tangent of the obtuse angle can be written as, a negative physical quantity. so in the

decreasing part of curve we can say with time the displacement is coming down, or displacement

is decreasing. or, as if we talk about the position of particle it is moving towards

origin. so we can state vector ally the velocity will be, negative. we can also talk about

various situations, like, for a practical situation. if say, a particle moves, in such

a way, that, first it accelerates, than it moves uniformly, and then say it retards. initially

say it was at rest, and finally also say it'll come to rest. so first it accelerates its

velocity increases, than it moves uniformly, and then finally, it comes to rest. now

in such situations, if particle is accelerating we can simply state the slope will first increase.

and then it moves uniformly that mean its slope remains constant, because you can see

the slope is giving as the instantaneous velocity. and if it it retards, that mean the slope

decreases and finally it becomes zero. so if we draw, the displacement time graph, of

such a motion, we can state first slope is increasing, the curve goes like this you can

see, continual sly the angle which, tangent makes with the time axis increasing. and then

say, for a time t 1 it is, accelerating, and from time t 1 to t 2 or you can say for a

duration t 2, it moves uniformly so we can draw a straight line. so here, the whole slope,

for the duration t 2 remains constant, then it retards, so you can simply draw a curve

like this. which for another duration say t 3. now in this situation finally you can

see the slope become zero and earlier also slope was zero. this is the curve, which

is representing a motion where particle first accelerate, then moves uniformly and then,

retards. similar to this if we just, consider an experimental

situation like, say this positive direction of x axis. from origin a particle starts.

it moves with a velocity v. it goes up to a particular position in a time t 1. then

for a time t 2 it remains at rest over there, and then it comes back to origin, with the

same velocity v. in a time t 3. so from zero to t 1, it was moving uniformly, up to, this

position, say we write maximum displacement x m. for a duration t 2 it remains at rest,

and then, for at time t 2 it'll start, moving in opposite direction, and time t 3 it comes

back. now if we draw, the, position versus time graph, for this motion. you can simply

state it t = 0 particle starts, with an uniform velocity, uniform velocity means the slope

remains constant here we can write tan theta = v. this was the time t 1 for which the particle

was moving uniformly. then you can state up to time t 2, or for the duration t 2 minus

t 1 it remains at rest. so its position remains constant i.e. at, x m. and then, it'll start

coming back so the velocity, is in opposite direction or we can say, when it was moving

toward (right) velocity was positive and now velocity is negative. so it comes down and

at a time t 3 it'll reach the, original position back. so, you can simple state again x becomes

zero. and say this angle is theta dash, so we can again write tan theta dash is equals

to v. now this angle will be, 180 minus theta, and we can state the, tangent of obtuse angle

is negative. so this angle theta dash can be directly taken as the angle by which we

can directly calculate the negative slope. so this is the, curve which is drawn, for

uniform motion then rest for some duration, and then again uniform motion in opposite

direction. now if similar, this is the curve which we call as position time curve or position

time graph. if similar graph is drawn for distance time.

let us draw distance time graph for the same, motion of particle when it is moving then

rest, taking rest and then coming back. so you can simply state, if we talk about displacement,

it first increases to x m then decreases to zero. but when we talk about distance, we

can state distance is continually increasing, because from here to here the distance is

x m, and when it comes back, the total distance travelled by the particle will become 2 x

m. now only difference in position time and distance time graph, can be taken, that, distance

time graph, if this is taken as distance, distance time graph will never come down.

say it'll first increase to a position, of x m, for a time t 1, than, it remains, at

rest, up to a time t 2, and then again it returns back, but if we talk about, position

it is coming down, but if we talk about distance it is still increasing, so the same graph

can be, drawn in reverse direction. so up to a time t 3, it will be able to cover a

distance of 2 x m. this is the distance time graph for the same motion, you can simply

state if we are having a displacement time graph, then for those portions of displacement

time graph, where the curves is coming down, you can draw the mirror image with respect

to time axis in upward direction, that will become, distance time graph.

if we talk about velocity time graphs. these are the graphs relating velocity with time.

say we draw, graph in, velocity and time, for motion of particle, this graph is drawn,

for the function of velocity how it varies with time. at, any position of this graph,

similar to, that of displacement time graph. here if you draw tangent, and you find out

the slope , of this graph, say at point x, we can simply state this point is relating

time with, velocity . and here the slope can be written as d v by d t or it can be written

as tan theta. and here the slope is giving us, the acceleration of particle at the position

x. so always remember that the slope of velocity time graph gives us the, instantaneous acceleration

and, if a slope is positive like, here you can see acceleration at point x, it is

tan theta and theta is acute angle this can be taken as, positive acceleration. positive

acceleration means the velocity, and acceleration have same direction and you can simply state,

the, speed of particle is increasing or the magnitude of velocity is increasing in this

case. when we talk about the decreasing part of the curve, at any position if we draw

tangent, you can see the angle theta dash is obtuse. so this the point y, so we can

say acceleration at point y it'll be tan theta dash, which is an negative quantity. so here

you can see the velocity is decreasing so acceleration we considered to be negative.

so be careful about, the situation, where we have finding the slope of velocity time

curve as, acceleration. along with this we are already studied, in calculus, that area

under a curve can be given by, for between, two, coordinates on time axis, say t 1 and

t 2. if we find out the area of this curve. so area under the curve can be given as,

integration of v d-t from t 1 to t 2 . here you can see, this integration of v d-t, will

be given as displacement only. because, if we talk about v into d-t, it is the displacement

covered by the particle during the time d-t. so if we calculate the total displacement

of particle, from point t 1 to time t 2, it can directly be given as, integration of v

d-t from t 1 to t 2, it'll give us the displacement of particle. from t =, t 1 to, t 2. this

is another advantage of using velocity time graph, that from velocity time graph using

slope we can find out the instantaneous acceleration of particle, and finding out the area under

the curve, like say if we find out this area by using integration, this area under the

curve gives us the, displacement of particle, between two given time instants, in the

given situation.

if we just have a look on motion situation, as shown in the velocity time graph. a particle

moves in such a way that, t= 0 its initial velocity was zero, first velocity increases

that means it was accelerating, and then after some time it'll decreases and again

it become zero at time t 1. than velocity becomes negative, you can say, this is the

negative direction of velocity, and velocity becomes negative that means particle as returned

in opposite direction, and at time t 2 (again) its velocity become zero. so in such situation

you can say from time 0 to t 1. the area between the curve and the time axis, above the time

axis this, positive. and from time t 1 to t 2 you can see, that this area is below the

time axis, so this is written as negative. say, this total area is s1 and this total

area is s 2. so we can state, total displacement. of particle. from t = 0 to t 2. is, total

displacement can be written as s 1 minus s 2. but when we talk about distance travelled.

you can always write distance travelled= s 1 + s 2. because s 1 is the distance travelled,

in positive direction and s 2 is the distance travelled in, opposite direction. so displacement

will be s 1 minus s 2, but when we talk about distance travelled it will be s 1 + s 2, so

be careful about such situations , while drawing velocity time curves. similar to this we can

also talk about, acceleration time graphs. but there is nothing much to discuss about

acceleration time graphs. like if we draw acceleration time graph, for a given motion,

you can simply state in acceleration time graph if we find out the slope. that a slope

will give us the (rate) with which will the acceleration is varying. which is not of much

import ants, in, our limitations, or, in the syllabus we are analyzing the things, but

when we talk about the, (area) under the acceleration time curve or area between the acceleration

time curve and time axis, say between to instants t 1 and t 2, so when it is of, quite importance

like, if we find out this area. this area is say (a) so this (a) can be written as integration

of (a) d-t from time t 1 to t 2. this (a) d-t will give us, net change. in velocity,

of particle. from, t 1 to t 2. there is something which is important for us to keep in mind,

integration of (a) d-t from t1 to t 2 gives us the net change in velocity of particle

in going from, time t 1 to, time t 2. this, you should always keep in mind

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