Showing posts with label Science Notes. Show all posts
Showing posts with label Science Notes. Show all posts

दुनिया की सबसे तेज दौड़ने वाली कार -ब्लड हाऔंड सुपरसॉनिक कार



दुनिया की सबसे तेज दौड़ने वाली कार -ब्लड हाऔंड सुपरसॉनिक कार 
कार की स्पीड – 1600 किमी/घंटा      
लागत – 500 करोड़ , यूरो फाइटर जेट के इंजिन लगे है
पहले रेकॉर्ड – 1228 किमी/घंटा
ब्रिटेन मे निर्मित दुनिया की सबसे तेज दौड़ने वाली कार का बुधवार को रनवे पर टेस्ट किया जाएगा I इसके लिए इसे कार्न्वेल एयरपोर्ट पर लाया गया है I इसे डिज़ाइन किया है 85 साल के रॉकेट साइंटिस्ट रॉन एयेर्स ने I इसे चलाएँगे 55 साल के अंडी ग्रीन I अंडी ग्रीन एयर फोर्स मे पायलट रह  चुके है I टीम का दावा है की इस कार की स्पीड 1600 किमी/ प्रति घंटा है I करीब 3 किलोमीटर लंबे रनवे पर यह 350 किमी/घंटा की स्पीड से दोड़ेगी I अभी तक तेज स्पीड का रेकॉर्ड 1228 किमी/घंटा है I 19997 मे ये रेकॉर्ड इसी टीम ने बनाया था I ब्लड हाऔंड के दो चरणों मे 1247 किमी/घंटा और 1609 किमी/घंटा की स्पीड पकड़ने की बात कही जा रही है I प्रोजेक्ट की घोषणा 2008 मे हुई थी , लेकिन इस पर काम 2015 मे सुरू हुआ I

Earth’s Atmosphere

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Atmosphere:-

The earth is a unique planet due to the presence of life. The air is one among the necessary conditions for the existence of life on this planet. The air is a mixture of several gases and it encompasses the earth from all sides. The air surrounding the earth is called the atmosphere.
  • Atmosphere is the air surrounding the earth.
  • The atmosphere is a mixture of different gases. It contains life-giving gases like Oxygen for humans and animals and carbon dioxide for plants.
  • It envelops the earth all round and is held in place by the gravity of the earth.
  • It helps in stopping the ultraviolet rays harmful to the life and maintains the suitable temperature necessary for life.
  • Generally, atmosphere extends up to about 1600 km from the earth’s surface. However, 99 % of the total mass of the atmosphere is confined to the height of 32 km from the earth’s surface.
 Composition of the atmosphere:-
  • The atmosphere is made up of different gases, water vapour and dust particles.
  • The composition of the atmosphere is not static and it changes according to the time and place.
  • The atmosphere is a mixture of different types of gases.
  • Nitrogen and oxygen are the two main gases in the atmosphere and 99 percentage of the atmosphere is made up of these two gases.
  • Other gases like argon, carbon dioxide, neon, helium, hydrogen, etc. form the remaining part of the atmosphere.
  • The portion of the gases changes in the higher layers of the atmosphere in such a way that oxygen will be almost negligible quantity at the heights of 120 km.
  • Similarly, carbon dioxide (and water vapour) is found only up to 90 km from the surface of the earth.

    1. Carbon dioxide:

  • Carbon dioxide is meteorologically a very important gas.
  • It is transparent to the incoming solar radiation (insolation) but opaque to the outgoing terrestrial radiation.
  • It absorbs a part of terrestrial radiation and reflects back some part of it towards the earth’s
  • surface.
  • Carbon dioxide is largely responsible for the greenhouse effect.
  • When the volume of other gases remains constant in the atmosphere, the volume of the carbon dioxide has been rising in the past few decades mainly because of the burning of fossil fuels. This rising volume of carbon dioxide is the main reason for global warming.

2. Ozone gas:

  • Ozone is another important component of the atmosphere found mainly between 10 and 50 km above the earth’s surface.
  • It acts as a filter and absorbs the ultra-violet rays radiating from the sun and prevents them from reaching the surface of the earth.
  • The amount of ozone gas in the atmosphere is very little and is limited to the ozone layer found in the stratosphere.
3. Water Vapour:-
  • Gases form of water present in the atmosphere is called water vapour.
  • It is the source of all kinds of precipitation.
  • The amount of water vapour decreases with altitude. It also decreases from the equator (or from the low latitudes) towards the poles (or towards the high latitudes).
  • Its maximum amount in the atmosphere could be up to 4% which is found in the warm and wet regions.
  • Water vapour reaches in the atmosphere through evaporation and transpiration. Evaporation takes place in the oceans, seas, rivers, ponds and lakes while transpiration takes place from the plants, trees and living beings.
  • Water vapour absorbs part of the incoming solar radiation (insolation) from the sun and preserves the earth’s radiated heat. It thus acts like a blanket allowing the earth neither to become too cold nor too hot.
  • Water vapour also contributes to the stability and instability in the air.
  4. Dust Particles:-
  • Dust particles are generally found in the lower layers of the atmosphere.
  • These particles are found in the form of sand, smoke-soot, oceanic salt, ash, pollen, etc.
  • Higher concentration of dust particles is found in subtropical and temperate regions due to dry winds in comparison to equatorial and polar regions.
  • These dust particles help in the condensation of water vapour. During the condensation, water vapour gets condensed in the form of droplets around these dust particles and thus clouds are formed.

    Structure of the atmosphere:-

     

    The atmosphere can be divided into five layers according to the diversity of temperature and density. They are:
  • Troposphere
  • Stratosphere
  • Mesosphere
  • Thermosphere (Ionosphere)
  • Exosphere

    Troposphere

  • It is the lowermost layer of the atmosphere.
  • The height of this layer is about 18 km on the equator and 8 km on the poles.
  • The thickness of the troposphere is greatest at the equator because heat us transported to great heights by strong convectional currents.
  • Troposphere contains dust particles and water vapour.
  • This is the most important layer of the atmosphere because all kinds of weather changes take place only in this layer.
  • The air never remains static in this layer. Therefore this layer is called ‘changing sphere’ or troposphere.
  • The environmental temperature decreases with increasing height of the atmosphere. It decreases at the rate of 1 degree Celsius for every 165 m of height. This is called Normal Lapse Rate.
  • The zone separating troposphere from the stratosphere is known as tropopause.
  • The air temperature at the tropopause is about – 80 degree Celsius over the equator and about – 45 degree Celsius over the poles. The temperature here is nearly constant, and hence, it is called tropopause.

Stratosphere

  • Stratosphere is found just above the troposphere.
  • It extends up to a height of 50 km.
  • The temperature remains almost the same in the lower part of this layer up to the height of 20 km. After this, the temperature increases slowly with the increase in the height. The temperature increases due to the presence of ozone gas in the upper part of this layer.
  • Weather related incidents do not take place in this layer. The air blows horizontally here. Therefore this layer is considered ideal for flying of aircraft.
  • The upper limit of the stratosphere is known as stratopause.
  • One important feature of stratosphere is that it contains a layer of ozone gas.
  • The relative thickness of the ozone layer is measured in Dobson Units.
  • It is mainly found in the lower portion of the stratosphere, from approximately 20 to 30 km above the earth’s surface.
  • It contains a high concentration of ozone (O3) in relation to other parts of the atmosphere.
  • It is the region of the stratosphere that absorbs most of the sun’s ultra-violet radiations.

Mesosphere

  • It is the third layer of the atmosphere spreading over the stratosphere.
  • It extends up to a height of 80 km.
  • In this layer, the temperature starts decreasing with increasing altitude and reaches up to – 100 degree Celsius at the height of 80 km.
  • Meteors or falling stars occur in this layer.
  • The upper limit of the mesosphere is known as mesopause.

Thermosphere

  • This layer is located between 80 and 400 km above the mesopause.
  • It contains electrically charged particles known as ions, and hence, it is known as the ionosphere.
  • Radio waves transmitted from the earth are reflected back to the earth by this layer and due to this, radio broadcasting has become possible.
  • The temperature here starts increasing with heights.

Exosphere

  • The exosphere is the uppermost layer of the atmosphere.
  • Gases are very sparse in this sphere due to the lack of gravitational force. Therefore, the density of air is very less here.
  •  

The Big Bang Theory

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The Big Bang Theory:-    

 Big Bang Theory is about the origin of Universe. It suggests that about 13.7 billion years ago, all matter and energy in the universe was concentrated into an area smaller than an atom. At that time nothing like matter, energy, space and time does not exist. Then suddenly with a bang, the Universe began to expand at an incredible rate and matter, energy, space and time came into being. As the Universe expanded, matter began to coalesce into gas clouds and the stars and planets. Some scientists believe that this expansion is finite and will done day cease. After this point in time, the Universe will begin to collapse until a Big Crunch occurs.

Before the Big Bang:-

No one knows what the universe was like at this time. The best current theory, the “inflationary universe” model assumes that all of space is filled with an extremely concentrated, unstable form of energy that will be transformed into particles of matter at the instant of the Big Bang. But no one knows how space and time came into existence in the first place.
After the initial expansion, the universe cooled sufficiently to allow the formation of subatomic particles, including photons, electrons, protons and neutrons.Though simple atomic nuclei formed within the first three minutes after the Big Bang, thousands of years passed before the first electrically neutral atoms formed. The majority of atoms that were produced by the Big Bang are hydrogen, along with helium and traces of lithium.

Earlier  Universe:-

Photons (light) being elementary particles would have been formed soon after the Big Bang. But these photons would have been scattered by the early electrons. As the Universe continued to cool, it would have eventually reached the temperature where electrons combined with nuclei to form neutral atoms (recombination). Before this “recombination” occurred, the Universe would have been opaque because the free electrons would have caused light (photons) to scatter the way sunlight scatters from the water droplets in clouds. But when the free electrons were absorbed to form neutral atoms, the Universe suddenly became transparent. Those same photons – the afterglow of the Big Bang known as Cosmic Background Radiation – can be observed today.

 Universe is expanding:-

It had always been assumed that the matter of the Universe would slow its rate of expansion. Mass creates gravity, gravity creates pull, the pulling must slow the expansion. But supernovae observations showed that the expansion of the Universe, rather than slowing, is accelerating. Something, not like matter and not like ordinary energy, is pushing the galaxies apart. This “stuff” has been dubbed dark energy, but to give it a name is not to understand it. Whether dark energy is a type of dynamical fluid, heretofore unknown to physics, or whether it is a property of the vacuum of empty space, or whether it is some modification to general relativity is not yet known.

Inflationary model:-

Our investigation shows that the early Universe was too homogeneous. How could pieces of the Universe that had never been in contact with each other have come to equilibrium at the very same temperature? This and other cosmological problems could be solved, however, if there had been a very short period immediately after the Big Bang where the Universe experienced an incredible burst of expansion called “inflation.” For this inflation to have taken place, the Universe at the time of the Big Bang must have been filled with an unstable form of energy whose nature is not yet known. Whatever its nature, the inflationary model predicts that this primordial energy would have been unevenly distributed in space due to a kind of quantum noise that arose when the Universe was extremely small. This pattern would have been transferred to the matter of the Universe and would show up in the photons that began streaming away freely at the moment of recombination.

Proofs of Big Bang:-

  1. Expanding galaxies: Hubble in 1929, noted that galaxies outside our own Milky Way were all moving away from us, each at a speed proportional to its distance from us. He quickly realized what this meant that there must have been an instant in time (now known to be about 14 billion years ago) when the entire Universe was contained in a single point in space. The Universe must have been born in this single violent event which came to be known as the “Big Bang.”
  2. Cosmic Background radiation: Those early photons – the afterglow of the Big Bang known as cosmic background radiation – can be observed today.

Main Points:-

  1. Cosmic Background Explorer (COBE) : NASA has launched two missions to study the cosmic background radiation, taking “baby pictures” of the Universe only 400,000 years after it was born. The first of these was the Cosmic Background Explorer (COBE).
  2. Wilkinson Microware Anisotropy Probe (WMAP)The second mission to examine the cosmic background radiation was the Wilkinson Microware Anisotropy Probe (WMAP). With greatly improved resolution compared to COBE, WMAP surveyed the entire sky, measuring temperature differences of the microwave radiation that is nearly uniformly distributed across the Universe. The picture shows a map of the sky, with hot regions in red and cooler regions in blue. By combining this evidence with theoretical models of the Universe, scientists have concluded that the Universe is “flat,” meaning that, on cosmological scales, the geometry of space satisfies the rules of Euclidean geometry (e.g., parallel lines never meet, the ratio of circle circumference to diameter is pi, etc).
  3. Planck: A third mission, Planck, led by the European Space Agency with significant participation from NASA, was launched in 2009.  Planck is making the most accurate maps of the microwave background radiation yet. With instruments sensitive to temperature variations of a few millionths of a degree, and mapping the full sky over 9 wavelength bands, it measures the fluctuations of the temperature of the CMB with an accuracy set by fundamental astrophysical limits.