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Energetic Particles

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What is Energetic Particles ?


Ions that stripped of their electrons , be in ~2 million degree plasma from the free ions and electrons in plasma behave the same way. Knowing the temperature of the high atmosphere of Earth, or that of the Sun, we can calculate energies expected of ions and electrons found there. However, ions and electrons actually observed in space are often much, much more energetic, and may move at a respectable fraction of the velocity of light (300,000 km/sec or 186,000 miles/sec).


Low energy particles (E<100 MeV/nucleon) are present throughout the heliosphere in different intensities and time scales. The source of most of these particles in the heliosphere are the Sun, the planet's magnetospheres, and the interplanetary shock waves. Spacecraft observations have established direct evidence that particle acceleration occurs near all collisionless shocks found in interplanetary space, including the Earth's bow shock, shocks triggered with transient solar activity, and corotating shocks.

The "solar energetic particle"(SEP) events, a time limited increases of low-energy particles, are often observed in the near earth space environment, outside the magnetosphere and in the earth polar caps (where they were discovered), but also observed everywhere in the interplanetary medium. In recent years it has been widely accepted that there are two kinds of SEP events:


1.) The  gradual events have a duration of several days, they are proton rich and they have, on average, the same element composition and ionization states as those in the low-density ambient plasma of the high corona or solar wind. They are associated with gradual X-ray flares, type II and type IV radioemission and coronal mass ejections (CMEs). Such events are observed over a broad range of heliolongitudes.


2). The impulsive short-duration events are only observed from magnetically well-connected locations on the Sun. They are electron-rich and they have an strong association with impulsive H-alpha and X-rays flares, and type III radio bursts. The high ion charge state indicates their origin in plasma heated by flares.
Recent observations do challenge an strict separation of all SEP events in these two types. There are large gradual events with abundances more like those of impulsive events. It also seems that abundance variations are organized by the heliolongitude of the parent solar activity.
 



The Measurement ¨CElectron Volt

There is a convenient unit to measure such energies, the electron volt (ev). It is the energy gained by an electron (or proton, same size of electric charge) moving through a voltage difference of one volt.


In the picture tube of a color TV, electrons are accelerated by about 30,000 volts, so that their energy when they hit the screen is about 30,000 ev. That is actually quite a lot: those electrons move at about 1/3 the velocity of light.


Particle Energies in Nature


How does nature compare?
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0.03 ev
o The energy of a molecule of oxygen or nitrogen in the air we breathe. It moves as fast as a speeding bullet, but is still rather low on the scale of energies.
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0.5 eV
o An atom or molecule at the temperature of the Sun's surface.
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Near Real-Time images from the LASCO C3 
coronagraph on board the SOHO spacecraft

Near Real-Time images at 304 A from the
EIT instrument on board the SOHO spacecraft

It happens right now.

0.67 ev
o The energy needed by a proton or neutron to escape the Earth's gravity.
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1000 - 15,000 ev
o Typical energy of an electron in the polar aurora.
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40,000 ev
o Energy required by an electron to penetrate a thin-wall Geiger counter.
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50,000 ev
o Typical energy of an ion in the ring current.

Hold it!We need bigger units:

o 1,000 ev = 1 kev (kilo-electron-volt, pronounced kay-ee-vee)
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o 1,000,000 ev = 1 Mev (mega-electron volt or em-ee-vee)
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o 1,000,000,000 ev = 1 Gev (giga-electron-volt or gee-ee-vee)

1.4 Mev
o The energy of electrons from radioactive potassium, a major source of the Earth's internal heat.

4.2 Mev
o The energy of alpha particles from radioactive uranium 238, another source of the Earth's heat (and of its helium as well--see positive ions, history).
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10-100 Mev
o Typical proton energies in the inner radiation belt.
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10-15,000 Mev
o Range of energies in solar outbursts (see Sun).
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1-100,000,000,000 Gev
o Range of energies among cosmic ray ions. However as their energy goes up, their intensity goes way down, so that ions at the high energy end are quite rare.

Note on Relativity ˇˇ

While the theory of relativity allows no particle with mass to move with a velocity exceeding (or even equaling) that of light, there is no limit on its energy. Close to the speed of light, however, the addition of energy only slightly increases the velocity. An ion accelerating from 0.9 to 0.99 times the speed of light needs several times more energy than the amount it needed to reach 0.9 times in the first place, though its energy makes it considerably heavier.
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Why and How


Where do single electrons and ions acquire such high energies? Excellent question. We guess magnetic and electric fields may be involved, and have learned a great deal in that direction, but the exact processes (probably more than one) remain to be nailed down. Acceleration takes place in solar flares and CMEs (see Sun) but, like a clever conjuring trick, although it happens right in front of our eyes, we still don't get it.


Powerful shocks--abrupt discontinuities piled up in front of rapidly moving gas--can also do it, and at least one interesting event of this sort was observed in the Earth's magnetosphere. The most powerful shocks occur in the envelope of gas expanding from the site of supernovas, and it is widely believed that such shocks (which carry a great amount of energy) are the source of most cosmic ray particles.

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Here you may see, as an example developed by B. Sanahuja*, A. Aran and D. Lario, Departament d'Astronomia i Meteorologia, Universitat de Barcelona. Spain and Institut d'Estudis Espacials de Catalunya. Spain. & **Applied Physics Laboratory. The John Hopkins University. USA Sponsored by ESA/ESTEC, the DGCYT (MCyT) and NASA, the aplication of the model for a limited set of choices. Just fill in or reply to the following questions:

Heliocentric Distance AU
Heliolongitude deg (EXX,WXX)
Transit Time hr
Shock Width deg
Mean Free Path AU
Turbulence Foreshock Region

Note: For longitude and transit time, the closest values to the specified parameters will be selected from our dataset.

   

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