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The photovoltaic effect is the basic physical process through which a PV cell converts sunlight into electricity.Thus, a 12% efficiency solar cell having 1 m2 of surface area in full sunlight at solar noon at the equator during either the March or September equinox will produce approximately 120 watts of peak power.For systems large enough to justify the extra expense (say, ~1 kiloWatt ), a power point tracker tracks the instantaneous power by continually measuring the voltage and current (and hence, power transfer), and uses this information to dynamically adjust the load so the maximum power is always transferred, regardless of the variation in lighting.This term is calculated using the ratio of P m, divided by the input light irradiance under "standard" test conditions ( E, in W/m 2 ) and the surface area of the solar cell (A c in m2). At solar noon on a clear March or September equinox day, the solar radiation at the equator is about 1000 W/m 2 . Hence, the "standard" solar radiation (known as the "air mass 1.5 spectrum") has a power density of 1000 watts per square meter.They have long been used in situations where electrical power from the grid is unavailable, such as in remote area power systems, Earth -orbiting satellites and space probes, consumer systems, e.g. handheld calculators or wrist watches, remote radiotelephones and water pumping applications.Scientists have concentrated their efforts over the last several years on improving the efficiency of solar cells to make them more competitive with conventional power -generation technologies.We use crystalline silicon to explain the photovoltaic effect for several reasons.Other PV cell materials have band -gap energies ranging from 1 to 3.3 eV. The energy of individual photons in light is also measured in eV. Photons with different energies correspond to distinct wavelengths of light.The electrons farthest from the nucleus interact with those of neighboring atoms to determine the way solid structures are formed.The silicon atom has 14 electrons.Visible light represents only a fraction of the total radiation spectrum; infrared and ultraviolet rays are also significant parts of the solar spectrum.In a crystalline solid, each silicon atom normally shares one of its four valence electrons in a covalent bond with each of four neighboring silicon The solid, then, consists of basic units of five silicon atoms: the original atom plus the four other atoms with which it shares its valence electrons.This technique, known as "doping," introduces an atom of another element (called the "dopant") into the silicon crystal to alter its electrical properties.The entire spectrum of sunlight, from infrared to ultraviolet, covers a range of about 0.5 eV to about 2.9 eV. Red light has an energy of about 1.7 eV; blue light has an energy of about 2.7 eV. One key to obtaining an efficient PV cell is to convert as much sunlight into electricity as possible.The electrons orbit the nucleus at different distances, depending on their energy level; an electron of lesser energy orbits close to the nucleus, while one of greater energy orbits farther away.This regular, fixed arrangement of silicon atoms is known as the crystal lattice.When a photon of sufficient energy strikes a valence electron, it may impart enough energy to free it from its connection to the atom.The absorbed photons generate electricity.The energy of a photon is transferred to an electron in an atom of the semiconductor device.Vm x Im = Pm in watts.
indicate radiation with different amounts of energy; the longer the wavelength, the less
the energy. Red light, for example, has a longer wavelength and thus has less energy than
violet light.
Each second, the sun releases an enormous amount of radiant energy into the solar
system. The Earth receives a tiny fraction of this energy; still, an average of 1367 W
reaches each square meter (m
2
) of the outer edge of the Earth's atmosphere. The
atmosphere absorbs and reflects some of this radiation, including most x
-rays and
ultraviolet rays.Yet, the amount of sunshine energy that hits the surface of the Earth every minute is
greater than the total amount of energy that the world's human population consumes in a
year.
When sunlight reaches Earth, it is distributed unevenly in different regions. Not
surprisingly, the areas near the equator receive more solar radiation than anywhere else
on Earth. Sunlight varies with the seasons, as the rotational axis of the Earth shifts to
lengthen and shorten days as the seasons change. The quantity of sunlight reaching any
region is also affected by the time of day, the climate (especially the cloud cover, which
scatters the sun's rays), and the air pollution in that region. These climatic factors all
affect the amount of solar energy that is available to PV systems.
The amount of energy produced by a PV device depends not only on available solar
energy but on how well the device, or solar cell, converts sunlight to useful electrical
energy. This is called the device or solar cell efficiency. It is defined as the amount of
electricity produced divided by the sunlight energy striking the PV device. Scientists
have concentrated their efforts over the last several years on improving the efficiency of
solar cells to make them more competitive with conventional power
-generation
technologies.We use crystalline silicon to explain the photovoltaic effect for several reasons. First,
crystalline silicon was the semiconductor material used in the earliest successful PV
device. Second, crystalline silicon is still the most widely used PV material. And third,
although other PV materials and designs exploit the PV effect in slightly different ways,
knowing how the effect works in crystalline silicon gives us a basic understanding of how
it works in all devices.
As you know, all matter is composed of atoms. Atoms, in turn, are composed of
positively charged protons, negatively charged electrons, and neutral neutrons. The
protons and neutrons, which are of approximately equal size, comprise the close
-packed
central nucleus of the atom, where almost all of the mass of the atom is located. The
much lighter electrons orbit the nucleus at very high velocities. Although the atom is built
from oppositely charged particles, its overall charge is neutral because it contains an
equal number of positive protons and negative electrons.
The electrons orbit the nucleus at different distances, depending on their energy level; an
electron of lesser energy orbits close to the nucleus, while one of greater energy orbits
farther away. The electrons farthest from the nucleus interact with those of neighboring
atoms to determine the way solid structures are formed.The silicon atom has 14 electrons. Their natural orbital arrangement allows the outer four
of these to be given to, accepted from, or shared with other atoms. These outer four
electrons, called valence electrons, play an important role in the photovoltaic effect.
Large numbers of silicon atoms, through their valence electrons, can bond together to
form a crystal. In a crystalline solid, each silicon atom normally shares one of its four
valence electrons in a covalent bond with each of four neighboring silicon The solid, then, consists of basic units of five silicon atoms: the original atom plus the
four other atoms with which it shares its valence electrons.
The solid silicon crystal is composed of a regular series of units of five silicon atoms.
This regular, fixed arrangement of silicon atoms is known as the crystal lattice.When a photon of sufficient energy strikes a valence electron, it may impart enough
energy to free it from its connection to the atom. This leaves a space in the crystal
structure where an electron once resided (and bonded), called a "hole." The electron is
now free to travel about the crystal lattice. The electron is now a part of the conduction
band, so called because these free electrons are the means by which the crystal conducts
electricity. Meanwhile, the atom left behind by the freed electron contains a net positive charge in
the form of the generated hole. This positive hole can move almost as freely about the
crystal lattice as a free electron in the conduction band, as electrons from neighboring
atoms switch partners. These light
-generated charges, both positive and negative, are the
constituents of electricity. Photovoltaic cells contain an electric field that is created when semiconductors with
different electrical characteristics come into contact. The electric field drives positive and
negative charges in opposite directions. The movement of charge carriers (through an
external circuit) is what defines electricity.
There are several ways to form the electric field in a crystalline silicon PV cell. The most
common technique is to slightly modify the structure of the silicon crystal. This
technique, known as "doping," introduces an atom of another element (called the
"dopant") into the silicon crystal to alter its electrical properties. The dopant has either
three or five valence electrons, as opposed to silicon's four.
Phosphorus atoms, which have five valence electrons, are used for doping n
-type silicon
(so called because of the presence of free negative charges or electrons). A phosphorus
atom occupies the same place in the crystal lattice that was occupied formerly by the
silicon atom it replaced. Four of its valence electrons take over the bonding
responsibilities of the four silicon valence electrons that they replaced. But the fifth
valence electron remains free, without bonding responsibilities. This unbonded valence
electron behaves like a permanent member of the crystal's conduction band.
When numerous phosphorus atoms are substituted for silicon in a crystal, many free,
conduction
-band electrons become available. The most common method of substitution is
to coat the top of a layer of silicon with phosphorus and then heat the surface.
This allows the phosphorus atoms to diffuse into the silicon. The temperature is then
lowered so that the rate of diffusion drops to zero. Other methods of introducing phosphorus into silicon include gaseous diffusion, a liquid dopant spray
-on process, and a
technique in which phosphorus ions are driven precisely into the surface of the silicon.
This n
-type silicon cannot form the electric field by itself; it is also necessary to have
some silicon altered to have the opposite electrical properties. Boron, which has three
valence electrons, is used for doping p
-type (positive
-type) silicon. Boron is introduced
during silicon processing, where silicon is purified for use in PV devices. When a boron
atom assumes a position in the crystal lattice formerly occupied by a silicon atom, there is
a bond missing an electron, in other words, an extra hole. In p
-type material, there are
many more positive charges (holes) than free electrons.
Holes are much more numerous than free electrons in a p
-type material and are therefore
called the majority charge carriers. The few electrons in the conduction band of p
-type
material are referred to as minority charge carriers. In n
-type material, electrons are the
majority carriers, and holes are the minority carriers.
The majority charge carriers, however, have excess energy that is not bound up in
valence bonding with neighboring atoms. This higher energy allows them to traverse the
crystal lattice. The majority carriers
-electrons in n
-type and holes in p
-type silicon
gap energy of the material determines how much of the sun's spectrum can be absorbed.
Silicon, for example, requires photons to have an energy of at least 1.1 eV to be absorbed
and create pairs of charge carriers. Photons with less energy either pass right through the
silicon or are absorbed as heat. Photons with too much energy are absorbed and
contribute free charge carriers, but they also heat up the cell. About 55% of the energy of
sunlight cannot be used by most PV cells because this energy either is below the band gap or carries excess energy. Researchers are working on advanced cell designs that can
reduce those losses.
Materials with lower band
-gap energies can exploit a broader range of the sun's spectrum
of energies, creating greater numbers of charge carriers (greater current). We might
conclude that material with the lowest band gap would thus make the best PV cell. But it
isn't quite that simple. The band
-gap energy also influences the strength of the electric field, which determines
the maximum voltage the cell can produce. The higher the band
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