For thousands of years, astronomers have watched comets travel close
to Earth and light up the night sky. In time, these observations led to a
number of paradoxes. For instance, where were these comets all coming
from? And if their surface material vaporizes as they approach the Sun
(thus forming their famous halos), they must formed farther away, where
they would have existed there for most of their lifespans.
In time, these observations led to the theory that far beyond the Sun
and planets, there exists a large cloud of icy material and rock where
most of these comets come from. This existence of this cloud, which is
known as the Oort Cloud (after its principal theoretical founder),
remains unproven. But from the many short and long-period comets that
are believed to have come from there, astronomers have learned a great
deal about it structure and composition.
Definition:
The Oort Cloud is a theoretical spherical cloud of predominantly icy
planetesimals that is believed to surround the Sun at a distance of up
to around 100,000 AU (2 ly). This places it in interstellar space,
beyond the Sun’s Heliosphere where it defines the cosmological boundary
between the Solar System and the region of the Sun’s gravitational
dominance.
Like the Kuiper Belt and the Scattered Disc, the Oort Cloud is a reservoirs of trans-Neptunian objects,
though it is over a thousands times more distant from our Sun as these
other two. The idea of a cloud of icy infinitesimals was first proposed
in 1932 by Estonian astronomer Ernst Öpik, who postulated that
long-period comets originated in an orbiting cloud at the outermost edge
of the Solar System.
In 1950, the concept was resurrected by Jan Oort, who independently
hypothesized its existence to explain the behavior of long-term comets.
Although it has not yet been proven through direct observation, the
existence of the Oort Cloud is widely accepted in the scientific
community.
Structure and Composition:
The Oort Cloud is thought to extend from between 2,000 and 5,000 AU
(0.03 and 0.08 ly) to as far as 50,000 AU (0.79 ly) from the Sun, though
some estimates place the outer edge as far as 100,000 and 200,000 AU
(1.58 and 3.16 ly). The Cloud is thought to be comprised of two regions –
a spherical outer Oort Cloud of 20,000 – 50,000 AU (0.32 – 0.79 ly),
and disc-shaped inner Oort (or Hills) Cloud of 2,000 – 20,000 AU (0.03 –
0.32 ly).
The outer Oort cloud may have trillions of objects larger than 1 km
(0.62 mi), and billions that measure 20 kilometers (12 mi) in diameter.
Its total mass is not known, but – assuming that Halley’s Comet is a
typical representation of outer Oort Cloud objects – it has the combined
mass of roughly 3×1025 kilograms (6.6×1025 pounds), or five Earths.
Based on the analyses of past comets, the vast majority of Oort Cloud
objects are composed of icy volatiles – such as water, methane, ethane,
carbon monoxide, hydrogen cyanide, and ammonia. The appearance of
asteroids thought to be originating from the Oort Cloud has also
prompted theoretical research that suggests that the population consists
of 1-2% asteroids.
Earlier estimates placed its mass up to 380 Earth masses, but
improved knowledge of the size distribution of long-period comets has
led to lower estimates. The mass of the inner Oort Cloud, meanwhile, has
yet to be characterized. The contents of both Kuiper Belt and the Oort
Cloud are known as Trans-Neptunian Objects (TNOs), because the objects
of both regions have orbits that that are further from the Sun than
Neptune’s orbit.
Origin:
The Oort cloud is thought to be a remnant of the original protoplanetary disc
that formed around the Sun approximately 4.6 billion years ago. The
most widely accepted hypothesis is that the Oort cloud’s objects
initially coalesced much closer to the Sun as part of the same process
that formed the planets and minor planets, but that gravitational
interaction with young gas giants such as Jupiter ejected them into
extremely long elliptic or parabolic orbits.
Recent research by NASA
suggests that a large number of Oort cloud objects are the product of
an exchange of materials between the Sun and its sibling stars as they
formed and drifted apart. It is also suggested that many – possibly the
majority – of Oort cloud objects were not formed in close proximity to
the Sun.
Alessandro Morbidelli of
the Observatoire de la Cote d’Azur has conducted simulations on the
evolution of the Oort cloud from the beginnings of the Solar System to
the present. These simulations indicate that gravitational interaction
with nearby stars and galactic tides modified cometary orbits to make
them more circular. This is offered as an explanation for why the outer
Oort Cloud is nearly spherical in shape while the Hills cloud, which is
bound more strongly to the Sun, has not acquired a spherical shape.
Recent studies
have shown that the formation of the Oort cloud is broadly compatible
with the hypothesis that the Solar System formed as part of an embedded
cluster of 200–400 stars. These early stars likely played a role in the
cloud’s formation, since the number of close stellar passages within the
cluster was much higher than today, leading to far more frequent
perturbations.
Comets:
Comets are thought to have two points of origin within the Solar
System. They start as infinitesimals in the Oort Cloud and then become
comets when passing stars knock some of them out of their orbits,
sending into a long-term orbit that take them into the inner solar
system and out again.
Short-period comets have orbits that last up to two hundred years
while the orbits of long-period comets can last for thousands of years.
Whereas short-period comets are believed to have emerged from either the
Kuiper Belt or the scattered disc, the accepted hypothesis is that
long-period comets originate in the Oort Cloud. However, there are some
exceptions to this rule.
For example, there are two main varieties of short-period comet:
Jupiter-family comets and Halley-family comets. Halley-family comets,
named for their prototype (Halley’s Comet)
are unusual in that although they are short in period, they are
believed to have originated from the Oort cloud. Based on their orbits,
it is suggested they were once long-period comets that were captured by
the gravity of a gas giant and sent into the inner Solar System.
Exploration:
Because the Oort Cloud is so much farther out than the Kuiper Belt,
the region remained unexplored and largely undocumented. Space probes
have yet to reach the area of the Oort cloud, and Voyager 1
– the fastest and farthest of the interplanetary space probes currently
exiting the Solar System – is not likely to provide any information on
it.
At its current speed, Voyager 1 will reach the Oort cloud in
about 300 years, and will will take about 30,000 years to pass through
it. However, by around 2025, the probe’s radioisotope thermoelectric
generators will no longer supply enough power to operate any of its
scientific instruments. The other four probes currently escaping the Solar System – Voyager 2, Pioneer 10 and 11, and New Horizons – will also be non-functional when they reach the Oort cloud.
Exploring the Oort Cloud presents numerous difficulties, most of
which arise from the fact that it is incredible distant from Earth. By
the time a robotic probe could actually reach it and begin exploring the
area in earnest, centuries will have passed here on Earth. Not only
would those who had sent it out in the first place be long dead, but
humanity will have most likely invented far more sophisticated probes or
even manned craft in the meantime.
Still, studies can be (and are) conducted by examining the comets
that it periodically spits out, and long-range observatories are likely
to make some interesting discoveries from this region of space in the
coming years. It’s a big cloud. Who knows what we might find lurking in
there?
We have many interesting articles about the Oort Cloud and Solar System for Universe Today. Here’s an article about how big the Solar System is, and one on the diameter of the Solar System. And here’s all you need to know about Halley’s Comet and Beyond Pluto.
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