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Posted on May 31, 2023 (Updated on July 9, 2025)

Why Tholins are Absent in the Inner Solar System: A Planetary Science Mystery

Natural Environments

Tholins are complex organic molecules formed by the irradiation of simple organic compounds such as methane, ammonia, and nitrogen. These organic molecules have been found on the surface of various bodies in the outer Solar System, including Pluto, Triton, and the icy moons of Jupiter and Saturn. However, they are not found in the inner Solar System. This begs the question: why are there no tholins in the inner solar system?

Tholins and the outer solar system

Tholins were first discovered by Carl Sagan and his colleagues in the 1970s during experiments that simulated conditions in the outer solar system. The researchers found that when simple organic compounds were exposed to high-energy radiation, such as ultraviolet light or cosmic rays, they formed complex organic molecules similar to the organic compounds found in meteorites and comets. They named these compounds “tholins” after the Greek word “tholos,” which means muddy.

Tholins are formed by a process called radiolysis, in which molecules are broken down by high-energy radiation. This process is most efficient in the outer solar system, where radiation levels are much higher than in the inner solar system. The outer Solar System is also home to a large number of icy bodies, such as comets and the moons of Jupiter and Saturn, which are rich in the simple organic compounds necessary for the formation of tholins.

FAQs

Why are there no tholins in the inner solar system?

Introduction

Tholins are complex organic molecules that are formed through the irradiation of simple organic compounds such as methane, ammonia, and nitrogen. These organic molecules have been found on the surface of various bodies in the outer solar system, including Pluto, Triton, and the icy moons of Jupiter and Saturn. However, they are absent in the inner solar system. This raises the question: why are there no tholins in the inner solar system?

Tholins and the Outer Solar System

Tholins were first discovered by Carl Sagan and his colleagues in the 1970s, during experiments simulating the conditions of the outer solar system. The researchers found that when simple organic compounds were exposed to high-energy radiation, such as ultraviolet light or cosmic rays, they formed complex organic molecules that resembled the organic compounds found in meteorites and comets. They named these compounds “tholins” after the Greek word “tholos,” meaning muddy.

Tholins are formed through a process called radiolysis, which involves the breaking down of molecules by high-energy radiation. This process is most efficient in the outer solar system, where the levels of radiation are much higher than in the inner solar system. The outer solar system is also home to a large number of icy bodies, such as comets and the moons ofJupiter and Saturn, which are rich in the simple organic compounds that are necessary for the formation of tholins.

One of the most famous examples of tholins in the outer solar system is on the surface of Pluto. The New Horizons spacecraft, which flew by Pluto in 2015, discovered a reddish-brown material on the surface that was rich in tholins. This material is thought to have formed through the irradiation of methane and nitrogen on Pluto’s surface.

Why are Tholins Absent in the Inner Solar System?

Despite the prevalence of tholins in the outer solar system, they are notably absent in the inner solar system. This is due to several factors, including the lower levels of radiation in the inner solar system and the lack of simple organic compounds.

One of the main reasons for the absence of tholins in the inner solar system is the lower levels of radiation. The inner solar system is shielded from high-energy radiation by the magnetic fields of the planets, which deflect charged particles away from the planets. This means that the levels of radiation in the inner solar system are much lower than in the outer solar system, making the formation of tholins much less efficient.

In addition, the inner solar system is lacking in the simple organic compounds that are necessary for the formation of tholins. These compounds are thought to have been delivered to the outer solar system by comets and other icy bodies, which formedin the

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