Planetary engineering

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Planetary engineering is the development and application of technology for the purpose of influencing the environment of a planet. Planetary engineering encompasses a variety of methods such as terraforming, seeding, and geoengineering.

Widely discussed in the scientific community, terraforming refers to the alteration of other planets to create a habitable environment for terrestrial life. Seeding refers to the introduction of life from Earth to habitable planets. Geoengineering refers to the engineering of a planet's climate, and has already been applied on Earth. Each of these methods are composed of varying approaches and possess differing levels of feasibility and ethical concern.

TerraformingEdit

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File:SRMtemperature-projections.jpg
Projected temperature and precipitation changes relative to preindustrial; end-of-century response without (a) and with (b) geoengineering to avoid temperature rise above 1.5C.<ref>Template:Cite journal</ref>
File:Terraforming of Mars.jpg
A theoretical design for a power station on Mars. Terraforming designs are not yet planned.

Terraforming is the process of modifying the atmosphere, temperature, surface topography or ecology of a planet, moon, or other body in order to replicate the environment of Earth.

TechnologiesEdit

A common object of discussion on potential terraforming is the planet Mars. To terraform Mars, humans would need to create a new atmosphere, due to the planet's high carbon dioxide concentration and low atmospheric pressure. This would be possible by introducing more greenhouse gases to below "freezing point from indigenous materials".<ref name="Pollack & Sagan 1993">Template:Cite book</ref> To terraform Venus, carbon dioxide would need to be converted to graphite since Venus receives twice as much sunlight as Earth. This process is only possible if the greenhouse effect is removed with the use of "high-altitude absorbing fine particles" or a sun shield, creating a more habitable Venus.<ref name="Pollack & Sagan 1993"/>

NASA has defined categories of habitability systems and technologies for terraforming to be feasible.<ref name=":1">{{#invoke:citation/CS1|citation |CitationClass=web }}</ref> These topics include creating power-efficient systems for preserving and packaging  food for crews, preparing and cooking foods, dispensing water, and developing facilities for rest, trash and recycling, and areas for crew hygiene and rest.<ref name=":1" />

FeasibilityEdit

A variety of planetary engineering challenges stand in the way of terraforming efforts. The atmospheric terraforming of Mars, for example, would require "significant quantities of gas" to be added to the Martian atmosphere.<ref name=":2">Template:Cite journal</ref> This gas has been thought to be stored in solid and liquid form within Mars' polar ice caps and underground reservoirs. It is unlikely, however, that enough Template:CO2 for sufficient atmospheric change is present within Mars' polar deposits, and liquid Template:CO2 could only be present at warmer temperatures "deep within the crust".<ref name=":2" /> Furthermore, sublimating the entire volume of Mars' polar caps would increase its current atmospheric pressure to 15 millibar, where an increase to around 1000 millibar would be required for habitability.<ref name=":2" /> For reference, Earth's average sea-level pressure is 1013.25 mbar.

First formally proposed by astrophysicist Carl Sagan, the terraforming of Venus has since been discussed through methods such as organic molecule-induced carbon conversion, sun reflection, increasing planetary spin, and various chemical means.<ref name=terra1>Template:Cite journal</ref> Due to the high presence of sulfuric acid and solar wind on Venus, which are harmful to organic environments, organic methods of carbon conversion have been found unfeasible.<ref name=terra1/> Other methods, such as solar shading, hydrogen bombardment, and magnesium-calcium bombardment are theoretically sound but would require large-scale resources and space technologies not yet available to humans.<ref name=terra1/>

Ethical considerationsEdit

While successful terraforming would allow life to prosper on other planets, philosophers have debated whether this practice is morally sound. Certain ethics experts suggest that planets like Mars hold an intrinsic value independent of their utility to humanity and should therefore be free from human interference.<ref name=":6">{{#invoke:citation/CS1|citation |CitationClass=web }}</ref> Also, some argue that through the steps that are necessary to make Mars habitable - such as fusion reactors, space-based solar-powered lasers, or spreading a thin layer of soot on Mars' polar ice caps - would deteriorate the current aesthetic value that Mars possesses.<ref>Template:Cite journal</ref> This calls into question humanity's intrinsic ethical and moral values, as it raises the question of whether humanity is willing to eradicate the current ecosystem of another planet for their benefit.<ref>Template:Cite journal</ref> Through this ethical framework, terraforming attempts on these planets could be seen to threaten their intrinsically valuable environments, rendering these efforts unethical.<ref name=":6" />

SeedingEdit

File:Mars Hubble.jpg
NASA's Hubble Space Telescope took the picture of Mars on June 26, 2001, when Mars was approximately 68 million kilometers (43 million miles) from Earth — the closest Mars has ever been to Earth since 1988. Hubble can see details as small as 16 kilometers (10 miles) across. The colors have been carefully balanced to give a realistic view of Mars' hues as they might appear through a telescope. Especially striking is the large amount of seasonal dust storm activity seen in this image. One large storm system is churning high above the northern polar cap (top of image), and a smaller dust storm cloud can be seen nearby. Another large dust storm is spilling out of the giant Hellas impact basin in the Southern Hemisphere (lower right) exploration.<ref>Template:Cite journal</ref>

Environmental considerationsEdit

Mars is the primary subject of discussion for seeding. Locations for seeding are chosen based on atmospheric temperature, air pressure, existence of harmful radiation, and availability of natural resources, such as water and other compounds essential to terrestrial life.<ref name="Todd">Template:Cite journal</ref>

Developing microorganisms for seedingEdit

Natural or engineered microorganisms must be created or discovered that can withstand the harsh environments of Mars. The first organisms used must be able to survive exposure to ionizing radiation and the high concentration of Template:CO2 present in the Martian atmosphere.<ref name="Todd" /> Later organisms such as multicellular plants must be able to withstand the freezing temperatures, withstand high Template:CO2 levels, and produce significant amounts of Template:Chem2.

Microorganisms provide significant advantages over non-biological mechanisms. They are self-replicating, negating the needs to either transport or manufacture large machinery to the surface of Mars. They can also perform complicated chemical reactions with little maintenance to realize planet-scale terraforming.<ref>Template:Cite journal</ref>

Climate engineeringEdit

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File:MarsTransitionV.jpg
Impression of the hypothetical phrases of the terraforming of Mars

Climate engineering is a form of planetary engineering which involves the process of deliberate and large-scale alteration of the Earth's climate system to combat climate change.<ref name=":4">{{#invoke:citation/CS1|citation |CitationClass=web }}</ref> Examples of geoengineering are carbon dioxide removal (CDR), which removes carbon dioxide from the atmosphere, and solar radiation modification (SRM) to reflect solar energy to space.<ref name=":4" /><ref>{{#invoke:citation/CS1|citation |CitationClass=web }}</ref> Carbon dioxide removal (CDR) has multiple practices, the simplest being reforestation, to more complex processes such as direct air capture.<ref name=":4" /><ref>{{#invoke:citation/CS1|citation |CitationClass=web }}</ref> The latter is rather difficult to deploy on an industrial scale, for high costs and substantial energy usage would be some aspects to address.<ref name=":4" />

Examples of SRM include stratospheric aerosol injection (SAI) and marine cloud brightening (MCB).<ref name=":4" /> When a volcano erupts, small particles known as aerosols proliferate throughout the atmosphere, reflecting the sun's energy back into space.<ref name=":4" /><ref name=":5">{{#invoke:citation/CS1|citation |CitationClass=web }}</ref> This results in a cooling effect, and humanity could conceivably inject these aerosols into the stratosphere, spurring large-scale cooling.<ref name=":4" /><ref name=":5" />

File:ShipTracks.jpg
Visible ship tracks in the Northern Pacific, on 4 March 2009. On an overcast day, the clouds look uniform. However, NASA MODIS images' sensor reveals long, skinny trails of brighter clouds hidden within. As ships travel across the ocean, pollution in the ships' exhaust create more cloud drops that are smaller in size, resulting in even brighter clouds.

One proposal for MCB involves spraying a vapor into low-laying sea clouds, creating more cloud condensation nuclei.<ref name=":3">{{#invoke:citation/CS1|citation |CitationClass=web }}</ref> This would in theory result in the cloud becoming whiter, and reflecting light more efficiently.<ref name=":3" />

See alsoEdit

ReferencesEdit

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Further readingEdit

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External linksEdit

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