Increasing albedo of dark volcanic plain

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My heroes have found a barely-tolerable 'greenhouse' planet, the upper part of a vast volcanic shield having acceptable temperature and pressure (*). The anoxic atmosphere is N2+CO2, but holds enough H2O for nightly dew near the summit.

So, can condense that, use for hydroponics, irrigate green-houses etc. Electrolyse some water for oxygen for habitats and, yes, crops, as latter need it to respire through the night.

Beyond the volcanic massif, they have ready access to dune-fields of silica sand. In fact, they're smelting such to glazing panels...

There's a suggestion that long days' heating of dark, low-albedo volcanic plain surrounding the base might be 'improved', mitigated by scattering pale sand...

Clearly, 'raw' sand would tend to vanish down irregularities in the old lava, while 'ping-pong' or 'marble' spheroids may be too big, so wasteful...

Okay, the experimental approach is to lay out 'test plots' of different 'gauge' material, see how they compare. Is there a better way to estimate 'mini-max' benefit and predict the 'sweet spot' ?
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*) Ambient pressure is 'SCUBA', with some helium in the habs' mix to mitigate the several Bar...
 
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Nik_2213 said:
*) Ambient pressure is 'SCUBA', with some helium in the habs' mix to mitigate the several Bar...
What does this mean?

No life already on planet?
Water condensing on the lava would tend to react with it an vanish from the atmosphere in a weathering process. This would tend to make it more useful for (earth) plants.

Nik_2213 said:
There's a suggestion that long days' heating of dark, low-albedo volcanic plain surrounding the base might be 'improved', mitigated by scattering pale sand...
This means it get too hot?
Growing plants (if possible) on the surface would mitigate that.

Nik_2213 said:
way to estimate 'mini-max' benefit and predict the 'sweet spot' ?
Sweet spot for what?
 
  • #3
Thank you for taking an interest in this topic.

The helium in the habs' breathing mix ? 'Technical' divers do this to mitigate oxygen / nitrogen toxicity.

Planet is anoxic, lifeless. That night dew shows there is still a meagre water-cycle. Not quite enough CO2+H20 for a 'runaway' greenhouse unto full Venusian. The next major shield eruption might achieve this, or perhaps the one after...

Yes, the old,, dark ;ava fields get too hot by day. Yes, growing plants would help. Snag, atmosphere is anoxic, and plants need some oxygen to respire in the dark. So, plants restricted to indoor hydroponics, or outdoor cloches / greenhouses with supplementary oxygen.

Spreading pale sand around would raise the local lava-field's albedo, staying cooler by day should mean faster cooling by night.

Snag, sand as-is would soon vanish down the old lava's irregularities. They already process silica sand to granules for 'ponics and greenhouse plantings. What size would be optimal for coverage ? Too small is lost, too large, whatever that size, is wasteful. So, how to figure the likely 'sweet-spot' ??
 
  • #4
Google up 'glass wool'.
With some handwavium you can scatter it 'on the fly' too (look up the manufacturing process).
Also can serve as a soil-replacement for plants (though rock-wool is more frequently used for that purpose).
 
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FAQ: Increasing albedo of dark volcanic plain

What is albedo, and why is it important for volcanic plains?

Albedo is a measure of the reflectivity of a surface, defined as the ratio of reflected radiation from the surface to the total incoming radiation. Increasing the albedo of dark volcanic plains is important because higher albedo can lead to lower surface temperatures, which may help mitigate local climate effects, reduce the heat retained by the ground, and influence local weather patterns.

How can the albedo of dark volcanic plains be increased?

The albedo of dark volcanic plains can be increased through various methods, such as applying lighter-colored materials (e.g., reflective coatings or light-colored aggregates), planting vegetation that reflects more sunlight, or using engineering techniques to modify the surface structure to enhance reflectivity.

What are the potential environmental impacts of increasing albedo?

Increasing the albedo of volcanic plains can have several environmental impacts, including altered local temperatures, changes in vegetation patterns, and potential effects on local ecosystems. It may also influence hydrological cycles and affect the behavior of wildlife, necessitating careful consideration of ecological balance.

Are there any risks associated with artificially increasing albedo?

Yes, there are risks associated with artificially increasing albedo, such as unintended consequences on local climate and ecosystems. For instance, increasing reflectivity could disrupt local weather patterns, affect rainfall distribution, and potentially lead to adverse effects on endemic species that are adapted to specific environmental conditions.

How does increasing albedo relate to climate change mitigation strategies?

Increasing albedo is considered one of the geoengineering strategies aimed at climate change mitigation. By reflecting more sunlight away from the Earth, it can theoretically reduce surface temperatures and counteract some effects of global warming. However, it is essential to integrate such strategies with other approaches to ensure comprehensive and sustainable climate solutions.

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