Money4Nothing
New Member
Hints of Life On Venus - Scientists detect phosphine molecules in high cloud decks
In my opinion the claim that phosphine molecules is indicative of possible alien life is so ridiculous, that it rises to the level of needing debunking. It looked to me like they detected signatures of phosphine molecules at concentrations of around 2 PPB (parts per billion).
The article said:
Furthermore, if phosphene is a byproduct of a microbial reaction, and it can be detected at 2 PPB, then we should be able to detect the change in sulfuric acid or hydrogen sulfide concentrations that would result from it. They also keep saying "so much phosphene! too much to explain!" But 2 PPB is nothing.
From Wikipedia
There's at least a few abiotic methods for producing phosphine on earth. Tell me why this couldn't happen in the atmosphere of Venus instead of by aliens.
This is my first new post, I'm trying to follow the posting guidelines correctly.External Quote:
An international team of astronomers, led by Professor Jane Greaves of Cardiff University, today announced the discovery of a rare molecule—phosphine—in the clouds of Venus. On Earth, this gas is only made industrially, or by microbes that thrive in oxygen-free environments.
Astronomers have speculated for decades that high clouds on Venus could offer a home for microbes—floating free of the scorching surface, but still needing to tolerate very high acidity. The detection of phosphine molecules, which consist of hydrogen and phosphorus, could point to this extra-terrestrial 'aerial' life. The new discovery is described in a paper in Nature Astronomy.
The team first used the James Clerk Maxwell Telescope (JCMT) in Hawaii to detect the phosphine, and were then awarded time to follow up their discovery with 45 telescopes of the Atacama Large Millimeter/submillimeter Array (ALMA) in Chile. Both facilities observed Venus at a wavelength of about 1 millimeter, much longer than the human eye can see—only telescopes at high altitude can detect this wavelength effectively.
Professor Greaves says, "This was an experiment made out of pure curiosity, really—taking advantage of JCMT's powerful technology, and thinking about future instruments. I thought we'd just be able to rule out extreme scenarios, like the clouds being stuffed full of organisms. When we got the first hints of phosphine in Venus' spectrum, it was a shock!"
Naturally cautious about the initial findings, Greaves and her team were delighted to get three hours of time with the more sensitive ALMA observatory. Bad weather added a frustrating delay, but after six months of data processing, the discovery was confirmed.
Team member Dr. Anita Richards, of the UK ALMA Regional Centre and the University of Manchester, adds: "To our great relief, the conditions were good at ALMA for follow-up observations while Venus was at a suitable angle to Earth. Processing the data was tricky, though, as ALMA isn't usually looking for very subtle effects in very bright objects like Venus."
Greaves adds: "In the end, we found that both observatories had seen the same thing—faint absorption at the right wavelength to be phosphine gas, where the molecules are backlit by the warmer clouds below."
Synthesized false colour image of Venus, using 283-nm and 365-nm band images taken by the Venus Ultraviolet Imager (UVI). Credit: JAXA / ISAS / Akatsuki Project Team
Professor Hideo Sagawa of Kyoto Sangyo University then used his models for the Venusian atmosphere to interpret the data, finding that phosphine is present but scarce—only about twenty molecules in every billion.
The astronomers then ran calculations to see if the phosphine could come from natural processes on Venus. They caution that some information is lacking—in fact, the only other study of phosphorus on Venus came from one lander experiment, carried by the Soviet Vega 2 mission in 1985.
Massachusetts Institute of Technology scientist Dr. William Bains led the work on assessing natural ways to make phosphine. Some ideas included sunlight, minerals blown upwards from the surface, volcanoes, or lightning, but none of these could make anywhere near enough of it. Natural sources were found to make at most one ten thousandth of the amount of phosphine that the telescopes saw.
To create the observed quantity of phosphine on Venus, terrestrial organisms would only need to work at about 10% of their maximum productivity, according to calculations by Dr. Paul Rimmer of Cambridge University. Any microbes on Venus will likely be very different to their Earth cousins though, to survive in hyper-acidic conditions.
Earth bacteria can absorb phosphate minerals, add hydrogen, and ultimately expel phosphine gas. It costs them energy to do this, so why they do it is not clear. The phosphine could be just a waste product, but other scientists have suggested purposes like warding off rival bacteria.
Another MIT team-member, Dr. Clara Sousa Silva, was also thinking about searching for phosphine as a 'biosignature' gas of non-oxygen-using life on planets around other stars, because normal chemistry makes so little of it.
She comments: "Finding phosphine on Venus was an unexpected bonus! The discovery raises many questions, such as how any organisms could survive. On Earth, some microbes can cope with up to about 5% of acid in their environment—but the clouds of Venus are almost entirely made of acid."
Other possible biosignatures in the Solar System may exist, like methane on Mars and water venting from the icy moons Europa and Enceladus. On Venus, it has been suggested that dark streaks where ultraviolet light is absorbed could come from colonies of microbes. The Akatsuki spacecraft, launched by the Japanese space agency JAXA, is currently mapping these dark streaks to understand more about this 'unknown ultraviolet absorber.'
The team believes their discovery is significant because they can rule out many alternative ways to make phosphine, but they acknowledge that confirming the presence of "life" needs a lot more work. Although the high clouds of Venus have temperatures up to a pleasant 30 degrees centigrade, they are incredibly acidic—around 90% sulphuric acid—posing major issues for microbes to survive there. Professor Sara Seager and Dr. Janusz Petkowski, also both at MIT, are investigating how microbes could shield themselves inside droplets.
The team are now eagerly awaiting more telescope time, for example to establish whether the phosphine is in a relatively temperate part of the clouds, and to look for other gases associated with life. New space missions could also travel to our neighboring planet, and sample the clouds in situ to further search for signs of life.
Professor Emma Bunce, President of the Royal Astronomical Society, congratulated the team on their work, "A key question in science is whether life exists beyond Earth, and the discovery by Professor Jane Greaves and her team is a key step forward in that quest. I'm particularly delighted to see UK scientists leading such an important breakthrough—something that makes a strong case for a return space mission to Venus."
Science Minister Amanda Solloway said, "Venus has for decades captured the imagination of scientists and astronomers across the world."
"This discovery is immensely exciting, helping us increase our understanding of the universe and even whether there could be life on Venus. I am incredibly proud that this fascinating detection was led by some of the UK's leading scientists and engineers using state of the art facilities built on our own soil."
In my opinion the claim that phosphine molecules is indicative of possible alien life is so ridiculous, that it rises to the level of needing debunking. It looked to me like they detected signatures of phosphine molecules at concentrations of around 2 PPB (parts per billion).
The article said:
With the lack of knowledge that we have about the surface of Venus and the types of chemical reactions that could be in play, to so quickly dismiss these in complete ignorance but yet give preference to an Alien Life hypothesis is unbelievable to me.Some ideas included sunlight, minerals blown upwards from the surface, volcanoes, or lightning, but none of these could make anywhere near enough of it.
Furthermore, if phosphene is a byproduct of a microbial reaction, and it can be detected at 2 PPB, then we should be able to detect the change in sulfuric acid or hydrogen sulfide concentrations that would result from it. They also keep saying "so much phosphene! too much to explain!" But 2 PPB is nothing.
From Wikipedia
"No known source". So why not hypothesize a new abiotic source? Why hypothesize an unknown biological source instead? This type of nonsense is why lay people distrust the scientific community. I guarantee within a few months or years someone will either fail to repeat the observations or come up with a far more plausible abiotic theory. I get so annoyed when the answer to anything knew is always "aliens". I guess this isn't a complete debunk scientifically since I can't prove a negative, but so many of the alternative theories such as lightning and volcanoes are so much more plausible, that I can actually imagine a chemical mechanism for how they can produce phosphine, far more readily than some weird living organism high up in the atmosphere with almost no access to hydrogen.External Quote:
Composition[edit]
Composition of the atmosphere of Venus. The chart on the right is an expanded view of the trace elements that all together do not even make up a tenth of a percent.
The atmosphere of Venus is composed of 96.5% carbon dioxide, 3.5% nitrogen, and traces of other gases, most notably sulfur dioxide.[12] The amount of nitrogen in the atmosphere is relatively small compared to the amount of carbon dioxide, but because the atmosphere is so much thicker than that on Earth, its total nitrogen content is roughly four times higher than Earth's, even though on Earth nitrogen makes up about 78% of the atmosphere.[1][13]
The atmosphere contains a range of compounds in small quantities, including some based on hydrogen, such as hydrogen chloride (HCl) and hydrogen fluoride (HF). There is carbon monoxide, water vapour and atomic oxygen as well.[2][3] Hydrogen is in relatively short supply in the Venusian atmosphere. A large amount of the planet's hydrogen is theorised to have been lost to space,[14] with the remainder being mostly bound up in sulfuric acid (H2SO4) and hydrogen sulfide (H2S). The loss of significant amounts of hydrogen is proven by a very high D–H ratio measured in the Venusian atmosphere.[3] The ratio is about 0.015–0.025, which is 100–150 times higher than the terrestrial value of 1.6×10−4.[2][15] According to some measurements, in the upper atmosphere of Venus D/H ratio is 1.5 higher than in the bulk atmosphere.[2]
In September 2020, it was announced that phosphine, a potential biomarker indicating the presence of life, had been detected in the atmosphere of Venus. No known abiotic source present on Venus could produce phosphine in the quantities detected.[10][16]
There's at least a few abiotic methods for producing phosphine on earth. Tell me why this couldn't happen in the atmosphere of Venus instead of by aliens.
Again from WikipediaExternal Quote:
Phosphine
A.V. Lyubimov, V.F. Garry, in Hayes' Handbook of Pesticide Toxicology (Third Edition), 2010
104.1.1 Physical Properties
Pure phosphine is an odorless and colorless gas with a molecular weight of 34.00 and density of 1.17 at 25°C. Commercial grade phosphine derived from aluminum or magnesium phosphide can contain to a variable degree higher molecular weight phosphines including diphosphines. These higher phosphines give commercial grade fumigants containing aluminum or magnesium phosphide odor characteristics described as decaying fish or "garlic-like." Commercial grade phosphine containing diphosphines can ignite and form explosive mixtures at concentrations exceeding 1.8% phosphine in air. The rate of conversion of the phosphide to phosphine is temperature and humidity dependent. Similarly, metal phosphides readily hydrolyze in water to yield phosphine, which is poorly soluble in water.
External Quote:
Preparation and occurrence[edit]
Phosphine may be prepared in a variety of ways.[10] Industrially it can be made by the reaction of white phosphorus with sodium or potassium hydroxide, producing potassium or sodium hypophosphite as a by-product.
3 KOH + P4 + 3 H2O → 3 KH2PO2 + PH3
Alternatively, the acid-catalyzed disproportionation of white phosphorus yields phosphoric acid and phosphine. Both routes have industrial significance; the acid route is the preferred method if further reaction of the phosphine to substituted phosphines is needed. The acid route requires purification and pressurizing. It can also be made (as described above) by the hydrolysis of a metal phosphide, such as aluminium phosphide or calcium phosphide. Pure samples of phosphine, free from P2H4, may be prepared using the action of potassium hydroxide on phosphonium iodide (PH4I).
Laboratory routes[edit]
It is prepared in the laboratory by disproportionation of phosphorous acid[11]
4 H3PO3 → PH3 + 3 H3PO4
Phosphine evolution occurs at around 200 °C. Alternative methods involve the hydrolysis of aluminium phosphide, calcium phosphide, and tris(trimethylsilyl)phosphine.
Last edited: