Category Archives: Science

I’ve Been Scraped!

Last week, this blog saw an unusual spike in traffic—roughly 350 visits higher than normal. Each visit appeared to be for a single post, with no clear theme among them. My best guess? An AI platform was scraping my content for something specific.

Suddenly, I feel a renewed sense of accountability for what I’ve written. What if—gasp—a sentence was inaccurate, or a sarcastic remark too obscure for most readers? The responsibility could be enormous! Think of the children!

The content choices lie somewhere between the bookends of accurate and complete fabrication. I’d rather be accused of being boring than being found in an untruth.

How does this mesh with my anonymity? Well, a handful of people know my identity and their respect is important to me. Eventually I will reveal my identity and suddenly the truth and accuracy (and spelling) of my 1700 posts will be forever connected to my real name. Skin in the game.

Disclosure-

Very occasionally I will write some fictional content, and it should be apparent as fiction from both the content itself, and the key words attached to the post. The example would be my posts on the fictional Poltroon University in Guapo, Arizona. I do enjoy the occasional jab at the culture of higher education and the institution of science.

However, as a scientist in matters of physical reality, I am dedicated and eager to describe content as truthfully, accurately and mellifluously as possible. When I’m on one of my political jags, I’ll admit to some amount of enhanced emphasis where others have tread more carefully with the source material.

The reason I write and blog is to help me think ideas through. Somehow the act of scribbling down sentences followed by multiple passes in editing is helpful. At any given time I have 20 to 30 unfinished posts languishing in draft space. The open-air aspect of blogging is to assure that I have done my best lest public humiliation, scorn and derision should come my way. Not just in the present, but more so in the future. Writing is thinking. To put it bluntly, there is a fear of publishing something I would regret forever. Absolutely the worst thing I could do as a blogger and as a scientist would be to post indefensible or phony science. Posts with linked references are direct connections to what I view as credible content on the internet. The reader only has to click a link to verify a factual statement thing I made.

Navigating the Rocky Coastlines of the Chemical Business

[Note: Formerly named “PhD Chemists are freaks!!,” this essay has been renamed to better match the content.]

Preamble: Yes, yes, yes. Obviously, I’m aware that my experience in no way represents the careers of nearly all chemists. As usual, I drift into adjacent chemistry topics. Get your hands away from the keyboard and just read.

Bud (a pseudonym), a PhD chemist consultant and coworker, claimed that people with the exalted PhD degree were freaks of nature. Bud opined “Just look at us! Who goes to school for as long as we did and then ends up in a place like this?” I didn’t add at that moment that between a BA, PhD, 2-year postdoc and a stint in the professor trade, I was in academics for 16 years and walked away from it. Just then I couldn’t defend how smart it might have been to tread down this path only to end up in an old office trailer where we were sitting at that moment.

Bud used to argue that PhDs in general were freaks in society. Only a small fraction of undergrads will go on to grad school and fewer still complete a PhD program. The fraction is smaller yet in the general population.

In science you need a PhD in order to have even a hope of leading an R&D project, technical C-Suite corporate position, institute or professorship. The degree isn’t intended to resemble a trade, but rather to be a highly educated scholar and a subject matter expert with good communication skills and a sharp mind. If one is investigating for new phenomena, an intimate knowledge of known phenomena is needed to discriminate a finding. No awards for rediscovery.

Bud retired from a career at a big chemical corporation only to jump back into the hairball as a sales consultant for us in his retirement. I was a couple of years into what would be my major career “choice” and was managing the sales & marketing department then. Somehow, I had stumbled into the business side.

Our other sales consultant, the “Great Gondini”, retired from a photocopier company as a PhD chemist developing magnetic media, charge transfer agents and other xerographic-related materials. From his soapbox he advised us to-

It’s not that non-chemical-company chemists couldn’t rise up the career ladder, but being in a niche subspecialty at a company that produced photocopiers was not the way to grow your career in chemistry. Often such a chemist may be the only chemistry PhD on site and is likely to suffer from professional isolation. Experience with project execution on time and on budget is a great way to rise in a company. Engineers frequently rise to top level positions because they understand technology AND quantitative economics.

I knew 2 BS/BA level chemists and 1 PhD level chemist who obtained MBAs. Their careers leapt into higher gear with their move to the business side. In business it is important for at least someone to understand how finance works in addition to the technology. Even graduating with a business minor might be helpful but not as much as an MBA. I got an A in ECON 101 but only I cared. Education in basic accounting is very helpful on the business side.

As I see it, some realities of being in industrial chemistry R&D.

In my organic-synthesis-oriented research group in grad school, the big dream was to get an R&D job in pharma R&D. Cool medicinal chemistry and a chance to help to cure disease for the benefit of mankind. It is an honorable and, if I may be permitted to say so, prestigious career as a pharmaceutical scientist. At least in the world of chemistry.

Since then, more than a few in my grad school cohort had been laid off by the pharma companies or joined another. A few have been laid off 3 times from what they believed were secure slots. Pharma companies, like most others, aren’t run by chemists for the most part. Quarterly EBITDA is a major driver for the board of directors. The C-Suites are packed with corporate and patent lawyers, retired CEOs, MBAs, Md/PhDs, CPA finance people and perhaps a PhD chemist heading up the R&D operation as a Director or Vice-President.

After my academic career and my short rotation through the polymer world, I ended up for 6 years in chemical sales and marketing which was limited by my personal geographic requirement of living in the mountainous western US. As my opinion of the pharma business matured, I discovered that, as a raw material vendor, to be ever so careful with pharma customer promises and purchase orders. Not because they are liars, but because many felt free to cancel orders even after bulk raw materials arrived and after our R&D effort to meet specs. Their interest in us was based on using our low bid to leverage another supplier on price. This is common actually and I have done it myself. They waved future business in our faces knowing that, probably, they would never send receive an invoice. Still, not unheard of. But the hassle and our wasted R&D and opportunity costs were especially galling. But we were a spot supplier and susceptible to such disruption. My company didn’t like to sign contracts at that time, so we always took the risk on spot buys. Spot sales gave us manufacturing flexibility as a custom chemical producer, but at the expense of uncertainty. Later, attracted by the same sweet songs of Lorali that led hapless sailors into the rocks, we would repeat this fool’s errand once more.

Off-topic advice

Back to our regularly scheduled programming

On one occasion a big pharma customer wanted a product delivered across the Atlantic to Ireland. Time and distance weren’t the issue, though. It would equilibrate and precipitate below about 15 oC on the transatlantic voyage, so we bought heated shipping containers and installed them in Ireland on a site that wasn’t afraid of the W (indicating a water-reactive hazard) on the hazard labels or the safety data sheets. Scheduling heated transport could be sketchy in fall, winter and spring because most were booked for shipping fruits and vegetables. So, a month into the campaign and after an encouraging site visit by two of us sales guys (Tipperary isn’t so far after all), I received a call saying that they had changed their process (!?) and that a competing European supplier was chosen to ship directly from the continent on demand and without the (our) expense of staging heated storage. Once a pharma company writes in each raw material into their drug filing, changing suppliers or a change in specifications requires the heavens to open up and thunder “make it so.” In the end, they reimbursed us for raw material costs only. &#$@%*&^!! This would happen again later but with a more difficult product to produce.

My early career path led me away from the fabulous pharma world and into undergraduate teaching, initially. The other group members achieved their goals of a pharma R&D position. While I spent the next 6 years in academia one way or another, my grad school colleagues were drawing big salaries with 401(k)s in well-equipped labs, but in locations on the US East Coast, Gulf Coast or Midwest- regions that I would never consider moving to. In the end, most buoyantly bobbled up the career ladder to become directors and vice-presidents of R&D or technology as their final positions. No disrespect, just envy.

A few talented chemist colleagues from grad school climbed up the corporate ladder without business training, learning what they need on the job. Most others, though, remained in the tech end. The reality of being a scientist in industry is that upward mobility in a large corporation very much depends on your improvements in job performance, profitability, volume or especially the successful execution of a capital project. But capital projects are normally given to engineers because they are trained to deal with the cost of the equipment and in the cost of operation.

In my experience, a BA/BS, MA/MS or PhD chemist can usually retire as a senior bench chemist, analyst or lab project leader managing bench chemists. If you enjoy lab work, this is it. By retirement you’ve already topped out on the salary scale and have put away a fair sum in the 401 (k). It is a good life for a great many. But for myself, my interest in bench work dropped from hot to tepid after my 2-year postdoc. I got into molecular modeling and dynamics as a postdoc and actually answered a vexing question about kinetic vs thermodynamic control in a reaction that gave contradictory results. Even got a JACS paper out of it. It was fascinating stuff, but it made me look away from straight synthetic chemistry long enough to appreciate computational and physical chemistry.

As a postdoc I used AMBER and SPARTAN, I did molecular dynamics and molecular mechanics to make a stab what was possibly the global minimum strain energy. Ring strain calculations were used as a coarse screen for potential comonomers for the ring-opening polymerization (OP) reaction we were hoping to commercialize. The homopolymer was amber colored, brittle and rattled when handled as film. The comonomer idea based on the notion that the homopolymer contained too much crystallinity. The glass transition temperature needed to be at least below room temp. Suppressing the crystallinity and retaining certain key properties along with biodegradability was crucial. Even worse, the proposed comonomer must participate in reactive extrusion with the original monomer and be available in commercial quantities at a low cost. Finally, the copolymer needed to be water white. The color spec was difficult to achieve.

Final Comments:

My comments in this essay are based on personal experiences in my world. Your world is almost certainly quite different.

I haven’t mentioned analytical chemists because their world continues to be overtaken by automated instrumentation that will calculate the results and put together a report for you. Sampling and wet chemistry are still hands-on operations as far as I can tell. But this is taken as a challenge to instrument makers who will try to engineer around the hands-on requirement to provide something that can be automated. In my world I see more employee turnover with BA/BS analytical chemists than with organic R&D chemists.

As far as employee turnover goes, analysts are under continuous pressure to produce results so that production can proceed or to get product out the door. With hundreds of raw mats, intermediates, and final products, each with their own standard test methods and specs, I certainly wouldn’t last long as an analytical chemist.

Cancer, Cancer Everywhere.

First let me say that I have never been a smoker, drug user or sun bather. As a chemist I have always been cautious about chemical exposure. I have numerous cancers now with the two serious ones in remission. The new ones- who knows.

I use a university hospital and have been visited by flocks of med students looking at me in wonder, sometimes looking down my throat. I get a kick out of it. I always try to joke with them. All cancer diagnoses go before a faculty tumor board for collective assessment. That in particular drew me to this hospital.

My experience with numerous radiation, medical, ENT, and head & neck oncologists is that they absolutely do not want to discuss end of life issues. Maybe that is because I’m not near the end yet, though. But more likely they have production quotas and need to stick to the timeline. My head and neck oncologist did say that they were trying to keep me above the grass, though. That was cheerful.

Since July 22 of this year, I’ve had a partial glossectomy to remove a tumor resulting in a nickel-sized piece of the left edge of my tongue being removed, my first colonoscopy, a neck dissection looking for more cancer, and tomorrow is a root canal. Sonofabitch!

The glossectomy resulted in giving me slurred speech and then the neck dissection made it much worse with the added joy of serious swallowing difficulty. Liquids must be thickened with carrageenan gum to mostly avoid inhalation of food and drink. I’ve already been hospitalized with pneumonia resulting from inhaled food.

My 68th birthday was last week and while I received my well wishes, not a single person was moved to suggest a gerontologist, elder care facility or even as little as when the word “elderly” is used. I’m left up in the air …

It never occurred to me earlier in life that a piece of my tongue could be sliced out. What part of your body is more intimate in your daily consciousness than your mouth? I’ve had surgeons say “give me control of your tongue”. A fella doesn’t hear that very often.

The colonoscopy revealed 2 polyps suspected of being cancerous. So, to tally up the score, I have stage 4 prostate cancer, stage 4 throat cancer, tongue cancer, basil cell skin cancer, and possible colon cancer. Jesus H. Christ!! What next?.

The radiation of my throat resulted in the loss of about 1/2 of my salivary glands and taste buds. I’ve had dry mouth since radiation treatment in 2013, resulting in the loss of numerous teeth.

I was given radiation treatment of my prostate in 2014 and again last summer when the PSA score breached the 4.0 level. Since the 2014 treatment the thinking has changed on radiation dosage. Previously I was given about 1.8 Gray per dose. This time it was 5.0 Gray per dose over fewer doses. The thinking is that it is better to try to break the cancer cell DNA in 2 places at once rather than in just one place. In two rounds of x-radiation treatment of my prostate, I have experienced no pain or discomfort. I’ve had two rounds of 18F-Glucose injections for PET/CT scans.

The throat radiation was a different story. It gave me the world’s worst sore throat. I was fed through a stomach tube and was on opioids for an extended period. Let me say that I detest opioids and the constipation they bring. How do opioid addicts deal with this??

The throat cancer was from the HPV virus and that form is quite treatable, fortunately for me. The tongue cancer was also a squamous cell carcinoma but not of HPV origin.

Life on our lonely pale blue dot is strange. I’ll never get a full grasp of it. I’ll be on the top side of the grass for a while yet and until that changes, I’ll still be a student of the sciences and will continue to write about it.

New USGS Geological Map of USA

The United States Geological Survey, USGS, has released an interactive geological map that includes 4 layers of stratigraphy- Surface, Quaternary, Pre-Quaternary and Precambrian layers with color coded rock units displayed. A click of the cursor on the map reveals the type of rock unit chosen. The website is called The Cooperative National Geologic Map.

Credit: USGS. Surface view shown.

A Few Conclusions and Refutations on Molecular Evolution

Summary:

What can a chemist possibly have to say that could be even marginally interesting about extraterrestrial life or evolution? Well, as far as extraterrestrial life and the search for it goes, I would say that all of the metallurgy, semiconductor fabrication, liquid hydrocarbon fuels, chemicals, transportation technology or polymers exploited in radio or optical astronomy, have some element of chemistry in their manufacture.

………………..

The quest to discover life beyond Earth captivates many in the broad field of space science. The Search for Extraterrestrial Intelligence (SETI) has played a significant role in astronomy and space science communities. However, the search extends beyond intelligent life; any form of life or even the essential components and conditions conducive to life, are of keen interest.

It is widely accepted that the physics governing our planet and solar system likely applies universally. While this is a hypothesis, it is a reasonable one. If the physics are consistent, then the chemistry should be as well. Consequently, the behavior and limitations associated with matter would be uniform across the cosmos. This reasoning suggests that life elsewhere in the universe would be governed by the same chemical and quantum mechanical principles familiar to us.

The “Anthropic Principle” has caused much debate, with Wikipedia noting that “Anthropic reasoning is often employed to address the notion that the universe appears to be precisely calibrated for life.” The mystery of why numerous physical constants and their ratios needed to be exactly as they are for life to emerge on Earth has intrigued many.

To say the Big Bang’s initial pressure and temperature were high is an understatement. As the universe expanded and cooled, energy barriers emerged that shaped the interactions of matter and of photons, placing boundaries on the spontaneous transformation behavior of matter. Pathways of interaction emerged, steering transformations towards increasingly specific outcomes. Essentially, it’s basic kinetics: the quickest transformations and their stable products start to prevail and fill the universe.

If physical constants are emergent at the moment of the Big Bang and become manifest down the timeline, could it be that another Big Bang could happen that is not conducive to life? There would be nobody there to ponder these questions. Life is here because it was possible and maybe even likely here and there.

The phrase “finely tuned for the existence of life” seems to leave open a crack for a creationist view. Absent the many spooky bronze and iron-age theories still in practice today, naturally a sentient being can look at her/his/its existence and marvel at how beautifully synchronized and proportioned the machinery of the universe is. Certainly, there must be a hidden message in this, right?

ET? What th’ …?

Animals like mammals, birds, fish, and even some invertebrates like octopi and crabs are considered to be sentient. According to Google, sentient animals are those that can experience feelings and sensations, both positive and negative, like pleasure, pain, joy, and fear. So, while an octopus may have elements of sentience, could distant observers elsewhere in the galaxy detect them from optical or radio astronomy techniques? Try as it might, the ability of an octopus to construct a powerful radio transmitter and beam a message into the cosmos is sorely limited by its physical anatomy. Except for humans, no other sentient life form on Earth is known to construct a radio transmitter that would serve as a beacon of sentient life.

Until recent history, SETI was limited by the lack of technology to light up the universe with our own signals or to detect faint manufactured signals across interstellar space. At such point that metallurgy, electrical engineering and the hundreds of other critical and apex technologies bloomed into a sufficient state of development, no intelligent emanations from Earth found their way into space.

While TV and radio broadcasts began their journey into space, it is important to realize that our signals were encoded onto carrier waves. Amplitude modulation (AM) signals carry their information by simply varying the magnitude of a single frequency in time with the human voice or music. This is most likely to be grasped by alien radio astronomers. Frequency modulation (FM) is a bit more challenging because audio signal is mixed with a carrier signal by a heterodyne circuit. Extracting useful information would require them to pull audio frequency information from the heterodyned signal.

Television is much more difficult. While the alien radio astronomers may have figured out FM encoded radio information, the particular details of the TV raster scan are based how human engineers decided to interlace and sequence scans to produce an image on a screen of a particular aspect ratio. TV designers took advantage of the human’s persistence of vision to seamlessly follow moving pictures to give continuous images yet maintaining a fast enough frame rate to avoid flickering. The television’s electronic timing is based on frame rate, the number of interlaced lines, and the aspect ratio of the screen.

The point of this TV discussion is that a TV signal must be deconvoluted into a signal that properly displays an image and plays the sound on a particular piece of equipment. This could be challenging for an alien radio astronomy research group to decode.

All of this talk about an octopus developing radio astronomy presupposes that its unique octopussian sentience includes such desires.

It could be that the initial energy at t = 0 yielding the primordial plasma constituting the early Big Bang was only capable of producing a specific set of fields producing elementary particles which then give way to a specific set of quantitative relationships and properties. The burst of energy causing the Big Bang must have had constraints driving its transformation into matter, which is also constrained by quantum mechanics, etc. Maybe the present universe is simply what primordial energy naturally does when expanding as a universe. Why do the quantitative values of physical constants need to be variable? An imaginary and feverish conundrum.

As the highly energized primordial plasma of the Big Bang began to cool, matter and energy channeled into particular states. The particle energy states that had the highest barriers coalesced first followed by subsequent lower energy plasma condensing into other particles. I’m drawing a crude analogy to the process where individual minerals form from cooling magma according to their melting points.

There is a notion prevalent among Creationists that the probability of a life form spontaneously forming from individual atoms is 1 in 10large or some other inconceivably miniscule chance. And if that was how life had to form, then the Earth would still be a sterile wet rock. But that is not how chemical transformations work.

Central to the Creationist view is that evolution cannot happen because there is nothing but random chance to guide the molecules of life into a highly complex organism. They start with the assumption that life arose purely from random chance. I hope to show that this assumption is false.

All atoms and molecules have properties that either qualify or disqualify them as a candidate for a given atomic or molecular transformation. All molecules have properties that either qualify or disqualify them to take part in a transformation resulting in a given product. The words “qualify” or “disqualify” could mean that something will or will not happen absolutely. But just as likely, the words could mean that a transformation is just too slow at a given temperature to give the desired effect. As it happens, temperature is critically important to molecular transformations. At a low enough temperature, most transformations will slow to a negligeable rate, shutting down that particular transformation channel. In general, where there are competing transformation channels, the fastest channel will prevail in producing its product.

All molecules have a limited set of reaction channels at a given temperature as a result of their particular reactivity.

What we think of as ‘ordinary’ chemistry is more precisely the electronic behavior of valence electrons. Nuclear chemistry also exists but in the domain of nuclear change.

Valence electrons on earth will behave the same everywhere in comparable conditions. Chemistry happens at the outer, valence level of ions, atoms and molecules. So, we should expect that bond forming and bond breaking mechanisms should be the same throughout. All of this leads to the high likelihood that chemical reaction mechanisms elsewhere in the universe should not be unfamiliar to Earthlings in general.

Life on earth exists as a result of the behavior of particular chemical substances within a range of chemical and thermal environments. The range of chemical environments and substances present during the initiation of life is thought to be quite different than what we find on earth at the present time. For instance, gas phase molecular oxygen was not present until a considerable time after life began. The initiation of life on earth was under anaerobic conditions and was able to start and survive with the materials at hand. Biochemistry is a series of reduction/oxidation events driven by the Gibbs energy of a transformation as is all of chemistry. Even on anoxic earth, diverse oxidizers were present.

Today, anaerobes are known to use the oxidative properties of inorganic species like sulfate (SO42-), nitrate (NO3-), ferric iron (Fe3+), carbon dioxide (CO2) and manganese (Mn 4+). Other anaerobic oxidants include chromate (CrO42-) and arsenate (AsO43-) which may have been present as well. Reductants include nitrite (NO2-), ferrous iron (Fe2+), and sulfide (S2-).

Oxygen is the third most abundant element in the universe and the second most abundant heavy element on earth behind iron. Many elements are strongly attracted to the abundant oxygen so it is no wonder that so many minerals are oxides of one sort or another. Oxyanions like silicates, carbonates, sulfate, nitrate, and oxides like CO2 or any number of metal oxides all contain oxygen that has been bound with another element. The oxygen pulls negative charge away from the central element making it electron deficient. In the case of sulfate and others, the actual oxidizing part is the atom with the oxygens attached, in this case the sulfur.

Not every transformation of matter is within reach in a given condition. Chemical reactivity which comprises kinetics and thermodynamics has the effect of channeling matter into a finite number of probable pathways. This bestows the property of selectivity. For any given chemical substance, only a certain limited group of transformations are possible or likely, given the conditions.

Life as we know it exists because our biomolecules were robust enough to survive their chemical and thermal environments, but not so robust that they resist the needed transformations. Life depends on biomolecules being moderately stable but not by too much. Biomolecules can organize into particular structures that are physically robust, like the chitin shells on shellfish. In the chemistry of life, chemical transformations must be tolerant of the aqueous environment in and around an organism, but not so tolerant that the necessary reactions are too slow or too fast within the narrow range of environmental temperatures available.

Organisms on earth are tolerant of water at the level of molecules. The internal apparatus of the cell is an aqueous environment having some amount of viscosity. In order for molecules to interact, they must collide with each other. Life in the solid phase would mean that biomolecules would be immobilized and unable to collide and react. Cell structure for metabolism and reproduction would not be feasible. Life in the gas phase is limited by the vapor pressure of the necessary substances. Many, if not most, biomolecules would not tolerate the heat necessary to volatilize. They would decompose.

A diversion into molecular evolution.

I’ll just blurt it out- ongoing evolution requires heritable change in a genome. A genetic change must be survivable for the parent cell to reproduce and produce viable daughter cells. The inherited mutation must not be deleterious to further reproductions of the subsequent generations. A mutation may randomly result in something that has either a lethal effect, no effect, or produces some biomolecular improvement. The mutation may be as modest as an enzyme alteration causing it to bind either more or less tightly to a ligand resulting in a few percent change in rate of some the enzyme’s function. This could translate into better efficiency in producing some cell structure or better use of energy. It could also be that nothing changes as a result of the efficiency alteration, or that it has an overall negative effect further challenging the survival of the cell line in a nonlethal way.

There are two kinds of changes that can occur with DNA. One is a change in the sequence of the DNA molecule itself. The other kind is “epigenetic” which is heritance not reliant on changes on the DNA sequence.

Creationists like to make a show of the probability of random chance producing even simple ordered sequences as fantastically small. Actually, their superficial analysis of permutations and probability looks plausible. I can’t argue with the low probability of individual atoms coming together randomly to form a living organism all at once. However, the beginning assumptions are wrong. Life did not spontaneously form out of a bunch of loose atoms by simply condensing into a centipede or a human. Change in evolution happens at the molecular level a step at a time. A change in the amino acid sequence of any given enzyme must trace back to a change in the DNA sequence to pass along a heritable mutation. Evolution moves by fits and starts. A mutation may have no effect, advantageous effect or deadly effect.

At the level of molecules, change happens through very definite chemical mechanisms. Molecules are constrained to do certain things and in a particular way. It’s like a channel. Sometimes two or more channels may be possible. In this case, the fastest channel will dominate in output and influence. An evolutionary change might cause a biochemical transformation to stop, speed up, slow down, or be more or less specific in outcome.

Molecular bonds vibrate in the range of 1013 to 1014 Hertz. A hydrogen molecule will reportedly undergo 2.5 x 1010 collisions per second at 2 bar and 24 oC. If two atoms or molecules are to react, then they must collide. At a given temperature, a collection of hydrogen atoms will be dispersed over a statistical distribution of energies.

Biochemistry on earth has evolved around water and takes advantage of certain properties of water. Its ability to hydrogen-bond is exploited extensively in biomolecule structures. Water has the ability to accommodate charged species or neutral dipolar species. This is called hydrophilicity. It is important not just to keep ions and molecules in solution, but also to stabilize the transition of a reaction if it generates a momentary dipole.

Water is immiscible with substances having a large hydrocarbon protuberances like fatty acids, phospholipids or certain side groups found on a few amino acids. This is called hydrophobicity. Terrestrial biochemistry exploits both hydrophilicity and hydrophobicity.

Source: Wikipedia.
Some larger molecules like the fatty phospholipids above have both hydrophilic and hydrophobic regions. Given the chance, phospholipid molecules will spontaneously orient themselves in a way that when combined the water ‘repellant’ hydrophobic tails will tend do aggregate. This leaves the hydrophilic phosphate features at each end to remain in contact with the water environment.

Cells have compartmentalization and cell walls simply because of the incompatibility of the polar water molecule and nonpolar hydrocarbons. These two incompatible liquids arrange in a way that minimizes the surface area of contact between them. They will form layers when stationary or droplets when one is dispersed in the other. This is the minimum energy condition they spontaneously go to. Micelles will even form spontaneously in your soapy dishwater.

Life on earth presently requires many environmental conditions to be just right. Cells of micellar-like construction take advantage of the hydrophobicity of substances with long chain hydrocarbon parts on one end and charged or polar features on the other side. Micelles are structures that spontaneously form in water. Living cells adopt a bilayer structure based upon the tendency for “likes to dissolve likes.” That is, non-polar hydrocarbon features “prefer” not to be in contact with polarized water, but rather cluster in a way that minimizes water-hydrocarbon surface contact. The effect of carbon chain structures in the biochemistry of earth is the stability of carbon-based structures and the wide variety features it can accommodate. These features include stable carbon-carbon chains as well as carbon bonds to hydrogen (H), nitrogen (N), oxygen (O) and sulfur (S) in particular. Carbon is unique in that it readily allows the formation of stable double bonds with itself or N, O, or S. Carbon also can form triple bonds with itself or N. Cyanide and acetylene are examples. The ease and stability of carbon bonded to C, N, O and S, along with the stability of multiple bonds on carbon all point to it as an excellent candidate for as the ideal building block for biomolecules.

It is often mentioned that since silicon has certain similarities to carbon why isn’t life based on it? Silicon-silicon bonds are prone to oxidation and not found in nature. Silicon is almost always found in nature as silicate in its various forms in minerals and very often in variety of silicate oligomers and polymers. Silicon-nitrogen and silicon-sulfur substances are not easy energetically. Furthermore, silicon does not form double bonds with itself or other elements. So, the variety of structural motifs silicon can form isn’t as broad as carbon. Silicon vastly prefers to be silicate in nature. Silicon is not found in biomolecules despite its high abundance in the nature.

Conclusion

I’m trying to make the point that extraterrestrial life will surely be different from life on earth at the macroscopic scale but maybe not so much at the level of molecular transformations. Every living species today trails behind it a unique evolutionary history, some of which remains in their genomes. Despite the huge variety of life forms on earth and all of the attendant structural variability that goes with it, we all share the use of DNA/RNA, proteins, carbohydrates, phosphates, lipids, calcium, magnesium, potassium, sodium, etc. All life forms on earth are able to capture and use energy as well as reproduce.

The history of life reveals an obstacle course through which organisms struggled to stay alive. Those that did survive had no way to anticipate the future and no way to prepare for it even if they were able to “anticipate” at all. The history of life is the history of challenges to survival.

Humans exist today because our ancestors going back into deep time were able to survive both anaerobic and oxygenated earth, snowball earth, competitive pressures from other life forms, vulcanism, cometary impact, solar UV radiation, chemical toxicity from the environment, disease and climate.

Today we can add stupidity to the list of survival challenges. Can we survive the results of our behavior? Humans have a brilliant streak in developing weapons- explosives, guns, nuclear, biological and chemical weapons. If all else fails, there will always be the sharp stick and club.

Humans are the way we are because of the way that natural history unfolded. A planet with the same makeup and conditions 3 billion years ago would evolve life in a different way than we went. Evolution happens because of the ability of our genetic material to be just a bit unstable and to be passed on in reproduction. But this change is a random process in both features and time. A genetic change can be fatal or helpful. The manner and schedule in which random genetic alterations happen is impossible to predict. Evolution is blind going forward. Another try at evolution is highly unlikely to produce Homo sapiens again.

Any given “intelligent” species may or may not invent or use radio technology. Therefore, they may or may not emit or receive radio transmissions. Such creatures would be undetectable using radio astronomy. Although two patents for wireless telegraphy came out in 1872, humans have only had useable wireless telegraphy since 1895 (Marconi). As of this writing, only 128 years have elapsed since Marconi sent his first long distance (1.5 mile) radio communication.

We have only had radio communications for 128 years in the entire history of our species. In order to have this invention in 1895, the European enlightenment had to happen leading to the idea of scientific inquiry and a minimum understanding of physics and chemistry. The voltaic pile had to be invented which gave way to further refinement of electricity. At minimum, the metallurgy of iron, copper and zinc (for brass) had to be in place for the for the discovery and use of electricity. The path to broadcasting and receiving radio waves required a fair degree of curiosity and industrialization.

The How and Why of Science

Preamble

There are more than a few definitions of science out there. Every scientist you ask will give their favorite variation on a common theme. The whole business of science is built ideally around the concept of the scientific method. One of the better broad definitions of the scientific method is this-

Wikipedia as a Source of Authoritative Information

First, a homily on Wikipedia as a resource. It’s been my observation that in areas that I am familiar with, i.e., chemistry, aviation, the history of science and a few others, the content I’ve encountered comports well with my general knowledge. The more links and references, the better. And, more often than not, the links actually reflect the content that referenced it. What’s more, Wikipedia encourages input and corrections by the broader community and if you go into edit mode, you can see the list of edits over time. I’ve contributed to a few edits myself. Are there errors or just simple BS in Wikipedia? Well, of course. It’s been said that a camel is a horse designed by committee. While Wikipedia may reveal some of this camel design in places, basically most everything we read or hear is subject to this shortcoming. The freedom to edit a Wikipedia entry is a type of “peer review” but the qualifications of the peers is unknown. Believe me, in science publishing, anonymous peer reviewing is populated with more than a few sanctimonious jerks whose motivations may not be pure.

I’ve spent my career diving into the primary chemical literature via Chemical Abstracts. Primary literature is crucial, but it is usually very narrow in scope and often subject to later revision. This is why review articles, books and monographs are so important. Someone has combed through the primary literature and brought together some structure in an area of study. Wikipedia has become a third tier of scientific information and access for anyone. While it seems quite accurate, we should always be using our best judgement as we read the content. Do the links support the statements? Are there enough links, etc.?

A great deal has been written about the scientific method by those more capable than I so I won’t attempt to blather through it. Instead, I will share an example of how asking a very basic question led me to a treasure trove of information expanding my understanding of the universe.

Science is frequently regarded with excessive reverence, suggesting that it is solely the realm of “proper scientists” and embodies the ultimate truth. However, in reality, it is open to anyone armed with curiosity and resolve. Curiosity drives inquiry, but it is also enhanced by a prepared mind. Some questions illuminate, while others can deceive. A well-posed question can propel one towards the heart of a matter. A ready mind can recognize false trails early on and steer clear of them.

How or Why?

I favor “how” questions over “why” questions because they foster a more mechanistic inquiry into nature and adhere to established physical principles. “Why” questions often carry philosophical or religious connotations and can be laden with presupposed motives or assumptions. This doesn’t render “why” questions invalid; however, they may veer away from the realm of observable natural phenomena, the foundation of scientific inquiry. Asking “How did Stella move the lamp?” may differ from “Why did Stella move the lamp?”. The interchangeable use of ‘why’ and ‘how’ in everyday language can result in imprecise thinking and sloppy conclusions.

Obviously both how and why questions are useful is answering a question. Judicious use of ‘how’ and ‘why’ can lead to more focused thinking about either a mechanistic or motivational question. ‘How’ gets to physical causality whereas ‘why’ often seeks mechanist details but may also leave room for psychological motivation. Either entry into a question is valid depending on what a person wants to know: Physics or psychology.

Sharply pointed scientific inquiry requires the meticulous use of language to convey exact meanings. This scrupulous attention to language demands a precise vocabulary that narrows the scope of interpretation. While this may seem tedious, the benefit lies in getting quickly to the heart of a question. Similarly, lawyers have developed their specialized legalese for this very reason.

Being more precise in one’s use of language is very useful if you’re plagued with complex situations, incomplete information or the need to focus on a mechanistic pathway. ‘How‘ thinking helps with this.

As one accumulates a greater vocabulary over time, the ability to apply nuances into your thinking and communication increases as well since even synonyms can differ a bit in their meaning. As you spend more time in scientific pursuits, you start to realize the value of having good questions to ask. In fact, the skill with which you formulate questions can drive your research further into the unknown, which is where everyone wants to go.

Albumin- A Molecular Ox Cart.

It is amazing what you’ll find by just looking around. While reviewing recent blood test results it occurred to me that I didn’t know the first thing about albumin as a protein. A Google word search led to numerous links but provided many images as well. The crystal structure is below.

Source. The crystal structure of human albumin. The albumin was crystallized in the presence of excess palmitic acid for x-ray analysis. Front. Immunol., 25 January 2015, Sec. Vaccines and Molecular Therapeutics Volume 5 – 2014 | https://doi.org/10.3389/fimmu.2014.00682

It is not uncommon to describe the enzyme-substrate complex as a highly specific lock and key structure. In the earlier literature is was axiomatic that enzymes are described as being highly substrate specific and use a single binding site for a given substrate. This notion is not always correct as the above graphic shows. Albumin is produced in the liver and is sort of a molecular ox cart- it can transport many substrates in the blood.

The job of human albumin is to get various substrates mobilized in the bloodstream and offer them at a desirable location. With the high molecular weight of enzymes, and the consequent low molarity available, it is astonishing that the heat of binding of substrate to enzyme can be measured at all.

One way to determine binding enthalpy and stoichiometry of a substrate to enzyme is ITC- Isothermal Titration Calorimetry. These calorimeters are available from several manufacturers such as TA Instruments and Malvern. ITC is just a type of reaction calorimeter that allows for immediate access to the reaction mixture. It is a microscale RC1 in effect. An enzyme solution can be titrated with substrate allowing for a visual determination of an equivalence point where 1 eq of enzyme active sights just matches the titrant equivalents. From such an experiment both enthalpy and stoichiometry can be measured. The image below is from TA Instruments and nicely shows the graphic output of an ITC experiment.

Source: TA Instruments product brochure. Each peak is an aliquot of titrant. Note how cleanly the signal goes to baseline between aliquots.
This graphic shows the baseline signals from titrating directly into buffer. This is subtracted from an actual run. From TA Instruments sales brochure.

Above, the background signal from the buffer represents noise in the enthalpy signal.

Graphic from TA Instruments sales brochure.

TA Instruments also offer equipment for so-called nano scale experiments. See below.

The TA ITC specification table. Note the minimum heat in the low volume column: 0.04 to 0.05 microJoules with a 190-microliter sample cell size.

Albumin is endowed with binding sites open to a variety of substrates. It is like a wheelbarrow or an ox cart. It can ‘carry’ numerous substrates across several categories.

The downside of such low specificity is that albumin can bind many drug compounds at the expense of dose delivery to the desired site. Doses of drugs must be adjusted to account for drug lost to blood proteins like albumin.

The Gift of a Jumbo Jet to the ‘Great One’

Some folks have all the luck. America’s Orange Jesus has been (or will be) offered a Boeing 747 to use in place of the two presidential B747s which had developed an annoying rattle and had to be taken out of service. They are presently parked at Oskar’s Jet Shop and Grill somewhere in the Pacific Northwest. In sympathy to this niggling inconvenience to #47, an old man, the royal family of Qatar has generously stepped forward and offered a super luxury B747 for the Great One for his weekly trips to his many resorts. The B747 will transfer to #47’s Presidential Library foundation where it will remain. Some are saying that it will cost a gigabuck to upgrade it as necessary.

Keeping a third B747 ready to fly at any given moment will be expensive as are the 2 presidential jets now in the shop. In the new B747, the lavatories will have to be reduced in size for the media’s discomfort. Vending machines will be added for feeding the media but will be limited to exact change only. The machines will also offer #47’s trading cards which will include a 5 % discount coupon for his golden sneakers. As always, payment can be made with #47’s cryptocurrency plus a $50 service charge.

As the authoritarian regime of #47 continues to take hold, an increasing number of governments will express fealty and line up to offer something special, which #47 will gladly take and keep, the emoluments clause notwithstanding, found in Article I, Section 9, Clause 8 of the U.S. Constitution. It has already begun to turn stomachs worldwide but others will be attracted to the new ‘democratic dictatorship’ ramrodded by the GOP and led by the Orange Jesus himself. Many people around the world tolerate authoritarian leaders or see them as admirable strongmen. Kick ass and take names, some say. But too often the names aren’t taken or made available to anyone. There is just the ass kicking and transfer to a holding facility. Habeas Corpus? Gone! Evidence of a crime? Nah. Filing an appeal? What, are you being serious?

To the many readers outside the USA, know that a very large number of US citizens are horrified and in serious opposition to #47 and his MAGA movement. However, it seems that the Founders of this country failed to anticipate a situation where a single party rules both houses of Congress, the White House, the Supreme Court, and the governors and legislative bodies of many states. The Founders assumed that the checks and balances between the three co-equal branches of government and built into the government they designed would protect the democratic republic and keep essential government services working. They could not anticipate a simmering populist movement amplified by instantaneous social media. Whereas in times before the internet and smart phones, a large number of disaffected and under-educated citizens in America now have access to media of all kinds and can gravitate towards whatever populism that appeals to them. There seems to be little in the way of concern about truthfulness.

The single party dominance of MAGA in US government means that enforcement of federal laws or procedure will be ignored. The Department of Justice has been slow to enforce checks and balances or just ignore it altogether. MAGA GOP politicians know that endorsement by #47 ensures that they will get votes from MAGA block and assure their political careers.

Roughly 30 % of the voting population will support #47 until their dying day, regardless of his behavior. Resistant to the lessons of history and logic, they are essentially lost to modern times. They are angry from seeing and hearing the hype surrounding modernity and the corrosive conspiracy theories involved. Not having a college education, they missed out on opportunities that open up by living in a college environment. All of the job descriptions and opportunities requiring college education aren’t necessarily posted off-campus and are therefore missed.

Until I entered the university, I was completely unaware of a host of career choices available. I grew up in a rural midwestern blue collar environment and was completely unaware of the various futures available. Many have glorified our rural culture, but I found it quite boring in my years from birth to 14 years. Sure, there are wide open spaces and nature. But the fifth time you wander out into a large pasture you begin to realize that solitude is nice but quite boring.

I was introduced to science and technology by watching the progress of the Apollo moon mission in the 1960s. It was thrilling but there was no one around who could hold a decent conversation about it with me. Basically, if you were a kid into science at that time in my state, you were alone. Just knowing about sciency topics wasn’t enough. It is nice and necessary to have discussions to explore ideas and ask better questions. To share in the wonder and majesty of the universe. That’s not too much to ask, isn’t it?

A Swerve into the Weeds of Asteroid Mining

Notice: As an organic chemist and not a geochemist I will be using descriptions and vocabulary that may not ordinarily be used in geology. While a geochemist might easily write a lovely article that could bring tears to the eyes of the most sour geochemist, I will stumble forward with just my trailer park chemistry background- organometallic, organic, inorganic, physical and quantum chemistry.

When you step back and view mining technology as a whole, it becomes apparent that two of the largest scale inputs in mineral refining are water and electrical energy. On Earth diesel is also required in large quantities.

A good question for those who propose mining asteroids is this: Have you solved the water and electric power requirements for unit operations? Let’s say it is solved for one mineral. How will the value be mined, transported and gently lowered to the Earth’s surface without breaking into flaming pieces on re-entry or forming a crater in a city? Is there an element or mineral that is so valuable as to justify the costs and risks to be met for a space mining mission? Is it rhodium? Gold? Diamonds? Or what?

Do the people behind the fanciful images and hype believe that they only have to dock with the asteroid and grab valuable minerals from the surface? There is a good chance that the target ore will need exploration, excavation, and possibly some kind of blasting. The target elements may well be dispersed within the host rock. This will require comminution in preparation for further processing. The ore will likely need ore dressing which is the job of removing undesired rock from the valuable ore. This lowers the quantity of ore to be processed.

The rocky bodies in the solar system have surfaces of regolith. Regolith is an unconsolidated jumble of loose rock and dust presumably overlying a solid body. Given that the regolith may well be consist of rocks and dust accreted from a distant source, merely assaying the regolith might not reveal the minerals that could be there in abundance just below the regolith. There is no way around it- core samples will be needed to properly assess the economic geology.

PGM Mining on Earth

A look at the large-scale Platinum Group Metal (PGM) production activity in South Africa is instructive. The Bushveld Igneous Complex (BIC) near Limpopo and North-West provinces contains some of the richest PGM deposits in the world. The BIC is found in the Kaapvaal craton. The BIC also extends into Zimbabwe.

The Bushveld complex is located on a ‘craton‘ which is a section of continental crust that has been stable for 400 million years or so. Over that time period some portion of crust has not been subjected to subduction or rifting as an effect of continental drift. A craton is relatively untouched by continental drift over some lengthy time interval and as a consequence the crustal rocks found in a craton may be quite old. Here, ‘old’ means rock that has not been metamorphosed recently, vented out of a volcano or eroded and stratified in a sedimentary formation within several hundred MA.

The Bushveld complex is found in the Kaapvaal craton of South Africa, extending into Zimbabwe. A consequence of this location on a very stable parcel of continental crust is that vertical transposition of rock formations, i.e., subduction activity, has not led to metamorphism or folding of strata. This stability has allowed a relatively undisturbed magma chamber to form and cool, producing layered cumulates.

The formation of cumulates is a partitioning process within the magma chamber that produces solid minerals that can float or sink within the magma. Cumulates with higher density than the magma will tend to sink, building a layer, and lower density minerals will float to the top of the chamber and form an upper layer. In this way, minerals can self-purify and stratify by fractional crystallization.

While fractional crystallization can result in enhanced purity of specific minerals, the melt from which the crystals precipitate is also changing in composition. Magma is a viscous fluid and its components can undergo anion/cation exchange to produce new minerals upon further cooling. Anions include silicate, aluminate, sulfide, hydroxide, chloride, oxide, and a whole basket of metal oxyanions like titanate, tungstate, molybdate, chromate, etc. Cations include most every metal, sometimes including the noble metals. Every metal has a set of positive oxidation states that may be subject to reduction or oxidation to afford a different oxidation state or charge.

While both anions and cations present in magma have a particular charge, their individual size is important as well. Size and charge matter most when crystals are assembling. When, for instance, a calcium-containing mineral is crystallizing, the crystal lattice is subject to collisions with the whole gamut of species in the magma. If the temperature and pressure are appropriate, calcium (+2) cations nestle into a vacancy in the lattice. This is controlled by the concentration, temperature and Gibbs energy of the placement of the cation. However, if a different cation of +2 charge and similar ionic radius happens by, that different +2 cation may find itself occupying calcium’s place in the lattice. An example would be where the Ca+2 cation was replaced by Mg+2 or Fe+2.

Mineral crystal formation is a type of equilibrium wherein lattice anions and cations at the surface of the crystal are in equilibrium with anions and cations in the melt. The rate of crystallization or dissolution is driven by several things. Substitution of a Ca+2 ion in a lattice with Mg+2 or Fe+2 ions retains the charge balance in the lattice. But if a too large or too small +2 cation attempts to sit in place of Ca+2, a mismatch occurs which may be energetically favorable, but as a result may be much more prone to removal by equilibration. The interloping cation could be of such a size that its heat of formation is small and therefore subject to replacement by equilibration. Or not. The resulting mineral could be comprised of Ca+2 cations and M+2 cations in a non-stoichiometric ratio. Or a new mineral comprising a stoichiometric ratio of both cations.

The anions in a mineral substance can be quite varied and several may exist in a mineral at the same time as in the case of anions silicate and aluminate.

The Stillwater Igneous Complex in Montana, USA; the Sudbury Basin in Canada; and the Norilsk-Talnakh deposits north of the arctic circle on the Siberian Craton.

The Stillwater Igneous Complex in south central Montana, USA. Source: Google Maps.
Image from Google Maps. Elevator shafts for the Sibanye-Stillwater K3 Shaft, South Africa.
Image from Google Maps. The Sibanye-Stillwater K3 shaft, South Africa.

Russia is the leading producer of palladium with 40 % of the global market. Norilsk Is also known as a center of non-ferrous metallurgy as well as noble metals. Norilsk Nickel, also known as Nornickel, is a mining and smelting company. Platinum Group Metals (PGM) have been recovered as a side stream of nickel and copper mining by Norilsk Nickel.

Open pit mile near Norilsk, Russia. Norilsk was originally started as a gulag in the far north of Siberia and eventually became a mining community.

The aerospace proponents of asteroid mining should spend some time at an actual mine. Breaking rock and hauling it around is simple on Earth but consider doing this in a vacuum at near-zero gravity. Look at all of the methods of conveyance and processing in operation at a mine that works only in a gravitational field. Blasting, front-end loaders, haul trucks, conveyor belts, crushers, ball and rod mills, flotation and settling tanks, lixiviation in sulfuric acid and several shifts of staff to operate and maintain it. Don’t forget the analytical lab and chemist or the maintenance group.

A human trip to an asteroid, which is always in orbital motion and probably rotating, to mine and return with paydirt for the investors will always be high cost. Bodies outside of the Earth-Moon system will be nearby only for a short time, depending on the orbital period of the asteroid. While our Earth is measurably overheating, the biosphere is disintegrating and political turmoil is rampant on Earth, perhaps we should focus closer to home?

I do believe that eventually somebody will design mining technology to solve the unique problems of mining smaller asteroid bodies with negligeable gravity. Energy dense power sources will be needed to move commercial scale machines and ore. The big problem will be the economics. What mineral is so valuable as to justify the trillion-dollar expense of finding an asteroid with suitable quantities of mineral, up front R&D costs, and beneficiation and isolation of the mineral?

Minerals dispersed in the regolith matrix will need comminution, extraction by lixiviation, floatation, isolation and packaging. Now, we can get it back to earth orbit but then what? Do we just deorbit in the usual way?

Bringing home the paydirt

Let’s say they return 1000 kg (contained) of rhodium valued at todays price of $5400/toz (toz = troy ounce). 1000 Kg contained of rhodium = 32150.7 troy ounces, so 32150.7 toz x $5400/toz = $173,613, 780. However, just the rumor of 1000 kg of new rhodium about to come on the market will drive rhodium prices down. So, $174 million sounds like a lot of money and in a sense it is. But in aerospace and heavy industry, millions are quickly consumed.

Rhodium was chosen for its general scarcity and high price. There is no reason to suppose that rhodium will be more abundant on a given asteroid than on earth so numerous asteroids may need exploration by geologists. Core samples might be needed for the economic geologists to sketch out the size and value of an ore body.

There will be a threshold price of rhodium that must me exceeded before rocket launching and asteroid digging begins. This is how mining works on earth. Until then, the celestial rhodium discovery will just keep orbiting the sun into the future.

The North American craton. Source: Wikipedia.

An aspect of PGMs is that the very few mines that produce them do so in a unique geological feature on a craton. The mechanism for PGM mineralization in districts like the Bushveld Igneous Complex in South Africa took place in a magma chamber where over time the magma began to cool. Magma gets its minerals from the mantle far below and from the walls of the magma chamber. In subduction zones the subducting crust is pushed downwards causing rising temperatures.

Subducting oceanic crust is loaded with water in several forms. Many minerals are ‘hydrated’ meaning that one or more water molecules are strongly attached to the mineral. These might be called coordinated water. The oxygens are strongly attracted to a cationic feature of the mineral. Interstitial water molecules may be occupying voids in the mineral lattice. Discrete water is only weakly attached and may diffuse elsewhere. Interstitial and discrete water may evaporate readily if exposed to air or heat. At the elevated pressures and temperatures of magma at depth, the three kinds of water are hot enough to flash to steam if the pressure was released. However, as the magma rises to the surface to cooler surroundings and lower pressures, eventually the water will flash to the gas phase moving magma in the direction of lower pressure. Just below the surface the dissolved gases including CO2, steam and SO2 will expand as a gas and push magma to the surface causing a volcanic eruption.

As the magma cools, the substances with the highest melting point begin to crystallize. If the crystals that have a higher density than the magma, they will settle lower in the magma chamber and form a distinct layer. While this layer is building, other minerals will follow in a similar process. The layers of precipitated minerals are called cumulates.

The process of minerals selectively crystallizing and precipitating to the upper or lower zones of the magma chamber. The overall process is called fractional crystallization and layers called cumulates can form. In the photo below are several layers of dark chromite cumulate.

From the Bushveld Igneous Complex. Exposure of cumulate layering of dark chromite. Mining involves following the cumulate layers.

Now that I have expressed my doubts about asteroid mining, I must ask ‘Am I being a Luddite’? Maybe a little bit, but even the doubts of a Luddite can be on the mark now and then. Asteroid mining will be an adventure for a few astronauts, profitable for aerospace contractors and an entertainment spectacle for the public; however, resources seem better used on Earth for remediation of the biosphere, diplomatic solutions for the conflict of the week, lower hydrocarbon consumption and better education, especially in the area of civics.

The whole purpose of mentioning PGM geology and mining in a post titled Asteroid Mining is that we on Earth are fortunate to have concentrated mineral deposits that exist only because of unique geological processes. These processes only work in Earth’s gravitational field. The upwelling of lower density hot hydrothermal fluids. The formation of evaporites rich in borax. Lithium brines.

Take my uranium, please

The formation of cumulates in lava chambers relies on differential density driven by gravity. The ability of rain and snow runoff to mobilize gold sulfides will produce lode gold and placer deposits. The ability of oxygenated meteoric water to oxidize insoluble U4+ to soluble U6+ in sandstone formations to form concentrated roll front deposits. The ability of oxygen to switch uranium oxidation states from U4+ to produce a soluble form (U6+) that can migrate and concentrate leading to the partitioning of U6+/U4+ species. Underground formations of uranium can be dissolved in a solution of sodium bicarbonate by injection and pregnant solutions of the uranium carbonate can be brought to the surface as a solution. This solution is run through a column of ion exchange resin beads which exchange chloride ions for the uranium complex. Once loaded, the beads are washed with a special solution to remove the uranium (6+) concentrate.

Oxidation and isolation of U6+ from U4+. Graphics by Arnold Ziffel.

Our ability to mine and isolate minerals is uniquely enabled by planet earth. The ability of nature to dissolve, mobilize and concentrate minerals into ore bodies from highly dispersed placement in source rock has been positive for humanity. A great many elements are found in a dispersed condition in the continental crust. For some, there are natural processes for concentration. For others, they form secondary minerals that end up mined with the primary ore. A few like gallium, indium and bismuth are valuable but are only available as a side stream from the primary ore. Copper is an excellent example of a primary metal whose ore includes many other metals like zinc and bismuth. Copper can be electro-refined to 99.99 % purity. The slimes left behind after the electrolysis and dusts caught in ventilation systems can be enriched in useful metals and are often collected for processing.

The purpose of citing the large-scale processes in use on the home planet is not to suggest that asteroid mining must start out at large-scale. It would likely start out as a small-scale surface or underground operation with a small crew or with robotics. Only a few select minerals would be economically suitable for recovery. Platinum Group Metals are mentioned above because of their high intrinsic value and ability to exist as the native metal. If luck is with the astro-miners, the motherlode might be easily visible so later the gangue material can be chipped off. The process of trimming ore to retain the value and discard the gangue was called ore dressing. Being quite dense, the volume of PGM metal ore may be low, but the density and mass is quite high.

If a given asteroid has never been part of a larger system with magma and sufficient gravity to force stratification by density, the cumulate model may not apply. A given asteroid having never been exposed to bulk water and consequently never been subject to hydrothermal flows and weathering may not have minerals that here on Earth are known to be formed with water or partitioned as a result of hydrothermal flows. Lake and ocean sedimentary units are almost surely absent as are processes requiring aqueous migration through porous rock as in the case of uranium roll fronts.

Asteroid mining will be a totally new activity and most all of the natural geological processes on earth will have been absent. Many geological processes on earth produce economic ore bodies. These will be largely absent on an airless, dry asteroid.

One thing to consider: Most of the rock accessible at the Earth’s surface is not economic ore. The surface of the Earth brimming with carbonates, silicates and aluminates bound to a variety of ‘ordinary’ metals like calcium, magnesium, iron, sodium, potassium and a handful of other common metals. While there are important and valuable uses for these common metals, they are predominantly found dispersed in surface rock comprised of many individual minerals, or that an ore body is too small for economic recovery.

The fraction of the desired mineral in the ore can be highly variable. Depending on the market, some parts of the ore body may be economical to mine while other parts may not. This is why cores are drilled to locate the 3-dimensional extent of the ore body, estimate the potential value and minimize the expense of digging and processing uneconomical ore.

On Earth many mineral deposits have been located historically by surface exposures that are part of a larger ore body. The economics of isolating any one mineral or metal in the presence of the others will depend heavily on the % concentration of the target mineral, the processing methods available and the market price of the final product. A market downturn can last months, years or represent new long-term realities in demand for the product.

Lamentations on Science Infotainment Rev 2.

Note: This post appeared May 15, 2007, as “Infotainment, Chemistry, and Apostasy“. I have pulled it up through the mists of time for another go and with a few edits.

In the normal course of things I used to give school chemistry talks or demonstrations a couple of times per year and until recently, I had been giving star talks at a local observatory more frequently.  The demographic is typically K-12, with most of the audience being grades 3-8.  From my grad student days through my time in the saddle as a prof, I was deeply committed to spreading the gospel of orbitals, electronegativity, and the periodic table. I was convinced that it was important for everyone to have an appreciation of the chemical sciences.  I was a purist who knew in his bones that if only more people were “scientific”, if greater numbers of citizens had a more mechanistic understanding of the intermeshing great world systems, the world could somehow be a better place. 

In regard to this ideology that everyone should know something about chemistry, I now fear that I am apostate.  I’m a former believer.  What has changed is an updated viewpoint based on experience.  

Let me make clear what science is not. It is not a massive ivory tower that is jealously guarded ajd intended to be impenetrable by mortal folk. Big science requires big funding and organizational support, so big administrative structure forms around it. At its core, science is concerned with learning how the universe works by observation, constructing a good first guess (theory) on what is happening, measurement (conducting quantitative experiments), analysis (quantitative thinking), documentation and communication. The common understanding is that a scientist is someone who has been educated and employed to do these activities. However, anyone who conducts a study of how some phenomenon happens is doing science whether for pay or not.

What science has learned is that the universe is quite mechanistic in how it works. So much so that it can be described by or represented with math. At the fundamental level of ions, atoms and molecules, constraints exist on how systems can interact and how energy is transferred around. At the nanometer-scale, quantum mechanical theory has provided structure to the submicroscopic universe.

Chemical knowledge is highly “vertical” in its structure.  Students take foundational coursework as a prerequisite for higher level classes.  Many of the deeper insights require a good bit of background, so we start at the conceptual trailhead and work our way into the forest. But in our effort to reach out to the public, or in our effort to protect a student’s self-esteem, we compress the vertical structure into a kind of conceptual pancake.  True learning, the kind that changes your approach to life, requires Struggle.

What I found in my public outreach talks on science- chemistry or astronomy- was the public’s expectation of entertainment. Some call it “Infotainment”.  I am all in favor of presentations that are compelling, entertaining, and informative.  But in our haste to avoid boredom, we may oversimplify or skip fascinating phenomena altogether. After all, we want people to walk out the door afterwards wanting more. We want science to be accessible to everyone, but without all the study.

But I would argue that this is the wrong approach to science.  Yes, we want to answer questions.  But the better trick is to pose good questions.  The best questions lead to the best answers. People (or students) should walk out the door afterwards scratching their heads with more questions.  Science properly introduced, should cause people to start their own journey of discovery. Ideally, we want to jump-start students to follow their curiosity and integrate concepts into their thinking, not just compile a larger collection of fun facts. 

But here is the rub. A lot of folks just aren’t very curious, generally.  As they sit there in the audience, the presentation washes over them like some episode of “Friends”.  I suspect that a lack of interest in science is often just part of a larger lack of interest in novelty.  It is the lack of willingness to struggle with difficult concepts.  But that is OK.  Not everyone has to be interested in science.

Am I against public outreach efforts in science?  Absolutely not.  But the expectation that everyone will respond positively to the wonders of the universe is faulty.  It is an unrealistic expectation on the 80 % [a guess] of other students who have no interest in it. I’m always anxious to help those who are interested.  It’s critical that students interested in science find a mentor or access to opportunity.  But, please God, spare me from that bus load of 7th graders on a field trip. 

What we need more than flashier PowerPoint presentations or a more compelling software experience is lab experience.  Students need the opportunity to use their hands beyond mere tapping on keyboards- they need to fabricate or synthesize. You know, build or measure stuff. 

It is getting more difficult for kids to go into the garage and build things or tear things apart.  Electronic devices across the board are increasingly single component microelectronics.  It is ever harder to tear apart some kind of widget and figure out how it works.  When you manage to crack open the case what you find is some kind of green circuit board festooned with tiny components. 

And speaking of electronics or electricity, I find it odd that in a time when electric devices have long been everywhere in our lives, that so FEW people know even the first thing about electricity. I instruct an electrostatic safety class in industry and have discovered that so very, very few people have been exposed to the basics of electricity by graduation. I spend most of the course time covering elementary electrostatic concepts along with the fire triangle so the adult learners can hopefully recognize novel situations where static electric discharge can be expected. Of course, we engineer away electrostatic discharge hazards to the greatest extent possible. But if there is a hole, somebody will step in it. It’s best they recognize it before stepping into it.

The widespread educational emphasis on information technology rather than mechanical skills ignores the fact that most learners still need to handle things. There is a big, big world beyond the screen. A person will take advantage of their mechanical skills throughout their life, not just at work. Hands on experience is invaluable, in this case with electricity. Computer skills can almost always be acquired quickly. But understanding mechanical, electrical and chemical systems need hands-on experience.