Category Archives: Chemical Industry

Cresson Gold Mine, Part 2.

We collected samples of the lamprophyre in the bottom of the pit. The formation appeared whitish green in on the weathered surface owing to oxidation. However, if a fresh surface was exposed, the rock was composed of sugary dark xtals with the occasional biotite phenocryst.

Outlined Lamprophyre at bottom of Cresson open pit mine

Outlined Lamprophyre at bottom of Cresson open pit mine. Copyright 2009 Gaussling.

Cresson Mine Lamprophyre Close-up

Cresson Mine Lamprophyre Close-up. Copyright 2009 Gaussling.

Mafic or ultramafic rocks are low in silicates and enriched in Fe and Mg oxides. The lamprophyre above is mafic in composition with a sugary xtal matrix with biotite and other phenocrysts.

Breccia from Cripple Creek Diatreme

Breccia from Cripple Creek Diatreme. Copyright 2009 Gaussling.

The breccia above is characteristic of the Cripple Creek diatreme. Relatively rounded clasts populate the mass of the aggregate, indicating that the clasts were rounded by some process prior to deposition.

The gold is generally too dispersed to see, however, you can see pyrite with a hand lense in many of the samples. Pyrite often accompanies gold.

Cresson Gold Mine, Part 1.

Early saturday morning 50 intrepid geotouristas packed into vans and drove to the CC&V mine in the Cripple Creek district of Colorado. Most of the group were professional geologists- professors, teachers, and geological survey folks. There were only a few interlopers like myself who were interested but untrained in geology. Not surprisingly, a background in chemistry is nearly useless when the discussion turns to stratigraphy and rock morphology.

The Cripple Creek gold district consists of an extinct volcanic structure called a diatreme. A diatreme is characterized by the presence of a volcanic pipe structure filled with brecciated rock. It is thought that the combination of shallow hot rock and ground water lead to violent explosions that resulted in fractured rock. Cripple Creek breccia has rounded clasts, indicating the rock fragments were exposed to rough, erosive treatment leading to attrition and rounding of the clasts prior to consolidation of the breccia.

In the past, gold mining at Cripple Creek was a underground activity. The district contains an extensive network of remnant subsurface works of drifts and shafts. Today, CC&V’s mining activity is limited to high throughput open pit excavation supplying pulverized rock to a cyanide heap leach field. A constant flow of ca 100 ppm aqueous sodium cyanide solution is leached from the top down through as much as 800 vertical ft of gold bearing rubble.

Abandoned Drift and Blue Bird Dike

Abandoned Drift and Blue Bird Dike

Columnar formations can be seen in certain locations of the mine (See photo: some features are enhanced with lines to show the margins). As the pit expands, drifts and shafts are exposed as seen in the photo above. The Blue Bird dike is an igneous intrusion into the surrounding formation. It is no coincidence that the drift in the photo is near the dike. It is common to see disturbed zones along the intrusion where gold can be found in higher abundance. The goal of the drift miner was to follow the enriched rock for more efficient reclamation of value.
Exposed Drifts During Pit Operations

Exposed Drifts During Pit Operations

A feature seen in the pit is a Lamprophyre, or igneous dike comprised of ultramafic, silica-poor, magnesium-rich rock. Biotite phenocrysts can be seen in samples. This is regarded as an unusual feature.

Lamprophyre formation in Cresson Mine

Lamprophyre formation in Cresson Mine

 The big haul trucks carry 300 tons of rock from the mine to the crusher. The crusher is actually a series of crushers that reduce the ore to pieces roughly 3/4 inch in diameter.

Haul Truck Carrying Rock from Blasting Site to Crusher

Haul truck carrying rock from blasting site to crusher The crushed rock is blended with lime and then driven to the leach pile for extraction. Another load for the leach heap.

 

A Massive Au/AuTe Deposit

Th’ Gaussling attended a geology seminar thursday evening at the Colorado School of Mines. It was given by the chief geologist at the Cripple Creek & Victor gold mine (now AngloGold Ashanti) and was concerned with 3-D modeling of the volcanic formation that forms the center of the deposit.

What is unusual about the CC&V mine is the extent to which tellurium is present. There are a dozen or more tellurium minerals and many of them are present in the ore body. The CC&V load was discovered relatively late- about 1891. Due to the extensive fraction of AuTe and AuAgTe minerals, the presence of the ore body was not detected by placer prospecting. 

Prospectors panning for gold in local streams had no way of knowing that extensive gold was present because AuTe(Ag) minerals do not have a gold-like appearance.  Legend has it that it was discovered by a drunken cowboy who noticed some native gold in an outcropping in the area and took a sample down for assay. As I have mentioned before, the Cripple Creek district has produced about half of all the g0ld to come out of Colorado.

What is key to the formation is the fact that it has zones of extensively altered volcanic rock disturbed both mechanically in the form of fractures and faulting, and chemically in the form of its potassic-alkali nature. The formation has strongly brecciated zones and is desribed as “vuggy”, meaning that there are extensive voids. Native gold and gold telluride mineralization can be found on the surfaces of the vugs. The mineralization was deposited by hydrothermal streams extracting Au and Te from unknown source rock.

Presently the operation is surface mining which feeds to a cyanide leach field for gold extraction. The surface pit mine is working downward, digging through the extensive network of mineshafts. In the early days at Cripple Creek the mining was limited to underground activity. Miners would follow the extensive subsurface network of gold-rich veins in whatever direction they might go. The result is a very complex and extensive matrix of tunnels and shafts that extend downward to as low as 3000 ft. In the early days, the economics of subsurface vein mining were attractive enough to sustain the operation. Today, the economy of scale dominates and pit mining with heap leaching of the lower grade ore is what sustains the operation.

The gold is recovered by a cyanide leach field that is 800 ft thick in places. This method produces ca 300,000 toz/yr. The process does not recover Au from AuTe. It is left untouched in the leach heap and constitutes ca 1/3 of the total gold present.

Curiously, during the many eruption cycles in the distant past (~32 ma), debris from the surface has washed back deep into the formation. Bits of woody debris have been recovered within cementitious rock hundreds of feet below the surface. The CC&V geologist showed a core sample with a wood fragment imbedded within it. For a time reference, the current episode of Rocky Mountains (the Laramide Orogeny) began ~65 ma.

Chemist Gaussling will blend in with a group of geologists tomorrow morning and take an extensive geology tour of the mine site. Hopefully, there will be pictures to share. We’ll be going up to ~10,000 ft, so it will be chilly.

LC Dreamin’

When I get to work this morning I’ll be greeted with a brand spankin’ new Agilent 1200 HPLC sitting on the bench in my lab. It has a diode array detector (no flippin’ MS this time). Pretty sweet.  Gosh, early 1990’s LC capability- already!

It is interesting how the installer assumed I’d be doing reverse phase work. Must be what most of the weenies in pharma are using. Carbon-heteroatom-carbon-heteroatom-carbon-heteroatom-carbon=heteroatom-carbon-heteroatom- … maleate.

Organic Symposium at CU

The 41st National Organic Symposium starts 7 June, 2009, in Boulder at the CU campus. I’m trying to decide if I want to go bad enough to pay the admission price.  The registration is rather pricey- $400-425, depending on your membership status. The symposium features a lineup of some of organic chemistry’s top rock stars and illuminati.

The whole fandango begins with a homily by Bobby Grubbs on what else? Metathesis. Good lord. I don’t think I can bear to see it again. I wonder if he’ll disclose the patented art during his talk? (These guys never point out that the cool and useful stuff is tied up in claims!)

I popped into a few web sites of the various rock stars who will be presenting. I noticed that Dale Boger is selling his lecture notes on-line for US$120 for a CD.  Fancy that.

Apparently, he is still working on Vinca alkaloids. Buried in the Boger website is a graphic showing the various and complex compounds that his groups have prepared. It is pretty amazing, really. But it is as much an indication of what generous funding and hordes of rabid post-docs and grad students can provide as anything else. Boger is listed as an inventor on 25 US patents (with Scripps as assignee) by my count. Scripps owns a bunch of Boger technology. I wonder if any of it is commercialized? I don’t know the guy, so I don’t want to be too obnoxious here.

If an advisor is patenting the work that a student is doing for her/his dissertation, how do they manage the notebooks (i.e., disclosures) and the meetings with the students committee? If the student is helping to develop IP for someone else, are they decently paid for it? Does the student have multiple notebooks for confidential and “public domain” work? What kinds of liability does a student have in terms of proprietary information after they graduate? Lots of sticky issues for a fresh graduate.

“Don’t Even Taste Like Sewage”

I spent 4 1/2 hours saturday touring our town’s water system from both ends. It was quite a detailed tour and, since it involved chemicals, how could I not tag along?

We began with the sewer reclamation plant first. Lots of interesting details here. Turns out that one of the big problems to running a waste treatment plant has to do with keeping large debris out of the pumps- rags, underwear, shoes, plastic parts, etc.  Once you get past the shock of learning what your fellow citizens can and do flush down the toilet, it is plain to see that a bit of money spent on screening out the the big chunks is returned in the form of reduced down time and pump repair costs.

Our little hamlet of 6,000 souls sends 450,000 gallons of waste water to the reclamation plant on an average day. The flow peaks at about 8 am every day in the form of a sudden 5-6 x increase in flowrate. It takes about 90 minutes for an average volume (i.e., a flush) of wastewater to get to the plant. A lot of groggy citizens hop into the shower at around 6:30 am.

After the incoming stream passes through a grit removing station at the entrance, it is lifted to the first treatment operation for aeration and fermentation. This is the physical high point in the process, meaning that the stream is subsequently transferred by gravity for the remaining process steps.

I won’t go into further process details other than to say that the final step prior to discharge into the stream is a sanitizing step where the effluent is exposed to a large jolt of UV radiation. At this point in our tour, the plant manager dipped a sampler into the flow and withdrew one liter of clear, colorless liquid with a few strings of algae floaters. Only too eager demonstrate his faith that the water was sanitary, he dipped a finger into the effluent, put it into his mouth and exclaimed with a grin as wide as his mullet

“It don’t even taste like sewage!” 

As he passed the sample around so others could share in the experience, I wandered over to the control panel and feigned interest in the LCD display. The UV just renders the wee beasties non-viable. Their little microbial carcasses are still there. Pathogen free it may well be, I didn’t have the stomach to taste it. Yes, I know that microbes are everywhere and that our notions of what constitutes “clean” are merely a fantasy. But I just couldn’t do it.

Beryllium Mining

The aerial view above shows the location of the Brush Wellman beryllium mine near Spor Mountain, Utah. It is reportedly the only major beryllium mining operation in the USA and one of the very few economic beryllium ore locations in the world. The host materal is called “tuff”- a compacted and cemented volcanic ash composition. Coincident with this Be deposit is low grade uranium and fluorspar. Occurances of Cu, Au, and other base metals can be found in the area.

The concentration of Be in the ore body is thought to be due to the mineralization action of meteoric and hydrothermal fluids. The region is marked by the presence of 3 Oligocene-era calderas, with the Spor mountain Be mineralization found along the ring structure of the Thomas caldera.

The action of hot, saturated aqueous flows transporting solublized components from distant host bodies is one of the chief mechanisms for the appearance of “ore bodies” near the surface of the earth. Very often, such deposits are found in regions of faults and fractures of various kinds of rock formations. Mineral laden water follows the fracture system and, as it moves toward the surface, begins to cool and deposits the burden of now insoluble compounds. Deposition can occur due to simple solubility properties, redox from exposure to atmospheric oxygen, or via ion exchange with available chemical species to form high Ksp compositions.

This is nothing new to geologists who have been aware of these mechanisms for generations. But for a non-geochemical chemist like myself, the matter of how elements like beryllium come to be concentrated is less than familiar. Indeed, the question of how any element comes to be concentrated in rock formations is a question of increasing interest to Th’ Gaussling. I hope to spend a lot of time in the future exploring this matter.

The Cresson Vug

The history of the Territory and State of Colorado is inextricably tied to base metals and precious metals. Gold and silver strikes were a big draw for the migration of population to Colorado from the 1859 Pikes Peak Gold Rush onward.  A map of the ore geology of Colorado reveals a few key districts or zones of enhanced mineral abundance. The Colorado Mineral Belt (CMB) is a band of ore deposits that are positioned diagonally across the middle of the mountainous part of the state, SW to NE, roughly from Durango to Boulder.

Other districts containing economically viable ore bodies exist outside of the CMB, notably the Thirtynine Mile Volcanic Field west of Colorado Springs. While rich deposits of gold were found near Central City and many other locations in the CMB, the relatively rare  gold/tellurium ore found near Cripple Creek and Victor on the periphery of the Thirtynine Mile Volcanic Field have provided approximately half of all the gold mined in Colorado. Gold has an affinity for tellurium and may be found combined with it in the form of the mineral calaverite.

In particular, the Cresson mine near Cripple Creek has been an especially rich producer of gold. In November of 1914, a 4 m x 8 m x 13 m cavity or “vug” at the 1200 ‘ level was found to be lined with gold telluride and other minerals.  Depending on which source you believe, it is reported that from 20,000 to 60,000 ounces of gold were removed from this small space.

The Cripple Creek volcanic complex is a highly altered, highly brecciated formation that has been described in detail elsewhere. The link provides a more detailed description and a bibliography.

Links updated 7/2/19.

Tuesday’s Select Linkography

Juan Enriquez talks about Homo evolutis. This is a TED video.

ARR Inc., is offering its Suparator (R) technology for separating an upper oil phase from water by means of a cleverly designed staged weir system. According to the product literature, the passive device collects, concentrates, and separates oil from flowing water. This widget uses Bernoulli effects to draw water from collection zones and top the upper phase over a final weir for isolation.

Admittedly, I have not kept up with the progress of wier technology, but to a non-engineer like myself, this seems pretty clever.

Suparator Diagram

Suparator Diagram

Energetic Materials Manufacture

Everyday in factories around the world, people manufacture energetic materials at the commercial scale. Yet we do not witness a continuous stream of reports describing industrial tragedies at these facilities. Plants for the manufacture of energetic compositions are often purpose built with many layers of protection (LOP) built-in. Such facilities may be constructed in remote locations and with assets separated by large distances.

What is telling about explosive chemical manufacturing is the extent to which the operators possess a deep level of knowledge of their materials and processes. The explosives industry has at its fingertips a wide variety of tests that assay certain manifestations of sensitivity.  There are many tests that assay for friction sensitivity and for shock sensitivity. Impact and electrostatic stimuli are also important dimensions not only for manufacture, but for use in the field.

For instance, a material with a high detonation velocity may have a large critical diameter, meaning that the packing density and bulk geometry must be sufficiently large for it to propagate a shock. Knowledge of impact sensitivity, shock sensitivity, or detonation velocity alone does not tell the whole story of the explosive.

There are several causes for this depth of knowledge. Easiest to see is the history of US explosives manufacture.  There have been many spectacular industrial accidents going as far back as the revolutionary war. Much has been learned about manufacture and handling at a very high cost to lives and property. The explosives industry has had to learn to develop safe manufacturing practices to prevent the loss of life and business interruption.

Another motivating influence for explosives safety is perhaps less than obvious to outside observers. Over time, the US military has been revising and modifying its munitions designs and specifications.  It is highly desirable that explosives and propellants provide maximum energy density for performance requirements, but at the same time be sufficiently insensitive to inadvertant stimulus so as to provide maximum safety for those handling the munitions.

The properties of military explosives- a major market driver- are highly specified by military procurement. The current library of explosive compositions have been highly refined through many years of evaluation and field testing. The effect has been that the compositions presently in the field are quite well understood in terms of their operational boundaries.

In addition to being driven by material specifications, manufacturing facilities and quality control systems are also driven by a selection process that is quite stringent.  We see fewer explosive plant disasters today not only because the explosives are safer, but also because plants are managed better.

The lesson in this for fine chemical operators is that depth of knowledge of materials and reaction mixtures can be highly desirable and potentially very useful. In particular, an intimate understanding of the behavior and sensitivity of materials under process conditions as well as off-normal conditions can lead to safer plant operations.

Seems like a “No-Brainer”. But the fact is that the activity leading to such knowledge can be difficult, time consuming, and expensive to obtain. The push to get product out the door can be irresistable and the urge to cut corners can happen quietly and without fanfare. It is very easy for institutional knowledge to be lost in the struggle to maintain output and profitability.

Fine chemical manufacturers can be hobbled in their understanding in other ways. On the producers side or on the users side of fine chemicals, it is not unusual for chemists to specify methods of analysis that are familiar to them. NMR or GCMS or a variety of wet chemical methods set up on the benchtop are commonly used to set specifications and to validate certificates of analysis. 

However, familiar methods of analysis tend to give profiles of familiar properties. Unfamiliar properties or contaminants may be invisible to any given method of analysis. A compound with a low threshold to decomposition or one that will exotherm vigorously and shed mass aggressively may reveal this attribute only through happenstance to an alert chemist.

What is especially interesting about explosives testing is the extent to which compositions are subjected to challenge tests. Rather than looking for a spectral signature, materials are subjected to a variety of stimuli in a manner that provides an unambiguous outcome. The card gap test for instance looks at the sensitivity of a composition to a standard stimulus that has been attenuated through a variable gap (set of spacers) of polymethylmethacrylate or air. Does it produce a hole in the witness plate or not?

There are people who go to work in nitroglycerin factories everyday knowing that they are working with a shock sensitive high explosive. Others may work in a lead styphnate factory filling primer cartridges by hand.

There are also people who go to work everyday in plants that have banned the use of diethyl ether or require peer review of even the simplest reaction they run in their fume hoods. The range of what is considered acceptable risk varies greatly.

Today, there is a mandate for IM- Insensitive Munitions. Here is the scenario- a TNT filled projectile is impacted by a large caliber projectile or shrapnel. There is a good chance the stimulus provided by the impacting body will initiate the TNT and cause the charge to explode, causing death or harm to those in the area.  It is desirable to have high explosives that detonate or deflagrate only when properly initiated.

A major push is being made at government and industrial labs to produce explosive compositions that are insensitive to inadvertant stimulus, yet energetic enough to perform the task.  One desired end of this activity is to phase out TNT in military explosives. The lack of US manufacturers of TNT is nearly as important a motivating factor as the sensitivity issues are. From the industrial hygiene side, some workers reportedly become sensitized to TNT, so the elimination of this toxicological dimension is desirable as well.

Green munitions are also part of a phase change in the munitions field. At first blush it seems silly to make explosive devices more environmentally friendly. However, explosive chemicals and their decomposition products can be widely dispersed in the environment as the result of warfare and training. The reduction of toxic residues can be considered a reduction in collateral damage.