Going to have to re-examine Socrates…

Figuratively speaking, of course, since he’s dead and all…

Man, Descartes so far is a serious disappointment. He seems to have an almost Dickensian tendency to verbal puffery (though thankfully the Descartes “Meditations” are much smaller than the big sack of tedium that was “David Copperfield”). It’s like he’s developed an unwholesome lust for his own thoughts and can’t keep his metaphysical hands off of them.

You’d think a guy clever enough to come up with “The Cogito™” could do better.

When I heard Descartes described years ago, I’d heard he started with “I think, therefore I am” and then from there proved the existence of The Supreme Being somehow. While I didn’t expect an unquestionable Proof, I did at least expect to see some spectacular theological philosophy taking place.

Instead, I (metaphorically, of course) show up at Descartes’ intellectual feast expecting some unique and exotic fare, only to see Descartes rummage around in his kitchen to come up with an old, freezer-burnt old package of leftover AquinasAnselm (oops), which he spottily defrosts in the consumer-grade-microwave of his argument. Bah. Not even worthy of dirtying my mental spork on. (There, do I sound arrogant enough to be an old-school philosopher myself yet?)

In other news: Celebration time! I’ve advanced all the way from 1st loser to 3rd loser! WOOHOO! It’s a bit of a jump to get up to the next tier (blogs getting an average of around 50-100 votes/day) but I can make it…

I’m an interdisciplinary nerd…

Oh woe! Oh woe! Last time I checked, I was dead last on the College Scholarship Blogging Competition! Now, as I’ve mentioned elsewhere, I may be a cynic but I’m an optimistic cynic, and therefore think that surely if I apply my full mighty nerd powers, I can figure out what’s wrong and fix it.

First, what is going wrong? I thought for a while, and came up with a few possibilities:

  • God Hates Me
  • God Loves Me And Wants Me To Win, But Doesn’t Exist And Therefore This Does Me No Good
  • The divine is not involved, but there is a conspiracy against me involving the CIA, the NSA, the BATF, The Teamsters, the Freemasons, and the World Aquaculture Society.
  • Blatant Age Discrimination by a bunch of dang whippersnappers (Git offa my lawn!)
  • Dang Yankees
  • Perhaps my young and under-promoted blog is simply still too obscure and not well enough established to have the large number of connections that older and better-promoted blogs have, and this is just a natural result of more popular blogs being able to get their “vote for me” message out to more people, who in normal human fashion will vote for the blog with which they are most familiar.
  • (Hey, I was brainstorming, so even crazy ideas like this were considered…)
    Then, finally, the problem became obvious to me:

  • It’s too much work to vote for me

It’s so obvious now! Hordes of adoring fans are coming out of the metaphorical woodwork and going to vote for me, but are becoming exhausted and collapsing before they manage to find my name, buried near the bottom of the list of 20 different blogs!

You may not realize this, but I’m back in college because I’m trying to start my life over. I may be microbial biotechnology nerd now, but in my former life, I was a professional computer nerd for 15 years. My amazing nerd powers are therefore being applied to solve this problem (see also the update at the end of this post):

There – one click on the image (aw, look, Cornelia wants you to vote for me!), click the confirm button that pops up, and you’ve voted for me. Problem solved. When clicked and confirmed, a new window should open and you should see the current standings. If you are presented instead with an unselected voting form, it didn’t work – let me know. Now go! Go, my fellow conspirators! Click us to victory!

But seriously – I may yet come up with a way to gain enough fame quickly enough to have a shot at the prize, but right now I’m in last friggin’ place…which means I’m free! I don’t have to worry at all about “oh, gosh, if I do that will I lose the crucial vote that loses me first place?!?!?” and I can pretty much do whatever I want, within the bounds of ethics and legality, and it’ll make no difference. Therefore, I want to point something out:

Down at the bottom of this post, you’ll see that this material is made available under a Creative Commons license. Basically, as long as you’re not a commercial venture and you give me credit, you’re allowed to take and use anything you like from here, including taking and remixing the one-click-vote thing there. And, yes, this explicitly applies to my competition (Money or no money, I really can’t imagine how a scholarship competition counts as “commercial”.)

I’ll even go one step further: if any of you other finalists happen to see this and would like to use this on your own blog, let me know and I’ll send you a version tweaked to vote for you blog instead of mine. I’ll even try to help you get it inserted into your blog if you’d like. All I ask is that you mention and link to my blog somewhere in one of your posts. Obviously I’d prefer something complimentary, but if you feel the urge to write “I hear that Sean at The Big Room rapes puppies, eats babies, and has an unnatural attraction for maple trees”, what the heck, as long as there’s a link…

What do you think? Good idea? Bad idea?
UPDATE: Dangit, I swear it looked like it was working yesterday, but the ‘one-click’ (plus confirmation) thing is unexplainably just not getting the vote in, though everything else was working correctly. For the moment, I’ve reverted to having the link bring up the official vote form in a separate window…

The offer to make it available to others still stands, however, if anyone’s interested. I’ll re-revise this post if I figure out how to get it working.

Do Not Taunt Happy Fun Park

Here’s a brief interlude for my new readers. Members of my immediate family have seen this before elsewhere, but what the heck, I may as well share with you all.

Related to my recent posts about this year’s field-trip to Yellowstone National Park, I am reminded of a trip my wife and I took last year to Norris Geyser Basin in the same park.

I’ve heard of “communing with nature”, when the natural world seems to speak to you and put you at ease. Well, on this occasion it didn’t just seem to be speaking to me, and it hardly put me at ease. The conversation between me and the park went something like as follows that day. (Forgive all the scrolling, it WAS a several-hour conversation after all. If it bugs you, feel free to say so in the comments…)

Sign:No Restroom in Geyser Basin

Well, okay, I don’t smoke, I didn’t bring a bicycle, we left the dog at home. And I guess we can hold it until later. It’s a small price to pay to go out to nice, happy, peaceful trails, away from, for example, all the annoying road construction.Traffic cone, in the middle of the trailWow! Look at that! Do I spy the Fruiting Body of the rare Yellowstone Giant Orange Holewarning Mushroom?!?!?No, wait…that’s just a traffic cone over a hole in the trail! What the heck? I thought I was getting away from road construction!

Well. Maybe things will get more natural-looking once we get a chance to walk off into the wilderness. Maybe the map’ll show where we can go.

Map of Norris Geyser Basin, with Warning to Stay On Designated Trails
Ah, look at all the lovely trails. Plenty of space to roam around in.
What? I can’t leave the trails?
sign:Stay On Designated Trails

Can’t I take a mere step or two off? Just a little bit???

Sign:Stay on TrailSign:Stay On WalkYeah, yeah, whatever. What are you going to do if I don’t – have me arrested?

 

Sign:Unlawful to Leave Walkway
What kind of criminal act could possibly be involved with just leaving the silly walkway? Littering? Vandalism?
Sign:It is UNLAWFUL and UNSAFE to: Leave the walkway in thermal areas or throw objects into or deface thermal features

Oh, come on! Look, there’s a beautiful green pool over there, full of no doubt fascinating little animalcules. Can’t I just go over and take a little look?

Sign:Keep Off - Thermal Area
“Thermal Area”? What the heck is that supposed to mean? It’s a little windy and chilly today, maybe I want to be warmed up a little. So, why not? What’s so bad about a “Thermal” area?

Sign:Hazardous Ground - Thin Crust - Boiling Water

What’s that supposed to mean?

 

Sign:Dangerous Ground -with illustration of kid falling into ground and getting broiled-
Children are prone to explode out of the ground unexpectedly?Walkway shown crossing the top of the steaming opening of Green Dragon SpringWhat the heck? Is Green Dragon Spring actually devouring the ground under that walkway?!?! Oh! I get it – you’re saying the park itself can swallow you up and and cook you?
So everything here is flaming hot death, then, right?

Sign:Warning: Trail My Be Icy

Is there no end to the dangers this place threatens innocent visitors with? Can there possibly be anything else this park can do to us?!?!?

 

Solfatara: Very Dangerous Landscape spewing Sulfuric Acid Gas!
“Thin Crust”? “Boiling Water”? Broiled flesh cooked in acid? Ice?
Is this a park, or the kitchen at a Chinese restaurant? Is this how “Hot and Sour Soup” is made?!?!? Is there nothing that can stand in this realm of violent burning chemical death without fear!?!?!?
Fearless Geyser

But what of us poor, fragile fleshy people? We aren’t safe here!That does it! I’m getting out of here! No more of these horrible Killer Thermal Death Areas of Doom for me! I think maybe I’ll just go look at the nice cuddly animals that Yellowstone is also famous for.
Sign: Caution - Wild Animals are Unpredictable and Dangerous!
This whole friggin’ place wants to gore, dismember, maul, cook, devour, and digest me! That does it. No more of this dangerous stuff for me – I think I’ll just go read a nice book for a while…
Bookstore:Closed
NOOOOOOOOOOOOOOOOOOOOOoooo!!!!!!

Yatta! I Fail to Reject the Null-Scholarship!

(Oops, got so excited I got carried away with the title. Fixed now.)

I am thrilled to notice this morning that I am in the running for the College Blogging Scholarship, honestly, if this even attracts a larger population of active readers, I’ll consider that alone an excellent “Runner-Up” prize.

Not that the scholarship money wouldn’t be much appreciated…but more about that later.

For the moment though: Hello, current and new readers, to the internet’s self-proclaimed foremost authority on Expired JellO, among other things. I suppose that since I’m asking people to vote for me, I should probably give a quick description of myself and this blog. I’ll keep it short for the moment:

My actual name is Sean Clark; the explanation for the “Epicanis” handle deserves a post of its own. I am a “non-traditional” student at Idaho State University, working on finishing my long-overdue B.S. in Microbiology. This is actually the 5th college institution I’ve attended. It’s not that I’ve been kicked out of the others or anything, just that I keep having to move and start over. I’m finally in one place here long enough to actually finish the degree. Where I end up doing my graduate work depends on where (and if) we end up moving next year – I’ll post about this if anybody’s interested.

My primary interest is in “applied” microbiology, particularly non-medical biotechnology. I’ve been convinced for many years that non-medical applications of microbial biotechnology are underappreciated and somewhat neglected, and I’d rather people not have to get sick before they can benefit from whatever I might come up with…

Incidentally, Hillary Clinton agrees with me (“we should increase investments in non-health applications of bio-technology” – see paragraph 23). Whether that helps or harms my position no doubt depends on your political opinions, but still, I appreciate that someone with some kind of official authority agrees with me. And, hey, maybe this means I’ll be able to find a decent job during or after graduate school. Anybody think the Office of Technology Assessment will be hiring again soon?…

This blog itself is primarily concerned with sharing some of my education, and science in particular, as an exercise in communicating science. I, for one, think I’ve gotten better as the blog has progressed.

A couple of important points: This is a blog, not a magazine: participation is encouraged. If nothing else, the voting for the scholarship looks like it goes on for a couple of weeks, so if you are thinking to yourself “Gosh, I’d vote for you, but you don’t talk enough about X” or “you talk too much about Y” or “I hate the background color of the webpage” or whatever, now’s your chance to speak up. You do not need to be logged in to comment (but I do screen comments, so spammers: you’re wasting both your time and mine), so please do. Also consider subscribing to the RSS feed, found in the upper-right area of the page.

I try to update at least a couple of times each week, though lately I’ve managed to maintain a nearly daily pace. Participation helps here, as comments from readers helps me come up with additional topics to post on. I’m getting a lot of enjoyment out of blogging, so I’ll post as often as I reasonably can…

One last quick note on using this blog: I try to put title tags on most special bits of posts, like images and links. And…bits of text like this, which you might think of as “inline footnotes”. If you hover over anything with that thick-dotted-underline, you should see some additional information. As of a week or two ago, if you click on them, the entire extra text will pop up in a separate box where you can read it all, assuming you don’t have javascript turned off. I haven’t yet gotten around to going back and doing this to the previous bits like this, but I will eventually.

So, again, welcome. Comments, questions, and suggestions will help me improve the blog, and are therefore strongly encouraged. Oh, yes, and please vote for me. Otherwise, I’m going to have to resort to selling blood plasma and begging outside of scientific conferences. Thanks.

Libel! Blasphemy! Slander!…

Injustice! Perfidy! HUMBUG!

Periodically, someone puts up a “could you pass a grade-school science class” quiz. The one linked to the image below goes to one that I just broke down and took, purely out of curiousity. Take a look at this outrage!:

JustSayHi - Science Quiz

Oh, sure, it LOOKS good, but what you don’t see is that it only gave me a 96%, implying that I missed one (it was a short quiz)! Sure, the quiz was very much in the modern fashion for “standardized testing” (aka the “No Child Left Awake” project) where the emphasis is on memorizing stuff for a test rather than actual comprehension. So, I thought, maybe I hadn’t correctly memorized which word was correct for one of the word-memorization questions. But, no, according to the “answer sheet”, the one I supposedly got wrong was this one:

(Note: If you’re planning to actually take that quiz, do so now before you read on and I give away one of the answers…)

“How do mammals respire?”

The options were:

  • Aerobically
  • Anaerobically
  • Both aerobically and anaerobically

Come on, I may hardly ever concern myself with perverse eukaryotic systems but…never mind just “mammals”, as far as I know, all eukaryotes (animals, plants, and fungi) only possess aerobic (oxygen-requiring) respiratory systems.

However, the “answer sheet” for the quiz claims that the answer is “Both aerobically and anaerobically”.

So….they’re wrong. I’m pretty sure what what they were intending to ask, given this answer, is “what kind of metabolism do mammals have?”, in which case their answer is correct.

See, “respiration” is only one part of the cellular energy-generating system. Specifically, it’s our friend, the Electron Transport Chain, which (to grossly oversimplify) harnesses the energy of oxygen sucking electrons off the end of the chain various biochemicals to recharge molecules of ATP. That’s not the only way a cell can get ATP, though. What the quiz authors are presumably alluding to is that there are non-oxygen-requiring biochemical pathways that animal cells can take to make energy – such as the one your muscles use when they can’t get enough oxygen, which involves production of lactic acid, which in turn gets blamed for the “burn” sensation you get when you work your muscles hard.

So, the authors of this quiz are bad, bad people, besmirching my reputation and harming my precious self-esteem by giving me less than 100% on that quiz!

On a related subject: breathing causes cancer in Sprague-Dawley™ rats!

No, seriously, it’s true – try raising one group of Sprague-Dawley™ rats with air, and one group with no air, and examing both populations 150 days later. I guarantee you’ll find many more cancerous growths in the “with air” group than in the group that was denied air to breathe…

What brought this outburst on? It was this blog article. “No, It’s for Real: Aspartame Causes Cancer”, the post proclaims. They’re talking about This study(pdf). Go ahead, take a look, but in particular, look at the tables of actual data, not the paper’s abstract. In particular, take a look at Figure 1, especially “D” and “E” (showing survival rates for the different groups of Sprague-Dawley™ rats as the study progressed), and at the number of “tumor-bearing animals” in Table 2.

Notice that at around 120 days on the survival graphs, the groups with the highest percentage of members still alive were the groups receiving the most aspartame in their feed. It’s worth noting that the highest-Aspartame group there was getting roughly the equivalent of a human drinking <em>thousands</em> of cans of diet soda every day. Also note, in fairness, that both graphs seem to show little difference between the groups, so rather than assuming that Aspartame makes Sprague-Dawley™ rats live longer, I would tend to assume that there’s really not much difference.

Notice also that in terms of the percentage of Sprague-Dawley™ rats that developed one or more tumors, there were fewer of them in the group that got the equivalent of 500 mg/kg of aspartame: which scaled up to human terms means about 200-250 cans of diet soda EVERY DAY worth of aspartame.

You may be wondering why I keep mentioning Sprague-Dawley™. It’s because this is a particular commercially-bred strain of rat that’s popular with labs for this kind of thing. One point that isn’t always mentioned is this: Sprague-Dawley™ rats are known to be prone to developing cancer spontaneously. This can be handy if you’re doing studies of “borderline” carcinogens. The hope is that if something has even a tiny ability to cause cancer, you’ll be able to measure the effect in a population of critters known to get cancer at the drop of a metaphorical hat, when in a human population the incidence might be so rare that you can’t distinguish it from random chance. To my admittedly-not-big-on-the-biochemistry-of-perverse-eukaryotes mind, this study really seems to show that there’s little or no effect – and certainly no dose-dependent effect – of aspartame even on cancer-prone lab rats.

I don’t know what it is, but “artificial sweeteners”, and especially aspartame, seem to generate such passionate hatred in some people. It reminds me a great deal of people’s reactions to “genetically modified” crops. People just really want to hate it. The authors of this paper are obviously trying REALLY hard to show somehow that aspartame is a dangerous poison, despite the inconclusive-appearing actual results. Though I suppose one could argue that they showed Aspartame to be at least as much of a deadly poison as Expired JellO®.

And now that I have exposed my readers to several times the Recommended Daily Allowance of Humbug, I bid you all a good night – I have Art History and Philosophy to attend in the morning…

Environmental Chemistry Field Trip – Day 1, part 3

Overview of Narrow Gauge Spring
Our final destination of the day was Narrow Gauge Spring, which is on the backside of the Mammoth Terraces area. Apparently, there’s only one other place in the entire world – somewhere in China – that has exactly the same kind of conditions as this place.

The process of making this kind of formation requires rainwater, healthy microbe-supporting soil, limestone, and heat. It goes something like this: rainwater seeps down through the soil, where lots of healthy microbial activity uses up the oxygen in it and excretes plenty of extra carbon dioxide into it, making it more acidic. The water sinks into the ground and runs into the limestone, which is Calcium Carbonate (CaCO3). Calcium Carbonate doesn’t dissolve well in plain water at all, but there are two things that make it dissolve better: acid and heat. The heat from the magma under the park and the acidity of the water combine to dissolve a whole lot of the limestone. Then, somewhere, the heated water gets forced back up to the surface through a crack.

Where the water comes back in contact with the air, it can let off the extra carbon dioxide and heat. This doesn’t happen very fast in a deep pool, since this can only happen in a thin area near the top. Where the water overflows, though, it’s very shallow, and the carbon dioxide and heat can escape very quickly into the air. This makes the water suddenly become less acidic and less hot, and all that extra calcium carbonate can no longer stay dissolved. It crystallizes, making a hard calcium carbonate “shell” along the edge of the pool. The edge can end up growing some much over time that it forms an overhang with stalactite-like formations underneath it:

Another view of Narrow Gauge Spring

You can just make out an overhanging area in the upper-left of the photograph.

It was fun taking measurements of the water here. Water freshly removed from a pool initially showed up off the scale on our “Total Dissolved Solids” meters, but if you waited a few seconds the reading would drop down to where the meters could read it, and keep falling. Out of the pool, the water was cooling off quickly enough that the extra dissolved Calcium Carbonate was un-dissolving out of the water in tiny bits even as we stood there.

The water appeared to be about 56°C at the top of the pool where it was initially emerging. If you want an idea of not only that I am a nerd but what kind of nerd I am, I will mention that I think of this as “stewpot temperature”, and often wonder if there is any useful or tasty effects to be discovered in the microbial processes done by thermophilic microbes that live in these conditions. I’ll find out one of these days…

Oh, and a couple of bits of trivia about the Apollinaris Spring area from a couple of posts ago. Firstly, it was apparently named after a spring in Germany with the same name. Secondly, we briefly discussed the chemistry of carbon dioxide in water in class this week, and it turns out that the pH of 5.9 that Apollinaris Spring has is probably more basic than plain distilled water would be.

Now, anyone who’s had basic chemistry is probably a little baffled by this – after all, isn’t a pH of 7 that of pure water by definition? The answer is yes, but we’re not talking about pure water, we’re talking about water exposed to the air, where carbon dioxide can dissolve into the water. Working through the mathematics involved showed that distilled water should end up with a pH of about 5.6-5.7, at least at “standard temperature and pressure” (roughly sea-level air pressure and a temperature of around 72°F.). I have a suspicion as to why the Apollinaris Spring water seems less acidic than I might have expected, though.

They actually took our Apollinaris Spring water and ran it through an analytical instrument of some kind (I wasn’t there for it, but the description of the results made it sound like it was a “liquid chromatography” type of device). They found NO nitrates or nitrites in it. Since we’re talking about spring water percolating through healthy soil, I would have expected some nitrogen. I noticed, though, that although they checked for nitrite and nitrate, they didn’t check for reduced nitrogen – that is, ammonia.

I managed to score a tiny vial of the water during lab last Wednesday. When I get a chance to hit the pet store for some ammonia testing supplies, I’ll check that. If it’s there, it might explain the possibly slightly higher than expected pH. Similar to what happens to carbon dioxide and water, when ammonia (NH3) is dissolved into water(H2O), there tends to be some recombination of the atoms to make “ammonium hydroxide” (NH4OH), which is basic.

I don’t know if that’s what’s going on, but I intend to check.

There’s one more post worth of Field Trip stuff, and then I’ll be back onto other topics. Here’s a hint of what might come up, though: can anybody tell me what the effective pore size of pectin and cornstarch gels might be?…

Environmental Chemistry Field Trip – Day 1, Part 3

There were two more stops on the first day of the field trip. After Appolinaris Spring, we stopped off at the “Sheepeater Cliffs”, named after the local natives’ use of mountain-goats for food. I did get a picture of the small cliff, but who cares. You’ve seen one columnar basalt formation, you’ve seen them all, right?

Oh, well, in case you haven’t seen even one yet, here’s one:

Columnar Basalt Formation: Sheepeater Cliffs, Yellowstone National Park

It’s actually kind of interesting – despite the fact that Yellowstone is essentially one gigantic crater left by a volcano explosion, lava doesn’t seem to be a common feature at all. The reason seems to be that the volcanic explosion was an explosion of steam, not melted rocks. Put simply, water seeps down into the ground and gets trapped on top of magma, which is naturally extremely hot. The water can’t boil away as steam, though, because it’s trapped under all that rock, which keeps the pressure high enough that it stays liquid even when it’s superheated. Then, one day (about 600,000 years ago, if I remember correctly) somewhere a crack opened up enough to start letting the water flow out. When it got out from under all the rocks, the reduction of pressure let the superhot water suddenly explode into a cloud of steam. As the water shot out as steam, it let off some of the pressure on the water still trapped underground, which could then also explode into steam….and the whole area got flung into the air on the exploding, superhot steam. Kind of like the way a perfectly innocent looking bottle of heavily carbonated beverage can suddenly erupt in a spray of bubbles if you open it too suddenly.

Or at least, that’s my I’m-not-a-Geologist understanding of the process. The point is, melted rocks aren’t really a big part of the park area’s surface, so it’s interesting to see the basalt cliffs here. The giant hexagonal columns are actually huge crystals of that formed as the melted rock solidified.

This was just a brief stop, though. We piled back into the field-trip vehicles and headed for the Mammoth area of the park. I was originally going to cram that stop into this post, too, but I’m still editing it down to make it less pedantic. Unless my Vast Horde of Loyal Readers would LIKE pedantic…

Incidentally, the College Blogging Scholarship submissions are done as of midnight tonight. Or midnight tomorrow morning, depending on whether you think of midnight as the end or beginning of a day. Finalists get announced on Monday. Here’s hoping I’ll be one of them. That also means that if anyone has any suggestions or comments about how I’m running the blog, the topics I’m picking, and so on, now would be a good time to speak up…

Meanwhile, a couple more posts on the field trip coming up (possibly another one later today) and then I’ll move on to other topics.

Environmental Chemistry Field Trip – Day 1, part 2

Our next stop was Appolinaris Spring, which seems to be an uncommon thing in Yellowstone National Park: ordinary springwater. No sulfuric acid, no steam, just plain old water that sinks into the ground and then comes back up later. For most of the park’s history, it seems like this used to be a popular place to stop to get a drink of water.

water emerging from small copper pipes
Although the signs around the spring now all suggest that you really shouldn’t drink it, at least not without filtering it first, I’m kind of kicking myself now for not having tasted it. Perhaps I’ll have to go back on my own time and try it.

Our on-site tests showed a pH of 5.9 (slightly acidic: milk is normally around 6.8 or so, Root Beer somewhere around a more acidic 4.0, cola beverages around 3.0, for reference…), relatively low TDS of about 100ppm, coming out of the ground cool (about 7°C, or 43°F), with very little dissolved Oxygen (about 6.0ppm) and faintly carbonated (300ppm CO2). It reportedly didn’t taste too good, but having foolishly missed out on tasting it, I don’t know why.

There were hints that perhaps contamination from surface water – like rain trickling through bison poo – but quite some time ago they sealed the spring up to protect it from that kind of thing. This is the actual spring now:

Appolinaris Spring is a concrete box in the ground with locked metal tops...
Even so, the signs still try to discourage people from drinking the water coming from the pipes that lead out of the spring, which I take to be the park service covering themselves just in case someone claims to get sick from it. (“Hey, we TOLD you not to drink it!”).

Appolinaris: This spring water has been used by visitors since early days of the park.  However modern water tests show periodic contamination.  Park waters, even though clear and running are subject to pollution by wildlife.  As with all untreated water, purify before drinking.
Periodic pollution by wildlife? What the…

The northern end of a south-bound bisonOh, right. Natural bottled-spring-water flavor. Hey, it’s natural, it’s got to be good for you, right?

And to end this post on a complete and totally baffling non-sequitur: the student lounge I’m sitting in right now has a television constantly tuned to some cheesy mass-media channel. Today it’s “E!®”. I overheard something on it just now that made me sit up and take notice: Evidently “Leprechaun” made a profit. Wow.

One never knows what kind of amazing things one might learn at college…

Environmental Chemistry Field Trip – Day 1, part 1

I can think of a number of things to complain about with regards to living where I do. However, it is nice that we live near enough to Yellowstone to day-trip there. In fact, it’s close enough for my local college to take field-trips there – which we did.

Environmental Chemistry spent the weekend there, examining the area, discussing the chemistry of the natural waters and geothermal features, and collecting samples (yes, we had a permit for this…).

We started with a stop by the side of the Madison River to collect a sample of the surface water. Clear, cool (12°C, or about 55°F), mildly basic (pH of about 8.0), and a TDS reading of about 300ppm, which is roughly the same as mildly to moderately hard tapwater, I suppose.

sampling water from the Madison river

The sampling device -seen being hurled over the water here – is kind of interesting – it’s a hollow tube (a bit of plastic pipe) with two spring-loaded balls that slam shut on either end to trap the water inside when you tug on the string. That lets you throw the device out and trigger it when it gets to the precise spot that you want to take a sample from.

We made a brief stop at Beryl Spring afterwards. We didn’t do any sampling here, but we did talk about acid-sulfate water systems. “Reduced” sulfur – as Hydrogen Sulfide gas – comes boiling out from underground along with steam, and ends up being oxidized by oxygen from the air to become sulfate in the end – combining with the water and forming sulfuric acid.

Sulfur-encrusted pipe at Beryl Spring

Of course, it doesn’t go from sulfide to sulfate all at once. There’s a stop along the way as elemental sulfur. The whitish-yellow stuff here is crystals of elemental sulfur. The black stuff you see is…also crystals of elemental sulfur. The difference is just how the atoms of sulfur collect together. The black form is actually a little less stable than the yellow, so it tends to form first, but then slowly convert to the yellow form over time as the sulfur atoms settle into a more stable arrangement. Being a chemistry class, we didn’t really discuss the possible microbial activity that might be involved here. Note the small patch of dark-green there. I suppose this could be a “Green Sulfur Bacteria“, which does something like photosynthesis except that it makes sulfur instead of oxygen in the process. These are normally anaerobic but perhaps the concentration of hydrogen sulfide (H2S) and carbon dioxide gas coming out of the ground right there is enough to crowd out the oxygen. Alternatively, it could just be a heat-loving cyanobacterium or something.

I really wish I wasn’t too poor to buy a good field microscope to go along with the good lab microscope that I am also too poor to buy…

The last two stops of the day – Appolinaris Spring and Narrow Gauge Spring – will be in the next post…

This weekend should be worth at least one decent post…

This weekend, one of the two of this semester’s classes that I have not yet used for a “what I learned in school today” post took a field trip.

Yes, Our “Environmental Chemistry” lab went to Yellowstone National Park and (legally – we had a permit and everything) did some water sampling. We got some on-site lectures about the types of water systems in the park, considerations involved in sampling things, and so on. All in all, I thought it was pretty interesting, but after spending the entire weekend either driving to or from the park or walking around in the park I’m a bit exhaustipated. Plus, bummed out that I can’t afford a good portable field microscope to go with the regular microscope which I also can’t afford. Woe unto me. I imagine the permit we had would have allowed me to also dangle some slides in the water to look at.

I did record a GPS track of both days field-trips, I got ICBM addresses for our sampling sites, and a number of photographs with my cheap and ancient digital camera along the way. Give me some time and I’ll get at least one real post out of it.

Meanwhile, a bit of trivia: “The Microsoft Network” search system is pretty Fupped Duck. I do get the occasional obviously relevant hit from one of their searches, but the great majority seems to be “hits” from random one-word searches, many of which seem to refer to words that appear nowhere on the site (and others of which are so broad I have no idea how many pages some MSN user would have to click through before hitting my site. For example, while I like to think I’m making a reasonable effort to do interesting science blogging, I’m having trouble imagining that this blog would show up in the first few pages for a search consisting solely of the word “science”…which one of the recent hits seemed to show.

Actually, this probably has less to do with users than with Microsoft itself – the hits for this don’t appear to be loading real views (it pulls one page and doesn’t reference, for example, images) though it is coming from “The Microsoft Network” addresses. Perhaps Microsoft has one of their bots masquerading as a real user (the user-agent string looks like regular “Internet Explorer 7″)…even the IP address resolves to a bogus name ” bl2sch1082217.phx.gbl.”, for example) which doesn’t resolve back the other way. Of course, it’s also possible the hit is ENTIRELY bogus and the “referer” tag that seems to indicate this is also faked. Perhaps it’s time to start blocking Microsoft…or maybe just messing with them. This apparent standards abuse and obfuscation of what exactly it is that they’re trying to do with my blog (and messing up my logs!) kind of bugs me. (Moral of the story is probably “Everybody should just use Google“…)

Sure “Cardboard Sarcophagus Instructions” is a pretty weird search, too, coming from Google, but at least I know why THAT one got here. I doubt the searcher – possibly from the Memphis, Tennessee area – was really searching for metaphors for expired JellO boxes.