Welcome to the first edition of Rock, Metal, and Water: Le GEM Blog! I am excited to
begin this new endeavor as a blogger chronicling the exploits of the GEM lab at
Central Michigan University. My name is Dr. Meghan Wagner, and currently I am a
postdoctoral researcher working with Professor Anthony Chappaz. I earned my
bachelor’s and master’s degrees in chemistry, and last year I completed my
Ph.D. in earth and environmental sciences. Having a background in both
chemistry and earth science allows me to act as a bridge between the two
sciences, and—I think—to look at earth science problems in nontraditional ways.
My personal research interests involve trace metal geochemical cycling,
climate, and the relationship between ocean circulation and oxygen concentrations
in the deep ocean.
The purpose of this blog is to give all of my readers an
insider’s view of what happens in an academic research laboratory, and what the
life of one postdoc is like. Each Friday, I will share our successes and
failures, bring my readers along for fieldwork and conferences, and try to
bring some clarity to scientific concepts and instrumentation that we will run
across. Above all I want this blog to be widely accessible and fun to read! I
am sure that my writing style and skill will improve with more practice, and so
I ask that you, my readers, please contact
me with questions, comments, and suggestions for things that you would like me
to blog about.
I hope that you will take a few minutes to explore the GEM
lab website to learn more about the people, our research interests, and
facilities. Briefly, we are aquatic geochemists interested in trace metal
chemistry. In other words, what are the trace metal concentrations in aquatic
waters and sediments? What can trace metals tell us about nutrient cycling,
primary productivity, oxygenation, and pollution? How and why are trace metals
preserved? How are trace metals transported through aquatic and terrestrial
systems?
And what are trace metals? Trace metals are metals present
in small quantities—around the part per million (ppm) or part per billion (ppb)
level. Usually this means transition metals, also known as d-block elements.
There is a wonderful website www.webelements.com
that has a wealth of information about all of the known elements. The
transition metals are the ones colored in pink. Some of these elements are
probably known to you, such as zinc (Zn) and copper (Cu), while others may be
unfamiliar, such as scandium (Sc) and ruthenium (Ru). In human physiology,
elements like zinc and copper are essential micronutrients. The same is true
for other organisms—more on this later.
In our laboratory, we are especially interested in the
interaction of the metal molybdenum (Mo) with dissolved organic matter (DOM). DOM
is a complex mixture of naturally occurring organic molecules. The size that
constitutes “dissolved” is not universally agreed on, but one common definition
is anything that will pass through a 0.45 micrometer filter. For comparison,
human hair is approximately 80-100 micrometers wide. So we are interested in very
small things! Last Friday Anthony and I went out to the field to collect some DOM for
our experiments. Here in central Michigan, we have recently had a lot of rain,
which has washed organic matter produced by trees and other plants into the
Chippewa River. So that day “the field” was a local park. Here I am collecting
river water into a carboy.
Yes, that’s right: For my job, sometimes I get to play in the river. Neener neener, desk denizens! Afterward we brought the river water back to the lab and filtered it to remove the large particles. Here you can see the filtration in progress and what we collected on the filters.
The carboys are sitting in black plastic trash bags to protect the DOM from light. This is because some DOM is broken down by light (photodegradation), and we want to preserve our sample. The next step was to concentrate the DOM using a reverse osmosis system built in-house by one of our lab volunteers, Jacob Spreitzer. Here is the reverse osmosis system and the concentrated DOM sample (on the right, clean water on the left for comparison).
After a resin treatment to remove metals bound to the river DOM, we have a DOM sample ready to use!
Yes, that’s right: For my job, sometimes I get to play in the river. Neener neener, desk denizens! Afterward we brought the river water back to the lab and filtered it to remove the large particles. Here you can see the filtration in progress and what we collected on the filters.
The carboys are sitting in black plastic trash bags to protect the DOM from light. This is because some DOM is broken down by light (photodegradation), and we want to preserve our sample. The next step was to concentrate the DOM using a reverse osmosis system built in-house by one of our lab volunteers, Jacob Spreitzer. Here is the reverse osmosis system and the concentrated DOM sample (on the right, clean water on the left for comparison).
After a resin treatment to remove metals bound to the river DOM, we have a DOM sample ready to use!
So long for now! Next Friday will be very exciting because I
will be writing from the Advanced Photon Source
at Argonne National Laboratory where Anthony has been awarded beam time.


These pictures were useful as I built a lecture that included a bit about DOM. Please keep posting more material like this, I always forget to take pictures in the field.
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