I am very happy that Xiaodan has successfully defended her PhD. It has been a pleasure to work with her over the past years. Xiaodan’s research topic was on the effect of lake N fixation on watershed N export. I still remember when she identified the question. We were looking at cyanobacteria from the Charles River under the microscope. Xiaodan noticed quite a few heterocysts (N fixing cells) in Anabaena. I initially dismissed this as unimportant, because the Charles River is generally believed to be P-limited (thats another point to discuss sometime). Anyway, she said, OK, but what will happen to all that N when it discharges to Boston Harbor and Massachusetts Bay? That was the initial question that eventually developed into a PhD thesis. Congratulations, Xiaodan!
Wednesday, December 3, 2014
Thursday, November 6, 2014
NEWEA Microconstituents Conference Report
Last week, I and several students in my Surface Water Quality Modeling class attended the NEWEA Microconstituents speciality conference at Bentley University. Microconstituents (aka emerging contaminants, pharmaceuticals and personal care products) are an important new problem we face as environmental engineers and this conference provided a good introduction to this topic. I made a presentation entitled “Where the Pipe Ends: Antibiotics and Antibiotic Resistance in the Ambient Environment”. You know, water quality models have evolved in step with environmental problems: Dissolved Oxygen (Streeter-Phelps) > Pathogens > Eutrophication > Toxics (e.g. PCBs) > Heavy metals > Harmful algae (e.g. cyanobacteria) > Pharmaceuticals and Personal Care Products (PPCPs). The development of models for antibiotic resistance is a natural next step for water quality modeling. Here are some pictures from the event:
https://plus.google.com/photos/106451974855194253783/albums/6078591575540040705
https://plus.google.com/photos/106451974855194253783/albums/6078591575540040705
Friday, September 12, 2014
Non-Darwinian evolution produces biogeography in model ocean microbe population
I am very happy that our
paper on agent-based modeling of global ocean microbe evolution is now
published. This study shows that neutral evolution and dispersal limitation can
lead to substantial biogeography in ocean microbe populations. In a nutshell: Microbes
evolve faster than the ocean circulation can mix them. I expect these results
will receive a lot of attention, and I look forward to the discussion. In this
post I want to highlight another aspect of the paper I am excited about,
focused more on modeling technology.
You know, when I start
my research program here at Northeastern about 10 years ago, I set out to
develop models that are consistent with the quantity and types of observations
we generate today. So I went to the literature and started looking at what
people are measuring. I ran across papers by Ed DeLong and Craig Venter that
presented metagenomics observations. My initial reaction of excitement quickly
turned to despair when I realized that the quantity of information generated by
modern observational
tools now greatly surpasses what we can get out of models. In this model we
simulate individual microbes, each with a full 1 Mbp genome. That approach
constitutes one possible direction towards closing this gap. In some ways, our
model application turns the table again, at least in terms of information
quantity. For example, one of our simulations (Fig. 1B in the paper, “start
uniform” simulation) includes 2.9e8 mutations and thus unique genomes, for a
total of 290 Tbp, which is far larger than metagenomics datasets (e.g. GOS has
6.3 Gbp) or what is currently in GenBank (160 Gbp, Feb. 2014). I have an opening for an undergraduate research
assistant to upload this data to GenBank (joke).
Here are links to the
paper, a perspective article, some news features and an animation (which has
been approved for going viral).
Thursday, September 4, 2014
Here we go …
Our fall semester is starting this week. This semester I am teaching my graduate Surface Water Quality Modeling course. I always enjoy this class, because the topic is very close to my research. The nature of graduate education is changing: For the first time I have more “online” than “inclass” students. Here is a link to the syllabus.
https://dl.dropboxusercontent.com/u/58018213/Syllabus%20CIVE7261.pdf
https://dl.dropboxusercontent.com/u/58018213/Syllabus%20CIVE7261.pdf
Wednesday, August 20, 2014
New project: Analysis of cyanobacteria sensor data
I am pleased to announce the start of a new project entitled “Robust Identification and Model Validation for a Class of Nonlinear Dynamic Systems and Applications”. This is a collaboration with Mario Sznaier and Octavia Camps from ECE, sponsored by NSF. In this project we will develop and apply data-driven models to high-volume environmental parameters (e.g. from cyanobacteria sensors) that hopefully will help us understand and manage water quality problems, including harmful algal blooms (HABs), in the Charles River and other water bodies. Here is a picture of a sensor buoy (courtesy GLEON) and a link to the project abstract.
http://www.nsf.gov/awardsearch/showAward?AWD_ID=1404163&HistoricalAwards=false
http://www.nsf.gov/awardsearch/showAward?AWD_ID=1404163&HistoricalAwards=false
Monday, July 28, 2014
2nd Public Swim in Charles River
On Saturday I jumped into the Charles River … again. This is a now annual event organized by the Charles River Conservancy. Last year there was one swim day. This year there were two scheduled, but the first one had to be cancelled because of a cyanobacteria bloom. Hopefully next year we will have even more and eventually a permanent beach or dock. Here is a link to CRCs web site: http://www.thecharles.org/projects-and-programs/swimmable-charles/
Wednesday, July 2, 2014
Summer Sampling Under Way
Our summer sampling program has started. This year, PhD student Frank Schellenger and YSP students Mia Kobs and Mindy Wu are exploring the role of phosphorus loading from lakefront septic systems to lakes. An interesting aspect of this problem is the time dimension. Because phosphate sorbs strongly onto the solids in the ground a lot of it remains there and does not reach the lake. But P is conservative, so it will get there (“break through”) eventually. When do we expect this to happen? Here is a picture of Frank, Mia and Mindy at the lake and a link to more pictures.
https://plus.google.com/photos/106451974855194253783/albums/6031449257339362673
https://plus.google.com/photos/106451974855194253783/albums/6031449257339362673
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