Tuesday, August 14, 2018

Wetland delineations (8/14/2018)

One of the classes that I teach introduces my students to wetlands, their value and how to recognize them.  Wetland regulations have been a contentious issue for quite some time here in the U.S.A., and I suspect it will not go away soon, although under the current administration things could change on a dime.  Wetlands always seems to cause a confrontation between the environmental community and sometimes the government on one side and landowners and developers on the opposite side: “Who are you to tell me what I can or cannot do on my property?  This is partially because there are periods in the year that some wetlands can be bone dry.  Let me explain:  Here in the U.S. a site is usually considered a wetland when the soil is continuously inundated or saturated for more than 5% during the growing season (or when there are leaves on the deciduous plants).  In my neck of the woods of eastern Virginia that is as short as somewhere between 9 to 12 days.  You can see how this can piss off a property owner who claims that his property is usually mostly dry.
While this may not be one of the most photogenic pictures I have ever taken, it illustrates the point I write about above.  This is a wetland and in the winter and parts of spring and fall, you walk through water here.  However, on a warm summer day this is dry as a bone as you see here.  A property owner could easily say: "What wetland?"
I teach my students this and what some of the additional red flags are in recognizing a wetland, just in case a landowner forgets to report a wetland when they are about to develop their property.  I mostly teach folks who deal with projects that are at that (early) stage of development; it is therefore important for them to recognize them, so they can let us know before it gets impacted by the construction of a new building, a subdivision or parking lot.  I tell them that I can absolutely not turn them into wetland scientists or wetland delineators; I just want them to be able to recognize some of the "red flags."

I often start out with telling my students how wetland delineators do their jobs and the way I started out in this business back in the early 1990s.  I was a part-time assistant professor at the Gallup branch campus of the University of New Mexico, when the Chair (and only full-time staff member) of the biology department got a call from an owner of an old sawmill just across the border in Arizona.  The sawmill had shut down, but in the past, they had treated their lumber with arsenic to make treated lumber.  My understanding was that the soil was contaminated, and they were going to be required to clean things up, but the site drained into a wetland, and they were either supposed to stay out of a wetland that was below the site, or only supposed to clean up the wetland since that was the place where all the arsenic had ended up.  Either way, they needed to know the extent of the wetland and were wondering if there was anyone at the university that could help them.  I was hungry and wanted to start my own consulting business, so I went for it (the chair was a human biologist and could not distinguish one plant from another, let alone identify a wetland).  Truthfully, I had never done it either, did not know what the heck I was doing or what it was about.  All I knew was that I was an ecologist, so, I thought, it must not be very difficult to figure out.

Being at a university I was able to get a hold of the Corps of Engineers “Wetland Delineation Manual” and I set out to work.  It was a very isolated site on the Navajo Reservation, not too far from Gallup, kind of interesting an abandoned sawmill, eerie but still neat.  I figured that it would not be very difficult, here we were in the Four Corners, in the Sagebrush Steppe which can be considered part of the Great Basin Desert or if you are a splitter it technically can be called the Colorado Plateau (Desert).  Whatever you call it, the area is dry, and a wetland should be darn obvious.  Boy was it ever!  That is the nice thing about working in the desert.

A few years later, after moving to the mid-west and gaining more experience I became quite the expert wetland delineator.  I first lived in Cincinnati and ended up traveling throughout the U.S. to do delineations.  While living in Virginia I traveled all over the eastern U.S.  In my blog post that contains my sermon I discuss some of the perils of field work, including being hit by a cottonmouth.  

What I had learned during my career as a wetland scientist was that desert ecology and wetland ecology was not that different.  Plants were under stress.  In wetlands plants had oxygen stress in their roots because of flooded soils, and because of that could often not take up water unless they had very specific adaptations.  Being an arid land physiologist by training (who could not find a job and thus ended up in consulting), I found that this was not very different from desert plants who were also often under (drought) stress and had very specific adaptations to survive.  The issue is that plants only have four major hormones and only one of those four hormones, ethylene, mediates stress.  I spent a lot of time studying this hormone; in the past it was thought that is was released as an adaptation to flooding and it helped with fruit ripening (that’s how we get evenly ripened fruit like bananas on the shelves in our grocery stores); however, we were able to show in the lab that it also made plants more tolerant to drought stress.  Oh well, I will leave it at that.

When I started my career as a wetland scientist I learned that I had to look for three main characteristics in the field: certain plants that are known to grow in flooded conditions, while other plants absolutely could not; soils that showed signs of flooding; and landscape features indicating flooding.  We also call this the three mandatory wetland criteria: vegetation, soils and hydrology.  This is what we look for when we examine a site, we look if it is a wetland or has pockets of wetlands.  Over time wetland delineations got easier and easier to a trained eye, although it was always exciting when you got to a new area in the country, where you had never delineated before.  You got to see new plant species and new soil types.  I was always a bit nervous to start out in such an area.  I usually studied the soil survey of the county to see what kind of soils I may encounter, while in the field I often collected plants to take back with me to my motel room or to my office so I could take my time to identify them.

We sometimes joke that we delineate with our feet; actually, it is a combination of feet and eyes.  With a bit of experience, you start noticing subtle changes in vegetation composition, and the consistency of the soil under your feet.  The ground might just get a little softer and at the same time it feels like you just stepped one or two inches lower in elevation.  This may be important, for as I described in the beginning of this post, wetlands can be bone dry, especially in the middle of the summer.  But, together with a minor vegetation change like the entrance or disappearance of one specific plant species may be enough to make you stop and wonder.  Now it is time to examine the soil.  Has the soil also changed when you crossed that subtle boundary you think you perceived in the field.  At first, I would take several soil samples with a probe or an auger on both sides of the boundary to compare.  Once I determine that I may have a soil that is representative of a wetland soil I may use a shovel to dig a decent soil pit to get a representative soil description.  Subsequently, I determine the boundary of the entire wetland, flag it and describe it, after which it is ready to be surveyed.  I often survey it with GPS, although that is not as accurate as a survey done by a licensed survey crew.  After that it is often up to the engineers, the owner and the developer to decide what to do with or to the wetland.

One of these days I may write more about wetland plants, wetland soils or the more illusive hydrology.  Stay tuned.


A wide-angle photo of one of the ponds behind our home.  There is still a little water visible in the center of the pond which is 6 feet (1.8 meters) deep in the middle.  In winter and early spring the water comes all the way to where I am standing.  As you can see, at that time and in early summer these trees stand submerged in water.  Species include: black gum, red maple, tupelo and overcup oak. They are what we call wetland species. 


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