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  Archived Posts From: 2021

wetland-assessments

Status and Trends: Wetland Losses 2007-2017

Written on: December 14th, 2021 in Wetland Assessments

By Alison Rogerson, DNREC’s Wetland Monitoring and Assessment Program

In this fourth installment reviewing the results of DNREC’s ten year wetland mapping update and Status and Trends analysis, we’re digging up the dirt on wetland losses. This is likely the wetland topic with the most sensitivity. People who value wetlands are upset that they are being lost. People being accused of causing wetland losses are defensive. People who had a bad experience with wetland regulations that prevent losses feel frustrated. We’re not forensic scientists but we have the best available mapping technology on our side.

An example of forested wetland loss due to clearing for timber harvest. Areas circled in light blue were mapped as wetlands in 2007 but have since been clear cut.

First off, how does one ‘lose’ a wetland? Where does it go? Lost is an interesting term and ‘converted’ or ‘destroyed’ may be more accurate. Wetlands exist when they have porous, spongy soils and have a connection to some source of water (rain, groundwater, overbank flooding etc.). A functioning wetland can be effectively destroyed if it becomes disconnected from its water source by a berm or a flood gate or dried out by ditching and channelizing streams. They can also be buried under loads of fill, say if someone tried to build on top of them. The compacted soils are rendered powerless to function normally. Without a water connection and functioning soils there will be no wetland plants- and the wetland is essential destroyed- or lost.

Who would want to live in or on a wetland, you ask? Not me! What right-minded homeowner would think that building a house or a business on a wetland is a good idea? Unfortunately, many missteps can lead to this situation. First, not all wetlands look like wetlands year round. Delaware’s most common wetland is forested but flat and holds water at or just below the surface even in the wet season, not flooded in pools and ponds. It’s not the obvious bog type wetland you may have envisioned. Because of this, they often go unmarked and, therefore, fall victim to conversion and loss. Also, by the time buyers see a house for sale, the ground has been so worked and pushed around that you would never suspect a wetland was underneath layers of fill dirt.

So did Delaware’s wetlands suffer a loss between 2007 and 2017 according to this statewide mapping project? Yes, and the figures indicated that the pace and source of losses have stayed consistent. Through an analysis of wetlands that were there in 2007 but were gone in 2017 to calculate the acreage, type (tidal or non-tidal) and sources of loss over the span of a decade. We classified sources into six categories: clearing, development, agriculture, transportation/utilities, environmental impacts and technique improvements. Technique improvements were a class of mapping changes related to the computer software and updates in technology, not changes on the landscape, and were therefore not included in loss calculations.

Our study showed that Delaware lost 3,011 acres of wetlands statewide between 2007 and 2017. Most of the wetlands destroyed or converted were non-tidal (92%), with losses to tidal wetlands making up the remaining portion (8%). Losses to non-tidal wetlands occurred mostly in forested, headwater wetlands

The sources of wetland losses over that decade vary greatly for non-tidal compared to tidal wetlands. Our coasts are being impacted by sea level rise and heavier, more frequent storms, so it’s no surprise that 66% of tidal wetland losses were due to environmental impacts such as erosion. Only 13% (31 acres) were deemed due to development and another 10% (23 acres) were lost to transportation and utility work. Land clearing, usually timber harvesting, may be a transition to development or may regrow, caused another 9% (22 acres) which leaves 2% (4 acres) lost due to conversion to agriculture (poultry, row crops, livestock).

Proportions of vegetated non-tidal wetland losses from different causes between 2007 and 2017. Only wetlands ≥ 0.25 acres in size are included in calculations of proportions.

Compare that to non-tidal wetlands, where 54% (1,508) of losses were due to clearing, 24% (654 acres) to development, 19% (533 acres) to agriculture and only 3% (75 acres) to transportation and <1% (2 acres) to environmental impacts. A very different picture between wetland types which is important to recognize. It’s also important to point out that wetland loss rates and causes vary around the state. Sussex County is host to nearly half (48%) of Delaware’s wetlands but accounted for 66% of wetland losses between 2007 and 2017. Subsequently, 23% came from Kent County and 8% from New Castle County.

For those of you who think in terms of watersheds instead of counties, we can speak your language too. Statewide wetland losses from 2007-2017 occurred mostly in the Chesapeake Bay Basin (62.5%, 1,884 acres), followed much further back by the Delaware Bay Basin (18.7%, 565 acres) and Inland Bays (16.6%, 501.5 acres). The Piedmont Basin which does is not comprised of many wetlands, contributed 1.9% or 60 acres of wetland lost during this time.

Unfortunately, this study reported many continuing trends compared to a similar study for 1992-2007. The Chesapeake Bay Basin and Sussex County were the main sources of loss, with clearing (timber harvesting) again as the main source, followed by development and agriculture. Forested freshwater wetlands continue to suffer the most losses. It is not that surprising , though, given that wetland regulatory programs have not been strengthened in the last 10 years and the push for economic growth continues to take priority.

Based on these results we know we have our work cut out for us. We need to do more to raise awareness for wetland values and protection against destruction. Looking ahead to 2027, we would like to see a decline in wetland losses, an evening out of trends among counties and basins and a decrease in forested wetland habitat loss.


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wetland-restorations

Shellfish Recruitment: Oyster Shell Recycling

Written on: December 8th, 2021 in Wetland Restoration

By Sarah Bouboulis, Partnership for the Delaware Estuary

The Partnership for the Delaware Estuary (PDE) has been interested in living shorelines and shellfish research since the early 2000’s, led by Senior Science Director, Dr. Danielle Kreeger. Since 2004 PDE has installed several living shorelines throughout the Delaware Estuary, primarily using materials such as coconut coir logs, Oyster Castles© and oyster shell bags. During the formative years of PDE’s Delaware Living Shoreline Initiative program (DELSI) and subsequent project monitoring, it became clear that oyster shell bags, in many instances, were one of the best choices for living shorelines based on shellfish recruitment and shoreline stabilization data. However, recycled oyster shell were becoming a hot commodity (i.e. expensive and hard to come by). Subsequently, PDE saw a need for an oyster shell recycling program within the Delaware Estuary.

It took quite a few years to have resources lined up in such a way that both space and funding, for management of the shell, were secure. The stars finally aligned in 2016 when space and funding became available simultaneously in Wilmington, Delaware.

Pre-pandemic, the program was collecting from 9 restaurants in Northern Delaware and one in Dover, Delaware. Between 2016 and 2019, the restaurant collections averaged 1,400 bushels a year (or 70,000lbs). Sadly during 2020 most restaurants closed for an extended period of time and, unfortunately, a few restaurants were forced to close permanently. Since businesses have begun to open back-up, collections have re-started and for 2021 the total collections will near 1,000 bushels.

Currently, collections are only with restaurant partners. Pick-ups are conducted weekly or bi-weekly, depending on the season, and the shell is brought back to the shell management area in Wilmington. Shell is cured in the open between 6-12 months, being turned at least once during that time before it is then, usually, bagged and ready for use on living shoreline or other restoration projects. The curing time is set to make sure the shell has properly cured and there is no risk of introducing disease, pathogens, or other foreign materials back into area waters.

Two large shell piles.The right pile is shell that has been cured for 6-12 months. The pile on the left is fresher shell in the curing process.

The next step is preparing the shells for transport and/or use on a living shoreline. This typically involves putting the shells into mesh bags. This is the most time and labor intensive portion of the process and it would not get done without the help of countless volunteers. It is also a group activity, needing around 10 volunteers per bagging session. Groups from University of Delaware, Delaware Technical Community College, Wilmington Green Jobs, Bank of America, the Camden Power Corps and many others have all helped with shell bagging. And PDE is so appreciative of their participation!

The fully cured shell goes primarily to living shorelines projects, many put in by PDE. Recycled shell is also sold to restoration partners for other projects such as reef creation and aquaculture research, as well as living shorelines being implemented by others. The main focus of PDE’s oyster shell recycling has always been to support projects within the Delaware Estuary, however, when excess shell exists it has been sold outside the Estuary. You can view a new story map outlining all of PDE’s living shoreline projects, most of which incorporate recycled oyster shell here.

Since inception, over 12,800 bags of shell have been created, which could secure over 4000 feet of shoreline! The shell has gone to support projects in all three states in the Estuary involving a tremendous amount of partners including the Philadelphia Water Department, DNREC, USFWS, The Nature Conservancy, Haskin Shellfish Research Laboratory, and University of Delaware, to name just a few!

Oyster shell bags being used as part of living shoreline installation in Delaware.

In 2022, PDE hopes to expand oyster shell recycling into the city of Philadelphia along with help and support from the Philadelphia Water Department. In such a major metropolitan area, and with a much larger shell management area, the program should be able to collect and cure several times more oyster shell than our current operations.


To learn more about the program, how to volunteer or to purchase shell, you can view our website here or contact Sarah Bouboulis; sbouboulis@delawareestuary.org.


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wetland-assessments

Stream Assessments 101

Written on: December 8th, 2021 in Wetland Assessments

By Brittney Flaten, DNREC’s Watershed Management and Assessment Section

Before I started at DNREC, I worked in Maryland conducting stream health assessments. When I joined the Wetland Monitoring and Assessment Program (WMAP) I was excited to learn that the team was working on a new stream assessment protocol. Let’s look at what a stream assessment is, and how stream health relates to the work that our team does in Delaware.

What is a stream assessment?

Stream assessments can be used by governments, nonprofits, or citizen scientists to document stream health in their area. Most states have their own protocol – WMAP is currently working on one for Delaware! Local environmental groups like Nanticoke Watershed Alliance and Delaware Nature Society have their own methods that volunteers use to collect data. While each organization may have a different protocol for assessing stream health, there are generally four kinds of data collected.

Water Quality

When WMAP is assessing stream health, we’re interested in measuring characteristics like water temperature, dissolved oxygen, and pH, which impact what kinds of animals can live there. In the field, we use a handheld water quality meter with sensors that can detect temperature, oxygen, and dissolved ions in the water. We also look for signs of water pollution like discoloration, oily sheens, excessive algae, or unusual smells. There are several organizations in Delaware that collect other kinds of water quality information like the concentration of nitrogen, phosphorus, and total suspended solids. If you’re interested in learning more, you can check out the Delaware Water Quality Portal.

Hydrology

To assess hydrology, we look for evidence that the stream’s shape has been altered by humans. Some examples of alterations include culverts, dams, or walls that straighten the stream. We’re also interested in the stream’s ability to connect with the surrounding floodplain, which we can determine by looking at how incised the stream is. Floodplain connection is particularly important during storm events. When water levels rise, the excess water and debris can spill out onto the floodplain, rather than causing damage to inhabited areas or infrastructure downstream.

High banks on White Clay Creek.

Habitat

Before looking for organisms, we assess the quality of habitat in the stream. Potential habitats include submerged aquatic vegetation (SAV), logs and other woody debris, piles of leaves, and root wads from trees. All of these provide a place for organisms like fish, crayfish, and insects to hide from predators and find food. We also look for signs of excess sedimentation in the stream, which can stress fish, invertebrates, and aquatic vegetation. Tall, eroded banks, muddy water, and lots of silt or clay covering the bottom of the stream are all signs that there is too much sediment.

This SAV in the Appoquinimink makes for a good hiding spot!

Biology

To find living organisms in streams, we sample habitat like logs and root wads using a D-net, which has very small holes that only let water escape. Most of the organisms we find in our nets are benthic macroinvertebrates like freshwater clams and mussels, snails, mayflies, water beetles, and dragonfly larvae. We use keys and guidebooks to help us identify, sort, and count them in the field. Of course, we also look for fish, salamanders, and frogs! Sometimes we’re lucky and find one in our D-net, or we see them but can’t catch them! In the office, we categorize organisms based on how tolerant they are to environmental stressors like pollution or low dissolved oxygen levels. For example, mayflies, stoneflies, and caddisflies are very sensitive to stressors, but worms and fly larvae are not. If we find many sensitive organisms in our sample, it’s likely the stream is in good condition.

Why are we interested in stream health?

Clean streams provide clean drinking water, good habitat for fish and other organisms, and opportunities for recreation. Also, stream health and wetland health are closely related. Riverine wetlands, for example, depend on water supply from streams that are well-connected to the floodplain. On the other hand, wetlands purify water before it enters streams and rivers by trapping substances like sediments, fertilizers, and pesticides. Both wetlands and streams are important in improving the overall health of our watersheds. If you’re interested in learning more, visit the Division of Watershed Stewardship’s website. If you’re looking to get involved in stream health in your community, there are several opportunities with Nanticoke Watershed Alliance, Delaware Nature Society, and University of Delaware Citizen Monitoring Program.


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education-and-outreach

Interview with a Wetland: Wading in a Critical Habitat

Written on: December 8th, 2021 in Education and Outreach

By Olivia McDonald, DNREC’s Wetland Monitoring and Assessment Program

Get ready to get down and dirty as we wade into Delaware’s wetland habitats for an interview.

Freshwater stream in Sussex County, Delaware

No better way to get to know wetlands than by chatting with one. Today we’re interviewing Delaware’s wetlands. Thanks for taking the time to join us today for a chat!

Of course, I love any opportunity to get the word out there about who I am.

Let’s start in the past. Could you tell us a little about your history? Like how you got to where you are today?

Well, the best way to put it is that it all started a very long time ago. Although some wetlands can form very quickly, many actually take thousands of years to develop. In the case of myself, as tidal and non-tidal habitat, it has been most common through the years for me to form when coastal lowlands flood, when rivers deposit sediment as they reach the ocean, through periodic flooding or high water tables, in isolated or low-lying areas surrounded by dry land, or through other forces of nature – including people! Over time, herbaceous plants, shrubs, and trees with special adaptations take root in my soil. Since about the 1600’s, at the start of colonial settlement in Delaware, I’ve been facing challenges ranging from land loss from development, to the effects of climate change, and that’s just in the past 30 years. Currently, I make up 20% of the land in Delaware, and around 5% of the land in the United States.

What is a day in the life like for a wetland?

Busier than you think! I actually have a lot of responsibilities for others, not just myself. Many species of birds and fish depend on my specialized habitats. Some of Delaware’s most unique species, like the Marbled salamander, call me their home. I also do tons of cleaning, and not like the tidying up kind. I filter toxins and pollutants out of the water through my spongy soil, and absorb carbon dioxide or other greenhouse gases. This helps with making sure that any water entering our streams, rivers, and groundwater systems is clean. I also divert floodwaters to keep them away from people and their property. And let’s face it, Delaware is not very high up off the ground. So negative impacts from large storm events, such as flooding or erosion, would occur more likely if I simply was not around. The easiest way to put it is that my job is to provide, purify, and protect. That’s what I spend my day doing and love it.

Marbled salamander in a freshwater wetland.

What is one strength and one weakness?

A strength? Hmmmm. I’m really good at giving people what they want. And I mean that in an economical and even emotional sense. Here in Delaware, the outdoor enthusiast lifestyle is growing rapidly. Eco-tourism is a major component to the state’s economy, as well as the development industry. State parks, recreational activities, nature centers, they all rely on wetlands in some way. As for the emotional bit, it can be simply put; people rely on wetland ecosystems to make them happy. Whether it is kayaking at Killens Pond State Park, or fishing at the beach, people far and wide are getting outside to experience the great outdoors. And wetlands are gateway to that personal joy.

On the other hand, my weakness has more to do with perception. I’d say the hardest thing I deal with is being misidentified. I’m usually covered with water during the winter and spring months, then my surface is often dry during the summer and fall months. My tidal wetlands, or better known as marshes, tend to get the spotlight. Sometimes that shadow casts over my non-tidal, or freshwater wetlands, that come in all different shapes and sizes. I’ve got flats, depressions, riverine, swamps, and fens. My changing water levels and specialized habitat types can make identifying me as a wetland area very difficult, and that’s tough to deal with.

A freshwater wetland in the fall (left) and the winter (right).

What is your biggest challenge you face right now?

Policy and implementation. Take my non-tidal wetlands for example. Currently in Delaware, the state only regulates non-tidal wetlands of 400 contiguous acres or more. And my freshwater habitats make up 75% of all the wetlands in Delaware! That’s a large amount of uncertainty when it comes to my protection. When you think about implementation, that’s more along the lines of what can be done to protect me on any size scale. If you can believe it, 80% of my wetlands are actually on private property, which leaves another huge amount of planning to the average citizen. The challenge I’m seeing here isn’t that the public does not care, it’s that they simply don’t know! They’re not sure about incentive programs, people don’t have the scientific background in implementing restoration projects. But that doesn’t mean they can’t. For now, it’s an uphill battle, but one I’m certainly willing to walk. 

So what can we do as the general public or homeowners to protect you for future generations to come?

First and foremost, educate yourself. The first step in understanding what to do in the future is how to behave in the present. Leave plants or an un-mowed strip of land between developed areas. Plant native species in your yard and remove the invasive ones. Dispose of trash in proper locations or recycle where appropriate. These baby steps on an individual level can assist me with my job to provide, purify, and protect. If you want to get even more involved in protection, start looking around at what is on your property. I mentioned earlier a challenge I constantly face is being misidentified. There is an amazing mapping resource, The Freshwater Wetland Toolbox, that can assist you with finding wetlands or your property or in your local community. If you find out there’s a wetland on your property, you can use the Guidebook for Public Participation to learn about what you can do to manage my vital land. The information is out there and progress is moving forward for wetlands benefits, you just have to find it. 

Well, we certainly learned quite a bit without putting on waterproof boots or hopping in a boat. Thanks again for taking the time to chat with us!

No problem at all. If you’d like to stay up-to-date on how I am doing, my biggest supporters at DNREC’s Wetland Monitoring and Assessment Program are always doing work in my favor. I can’t thank them enough for always building me up when I’m sinking down! I’m sure you’ll see more from me in the near future. 


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wetland-assessments

Status and Trends: Wetland Gains 2007-2017

Written on: September 15th, 2021 in Wetland AssessmentsWetland Restoration

By Alison Rogerson, DNREC’s Wetland Monitoring and Assessment Program

Back in July we explored the status and trends of stormwater ponds in Delaware. This time around we’re digging into how and where Delaware ‘gained’ wetlands between 2007 and 2017, according to DNREC’s recent Statewide Wetland Mapping Project (SWMP) update.

How does one gain a wetland? Where did they come from? Weren’t we taught that wetlands take years and years under water-logged (saturated) conditions to create hydric soils and then grow water loving (hydrophytic) plants? Well, that is true- so the answer is- it depends. First, let’s take a look at the overall numbers and then explain where they came from.

Between 2007 and 2017, this project estimated that Delaware gained 1,406 acres of wetlands. This is about half as much as Delaware lost in this timeframe and represents just 0.4% of statewide wetland acreage in 2017. Half of those gained wetlands were in Sussex County, where most gains are attributed to stormwater ponds tied to development. In total, 90% of 1,406 acres gained were manmade, for a few reasons described below.

Sources of wetland gains between 2007-2017; includes only wetland gains more than .25acres

Better Mapping

Wetland maps and acreage are based on remote sensing- by computer basically- using photos taken from the sky combined with other maps such as elevation and soils to make a very educated guess at where functioning wetlands exist. As photo quality improves, as supporting information is updated, and as the computer technology evolves the ability to ‘find’ wetlands increases- so wetlands that may have already been there in the past but were not detected previously would count as a ‘gain’. They were already there, we just got better at seeing them.

Conditions

When wetland maps are created based on a snapshot in time- one set of aerial photos taken in the spring before leaves get in the way- the conditions that year can make a difference. Photos taken in a wet year when there has been a lot of rain may show greater wetland extent but during a dry year can show shrunken or fewer wetlands- which is why supporting information like elevation and soils are key to balance out what may just be fluctuations due to weather.

Restoration (Middle left photo)

In some cases, new wetlands really have been gained. Wetland restoration projects around the state can change the landscape by creating new wetlands or bringing a degraded wetland back to its former glory. Wetland creation often occurs in former ag fields and are often done to offset, or mitigate, wetland impacts somewhere else. Restoring degraded wetlands may involve restoring natural water flow to a previously farmed wet field. Large restoration projects can be picked up in wetland mapping and counted as a gain. In this project, wetland gains by restoration made up 5%, or 63 acres.

Industrial Sources (Middle right photo)

On the other hand, sometimes gains due to landscape changes are not true gains in functioning wetlands, such as mining for dirt and sand materials to use in construction. The borrow pits created during excavation often fill with water, creating large pools which can be picked up as a wetland gain but really do not provide functional value and should be counted separately. Industrial sources accounted for a third of wetland gains statewide.

Development (Top right photo)

As readers learned in July, the prominence of stormwater ponds in Delaware has continued to increase. As the housing boom continues with fervor, so does the creation of stormwater ponds, which every new neighborhood or commercial building requires. As previously mentioned, these ponds capture storm water but lack greatly compared to natural, vegetated wetlands. Another third of wetland gains were related to development through creation of retention and stormwater ponds.

Agriculture (Top left photo)

One source of both wetland loss and gain is due to or from agriculture. Wetland pockets are converted and are incorporated into tilled farm fields. Over time, crop production in those pockets may decrease. Farming a wetland is not easy, and if production is not worth the seed and fertilizer that goes into it, a farmer may opt to abandon trying to farm a former wetland pocket. When those pockets are no longer being tilled and mowed they revert back to grassy vegetation and can be picked up as a wetland gain.

Migration (Bottom left and right photos)

As we all know, Delaware is being impacted by sea level rise at an increasing rate, which prompts coastal wetlands to creep away to remain higher. This trend, called marsh migration, led to many small wetland gains along wetland upland boundaries. Forest edges have become wetter, leading to trees dying and wetland vegetation moving in. About 140 acres were natural gains associated with marsh migration.

As you have read, wetland gains come in many forms; some are more authentic than others. Some have potential for function, some do not. At the end of the day, though, wetland losses far exceed wetland gains so we have more work to do to tip the scales to the positive side. More on wetland losses next time!


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living-shorelines

A Homerun for Living Shorelines

Written on: September 8th, 2021 in Living ShorelinesWetland Restoration

By Joshua Moody, Partnership for the Delaware Estuary

Since 2014, the City of Lewes, Delaware has been actively renovating the downtown waterfront park and shoreline along the Lewes-Rehoboth Canal, including native plant landscaping, playground features, walking paths, and educational signage. This work has been a part of a larger plan by the city to provide public open space, enhance tourism, and provide greater opportunity for public engagement. The little league baseball field located next to the Lightship Overfalls museum is a prominent feature of the public area along the canal, serving as a community gathering and recreational area. A narrow fringe of salt marsh separates the ballfields from the canal, helping to protect them from flooding by absorbing water. However, flood protection is not the only service that the salt marsh provides. The band of intertidal vegetation serves important roles for many fish, birds, and other animals that call Delaware home. Juvenile fish feed and take refuge from predators in the flooded vegetation and in the intertidal creeks, birds nest and forage for food among the grass and along the adjacent mud flat, and shellfish settle intertidally to filter food (and pollutants) from the water while simultaneously fertilizing plants and providing habitats for many smaller invertebrates. Additionally, when water floods the salt marsh, the plants can take up nitrogen and trap sediments that can have negative water quality impacts. The eroding salt marsh was not just bad for the ballfields, but for the local ecology as well.

Figure 1. Location of the Lewes living shoreline (white box) along the Lewes-Rehoboth Canal behind the little league baseball fields off Pilottown Rd in downtown Lewes, Delaware

Stopping erosion while supporting natural habitats is not always an easy task. Many of the techniques historically used to stop erosion, such as bulkheads and rip rap, can harm wildlife and reduce usable habitat. Water reflecting off bulkheads can impact the valuable mudflat habitat in front of them, and rip rap can make it difficult for many motile species, such as turtles and horseshoe crabs, to move from the water up into the marsh. Additionally, these types of structures can ultimately sever the connection between the water and the land, reducing the intertidal salt marsh habitat and many of the important services it provides. In 2007, the Partnership for the Delaware Estuary and the Rutgers University Haskin Shellfish Research Laboratory began exploring new living shoreline techniques to provide erosion control with ecological uplift along the Maurice River in New Jersey. The goal of these efforts was to develop a methodology that capitalized on the naturally stabilizing structure of shellfish beds, both oyster and mussel, to reduce erosion. These efforts were of interest to the DNREC Wetland Monitoring and Assessment Program (WMAP), who approached PDE in 2013 to discuss collaborating on a living shoreline project. The renovation efforts with a focus on native habitats that were just beginning along the Lewes waterfront made the ballfields an ideal location to test a living shoreline (Figure 1). 

The living shoreline design focused on meeting the dual goals of erosion control and habitat uplift, employing ecologically beneficial materials placed to develop the proper ecological conditions for salt marsh plants and shellfish to thrive. Coir, or coconut fiber, logs were used to shape the waterward edge and build elevation, while recycled oyster shell bags provided protection to the logs and would serve as a home for developing oyster and ribbed mussel communities. In April of 2014, a series of shell bag-lined coir logs were installed in a cusp formation along 92’ of the eroding shoreline (Figure 2b), which was left to trap sediment and build elevation over the following five months, until a second tier of coir logs was added to build additional elevation in October (visible in Figure 2c). Achieving the correct elevation is very important to create the appropriate habitat for the native salt marsh plants that require a certain amount of flooding to survive and prosper. Purchased and salvaged Spartina alterniflora, the native salt marsh cordgrass, was planted in the living shoreline area as trapped sediment continued to build elevation throughout 2014. By the spring of 2015 the planted and pre-existing vegetation were moving into the newly built area (Figure 2c), which was almost completely vegetated by August 2016 (Figure 2d).

Figure 2. Time series for Lewes living shoreline looking southeast: a) pre-installation, April 2014; b) post-installation June 2014; c) June, 2015; d) August, 2016.

Over subsequent years, annual monitoring quantified the effects of the living shoreline on the horizontal and vertical position of the vegetation, the vegetation’s health, and the shellfish community, relative to no action at a paired control site 50’ to the east. The coir logs remained intact until 2017, when two sections deteriorated and were replaced with recycled oyster shell bags. Overall, the living shoreline was successful in reestablishing vegetation for an overall gain of 1,447 sqft of salt marsh habitat, while its paired control continued to erode (Figure 3). Importantly, the living shoreline was able to build and retain the appropriate elevation for vegetation persistence (Figure 4), and provide suitable oyster and ribbed mussel habitat via the shell bags, which have been densely colonized (Figure 5).

Figure 3. Positions of the contiguous vegetated shoreline along the treatment (living shoreline, green lines) and control area (red lines) in 2014 (light colors) and 2018 (dark colors). These data show the vegetation moving out towards the water in the living shoreline, and continuing to erode in the control area.
Figure 4. Elevation changes at fixed positions along transects oriented perpendicular to the shoreline at the living shoreline treatment and paired control. Numbers along the x-axis denote plot locations: 1) 1m waterward of the material placement line; 2 and 3) located in the area between the installed materials and original contiguous vegetation edge; 4) 1m landward of the original vegetated edge; and 5) 1m landward of the high marsh vegetation line. The redline indicates the mean tide line, the general lower threshold for Spartina alterniflora persistence. The black box indicates the impact area, or the area expected to be directly affected by the living shoreline installation in the treatment area relative to no action in the control area. The data in the black box show the living shoreline (treatment) achieving the proper elevation for vegetation to thrive (mean tide line) with a few years of installation, while the control area continues to site well below the proper elevation.
Figure 5. The 2014 living shoreline installation on June 22, 2021. Oysters have colonized the waterward toe of the living shoreline (main picture), and ribbed mussels throuought the roots of the vegetation (inset).

By 2020, the continued erosion along the adjacent control area became dire and encroachment on the Little League fields was imminent. In addition to the erosion, in 2020 a 50’ x 5’ section of marsh separated from the existing marsh and slid onto the mudflat. While the calved vegetation gave the illusion of waterward marsh growth, this unstable sediment and vegetation was highly vulnerable to erosion. Although worrisome, this situation provided an opportunity – if this material was trapped at its current position, over time it would stabilize and grow vertically to help rebuild much of the eroded salt marsh at the control site without relying on the need for outside fill. Concurrently, the USFWS Delaware Bay Estuary Project office had expressed interest in supporting a local living shoreline effort. PDE and DNREC WMAP presented the idea to expand the successful 2014 effort, which was well received, and a new project team was born. Collaboration between the three entities resulted in a design with the goals to stabilize and advance the vegetated edge at eroding area to the extent of the 2014 living shoreline and to provide additional habitat for the now robust oyster and ribbed mussel populations. The Lewes Historical Society (LHS), which owns the property, was very interested in stabilizing the salt marsh using ecologically friendly techniques, and supported the project team obtaining the appropriate state and federal permits. The new design was informed by the successful 2014 installation, while incorporating lessons learned from new living shoreline installations at other locations. As bagged shell has shown great longevity in maintaining position over time, while also providing shellfish habitat and retaining sediment across a multitude of installations, recycled oyster shell bags were selected as the primary construction material.

On June 21, 2021 over 1,200 shell bags were placed along 165’ of shoreline and positioned to create five sinuous, overlapping structures between 20’ and 40’ in length and 1.5’ high, with 5’ gaps between them, by PDE, DNREC WMAP, and USFWS DBEP (Figures 6 and 7). The curved formations allow for water drainage and faunal passage while interrupting direct wave passage between structures to the shoreline. Additionally, each structure contains at least one perpendicular “finger” to interrupt water transport and scour along the waterward edge. Finally, at four locations between the shell structures and the existing marsh edge, coir fiber logs were installed to help retain sediment. Annual monitoring will continue along the entire length of the living shoreline, encompassing both the 2014 and 2021 installations, and a seven-year pre-installation data set, will help the project team understand the impact of the newly deployed materials on the ecology. The project team is currently working with the LHS to develop informative signage to educate the many visitors to the waterfront on the goals and ecological importance of living shoreline efforts.


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education-and-outreach

Confessions of a Seasonal: Wetland Olympics 2021

Written on: September 8th, 2021 in Education and Outreach

By Katie Goulder, DNREC’s Wetland Monitoring and Assessment Program

Olympics Big and Small

The 2020 summer Olympic games. We waited an extra year for them to arrive, ready to cheer on fan favorites like Simone Biles and Katie Ledecky in their popular sports of gymnastics and swimming, as well as watch newcomers such as Athing Mu make running 800 m look fun and easy. This exciting international event only happens once every 4 (or in this case 5) years and has us all glued to our TV’s for NBC’s primetime coverage of our favorite sports. But did you know there was a secret Olympics that happened locally every summer?


That’s right! The lesser-known Wetland Olympic games happens every field season from late spring to early fall by local environmental scientists throughout Delaware’s many wetlands. As the 2021 seasonal wetland technician, little did I know that in accepting this job that I would also be competing in rigorous, albeit more obscure, Olympic events while performing my fieldwork duties.

Wetland Conditions

During the summer fieldwork season, the DNREC WMAP team is out monitoring and assessing both non-tidal and tidal wetlands throughout the state. Because wetlands come in many shapes and sizes, each site we evaluate presents its own set of challenges. Forested flat? Thick and thorny greenbrier vines ensnare your feet. Tidal mudflat? The mud may be a foot deep or it may be 3 feet deep. And there is no way to know until you take that step. Saltwater marsh? Changing tides can cause a small creek that was easily traversed in the morning to transform into a 4ft deep channel you have to wade through with your backpack over your head. Overall, working in wetlands provides unique opportunities to develop creative solutions to interesting problems. And thus, the Wetland Olympics were born.

The Events

I feel that the Wetland Olympic events emulate those of the actual Olympic Decathlon events in that they necessitate a combination of strength, agility, and endurance. A few of the most common events that the WMAP team competed in this summer include:

  • Hummock Hopping– Similar to a high-stakes game of “the floor is lava”, one must traverse across a tidal marsh only stepping on the hummocks, or islands of vegetation, that provide more stability while avoiding the hollows of bottomless mud. Under or overshoot your target? Next thing you know your leg is 3 feet deep in mud or water. Which leads into the next event…
  • Boot Balancing– Sometimes it is unavoidable that water spills over the top of your hip wader boots and you become waterlogged. This Olympic event comes into play as you perform one-legged yoga poses in an attempt to drain the water from your boot.
  • Mudflat Slogging– This event occurs while working in a mudflat with little to no vegetation and is the exact opposite of real Olympic speed walking. With every step you take, your foot sinks knee deep in mud and it is all you can do to keep moving at a snail’s pace.
  • High Kick Forging– On the flipside of mudflat slogging, this event requires a bit more flexibility. We break out the High Kick Forging when the vegetation is so thick that you must break through the plants in front of you to form a small path to reach an assessment area. New records of high kick are usually recorded when confronted with thorny plants or vines.
  • Equipment Launching– When the terrain is particularly difficult to traverse or obstacles such as deeper creeks are encountered, you must try to minimize your movement for the sake of efficiency. In these instances, one person will make it to the other side and a teammate will javelin or shotput the piece of equipment (usually marker flags or a tape measure) over the creek so that you can continue to collect the necessary data.
  • Balance Beam– While you may already be familiar with this event from the actual Olympics, there are some modifications in the Wetland Olympics. In our version, the beam is actually a 2×8 piece of wood that we carry out to a creek and lay across in order to cross the obstacle. While our beam might be wider than the one Simone Biles earned her bronze medal on, ours is covered in mud and therefore more slippery which adds 0.300 points of difficulty to our routines.

These are just a few examples of the athletic feats required of the wetland scientists on a daily basis in order to perform fieldwork in a difficult and dynamic environment.

Going for Gold

All in all, it has been a very exciting season working in wetlands throughout the state. I have learned so much about the different types of wetlands, the methods used to evaluate them and the variety of projects to preserve and protect the wetlands that remain and restore those that have been lost. While we don’t have medals in the Wetland Olympics, I can’t imagine a better team to train and “compete” with in each of these events.

When wetlands win, we all win.

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education-and-outreach

Senses in the Salt Marsh

Written on: September 8th, 2021 in Education and OutreachWetland Animals

By Kayla Clauson, DNREC’s Watershed Assessment and Management Section

A tidal creek in a salt marsh at low tide

If you’re anything like me and always looking for an adventure, maybe you should check out a tidal salt marsh! I’ll admit – I am slightly biased towards salt marshes due to my professional background, but I’ve exposed many individuals to the wonders of a salt marsh and it always ends up being an exciting trip.

Not only are tidal salt marshes amazing because of their important ecologic services, they are very aesthetically pleasing. Whether you enjoy birding, hiking, exploring, or just getting outside – a salt marsh might be a fun next adventure for you.

Here, I’d like to break down salt marshes for the five senses when you plan on visiting one.

This Great Egret doesn’t seem to mind the smell of a marsh while it hunts

First thing, smell:

I’ll just say it – smell will probably be least favorable on the senses when it comes to visiting a salt marsh. If you’ve ever been outside and stopped to smell the fresh air and instead get a whiff of rotten eggs…chances are you’ve smelled a salt marsh already. This smell happens because the marsh itself is situated on multiple layers of decaying plant materials, called peat. Bacteria that are decaying the dead plants use up a lot of oxygen in the process, creating low oxygen, or hypoxic, sediments. The remaining gas after the decaying process is called hydrogen sulfide – hence the rotten egg smell in the air.

The smells of the marsh vary, and don’t always smell of rotten eggs (unless I’ve gotten used to it at this point). Chances are if you’re in a salt marsh you will experience a mixture of earthy smells, including salt and mud.

Next up, touch:

If you were to walk out into a salt marsh and jump, you’d be quite surprised how that feels*. If you jumped on it, you would feel the hollowness of the peat when you land vibrate through the marsh. It feels very different than jumping on the grass in your backyard or local park. Salt marshes are very spongy, which is why they are so important in protecting us against storm flooding- they soak up excess water before it reaches our homes. If you had a handful of peat and squeezed it like a kitchen sponge, water will fall out!

Let’s talk about hearing:

An Osprey circling a salt marsh

Over the noise of your feet splashing in the creek or sucking into the mud, you’ll hear a suit of bird noises. Common birds you may find year-round are self-explanatory based on their common names, including Salt Marsh Sparrows and Marsh Wrens. There are other common birds that make the marsh a noisy place, such as Willets, Osprey, and Red-winged Blackbirds to name a few.

There’s also lots to see:

Because they are such an important habitat for wildlife, there is a lot you may encounter when visiting a salt marsh. If you’re looking in the water of a tidal creek, you may find small shrimp, crabs, fish, snails, and horseshoe crabs. As you look outward from the water you will see Fiddler Crabs and their burrows hidden among the Ribbed Mussels and low marsh plants, like Saltmarsh Cordgrass. As you look further outward towards the high marsh, you will see the vegetation shift from Saltmarsh Cordgrass towards the shorter, flatter Saltmarsh Hay. Some mammals including White-tailed Deer, Raccoon or even Mink, may be seen foraging in the marsh. 

If you get the chance to observe the variety of salt marsh plants closely, you may see some of them sparkling. This isn’t because they are covered in glitter, rather they are masters of their harsh saline environment and can excrete the salt from the water onto the blades of their leaves.

Best for last, taste:

A yummy patch of Seapickle along a bank of a tidal creek. I prefer to eat them when they are bright green early in the summer months

As ironic as it may be, one of my favorite snacks can be found in the salt marsh! Commonly known as Seapickle, the succulents of Salicornia spp. are often found in the low marsh and are a crunchy, salty snack. If you’re not into eating plants, Blue Crabs might be more appealing to eat due to its savory and tender meat. Blue Crabs are very reliant on tidal marshes for life-cycle development. However, you should cook them first!

A mistake one might make when looking for tasty snacks in the salt marsh is attempting to eat Ribbed Mussels. These bivalves do not taste as good as the popular Blue Mussel because of the high concentrations of sulfur they filter from the marsh. However, you may be able find other tasty bivalves, such as Oysters or Hard Clams, around a salt marsh in deeper water.

To wrap up:

A Blue Crab hiding among Ribbed Mussels in a tidal creek

Now that you’re prepared for some of the senses you will experience in a salt marsh, you may want some packing tips for your visit. I recommend:

  • Binoculars – You’ll want to see some of the birds up close
  • Bug spray – Keep away the biting insects and ticks
  • Sunscreen – It can get hot out there without shading foliage
  • Water – Although you’ll be around water, you won’t want to drink it due to its salt content
  • Phone/camera – Just in case you want to document any findings
  • Field guide – check out this wetland field guide to ID marsh plants

* Helpful hint: I do not recommend walking around in a salt marsh, they can be tricky places if you’ve never done it before! Instead, try visiting an educational facility with trails to experience the marsh. Some great marshes to visit are at St. Jones Reserve or Bombay Hook


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wetland-assessments

Status and Trends: Stormwater Ponds

Written on: May 27th, 2021 in Wetland Assessments

By Alison Rogerson, DNREC’s Wetland Monitoring and Assessment Program

In March we shared some results about the status of wetland acreage in Delaware between 2007 and 2017. This time we’re taking a closer look at the increasing number of stormwater ponds popping up across the state. Is this a good trend or something to be concerned about? How do ponds relate to wetland health?


You pass stormwater ponds every day. Along State Highway Route 1, next to the shopping center parking lot, or at the entrance of your neighborhood. Stormwater ponds are ubiquitous with development and we have a lot of development in Delaware.

Photo Credit: Environmental Protection Agency

In fact, between 2007 and 2017 Delaware experienced an increase of 1,260 acres of man-made retention or stormwater ponds around housing developments, ponds in industrial areas, or agricultural ponds. This represents 81% of all the acres of wetlands created, or gained, in this time period. The majority of open water gains occurred in Sussex County.

What is the issue with building more stormwater ponds and what does it have to do with wetlands? It just so happens that at the same time Delaware gained 1,260 acres of open water ponds, it lost 655 acres of freshwater wetlands, mostly forested, to development. In many cases, forested freshwater wetlands were lost to development and new developments require stormwater management, often as ponds.

Photo Credit: DelDOT

Unfortunately, created ponds do not function the same way natural, forested wetlands do. Man-made open water ponds offer stormwater holding capacity, but don’t offer the same filtration and slow release into natural waterways that floodplain wetlands do. Stormwater ponds can be used by generalist wildlife species such as red-winged blackbirds or mallards, but do not offer the specialized habitat qualities that Delaware’s wetlands can provide. Created ponds offer little in the way of plant community, often cattails or the invasive Phragmites, whereas natural wetlands provide a rich array of beneficial plants.

I wish I could say this trend of increasing stormwater ponds and decreasing wetlands was just a recent occurrence, but similar changes were observed in previous decades as well. According to our previous statewide mapping update and analysis done for 1992-2007, gains in ponds exceeded gains of any other wetland type by 115%.

Do we need stormwater ponds? Yes. Especially as weather patterns become more extreme, bringing heavy rain events upon us in Delaware, we need infrastructure to quickly handle flash events and heavy stormwater loads. Stormwater management keeps our roads and neighborhoods from flooding, and can prevent backups that lead to polluted waters being released.

However, it is not appropriate to replace natural wetlands with stormwater ponds in the name of development. The trade-off in functions and natural services does not add up. In addition, stormwater infrastructure has been modernized to more naturally offer storage and filtration services that are visually appealing.

Green stormwater infrastructure features can be planted with native trees and shrubs and may sit dry until a storm event. These structures are still ready and waiting to hold and manage storm events, but allow the soil and plants to play a beneficial role. Bioretention gardens are smaller features that can be incorporated into landscaping that are enjoyable to look at.

For more information on Green Stormwater Infrastructure visit this USGS webpage.


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wetland-restorations

WATAR You Up To?

Written on: May 17th, 2021 in Wetland Restoration

By Maggie Pletta, DNREC’s Coastal, Climate and Energy

Delaware is known for many things… like being first, Joe Biden, and horseshoe crabs. However, there are a few less flattering things that Delaware is known for, and one is a history of polluted waterways.

Adobe stock photo of the Christina River

A large number of Delaware’s waterbodies have a fish consumption advisory, with some of the strictest advisories in place on the tidal Christina and Brandywine Rivers. But starting in spring 2021, the DNREC Watershed Approach to Toxics Assessment and Restoration (WATAR) program is looking to change that and is embarking on an initiative to improve the waters of the Christina and Brandywine Rivers

The project is titled CBR4, which stands for “Christina & Brandywine River Remediation, Restoration, and Resilience.” The goal of the project is to address legacy toxic impacts within the watershed, and within the waterways themselves, to make the rivers drinkable, swimmable, and fishable in the shortest timeframe possible.

A Long History

Brandywine River, Photo Credit: Simon (flickr)

The Christina and Brandywine Rivers have played a pivotal role in the region’s economy and character since before the Swedes first arrived on the original Kalmar Nyckel in 1638. The river already was part of a route of warfare and trade between the Lenape (Delaware) Indians along the Delaware River (and tributaries like the Brandywine and Christina) and the Minqua (Susquehannock) Indians on the Susquehanna River to the west. When the Swedes sailed up the Delaware River and arrived at the mouth of the Christina River in Wilmington, they found an ideal port location to ship trade goods and supplies between the colonies and Sweden. Not only did the site provide easy access to shipping channels, but it also provided access to the Brandywine, where shad and shellfish abounded. Unfortunately, like many natural resources, as more colonists arrived, the rivers slowly became polluted. 

During the industrial revolution, the Christina and Brandywine riverfronts became populated by heavy industry, including shipbuilding, tanneries, and chemical factories. While these industries provided jobs for many, they also left heavy metals, polychlorinated biphenyls (PCBs), and other hazardous substances in the soil and waterways. Many of these are considered persistent, bio-accumulative, and toxic (PBT) compounds. As industries slowly shifted out of Wilmington, they left behind their toxic legacy. Neighborhoods that had developed along these rivers remained, and residents were subject to the environmental and economic impacts of this legacy.

Why now?

CBR4 Remediation Photograph

In the 1990s, the state and federal government began to remediate the many brownfields and superfund sites along the rivers. While there have been successes, there is still a long way to go until the rivers are swimmable, fishable, and drinkable again.

Thanks to decades of this previous work, the clean-up of many of the land-based pollutant sources have been completed, and concentrations of PBTs in the water and fish have been dropping. The time is now to begin the long planning process to clean up the waterways’ sediments while the last remaining land-based sources of pollutants are controlled.

Over the next two years, the WATAR team and the Delaware Coastal Program, Christina Conservancy, American Rivers, Brightfields Inc., Sarver Ecological, and the Delaware Nature Society will be creating a comprehensive plan to combine sediment remediation with ecological restoration/coastal resilience projects within the CBR4 project area.

Upon completion, the WATAR team will begin the more extended, arduous task of implementing the plan’s actions. While potentially complex and daunting, the team is ready and eager to lead the charge to return the Christina and Brandywine Rivers to their former glory.

For more information about CBR4, visit https://dnrec.alpha.delaware.gov/waste-hazardous/remediation/watar/.


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