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Posts Tagged ‘monitoring

03
Mar

The following post is a guest blog entry from Eric Martin, a Coro Fellow who interned with Nine Mile Run for the last eight weeks.

Hello!

My name is Eric Martin and I am currently working at Nine Mile Run as part of my nine month long experience as a Coro Fellow. What is the Coro Fellowship in Public Affairs? The Coro Fellowship is a leadership development program in Pittsburgh for young adults who want to pursue a career in public affairs. The Fellowship is focused on training individuals who, as citizens and leaders, will all their lives act constructively and competently to build up and improve their communities and society as a whole.

I am originally from Fairmont, WV and graduated in 2010 from West Virginia University with a Bachelor of Science degree in Industrial Engineering. In my time since graduating, I have been fortunate enough to have been able to work in short, but connected, experiences that have allowed me to live in other parts of the country and the world while gaining a wide range of skills. Before joining Nine Mile Run for my eight week placement, I was placed at the Pittsburgh Cultural Trust, where I was tasked with consulting and recommending improvements to their Operations Department.

Eric helps sample water in Nine Mile Run

Eric helps sample water in Nine Mile Run

At Nine Mile Run, I have been fortunate enough to be thrown right in the mix! On my second day, I found myself in the heart of the Nine Mile Run stream helping Maranda and Abbey with our monthly stream sampling. It is unbelievable to think that that was during the second week of January and it is now almost March, and my time here is almost over. In between, I have helped with marketing and project initiatives with Mike, accounting with Lindsey-Rose, learned how to build rain barrels with Paul, attended Clean Rivers Campaign meetings with Brenda, and worked a lot with Jared and the StormWorks crew! Phew!

I want to thank everyone here for being so welcoming and nice! I have felt right at home and a part of the team from the moment I started working here. My hope is that I have helped here in some way and will continue helping to advance the mission of Nine Mile Run in my final weeks here as well as moving forward in my career!

11
Feb

This guest post was written by Rob Rossi, a graduate student in the department of Geology and Environmental Science at the University of Pittsburgh. He was a graduate summer intern of NMRWA in 2015.

Road salt is a common part of winter for many Pittsburgh residents.  In Pennsylvania, more than 840,000 tons of road salt (sodium chloride, or table salt) were applied to roadways between 2009 and 2014.  Although it helps keep our roads and sidewalks ice and snow free, road salt has unintended consequences.  Many people are familiar with the ever annoying winter problems of salt stained clothing or shoes/boots, but the environmental effects of road salt are less obvious.  Road salt can have numerous negative effects on the environment, such as increased fresh water and soil salinity, and less obvious effects, such as increased time necessary for rain to soak into the soil.  Additionally, when road salt dissolves in highway runoff, these waters have high total dissolved solids (TDS), which can flush roadside soil metals from clay particles  (see animated Figure 1).  Metals flushed by these reactions can include plant nutrients (e.g., potassium, calcium, magnesium) or toxic trace metals (e.g., arsenic, lead, cadmium).

Road salt exchange gif

Figure 1. Animation of a cation exchange reaction. Potassium (K), calcium (Ca), and magnesium (Mg) ions bound to soil clay particles are exchanged by sodium (Na) ions in solution. Mobilized metals are then released into the soil water, and ultimately the ground or surface water.

Road Salt Study in Nine Mile Run

Lysimeter Working

Figure 2. Lysimeters are plastic tubes with a ceramic cup. To collect a soil water sample, a scientist applies a vacuum (arrow) and the lysimeter sucks up soil water (dashed lines) like a straw.

Rob Rossi, a graduate student in the Department of Geology and Environmental Science at the University of Pittsburgh, has been researching the effects of road salt on roadside soils in Nine Mile Run.  Specifically, Rob has been analyzing soil and soil water chemistry in samples collected from three roadside soil water sampler “nests”.  Each nest is a group of four lysimeters which behave much like giant straws, sucking up soil water samples when a vacuum is applied to the end of the soil water sampler (see Figure 2).  The lysimeters collect soil water at roughly 6, 12, 24, and 36 inch depths along a hill slope perpendicular to I-376.

In the soil samples, soil sodium concentrations are highest in soils collected from near the road.  Soil sodium concentrations decrease with distance from the roadway, approaching values observed in the local bedrock (see Figure 3).  One theory is that high sodium concentrations can be attributed to the minerals breaking down in the bedrock but because sodium concentrations in roadside soils are much higher than sodium concentrations found in the bedrock, minerals in the bedrock breaking down is likely not what inputs sodium to these soils.  Instead, the application of road salt to I-376 is likely causing high sodium concentrations in roadside soils.

Sodium concentration chart

Figure 3. Sodium concentrations in the sampled top (black), mid (red), and bottom (grey) hillslope soils. The vertical dashed line indicates the average sodium concentration in local bedrock. Parts per million (ppm) is a measurement scientists use to describe the concentration of an element. In other words, if a bucket holding a total of 1 million marbles contained 100 ppm of blue marbles, 100 of those 1 million marbles would be blue marbles.

Sodium concentrations in sampled soil waters peak at different times throughout the year relative to the location along the hillslope (see Figure 4).  In particular, the earliest peaks in soil water sodium concentrations occur in the top hillslope soil waters in late February/early March in the intermediate depth (39 and 61 cm depth) soil waters.  Additionally, soil water samples from the deepest top hillslope nest have, in general, the highest sodium concentration.  While sodium concentrations spike in soil waters collected from all depths of the top hillslope nest station, soil water sodium concentrations peak only in deeper soil waters of the mid hillslope nest.  Moreover, the peak in soil water sodium concentrations at the mid hillslope nest do not peak at the same time as when soil water sodium concentrations peak at the top hillslope nest.

NaTime

Figure 4. Sodium concentrations in top (a), mid (b), and bottom (c) hillslope soil waters collected between October 2013 and November 2014. The light blue box indicates the time of the year when road salt is not applied to roadways.

These patterns in soil water sodium concentrations suggest that the way soil water flows in roadside soils influences the movement of sodium through these soils.  Specifically, because the deeper top hillslope lysimeters (i.e., 12, 24, and 36 inch) peak before the shallowest (i.e., 6 inch) lysimeter, high TDS waters likely interact with deeper soils first.  High TDS runoff from the highway is often observed to enter the soil column via infiltration (i.e., water percolating downwards through the soil), which produces a peak in sodium concentrations in the shallowest soil waters first.  However, because this pattern in soil water sodium concentrations is not observed in samples collected from the Nine Mile Run transect, sodium is potentially transported to deeper soils via lateral flow originating from leaking highway drains and water flow between bedrock layers.

Previous scientific studies have observed that sodium loadings to soils persist beyond the period when road salt is applied to roadways, and this relationship is also apparent at this study site.  Specifically, sodium persists as slow moving wave, where peaks in top hillslope soil water sodium concentrations occur within a month of when road salting ends, and peaks in soil water sodium concentrations at the mid and bottom hillslope stations occur later in the year.  Thus, the distance from the roadside affects when soil water sodium concentrations will peak, suggesting that sodium is relatively slowly released from roadside soils throughout the spring and summer.

How does road salt affect the water quality of Nine Mile Run?

The results of this study suggest that sodium and metals are continually flushed to stream waters throughout the year. When sodium levels are high, the ecosystem cannot physiologically maintain a salt balance, which affects aquatic organisms living in the stream – particularly plants and animals that are not adapted to high concentrations of ions, and therefore cannot regulate the water and salt content within their cells. This stress can change the diversity of species within the ecosystem. The increased metal loading could impair the stream ecosystem, negatively impacting aquatic life such as fish.  Some metals may be either beneficial or toxic, depending on their concentration. The primary mechanism for toxicity to organisms that live in streams is by absorption or uptake across the gills. The metals that are most toxic to aquatic organisms are Copper, Iron, Cadmium, Zinc, Mercury, and Lead.

I-376 Sodium runoff model

Figure 5. A conceptual model of how sodium travels through the hill slope soils next to I-376. The color of the arrows indicates the relative timing of when sodium is transported via this flowpath. Blue occurs in mid to late February, dark grey in early March, orange in early May, and red in early August.

Thus, it is likely that road salt application impacts soils down the hillside of I-376, and that the negative impacts of road salt application are not limited to the winter and early spring.

27
May

As you may have seen in our Spring newsletter, since 2013 we have been working with the Pittsburgh Parks Conservancy (PPC) on a grant received from the National Fish and Wildlife Foundation’s Five Star and Urban Waters Restoration Program. One of the goals of our partnership on this grant was to develop a culture of stewardship for the Nine Mile Run watershed by engaging a wide range of ages in citizen science and stewardship activities. One way we approached this was to implement PPC’s Mission Ground Truth (MGT) program at Wilkinsburg Middle School.

MGT is an interdisciplinary ecosystem assessment program mapped to PA state academic standards for 7th and 8th grade students that includes in-class discovery activities as well as a field trip to Frick Park. During the field trip, students get to be ecologists for the day, and have the opportunity to use the same tools and sampling methods that scientists use to evaluate the health of forest and stream ecosystems.

Recently, NMRWA staff worked for two days in Frick Park with Environmental Educators from PPC to help lead the Wilkinsburg Middle School students through the field day programming.

Jared, Mike, & the students get ready for a leaf race!

Jared, Mike, & the students get ready for a leaf race!

We began each morning by discussing goals for the day, then broke into small groups. During the morning session, the groups each explored a section of the Fern Hollow stream while discussing questions such as “how can ecologists detect and measure pollution in a stream?” and “what benefits do humans and animals get from streams?” Then the students recorded data on physical and chemical water quality characteristics, such as temperature, pH, dissolved oxygen, conductivity, and velocity. Next, we explored the benthic macroinvertebrate populations by carefully overturning rocks and collecting samples using a net. To wrap up, we would discuss how everything tied together by asking questions like “based on the data we collected, is the stream healthy or unhealthy?“and “how does the quality of Fern Hollow affect the health of Nine Mile Run?

Mike & a student measure the diameter of a tree.

Mike & a student measure the diameter of a tree.

After a break for lunch, the students got to venture into the forest for a deeper look at the complex forest ecology present in Frick Park. We identified different tree and plant species and talked about the various ecosystem services that forests provide to animals, streams, and people. We asked questions like “why is biodiversity important in forests?” and “how is the health of this forest related to the health of Fern Hollow and Nine Mile Run?” Then the students used forestry tools to collect data on the location, size, and type of trees, and we looked for evidence of Asian long-horned beetles. To wrap up, we asked questions similar to the morning session, like “is this section of the forest healthy or unhealthy?

Over the course of the two days, we had a wonderful & enriching experience working with the students and with the PPC staff. Thank you to Mike, Taiji, Steve, and Chelsea for their expertise & enthusiasm in implementing the MGT programming!

27
Apr

For the past two years, NMRWA has been working with the Pittsburgh Parks Conservancy (PPC) to increase the environmental stewardship capacity of our watershed community. Funding for this work was provided by a grant received from the National Fish and Wildlife Foundation’s Five Star and Urban Waters Restoration Program. Maybe you read about this in our recently released Spring newsletter?

Yesterday, as a part this program, NMRWA staff co-led a training workshop for Urban EcoStewards on streamflow monitoring in Nine Mile Run. Along with Sarah Lavin, a graduate student in the Department of Geology and Planetary Science at the University of Pittsburgh, Sara Powell & Paul Yanulavich spent a sunny Sunday morning working with eight volunteers to measure streamflow and take cross-section measurements of the stream.

It is important for us to understand streamflow patterns and how the stream channel is changing in Nine Mile Run, both for continued restoration efforts in Frick Park (e.g., erosion remediation), and also so we can assess how well management efforts in the upper watershed (e.g., green stormwater infrastructure, rain barrels) are reducing excess stormwater flows into the stream.

Unfortunately, continuous monitoring of discharge (the volume of water flowing through the stream during a unit of time) is complex and expensive. Instead, since last summer, we have been working with Urban EcoSteward (UES) volunteers to help us collect data that will allow us to create something called a stage-discharge rating curve.

This curve will allow us to ‘reconstruct’ a continuous discharge record – giving us a much better understanding of streamflow in Nine Mile Run!

So, at Sunday’s training, we demonstrated how UES volunteers can measure the stream’s velocity and cross-sectional area – two critical pieces to calculating discharge. We then used similar methods to measure the stream channel geometry.

The geometry of the channel is also important to understand, because storms can cause large volumes of water to surge rapidly through Nine Mile Run, changing the stream channel shape very quickly. These changes, whether they are due to erosion or damage to built rock features, put our restoration efforts at risk. Regular cross-section measurements will allow us to look at how the shape of the stream channel is changing over time, and to apply necessary management efforts as needed.

Thank you so much to all the Urban EcoStewards and interested volunteers for coming out on Sunday! We will be posting more photos from the day on our Facebook page, so make sure to check them out!

If you are interested in becoming an Urban EcoSteward, click here for more information or email .

 

05
Nov

People are often surprised to learn that yes, there are fish living in Nine Mile Run and in fact… there are rather a LOT of them!

Led by NMRWA Monitoring Committee members Brady Porter and Michael Koryak, fish sampling is performed on an annual basis, typically in the fall. Since the stream restoration was completed in 2006, their data have shown marked improvement in the number and diversity of fish in the stream.

Immediately post-restoration, the entire stream was electro-fished and only 116 fish comprising seven different species were found. Today, it’s impossible to sample the entire length of the stream in one day due to the number of fish and time it would take to process them all!

For example, last Wednesday, NMRWA Monitoring Committee members and other volunteers sampled for fish in lower Nine Mile Run. Beginning at the mouth of the stream near Duck Hollow in the morning, and traveling upstream to finish just below the pedestrian bridge in the late afternoon, we caught nearly 2,300 fish comprising 17 different species! This is the second highest species count ever found in this section of the stream – 21 species were found in 2011.

Additionally, we found two new species that had never been collected from Nine Mile Run before: Gizzard shad and Silverjaw minnows. The addition of these two species brings the total species count of fish collected from this stretch of Nine Mile Run since 1999 to 30!

This week, barring inclement weather, we will finish our fish sampling for the year when we sample a section of the stream in the main part of Frick Park.

As always, thanks to Brady and Mike and all the volunteers who help make this important sampling effort happen!

Want to learn more about our stream monitoring work? Head on over to our monitoring page for more information and nifty, interactive data maps!

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