Watershed Symposium 2017

KEYNOTE Unveiling the Anthropocene—A Super Wicked Story

Humanity’s disruption of the planetary climate system represents an existential threat to an organized global community. This is the robust conclusion of an extraordinarily large scientific community, based on an observational dataset of unprecedented scale. And yet, global climate disruption is but one of a host of existential environmental challenges we face, all emergent from the same underlying pathologies. At this juncture, with an unprecedented opportunity to begin the transformation to a truly sustainable human civilization, it is critical that we address our challenges holistically, each in context of all the others. Fortunately, solid frameworks are emerging for doing exactly this.

Year in Review: Comparing Harmful Algal Blooms from this Year to Last

Following an unprecedented year of harmful algal blooms (HABs), 2017, it was hoped, would provide a relief from these events. For some waterbodies, conditions had improved compared to 2016, but for others, conditions may have deteriorated. This discussion will compare 2017 HABs to last year-- exploring differences in diversity and concentration of cyanobacteria and their cyanotoxins. Additionally, it will cover the latest techniques adopted by UDWQ for tracking these events and the latest coordination processes implemented this year.

Deciphering Cyano-blooms Using Molecular Approaches in Utah Lake

Summary:
This abstract will present findings on our continuous monitoring of Utah Lake and tracking the diversity of Cyano Blooms with the help from Utah Division of Water Quality. .

Full Abstract:
Although there are several environmental problems associated with HABs, the presence of CyanoHABs is of particular importance because certain species of cyanoHABs produce cynotoxins which have direct health related negative implications. CyanoHABs cause serious environmental and economic losses. Shallow, eutrophic Utah Lake encountered an extreme algal bloom event in the summer of 2016. As for the summer of 2017, an algal bloom event was identified in one location at the lake, Provo Bay. Conventionally, microscopic identification is used as the main method for phytoplankton identification. However, microscopic counting methods are time-consuming and results given are in low resolution and can overlook smaller cyanobacteria. For example, light microscope techniques usually exclude the study of picocyanbacteria because of the lack of its morphological knowledge (Ouellette et al., 2005) and the small size of picocyanobateria (0.2 to 2.0 μm) (Jakubowska and Szeląg-Wasielewska, 2015). Morover, microscopic methods may not be able to differentiate between toxin-producing and non-toxin producing strains. For example, different strains of Microcystis aeruginosa can be morphologically identical but differ in toxigenicity (Otsuka et al., 1999). To overcome these problems, we have applied molecular methods for cyanobacterial speciation by sequencing all the bacterial DNA from water and sediment samples as well as targeting dominant species in Utah Lake by quantitive PCR. To establish the presence with their functionality, we have been also extracting mRNA and tracking gene expressions. Five sites were monitored in 2016 and cyanobacterial communities were genetically identified via high throughput amplicon sequencing. Similarly, seven sites were monitored in summer 2017. Sediments were collected in August of 2016 and August of 2017. Our findings for summer of 2016 show that temperature and chlorophyll a increased throughout. Nutrients and pH were the highest during the bloom. As for cyanobacteria identification via high throughput amplicon sequencing, Aphanizomenon flos-aquae and Synechocuccos sp (picocyanobacteria) dominated the water column. As for sediment cyanobacteria identification, Aphanizomenon flos-aquae dominated. Furthermore, sediments were dominated by Ca-bound phosphorus and sediment mineralogy contained around 70% calcite. As for summer of 2017 findings, pH, temperature and chlorophyll a increased significantly from early May to mid July. In Provo Bay where algal blooms appeared in 2017, nitrate was significantly reduced while the phosphate was high. Blooms faded towards the end of summer in Provo Bay. In addition, DNA was extracted for each site in 2017 for sequencing and cyanobacterial speciation analysis. Dominant gene expressions are detected by extracting mRNA. By analyzing our collected biological and chemcical data from both summers, we can get a better understanding of algal and cyanobacteria bloom occurences at Utah Lake and capable of determining ecosystem tipping point. Audience will be able to learn; (1) What is CyanoHABs and why they form, (2) what environmental factors trigger their formation, (3) what is the ecological diversity with seasonal changes and (4) how citizens can be involved in ongoing efforts to address water quality problems in Utah.

Urban Stormwater Impacts on the Jordan River: Who Could Have Guessed?

Summary:
Stormwater impacts have been shown to be significant and should be mitigated to increase DO and improve overall water quality in the Lower Jordan River.

Full Abstract:
In 2012 the Utah Department of Environmental Quality completed a total maximum daily load study on the Jordan River that concluded dissolved oxygen levels throughout the Lower Jordan are often below those necessary for the established beneficial use due to various sources of course particulate organic matter. A study by Richardson in 2014 evaluated the leaching of dissolved organic carbon (DOC) from coarse particulate matter entering storm drains during runoff events. His study found that the DOC generated from terrestrial grass and leaf debris in stormwater was readily biodegradable with a high long-term biochemical oxygen demand (BOD). To determine the extent that stormwater is responsible for the low DO in the Lower Jordan River, continuous data collected by an iUTAH aquatic monitoring station at the storm drain outlet at 1300 South were paired with lab results to quantify pollutant loads during both dry periods and storm events. Parameters available for continuous monitoring included fluorescent dissolved organic matter (fDOM) and specific conductivity, both of which dramatically spike during storm events. An Isco autosampler was installed at the site and programmed to begin sampling when certain thresholds of these parameters were met. These grab samples were brought back to the lab are analyzed for BOD, DOC, metals, phosphorous and nitrogen - all parameters that cannot be continuously measured with the installed probes. The goal was to then connect these values, particularly BOD and DOC, to the continuous parameters, particularly fDOM, available at the aquatic monitoring site, to determine correlations between continuous monitoring and lab generated data. These correlations were then used to estimate the fluctuations of BOD and DOC using continuous fDOM measurements in both the stormwater discharge and in the Lower Jordan River measured upstream from 1300 South. This presentation will highlight the fDOM/DOC/BOD relationships established for the 1300 South stormwater discharge and upstream in the Jordan River, will present the significant impact of the stormwater discharge to the Jordan during rainfall events, and will explore various green infrastructure approaches that could be implemented in the watershed to mitigate this impact over time.

Estimation of Future Sediment Load in the Jordan River

Summary:
Climate change and urbanization will modify hydrological processes in mountainous watersheds. Associated increases in erosion and acceleration of sediment transport will have direct impacts on water treatment processes, reservoir management, and the life cycle of aquatic species.

Full Abstract:
Sediment load from a watershed impacts soil carbon dynamics, life of the aquatic systems, water treatment processes, and reservoir planning and management. Multiple factors including climate, local biophysical environment, topography, land use, and land management practice have direct and indirect effects on the sedimentation-loading rate. This study investigates how erosion and acceleration of sediment transport in a mountainous watershed respond to land use change and increased peak streamflow due to a higher intensity of precipitation and escalated snowmelt. Results are presented for future land use change and climate change in the Jordan River watershed, including projected changes in sediment loads in the Jordan River for the decades centered on 2040 and 2090. The Weather Research and Forecasting (WRF) regional climate model was used to dynamically downscale future climate variables to 4-km horizontal resolution at hourly intervals under the Representative Concentration Pathway (RCP) 6.0 greenhouse gas emission scenario for 2090s, and additional climate forcing scenarios were obtained from statistical downscaling. Future land use was modeled using a spatial interaction model (business-as-usual growth) and a “regional vision” normative growth scenario with broad stakeholder currency (compact-growth). The runoff and water quality impact of the climate and land-use change scenarios were simulated using the HSPF model (Hydrological Simulation Program-FORTRAN). The results suggest that future precipitation in the watershed will increase ~20-30%, temperature will increase 1.5-6.0⁰C (depending on emission scenario), and snowfall and snowpack will decline by 25 to 50%. Impervious areas will grow by 19% and 3% in the business-as-usual and compact growth scenarios, respectively. The preliminary model results show that future annual sediment load will increase ~25-30% by 2040s and ~35% by 2090s. The results suggest that climate change will be the dominant driver, responsible for increasing sediment load by ~20-25% over the 2000 baseline; land use change is less significant, accounting for a ~5% increase. The presentation will also cover the estimated sediment loads considering multiple future changes scenarios (i.e. land use change alone, climate change alone, etc.). The learning objectives from this presentations will be to: (i) understand sedimentation building and wash off processes in a watershed, (ii) become informed on changes in future climate modeling and land use in Jordan basin, particularly with the HSPF model, and (iii) understand the impact of climate change and land use change on hydrological process and resulting indirect impact on the sedimentation processes in Jordan River. Keywords: climate change, land use change, hydrological modeling, sediment load, water quality

The poster session is a forum for presenters from around the world to highlight programs and to share successful ideas with colleagues by presenting a research study, a practical problem-solving effort, an innovative program, and more. Poster presentations provide other conference participants an opportunity to quickly and easily become acquainted with a variety of topics.

Check the POSTERS tab to see all poster presenters!

Evidence of groundwater connectivity in the Jordan River, Utah, USA

Summary:
We explored whether groundwater connectivity is evident in the Jordan River, where wastewater effluent represents ~ 25-40% of total flow. Concentrations of unreactive anions and cations, dissolved inorganic carbon, and isotopic signatures of water suggest that groundwater inputs continue to play an important role in riverine water quality.

Full Abstract:
Arid and semi-arid regions face increasing challenges for provisioning water for human consumption and ecosystem services under a changing climate and population growth. The role of urban water diversions and inputs on water quality in rivers remains poorly understood in many cities. We explored whether historic surface and groundwater connectivity is still evident in the water quality of the Jordan River, where wastewater effluent represents ~ 25-40% of total flow. The Jordan River is an 83 km, 4th order river that traverses the Salt Lake Valley in the state of Utah, USA. The river drains seven montane tributaries and connects Utah Lake to wetlands of the Great Salt Lake. Area urban water systems include four facilities collecting drinking water from the montane tributaries and four facilities treating wastewater (WRFs), which discharge effluent into the Jordan River. A major drainage canal diverts river water to prevent flooding of densely populated areas. The high degree of connectivity between natural and human systems in this area contributes to large spatial and temporal variation in water discharge, temperature, dissolved oxygen, pH, major ions, and isotopic signatures of water and dissolved inorganic carbon. Synoptic surveys of the river conducted over three seasons during one year show that variation in discharge (0.9-17.9 m3/s) and temperature (12.4-27.2 °C) were associated with snowmelt runoff, river regulation, and effluent inputs. Dissolved oxygen ranged from 2-21 mg/L, with a consistent decline in values each season from 10 mg/L to 2 mg/L below the surplus canal diversion. Values of pH ranged from 7.0-8.8, with circumneutral values found in WRF effluent and the oil drain downstream of the most northern WRF studied. We observed variation in concentrations of unreactive anions and cations (e.g., 42.3-111.3 mg/L calcium and 8.8-87.5 mg/L magnesium), concentration of dissolved inorganic carbon (25.1-97.7 mg/L), and isotopic signatures of δ13C (-4.9 to -11.9), δ2H (-45.6 to -115.9), and δ18O (-2.6 to -15.2, suggesting that seasonal shifts in the proportion of snowmelt vs. groundwater inputs or in-stream processes continue to play an important role in determining the water quality of the river. That groundwater continues to influence water quality in this urbanized river despite the highly engineered context is notable, especially since groundwater has been estimated to be a small fraction of total inputs. Taken together, our results suggest that effluent-dominated rivers can be strongly influenced by human modifications to surface water but also still be connected to the regional hydrologic basin via groundwater exchange. This implies that resource managers may need to account for the quality and quantity of not only surface waters but also historically overlooked groundwater inputs, in order to address water quality concerns and pollution exceedances in urban rivers.

Tracking Urban Water Flow Using Stable Isotopes of Water

Summary:
With increasing population and water demands, water managers are utilizing local, non-local and recycled water to supply urban water systems. Using water isotopes, here we present a novel way of tracking different water sources in an urban system, which is extremely important in context of water rights and contamination issues.

Full Abstract:
Stable isotopes of water have extensively been used to understand hydrological cycle in natural environment, however their application in highly managed urban water systems have been limited. Recent research has shown that water isotopes reflect urban water management practices and have potential application in understanding urban water supply network dynamics, evaluating effect of climate variability on water resources, geolocation and water monitoring and regulation. Previous work has highlighted strong and structured spatiotemporal variation in tap water isotope ratios of Salt Lake Valley (SLV) which has been attributed to complex distribution systems, varying water management practices and multiple sources used across the valley. Building on these observations, we collaborated with the largest water supply company in SLV, Jordan Valley Water Conservancy District (JVWCD) and expanded our project which now includes predicting the source (or sources) contributing to a given supply area. The different sources supplying JVWCD (such as Provo River system, Wasatch Creeks and groundwater wells) have similar yet distinct isotope ratios, providing an excellent opportunity to test the robustness of water isotopes in monitoring distribution pattern of the sources in the supply system. For this project, we collected more than 100 samples/month (between April 2015-May 2016), from different water sources (creeks, streams and groundwater wells), water treatment plants (WTP), storage reservoirs and delivery locations along the supply lines across the water distribution area, measured their isotopic ratio and developed isotopic mixing models using Hierarchical Bayesian (HB) framework to connect the different sources in the system to their supply area. In this study, we have used water isotopes to quantify the proportion of water supplied by different sources at various locations within the supply system. We have explicitly incorporated volumetric and spatial effects to constrain the contribution of each source, thus addressing identifiability issues associated with partitioning multiple sources with only two isotopes (δ2H and δ18O). Our initial results are in close agreement with those obtained by physical models used by JVWCD. Our result suggests that isotopes open a new line of investigative technique to analyze urban water systems which does not require details of the supply system information. HB isotopic models can be extremely useful in systems where the supply information is missing, or are proprietary. In general, comparing the results from the isotope model can help improve the robustness of the existing physical models. Considering the fact that isotopic measurements have become fairly easy and cheap, coupling the physical supply models with isotope data in future can make urban water supply systems analysis more robust and accurate. The only requirement for robust estimates from isotopic models is the presence of sufficient isotopic variations between the different sources in the system. In systems with sources having comparable or similar isotope values, the robustness of the estimates will be questionable.

Critical Outcomes, Lasting Impact: 5 Years of Science for Utah's Water Future

In this series of 5 presentations, research and education/outreach leads for iUTAH, a statewide, NSF-funded infrastructure-building project, present important outcomes and lasting impacts of the research, training, education and outreach activities conducted by iUTAH's 800+ current and former participants, 10 participating institutions of higher education, and over 100 partner organizations.

Full Abstracts:
* denotes presenter

I. Transcending system boundaries through integrative ecohydrologic research
Dr. Zachary T. Aanderud*, Brigham Young University, Amber Spackman Jones, Utah State University, Jeffery S. Horsburgh, Utah State University, David Eiriksson, University of Utah, Dylan Dastrup, Brigham Young University, Christopher Cox, Utah State University, Scott Jones, Utah State University, David Bowling, University of Utah, Jobie Carlisle, Utah State University, Greg Carling, Brigham Young University, and Michelle A. Baker, Utah State University

The effects of urbanization on water quality vary in time and are extremely hard to capture. Further, in the semi-arid Western U.S., variable snowpack levels due to a warming climate, seasonal flows from agriculture run-off, and unprecedented population growth and water use in metropolitan areas may create rapid changes in water quality. To more fully understand the temporal impact of urbanization on water resources, we created a real-time observatory network spanning three watersheds in northern Utah which possess similar climates and a common water source, mountain winter-derived precipitation, but differ levels of urbanization. The aquatic monitoring stations in the GAMUT Network include sensors to measure chemical (dissolved oxygen, specific conductance, pH, nitrate, and fluorescent dissolved organic matter, (fDOM)), physical (stage, temperature, and turbidity), and biological components (chlorophyll content and phycocyanin) logging every 15 minutes. As fall transitioned to winter, our high frequency water quality data captured runoff events in urbanized areas carrying pulses of nutrients and organic matter to rivers. In Red Butte Creek, the most urbanized of the GAMUT watersheds, pulses of fDOM occurred 22 times over a three-month period, sometimes lasting up to 3 days. By comparison, levels of fDOM remained relatively constant around 30 quinine sulfate units (QSU) in the Provo River and 1.5 QSU in the Logan River over the same time period. Further, urbanization led to more blooms demonstrated by Red Butte Creek experiencing 236 cyanobacteria blooms, measured as changes in phycocyanin. Over the same time period, 75 green algal blooms occurred, which increased chlorophyll-a concentrations an average of 313% per day compared to days without elevated levels. Photosynthetic pigment spikes were also present in the Provo River from mid-November to the end of December but to a much lesser extent (33 algal and 11 cyanobacterial). Our findings suggest that the built infrastructure, high percentages of impervious surfaces, and multiple storm drain outfalls that often accompanies the urbanization of rivers may lead to the flashier changes in water quality.


II. Innovations and integration in social and engineering water science
Dr. Courtney G. Flint*, Utah State University

iUTAH’s social and engineering water science investigated the drivers of water and land use management in the Wasatch Region Metropolitan Area as well as how natural, built, and social structures interact in the water system. We explored the potential for green infrastructure to improve water sustainability and modeled the impacts of urban growth and planning. Using innovative methods for integrating data representing water perspectives, alternatives, and actions across a diverse set of stakeholders, we have informed decision-making throughout Utah’s water system.


III. Coupling the human-natural water system: five years of participatory modeling and innovative visualization
Dr. Courtenay Strong*, University of Utah, and Dr. Sarah E. Null, Utah State University

iUTAH research on coupled human-natural water system modeling builds on Utah’s strengths in hydrologic modeling to enhance forecasting capabilities for water managers and stakeholders. Our teams have created new models and linked previously disparate models and data sets to investigate system processes and future water outcomes focused on supply, demand, quality, and ecosystem services. New capabilities include agent-based modeling of households, a framework for decadal-scale water supply criticality analysis, the HydroCouple Software framework which enables linkage of diverse modeling frameworks, methods for optimizing strategies for infrastructure changes such as water barrier removal, and impactful visualization technologies.

 
IV. Cyberinfrastructure to support large scale, collaborative water research in Utah: critical outcomes from the iUTAH project
Dr. Jeff Horsburgh, Utah State University, and Amber Spackman Jones*, Utah State University

iUTAH (innovative Urban Transitions and Aridregion Hydro-sustainability) is a statewide effort focused on water sustainability in Utah. Synthesis of diverse data collection and modeling by cross-disciplinary and cross-institutional research teams, such as those working on the iUTAH project, requires storage, software, networking, computational, and human resources. Over the past 5 years, our team has built cyberinfrastructure to support the full data life cycle and increase capacity for data collection, organization, management, sharing, synthesis to higher-level products, and integration with models. iUTAH cyberinfrastructure is comprised of hardware and software systems that have enabled iUTAH researchers and partners to share data, models, and other digital resources. This includes cyberinfrastructure deployed for management of streaming sensor data from iUTAH’s Gradients Along Mountain to Urban Transitions (GAMUT) network of aquatic and terrestrial monitoring sites, databases and web applications supporting publication of water quality and biological data derived from samples, tools for interactive dissemination of extensive social science survey datasets, and a sharing and publication workflow for the various other types of data collected by iUTAH researchers. In this presentation, we describe the challenges associated with creating cyberinfrastructure to support a research project of this scale, which are not unique to iUTAH, but are faced by many collaborative scientific groups. We describe how iUTAH Cyberinfrastructure coordinates across Utah universities, including provisioning hardware that enables hosting of data publication and sharing services as well as data storage resources for redundancy and for High Performance Computing. We also describe the hardware and software platforms that have improved data access and new tools for collaboration among iUTAH participants.


V. Advancing a water-literate workforce and citizenry for Utah
Dr. Mark W. Brunson*, Utah State University, and Ellen Eiriksson, Utah State University

Utah has both incentive and opportunity to lead the nation in innovative solutions for water management and sustainability. A critical component of iUTAH’s mission has been to help build a foundation for innovation in sustainable water management through education and outreach programs that can train students to meet the challenges facing our state while increasing awareness of those challenges by Utah residents. iUTAH’s Education, Outreach, and Diversity (EOD) activities have encompassed the work of four teams – Workforce Development, External Engagement, Diversity Enhancement, and Communications – whose efforts are designed to have lasting impact

KEYNOTE Salt Lake County's Climate Adaptation Plan for Public Health

The release of greenhouse gases into the earth's atmosphere has set the climate on a course to change drastically in the near future, and these changes are having a significant impact on human health in Salt Lake County. There is broad scientific consensus that climate change is occuring at a rate raste than previously anticipated, and is causing warmer temperatures, droughts, and more frequent extreme weather events in our region. It is important that we take action now, both to mitigate the impacts of climate change and to develop adaptation strategies that enhance the region's resiliency to the inevitable changes it will experience. Many responses to climate change could positively impact the region in multiple ways, simultaneously reducing the burden of disease, saving money, protecting the environment, developing community, and addressing inequality. Salt Lake County's Climate Change Adaptation Plan for Public Health will provide a plan for organizations in the Salt Lake region to respond to the health impacts of climate change, serving to build a healthier, more resilient community, and setting an example for other local health departments in Utah.

How’s our Watershed’s Health? Ask your Mouth-Feet and Mussels

Summary:
Our poster children and ultimate metric of watershed health, native mollusks, are rapidly disappearing from Utah

Full Abstract:
When it comes to our watershed, do we want to strive for: world class health, average American sloth-like health, or “whatever the government decides, is good enough for me” health? Measuring and monitoring watershed health is by no means an easy task, however we propose that any valid SLC watershed doctor’s toolbox should include the ultimate metric; native mollusk population viability, particularly mussel population viability. We will discuss why native mollusks are so important to the health of our watershed based on findings from several years of field surveys and several decades pondering that age old question, ‘by Jimini, just how do we measure and monitor watershed health’? and conclude that viable native mollusk populations are the go to tools. We then provide initial guidance on how to use them.

Historical Occurrence of Unionid Mussels in Utah and Ammonia Standards

Summary:
The Utah DWQ teamed with researchers from Utah State University to summarize the available reports of the occurrence of unionid mussels in Utah. The presence of absence of these mussels affects how stringent the water quality criteria will be for ammonia. The results of this work will be presented and water quality implications discussed.

Full Abstract:
In 2013, the USEPA (United States Environmental Protection Agency) published revised water quality criteria for ammonia. These revised criteria are more stringent if sensitive species of mussels (Order Unionoida) meet the USEPA definition of “residents.” Meeting the more stringent ammonia criteria will be potentially costly for publically-owned treatment works and the public that they serve. To determine if the more stringent criteria are appropriate for Utah’s publically-owned treatment works, the Division of Water will evaluate if the sensitive mussels are “residents”. The first step in this process was to review the available reports on the occurrences of the sensitive mussels in Utah. Researchers at Utah State University recently completed a report that summarizes these findings. The results are a database that can be viewed in tabular or map formats. In addition, the reliability of these reports was qualitatively evaluated. The results show that in portions of Utah, these mussels were present in the past. The next step in determining if the sensitive mussels are USEPA “residents” will be to conduct site-specific surveys to determine if the mussels are currently present. The Central Valley Wastewater Reclamation Facility has already conducted these surveys for portions of the Jordan River and no live sensitive mussels were found although historically, the reports indicate that they used to be plentiful. Wherever the sensitive mussels are not currently present but were present in the past, determining the likely reasons for the current absence is a critical step in determining the appropriate ammonia criteria.

Jordan River Phase II TMDL: The Organic Matter Conundrum

Summary:
The Jordan River TMDL is one of the first major TMDLs in the nation to address organic matter as the primary cause of low dissolved oxygen criteria violation. Because organic matter comes in many varieties, sizes and degree of reactivity, this presents particular challenges in understanding sources and potential mechanisms of restoration.

Full Abstract:
Phase I of the Jordan River TMDL concluded that the low dissolved oxygen was primarily the result of elevated values of sediment oxygen demand throughout the lower Jordan River. Considerable work has been performed to more fully understand the sources and transport of difference forms of organic matter, including dissolved organic matter, fine particulate organic matter and coarse particulate organic matter and fractions which may be refractory or more labile. This presentation will update the state of our knowledge with recent research findings and analyses integrated with earlier findings.

Media to Remove Metals, Nutrients and Other Runoff Pollutants

Summary:
It simple really. There are a whole host of available, green, and low cost media that can be used to remove pollutants in runoff. Design: filtration cell. Chemistry is the key to knowing what media to use given the target pollutant.

Full Abstract:
There is a revolution afoot in stormwater treatment. This is the use of a whole range of low-cost, non-proprietary, readily available, and green media that effectively and passively remove a range of pollutants in stormwater runoff. What’s removed? Metals, phosphorus, solids, color, and potentially bacteria, and organic chemicals. What’s the media: recycled scrap iron that rusts into an effective pollutant binder. Spent lime from municipal drinking water treatment waste that creates a pH environment that can precipitate metals, remove phosphorus, and kill bacteria. Other media such as steel mill slag and biochar have the potential to augment iron and spent lime when the conditions are required. Traditional stormwater treatment approaches predominantly remove solids and are largely ineffective at removing dissolved pollutants. Media can be placed in filtration cells to capture the dissolved pollutants. The outcome is high rates of total and dissolved pollutant removal. This presentation will demonstrate the use of these new media in full scale systems, how they are designed, and how they are performing.

Nutrient Cycling in the Jordan River: Seasonal & Spatial Variations

Summary:
Water reclamation facilities dominate nutrient loads to the river, although some processing by in-stream biota is also present. The influence of facilities varies spatially and seasonally.

Full Abstract:
Arid regions face increasing pressure to manage water quantity and quality in the face of urban expansion and climate change. As greater percentage of a catchment's water balance flows through engineered urban system, it is crucial to understand how these engineered flowpaths influence downstream ecosystems. The Jordan River, which drains the Salt Lake City urban region receives significant nutrient loading from four water reclamation facilities (WRFs), as well as urban runoff, and natural sources from seven alpine streams which flowing through the urban core before entering the river. The river experiences periods of seasonal hypoxia, especially in low-velocity reaches downstream of several nutrient sources. Nutrient availability can influence microbial respiration of organic matter in rivers. It is therefore crucial to understand the relative role of nutrient inputs and in-stream processing on N, P and C transport. We sampled the Jordan synoptically during three distinct seasonal hydroperiods (spring/snowmelt, summer, and fall drawdown) in order to better understand the river’s role as a transporter and transformer of nutrients throughout the year. Sampling locations included above and below each of three WRFs, as well as and ‘intensive’ reach every 1km downstream of the surplus canal near 1700S. We also sampled effluent outfalls. At each site, we measured concentrations of dissolved N and P species (nitrate, ammonium, organic N, phosphate, and organic P), particulate N and P, as well as DOC in surface water. Cumulative TDN and TDP loads from WRFs upstream of 1700S were equal to or greater than the riverine load at this location, however reach-scale patterns show substantial N and P removal from the water column. In the 13km reach between Jordan Basin and South Valley, TDN and TDP loads declined by 43 and 55% respectively during spring runoff. TDN increased in the reach between South Valley and Central (26 and 3% increase during spring and summer), while this reach remained a sink for TDP (25 and 53% removal in spring and summer). Shifting forms (organic vs. inorganic) of nutrients provided further evidence of biotic processing between WRF outfalls. Across seasons, we found that the organic character of the TDN was highest directly downstream of a WRF outfall, and became dominated by inorganic N downstream. TDP showed the opposite pattern, with the high inorganic P downstream of outfall sites, and increasing organic P content further downstream. Stable isotope content of NO3- increased steadily along the entire reach of the river between Utah Lake and 1700s, as expected in response to cumulative effluent loading. Unexpectedly, however, stable isotopes of N declined along the intensive reach (downstream of 1700), suggesting an additional NO3- sources in this reach. Our results suggest that, while nutrient loading to the river is dominated by point-source anthropogenic inputs, biotic processes and in-stream storage influence the quantity of N and P transported downstream, and additional nutrient inputs offset any ecological uptake.

Beyond Traditional Stormwater Project Delivery—Community-Based P3

Summary:
Prince George County, MD is required to treat urban stormwater to meet Chesapeake Bay TMDL requirements for nutrients and sediment. The County has entered into a Community Based Public Private Partnership (P3) to design and construct stormwater treatment facilities and provide contracting opportunities to target class and local firms

Full Abstract:
The effect of stormwater discharges to surface waters has fundamental impacts to economic development and a community’s quality of life. Local municipalities struggle with ways to improve the effectiveness of its stormwater infrastructure and compliance with water quality requirements while balancing the needs of competing capital investment funding priorities. Alternative delivery of public projects has been around for some time; however, with natural resource projects, the tried and true design-bid-build delivery has been the staple. Looking to balance risk, regulatory obligations and social needs, a new option has emerged called Community Based Public Private Partnerships (CBP3). A case study will be highlighted from one community’s entry into this new strategy of accessing the private sector’s efficiencies and expertise to develop, manage, and maintain stormwater control measures to meet MS4 permit compliance while also providing local workforce development and social values. Lessons learned will be shared, with real-world examples. Stormwater quality facilities to treat 2000 acres of impervious areas are designed, permitted and constructed in Phase 1 of this project- in the first 3 years. This will assist Prince George’s County in meeting the MS4 retrofit permit requirement for the Chesapeake Bay TMDL for nutrients and sediment.. Phase 2 will extend the contract for another 3 years and require another 2000 acres of treatment. Stormwater treatment focus on building new structural BMP’s (sand filters, micro-bioretention, submerged gravel wetlands) on urban sites ( schools, county and municipal libraries, public works stations, police stations), retrofitting existing wet ponds, by adding capacity to treat the WQCV and stream restoration. A team of 5 engineering firms find the sites, design and permit the BMPs. At about 60% design, a general contractor is assigned the project and leads constructability and value engineering reviews. After permits are received, the general contractor bids the work to a minimum of three sub-contractors to meet target class and local contractor goals. Bids are reviewed and work is awarded for construction. A third party agency inspects and certifies that the BMPs are constructed to design plans and treat the impervious areas within the drainage area. After certification and construction are complete, the facility will be maintained quarterly, inspected annually and recertified every 3 years.

Primary learning objectives:
• Discuss trends in stormwater project delivery
• Detail the elements of a community-based P3 program for stormwater management.
• Provide case study example of Prince George’s County, MD and its CBP3 program to provide stormwater treatment to meet Chesapeake Bay TMDL requirements for nutrients and sediment.

The CBP3 program strategy approaches stormwater quality management by involving the private sector in transferring risk of planning, design, and construction, adding in social value creation to have an emphasis on local small and disadvantaged business development and utilization, providing long-term sustainability through streamlined implementation and maintenance, and promotes flexibility in procurement of local contractors.

A Comprehensive Approach to Protecting Great Salt Lake's Water Quality

Summary:
The Great Salt Lake Water Quality Strategy is a comprehensive approach to protecting water quality in GSL through standard development, monitoring, and assessment. The Utah Division of Water Quality has made significant progress in implementing this strategy. Current directions include the development of wetland and nutrient components.

Full Abstract:
The Utah Division of Water Quality launched a Great Salt Lake Water Quality Strategy in 2012. The strategy was designed as a comprehensive approach for protecting the water quality of Great Salt Lake (GSL) and its surrounding wetlands and outlined a formal process for protecting GSL’s water quality through the development of a strategic monitoring plan, water quality standards, and beneficial use attainment assessment methods. DWQ continues to make progress in implementing the GSL Water Quality Strategy. Accomplishments to date include the implementation of a GSL monitoring program, the initial steps in numeric criteria development, and the implementation of an interim discharge permitting program to protect GSL’s water quality while standards and assessment methods are developed. Current directions for DWQ include the development of wetland and nutrient assessment components of the strategy. This presentation will provide an update on DWQ’s progress implementing the strategy to date and on current and future directions for the strategy. Attendees can expect to learn about: 1) DWQ’s vision for GSL, 2) DWQ’s authority under the Clean Water Act to protect GSL water quality, 3) regulatory mechanisms for protecting GSL’s water quality, 4) progress implementing DWQ’s GSL Water Quality Strategy to date, and 5) current and future directions for DWQ’s GSL Water Quality Strategy.

Creating a balance: Great Salt Lake Causeway Improvements

Summary:
Infrastructure improvements to the Great Salt Lake railroad causeway provided a new structure with control berms to modify the water and salt transfer to meet regulatory, industry and ecosystem objectives.

Full Abstract:
Getting trains across the Great Salt Lake has posed a challenge since the completion of the Transcontinental Railroad in 1869, almost 150 years ago. Built in 1902 and modified in 1959, the railway corridor consists of a rock causeway which had two concrete culverts allowing water, salt and boats to pass between the arms of the lake. The semi-permeable rock causeway divided the lake in two, creating a unique ecology where bacteria in the salt saturated north arm turns the water pink, while fresh water flowing into the less saline south arm keeps the water blue. Safety concerns led Union Pacific Railroad, current owner of the causeway, and environmental regulatory agencies to develop a phased permitting strategy to start the closure the culverts in 2012 and determine required mitigation to replace the water and salt transfer and navigability provided by the culverts. Union Pacific, regulatory agencies, and HDR’s environmental and engineering team developed an innovative solution: a new 180-foot-long bridge with a 150-foot control berm. Side adjustable earthen control berms, and a 5-foot invert berm on the lakebed, allow control of the salt and water transfer to meet ecological, industry and lake management objectives. To find the optimal causeway opening that would duplicate the culverts functionality, the team developed several water and salt balance model simulations, modifying the USGS’s Water and Salt Balance Model—the first extensive modeling of the lake since 1998. The effort included updating and recalibrating the model with 14 years of actual lake inflows, salinity and evaporation data, as the Great Salt Lake’s size and salinity is tied to water inflows and weather cycle fluctuations. The team ran various 25-year historical scenarios and compared salinity conditions for different causeway opening geometries. This effort, along with federal and state agency peer review, provided regulating agencies and stakeholders with new understanding of the water and salt transfer and make the updated model innovative and irreplaceable. Final permit was issued on September 9, 2015, and construction started on October 1, 2015. Designing and constructing a stable structure amidst difficult geological and chemical (high salinity) conditions was another significant challenge. The center of the causeway spans two tectonic faults, between which fills with soft sediment—the culprit behind the culverts failure. The new bridge was built in more stable geological conditions with 49 piles driven to over 200 feet—unique for a less than 35-foot-deep lake. Temporary access roads and a track shoofly routed maintenance vehicles and trains around the mid-lake site during construction of the bridge structure, berms and excavated channels. Project completion in December 2016, marks a renewed cooperative effort among Union Pacific, regulatory authorities and environmental advocates to protect and preserve the extraordinary assets of the Great Salt Lake. The project is highly valued by Union Pacific, which maintains causeway safety and operation; state officials, who have a long-term, lake management solution; and environmental groups, who see the lake’s ecological resources continuing to thrive.

Lower Jordan River Dissolved Oxygen—Is Additional Flow the Answer?

Summary:
Low concentrations of dissolved oxygen (DO) are a concern in some segments of the Jordan River. The Jordan River Commission and other stakeholders are looking for opportunities to address acute and chronic DO concerns in the lower Jordan River with flow management. Our presentation will provide an update on this effort during the past 3 years.

Full Abstract:
Low concentrations of dissolved oxygen (DO) are a concern in some segments of the Jordan River. The Jordan River Commission and other stakeholders are looking for opportunities to address acute and chronic DO concerns in the lower Jordan River with flow management. In 2014, the Jordan River Commission completed the first phase of a study investigating the use of flow manipulation as a potential mechanism for increasing DO during the late summer season in the Lower Jordan River (LJR). On the basis of data review and QUAL2Kw model output, the report recommended empirical studies to definitively answer two key questions: (1) Is there a defined, positive correlation between flow and DO, and (2) Is there a minimum flow threshold that will support DO levels above chronic conditions in the late summer months? Acting on that recommendation, the Jordan River Commission took steps to implement a flow experiment on the lower Jordan River in 2016/2017. The intent was to manipulate flows and monitor the resulting effects on DO in the problematic reach. Acquiring sufficient water rights has slowed implementation of the study, but significant progress has occurred from discussions with Utah Division of Water Rights and the project could realistically begin in 2018. A recent analysis of historic flow increases (non-storm events) to the LJR have shown high variability and both a positive and negative DO response. However, even small flow increases (< 30 cfs) during late summer and early fall seasons show positive improvements in DO. This experiment is unique in the history of Utah water quality remediation and could lay a foundation for similar work in other watersheds. The experiment goes beyond the simple philosophy of "the solution to pollution is dilution", as many factors and processes combine to influence DO in the Jordan River. Under certain conditions influenced by season, magnitude, and duration, additional flow can produce a negative DO response. Participants attending this session will gain an understanding of historic LJR water rights and how they have evolved to influence existing flow patterns in the river. They will learn about the proposed flow experiment and what challenges remain to implement long-term flow management. They will also learn about DO processes in the Jordan River and the patterns of diel DO recorded at permanent monitoring sites in the LJR from 2012 to the present.