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Proceedings of the 2019 Mohawk Watershed Symposium

Authors:
  • State University of New York Polytechnic Institute at Utica/Rome

Abstract and Figures

This is the abstract volume of the 11th Mohawk Watershed Symposium. Over the years this Symposium has taken on an important role in unifying and galvanizing stakeholders in the Basin. A coalition of concerned and invested stakeholders allows us as a group to tackle important issues that affect water quality, recreation opportunities, flood mitigation, and other basin-wide issues. This was a big year in the watershed with a number of important developments that centered on floods, dams, water quality, and stewardship. With another ice jam on the lower Mohawk River this winter, we were again reminded of the susceptibility of low-lying communities to flooding. A new initiative from the State seeks to get to the root cause of how, why, and where ice jams form, and perhaps what can be done about this hazard. Meanwhile the City of Schenectady has embarked on an ambitious plan to mitigate flooding in Stockade, the first historic district in the State of New York. A key to watershed management is our water infrastructure. The primary components of concern are dams and sewage systems and to a lesser extent transportation networks. Dams in the Watershed are used mainly for drinking water, canal supply, and hydropower. The Watershed has nearly 100 NYS Class C and Class B (high-hazard and intermediate-hazard ) dams, and hundreds of smaller Class C and D dams. We have a number of dams that are critical for drinking water, and the Gilboa Dam on the upper Schoharie Creek is a wonderful example: the recent major rehabilitation of the Gilboa dam resulted not only in dam strengthening and hazard reduction, but also provided changes that include a low-level outlet that can be used for conservation releases to sustain the downstream ecosystem in the summer. For dams that generate hydropower, the Federal Energy Regulatory Commission (FERC) issues licenses based on power generation, energy conservation, protection of fish and wildlife, preservation of recreational uses, and general environmental quality. As a result, the FERC review process can force significant environmental review of the ways in which dams integrate into the local ecosystem. Thus when dams come up for review, stakeholders have an important responsibility to get involved and have their voices heard. FERC reviews of the Blenheim-Gilboa Dam (on the Schoharie Creek) and the West Canada Creek Hydroelectric Project (on the West Canada Creek) have recently generated intense interest by local stakeholders. Some of the focus has been on not only how the dams are integrated into the ecosystem, but also how they are integrated into the fabric of local communities. Some dams have outlived their utility, and these dams should be removed both for the benefit of the local ecosystem and for the safety of those living downstream. Given the industrial heritage in the Mohawk Valley, it is not surprising that there are a number of abandoned dams that no longer serve their original functions. We know that dam removal can have tremendous positive impact on fish passage and the local ecology, but we also know that removal can be an expensive and involved process. Facilitation of fish passage is a primary driver in dam removal, although we have learned that it inevitably results in passage both by species that belong in this watershed and by invasive species, illustrating the point that some barriers are useful. Water quality remains a central issue in the Watershed. For a healthy and vibrant ecosystem we need clean water. We know that locally our waterways are impaired, and the indicators include pathogens and plastics. We now understand the health of our waters from hundreds of measurements taken across the watershed by students, educators, and dedicated professionals from SUNY Cobleskill, SUNY IT Polytechnic in Utica, Union, Cornell, Schoharie River Center, Riverkeeper, DEC, USGS, and others who have been addressing water quality through research. These critical measurements include quantifying the distribution, source, and fate of environmental contaminants including fecal bacterial, microplastics, nitrogen, phosphorus, and other compounds that affect water quality. Stewardship and education are a critical piece of effective watershed management. Stakeholder meetings like the Mohawk Watershed Symposium, and local water advocates (including West Canada Creek Alliance, Riverkeeper, and Dam Concerned Citizens) play a key role in identifying problems, educating the public, and effecting change where it is most needed. Youth education programs centered on water quality and ecosystem health, such as the Environmental Study Teams at both the Schoharie River Center and Fort Plain High School, insure that all our waterways pass into the hands of the next generation of active, engaged, and knowledgeable stewards. The Mohawk River Basin has a new Action Agenda and Watershed management plan. In 2009 the first plan was developed by NYS DEC and partners, and the new five-year plan (2018-2022) was completed at the end of last year (2018) and will be released here at the Symposium. The overall goal is consistent with the whole-Hudson approach of a swimmable, fishable, resilient watershed. There are four main goals of the plan: 1) Improve water quality; 2) improve fisheries and wildlife habitat; 3) reduce flood risk and build resilient communities; and 4) create and foster stewardship opportunities. This is our new plan, and you, as a stakeholder, should be part of making it successful. Our keynote speaker is Hon. Rep. Antonio Delgado, a native of Schenectady, who represents the 19th Congressional District. The 19th District is one of the largest in New York State, and it includes a wide swath of the Catskills, including the Schoharie Creek, part of the Mohawk, and a large section of the Hudson from the Capital District south to Poughkeepsie. In the short time he has been in Congress Rep. Delgado has demonstrated a commitment to our water infrastructure. He is founding member of the bipartisan Congressional PFAS Task Force, and he is a co-sponsor of the Water Affordability, Transparency, Equity and Reliability Act (WATER Act) of 2019. He serves on the House Agriculture Committee, the House Committee on Transportation and Infrastructure, and the Small business Committee. This year’s meeting features 30 presentations that cover a wide range of topics. We hope that the selection of talks and posters will shape the discussion and continue the conversation about issues within the basin. By the end of the day, the Mohawk Watershed Symposium series will have been the forum for 340 talks, posters, and special presentations since its inception in 2009. Thank you to all who have participated. New York City water supply and infrastructure upgrades at Schoharie Reservoir A. Bosch p. 1 The New York State Mesonet: Providing real-time, high-quality environmental information across the Mohawk watershed J. Brotzge, C. Thorncraft, J. Wang p. 3 Toward improved community resiliency: Developing and assessing ice jam and flood mitigation measures along the Mohawk River M. Carabetta, J. MacBroom, J. Gouin, R. Schiff, B. Cote p.5 Characterization of disinfection by-product formation potential in Mohawk River source waters to support TMDL implementation A. Conine, M. Schnore, Z. Smith, G. Lemly, C. Stoll, A.J. Smith p. 6 The Mohawk River Basin Action Agenda 2019-2023: A Five-Year Plan for a Swimmable, Fishable Mohawk K. Czajkowski p. 7 Hogansburg Dam decommission and removal: Removal of first impassible barrier restores connection between St. Regis and St. Lawrence Watersheds A. David p. 9 Fort Plain Waterways: Stories of then and now in an Erie Canal town L. Elliott, C. Herron, G. Hoffman, W. MaGinnis, S. Paradiso, S. Rogers 10 The 2019 mid-winter ice jam event on the lower Mohawk River, New York J.I. Garver p. 11 Expansion of Invasive Round Goby in the Mohawk River-Barge Canal System S. D. George, B.P. Baldigo, C.B. Rees, M.L. Bartron p. 17 Nature-induced and human-instigated water deprivation sparks conflict in the Middle East A. Ghaly p. 18 Oroville Dam's main and emergency spillways: two near-miss disasters A. Ghaly p. 19 Identification of a point source for plastic pollution in upstate New York: a case study of Mayfield Lake K.N. Hemsley, L.G. English, C Cherizard, D.J. Carlson, J. McKeeby, S. Hadam, E. McHale p. 20 Stockade Resilience: Feasibility analysis of flood mitigation alternatives and design of mitigation measures to protect Schenectady’s Stockade Neighborhood M. Irwin p. 27 A four-year series of snap-shots: Data and observations from a Mohawk River water quality project as it enters Year Five of a longitudinal study N.A. Law, B.L. Brabetz, L.M. Wanits, L. Cao, S. Rogers, C. Rodak, J. Epstein, J. Lipscomb, D. Shapley p. 33 Aquatic invasive species in the Mohawk River Watershed: the devil is in the details C. McGlynn p. 34 United States Coast Guard Auxiliary: Recreational Boating Safety in the Mohawk Watershed D. Miller p. 35 The impact of alternative preservation methods and storage times on the δ13C of dissolved inorganic carbon in water M. Miller, L. Piccirillo, A. Verheyden, D. Gillian p 36 The importance of the West Canada Creek and FERC re-licensing for the WCC hydroelectric projects B. Nador p. 37 Overview of the Schoharie Creek Watershed flood mitigation study P. Nichols p. 41 Observations on dissolved and total metal concentrations in the Mohawk River in Utica and Rome, NY C. Rodak and N. Diers p. 42 Phosphorus monitoring prioritization in Mohawk River basin sub-watersheds using LENS M. Schnore, A.J. Smith, B. Duffy, K. Stainbrook, C. Stoll, Z. Smith p. 43 What's up with the Mohawk Delta? Insights from community water quality monitoring at the mouth of the river D. Shapley, J. Lipscomb, J. Epstein, S. Pillitteri, B. Brabetz, N.A. Law, A. Juhl, C. Knudson, G. O’Mullan, C. Rodak p. 45 Confirming the presence of microplastics in Capital Region fish using a novel no-kill abdomen massage A. Shimkus, J.A. Smith p. 48 Extreme rainfall, high water, and elevated microplastic concentration in the Hans Groot Kill: implications for the Mohawk River J.A. Smith, E. Caruso, N. Wright p. 53 Reconnecting waters for eels and river herring: towards resilience building approaches for dam removal action in the Hudson River watershed K. Smith, A.M. Feldpausch-Parker, K.E. Limburg p 59 Innovative approach to deliver a $300 million treatment plant upgrade for Oneida County, New York J. Story, R. Ganley, S Devan p. 60 Characterization of carbon export in Upstate New York: initial geochemical characterization of six rivers J. Wassik, J. Gehring, C. Horan, M. Stahl p. 65 Baseline monitoring of physical parameters and Enterococci levels in the Hans Groot Kill, Schenectady, NY E. Willard-Bauer, J.A. Smith, J.I. Garver p. 69
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Poster
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Human data on microplastics is scarce. There is concern about microplastic contamination in foods and its potential health impact. This prospective study is the first investigation of microplastic residues in human stool. The study has been approved by the ethics committee of the Medical University of Vienna. Human stool samples from 8 different geographic regions were collected along with a food log protocol. To facilitate microplastic quantification in stool, new sample preparation techniques have been developed to unmask it in a complex biological matrix.
Article
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Microbes eat rocks and leave carbon dioxide The reaction of atmospheric carbon dioxide (CO ² ) with silicate rocks provides a carbon sink that helps counterbalance the release of CO ² by volcanic degassing. However, some types of rocks contain petrogenic organic carbon, the oxidation of which adds CO ² to the atmosphere, counteracting the drawdown by silicates. Hemingway et al. present evidence from the rapidly eroding Central Range of Taiwan showing that microbes oxidize roughly two-thirds of the petrogenic organic carbon there and that the rate of oxidation increases with the rate of erosion. Science , this issue p. 209
Conference Paper
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A 27 km (17 mile) long ice jam formed during a January mid-winter breakup event, and it stayed in place for most of the winter. By historic standards this was the longest to have formed in decades, and thickness estimates were made to better understand the hazard and the nature of the ice in constriction points. Unmanned aerial system (UAS) photogrammetry and Structure from Motion (SfM) at two sites was done to better understand the structure and thickness of the ice. In the toe of the jam, in the Rexford Knolls, thickness is estimated to be between ~1.2 and 3.0 m (4-10 ft) thick for floating and thickened ice that meets sheet ice near Lock E7. At Lock E9, about 22 km (13.5 mi) up river, topographic mapping on the deflated and ground ice rubble reveals that the ice was between 1.8 and 2.7 m (6-9 ft), but ridges are as thick as 3.6 and 4.6 m (12-15 ft). UAV/UAS use is in its infancy in ice jam work, but imaging and mapping will be transformative in work aimed at assessing the hazard and understanding the science behind jams. The 2018 Jam ultimately broke up on 22 February, but only after causing backup flooding in the historic Stockade district in Schenectady.
Conference Paper
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An ice jam of historic proportions formed in January 2018 on the lower Mohawk River. The ice jam was 27 km long, and the toe was lodged in the Rexford Knolls, a chronic jam point. The Knolls are a unique section of the river where late-glacial capture moved the channel to a bedrock incised gorge, and today the channel is narrow and deep with a prominent constriction. Along the length of the jam at least four other jam points also affected flow and progress of ice movement. The toe of the jam failed during high water at 21-22 February caused by rain and then exceptionally warm temperatures (21°C, 70°F). A significant release of water moved downstream, and water levels dropped 1.8 m (6 ft) in a few hours, which relieved flooding of homes in the Stockade of Schenectady.
Article
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A summary of 246 studies published in 2016 on topics related to the characterization and management of urban stormwater runoff is presented in the following review. The review is structured along three major topical areas: (1) general characterization of stormwater quantity and quality; (2) engineered systems for stormwater control and treatment, including erosion and sediment control practices, constructed stormwater ponds and wetlands, bioretention, permeable pavement, greenroofs, and rainwater harvesting and (3) watershedscale application of stormwater treatment and control practices. Common research themes and needs highlighted throughout this review include efforts to better understand stormwater transport and treatment mechanisms and their representation in models, advancements to optimize the design of stormwater control measures to meet specific hydrologic and/or water quality targets, and increasing understanding of the biophysical and social factors that influence watershed-scale implementation of low impact development and other stormwater control measures.
Conference Paper
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Conclusions: Our investigation indicates that fly ash and coal ash are nearly ubiquitous in the surface waters of the Mohawk River and Erie Canal. The presence of fly ash and coal ash in many of the samples indicates that the legacy of coal-burning in the Mohawk River Watershed remains with us, likely both as spoils piles exploited as a resource and as particulates incorporated into soil over time and released to the river through bank erosion and surface runoff. The relatively high concentration of fly ash and coal ash in samples bracketing the former power station located upstream of Lock 10 suggests that byproducts of coal-burning were initially deposited close to the source, but are being remobilized in the course of both typical river flow and flood events. It is possible that erosion associated with Hurricane Irene and Tropical Storm Lee in 2011 exposed sources of fly ash and coal ash particles that are being progressively introduced into the river, especially between Amsterdam and Rotterdam Junction where Lock 10 and Lock 9, respectively, experienced significant structural damage and catastrophic channel-widening. The potential environmental impacts related to leaching of heavy metals from fly ash and coal ash have been studied elsewhere. Further investigation of the chemical stability of fly ash and coal ash in the Mohawk River may be warranted.
Article
Tiny slivers of plastic are making it all the way into humans’ guts and into their feces, a new study shows.
Article
Steep soil-mantled hillslopes are thought to be important sources of sediments and organic carbon (OC) to rivers. Minerals in these sediments may protect OC from decomposition, yet the significance of such interactions in steep upland soils remains poorly constrained particularly in relation to erosion rates. We examined a tributary basin draining to the Middle Folk Feather River in California, where knickpoint migration has created a series of hillslopes with erosion rates varying over an order of magnitude (35 to 250 mm kyr⁻¹). This setting provides a unique opportunity to study soil OC pools and their erosional exports as a function of changes in erosion rates. Soil OC inventories were 37% lower at rapidly eroding sites relative to slowly eroding sites. This difference was driven by coarse rock contents as rapidly eroding soils had more rock fragments, limiting their capacities to store OC. Although clay contents in soils were negatively correlated with erosion rates, the total mineral specific surface area remained relatively invariant. Based on secondary phyllosilicate minerals present in the studied soils and our field observations of saprocks, we suggest that this discrepancy may have originated from different clay mineralogy (types and abundance) associated with different degrees of deep subsurface chemical weathering. Across the erosion gradient, the radiocarbon age of mineral associated organic matter (MOC) in saprock varied by a factor 2 (from 1045 to 2110 ¹⁴C years), while soil turnover times estimated from soil thickness and erosion rates varied from 17 to 5.4 kyr. At the site eroding at the fastest rate, the soil turnover time approaches the ¹⁴C age of MOC, suggesting erosion can potentially limit the timescale over which MOC is replaced. We found that organic matter generally covered <50% of the total mineral surface. The remaining OC-free mineral surface area, once eroded, may thus have a significant, and to date unquantified, capacity to adsorb additional organic matter, which may act as a long-term atmospheric carbon sink.
Article
The breakup of the ice cover in cold-region rivers is a brief but seminal period of their hydrologic regime, with important ecological and socio-economic implications. The main driver of ice breakup processes is the flow discharge hydrograph. It is generated by runoff from snowmelt and rainfall but can be modified by rapid release of water from storage as the ice cover recedes by ablation and mechanical breaking up. Despite its potential importance, there is very limited quantitative information concerning the hydrodynamic processes that control storage release during ice breakup in rivers, while the issue of climate change underscores the need for improved understanding of the relevant mechanisms. Quantitative analysis for assumed prismatic channels shows that ablation and sustained ice dislodgment and breaking can cause significant flow enhancement via storage release. The latter process is far more dynamic than ablation and, under certain conditions, may lead to formation of a self-sustaining wave (SSW). Analytical results are applied to natural stream conditions, using the Lower Peace River as a case study. Observed rates of ice recession typically indicate ice melt as the dominant process. A rare occurrence of rapid ice breaking over hundreds of kilometres (2014) indicated partial agreement with the SSW concept and revealed that discrepancies may arise from the characteristic irregularity of rivers. Impacts on storage release by climate-driven changes to river ice regimes are examined, along with their implications to ice-jam formation and associated flooding.