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Session 2: WATER QUALITY             

ASEC 205 Moderator:Melissa McCutcheon

Molecular characteristics of dissolved organic matter from three South Texas rivers: Insights provided by thermal slicing pyrolysis gas chromatography mass spectrometry and amino acid analysis

John A. O'Connor*; Kaijun J. Lu; Jianhong Xue; Zhanfei Liu

Thursday, November 8

9:15

River transport of dissolved organic matter (DOM) provides a crucial energy subsidy to coastal ecosystems through remineralization processes. Understanding both the quantity and the molecular characteristics of riverine DOM is key to understanding the potential for coastal DOM remineralization. In South Texas, there is extreme interannual variability in hydrologic controls on freshwater inputs from rivers to coastal embayments, and thus total DOM transport. Utilizing three coastal rivers from three distinct watersheds, the Mission, Aransas, and Nueces Rivers, we sought to decipher variability in both quantity and quality of the South Texas riverine DOM matrix with a unique thermal slicing pyrolysis-gas chromatography/mass spectrometry (Py-GC/MS) technique. River water, collected in June of 2017 and January of 2018, was pre-filtered before DOM isolation by solid phase extraction (SPE). SPE-DOM was pyrolyzed at five thermal slices before chromatographic separation then molecule identification by mass spectrometry. The thermal stability of each river’s DOM matrix was similar, as ~90% of all pyrolyzates were released between 190 and 530°C. Of the pyrolyzates detected, there were 14 significant compound classes, and their proportions varied tremendously between rivers. However, methanol, acetic, benzenes, and CO2, likely sourced from polysaccharides, lignin-like materials, and carboxyl-rich alicyclic molecules, were predominant in all rivers.  Results of total hydrolysable amino acids (THAA) analysis also showed consistent amino acid composition in these DOM samples, dominated by aspartic acid, glycine, beta-alanine, and alanine. Analysis for δ13C, δ15N, C:N, and %-OC are ongoing, but the preliminary results show that the DOM isolated by SPE is compositionally similar among the three rivers, and no seasonal trend was observed between diagenetic state and molecular diversity. Despite different sources and hydrologic conditions driving differences between proportions of compound classes, DOM characteristics between these rivers showed little variability

Synthesis of water quality studies in Baffin Bay with a view towards solutions

Michael S. Wetz; Emily K. Cira; Kenneth C. Hayes

Thursday, November 8

9:30

Baffin Bay is an economically and ecologically-important estuary on the South Texas coast. In the past few decades however, it has begun to exhibit symptoms of eutrophication including high and increasing chlorophyll concentrations, episodic hypoxia/anoxia, recurring blooms of the harmful brown tide alga Aureoumbra lagunensis, and fish kills. Unfortunately, our understanding of the causes of the water quality degradation has been limited due to lack of data.  Results from a 5-year (ongoing) water quality study as well as analysis of historical TCEQ data is now providing answers.  Results show that dissolved organic nitrogen and total Kjeldahl nitrogen concentrations in Baffin Bay are 2-5 fold higher than in other Texas estuaries.  In contrast, inorganic nitrogen (ammonium, nitrate) and phosphate concentrations are relatively low except following episodic rain events.  The dominance of organic nutrients compared to inorganic nutrients, prolonged hypersaline conditions during drought, and a long-term increase in spring-summer water temperature create conditions favorable for “brown tide” persistence in this system.  Given the long residence time (> 1 year) of Baffin Bay, the system is likely sensitive to nutrient inputs and thus reductions in loadings are be needed to prevent further water quality degradation.

Long-term water quality trends in Texas estuaries: Relationships with climatic variability and watershed land use change

Kalman Bugica*; Blair Sterba-Boatwright; Michael S. Wetz

Thursday, November 8

9:45

Estuaries are critical habitats for numerous bird, fish, and shellfish species, and they play a critical role in the economy of coastal communities. Despite this, eutrophication, with accompanying water quality and habitat degradation, is becoming pervasive in many estuarine systems. Here we report findings from a study of long-term changes in water quality in 40 bays along the Texas coast. Seasonal increases in water temperature were observed for most systems, as were annual increases in salinity. Indicators of eutrophication were found throughout Texas coastal waters, from small systems (e.g., Oso Bay and Carancahua Bay) to larger estuaries (e.g., Galveston Bay). One heavily impacted area is the Upper Laguna Madre, which includes Baffin Bay. Baffin Bay displayed multiple symptoms of eutrophication including high organic carbon, organic nitrogen, and chlorophyll concentrations. In addition, statistically significant long-term annual increases in chlorophyll a and salinity were observed, while long-term seasonal increases were observed for water temperature. Much of the increase in chlorophyll coincided with blooms of the mixotrophic “brown tide” phytoplankton species, Aureoumbra lagunensis, which is thought to be favored under high proportions of organic to inorganic nitrogen. One notable exception to the widespread eutrophic conditions found throughout coastal Texas was the Nueces-Corpus Christi Bay system, which conversely displayed symptoms of oligotrophication. Annual and seasonal decreases in phytoplankton biomass, including during the winter-spring bloom period, are occurring. These varied shifts in Texas water quality, combined with land use changes and population growth, can have serious implications for the benthos and fisheries of Texas. Identified systems of poor water quality can be used to drive future higher resolution studies to better understand potential drivers of changes in estuarine health.

Hydrology, water chemistry and biological indicators used to assess effects of treated effluent flowing via groundwater to the Lower Laguna Madre

Rosamarie Perdomo*; John Garcia; Eli Gonzalez; Chu-Lin Cheng; Hudson R. DeYoe

Thursday, November 8

10:00

Water treated by the Laguna Vista Waste Water Treatment Plant contains nutrients such as ammonium, nitrate, and phosphate that can lead to nutrient loading of adjacent coastal water. The effluent is released into a designated and confined reservoir about 1.5 km from the shores of the Lower Laguna Madre. Our research indicates that elevated levels of nutrients observed in the surface water of the reservoir enters the water-table and flows towards the lagoon possibly affecting the lagoon ecosystem. This study monitored hydraulic flow of the pond effluent, water composition of surface and groundwater. Potential environmental effects were assessed by use of nitrogen isotopic analysis of common coastal vegetation- black mangrove Avicennia germinans, turtlegrass Thalassia testudinum and honey mesquite Prosopis glandulosa. The presence of effluent sourced nutrients should affect the nitrogen isotopic signature of these plants. Examination of chlorophyll, and E. coli presence will be used this fall to assess environmental health in areas where effluent flows outside reservoir boundaries.  

Comparative analysis of nitrate levels in Pensacola Bay area rain water

Jade Jacobs*; Jane Caffrey; William Landing; Alexander Maestre; Subhash Bagui

Thursday, November 8

10:15

There is reason to believe that there is a correlation between atmospheric NOx levels and nitrate levels of rain water. This specific link between air and water quality was tested over a course of summer 2017 and compared to data from 2005-2012. Rain water samples collected from late May through early July of 2017 were tested for their pH levels and nitrate concentrations. These months were one of the stormiest on record for the Northwest Florida region. The data analyzed from these rain events was compared to previous data through the PERCH study (2005-2012 data) to show the trends of nitrate and pH levels in the rainwater since the project’s conclusion. According to the paper published as part of the PERCH study, “There was a significant drop in deposition and VWM concentrations between 2006 and 2007,” (Caffrey 2013) suspected to be caused by the implementation of a scrubber at Plant Crist coal fired power plant in 2007. Following analysis, a statistical comparison testing for correlation between atmospheric NOx and rainwater NO3 was run to determine broader impacts on both air and water quality.
 

Sediment nitrogen cycling and removal in tidal freshwater zones of two Texas rivers

Xin Xu*; Hengchen Wei; Kevan Moffett; James McClelland; Amber Hardison

Thursday, November 8

10:30

Nitrogen is the major limiting nutrient in marine ecosystems, and river-borne sources provide 20-30% of nitrogen input to global oceans. Tidal freshwater zones (TFZs) in the lower reaches of rivers may substantially alter the amount and composition of nitrogen transported from watersheds to estuaries due to longer water residence times (compared to non-tidal river reaches) and associated build-up of organic-rich sediments. We conducted flow-through sediment core incubations from TFZs and upstream riverine sites in the Aransas and Mission rivers in south Texas during multiple seasons and years. We measured net fluxes of different constituents (O2, N2, DIC, NH4+, NO3-) across the sediment-water interface to quantify organic matter decomposition and major nitrogen cycling processes. Our results showed higher respiration and denitrification rates in TFZ sediments than in non-tidal riverine sediments. Average O2 fluxes were -771±35 μmol m-2 hr-1 and -797±69 μmol m-2 hr-1 in summer in the Aransas River TFZ (AR) and the Mission River TFZ (MR), respectively; and -363±38 μmol m-2 hr-1 and -484±70 μmol m-2 hr-1 in winter, with negative values indicating net O2 consumption. Average N2 fluxes were 53±8 μmol m-2 hr-1 (AR) and 22±5 μmol m-2 hr-1 (MR) in summer and 36±8 μmol m-2 hr-1 (AR) and 30±6 μmol m-2 hr-1 (MR) in winter, with positive values indicating net denitrification. Average dissolved inorganic nitrogen (DIN) fluxes were 49±9 μmol m-2 hr-1 (AR) and 106±9 μmol m-2 hr-1 (MR) in summer, and -12±11 μmol m-2 hr-1 (AR) and 22±6 μmol m-2 hr-1 (MR) in winter, with negative values indicating net DIN removal. Within the TFZs, rates of biogeochemical processes varied as a function of sediment physical properties, nutrient loading, and seasonal temperature changes.

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