Joint 69th Annual Southeastern / 55th Annual Northeastern Section Meeting - 2020

Paper No. 69-6
Presentation Time: 1:30 PM-5:30 PM

TRACE METAL ANALYSIS IN LONG ISLAND MARSH CORES


ACHEK, Moread1, FARMER, E. Christa1, BUCHBINDER, Brandon1, BOWEN, Joyce1, DARNAUD, Denis1, DWYER, Sophia1, EPSTEIN, Alexander1, JOHNSON, Anthony1, MAHONEY, Lauren1, MALISZKA, Miranda1, REARDON, Avery1, RENNER, Faith A.1, LOPEZ-RODRIGUEZ, Paola2, SANTELLA, Kiley1 and BARBERA, Phillip3, (1)Department of Geology, Environment and Sustainability, Hofstra University, 114 Hofstra University, Hempstead, NY 11549, (2)Department of Geology, Environment and Sustainability, Hofstra University, 145 Gittleson Hall, Hempstead, NY 11549; Department of Geology, Environment and Sustainability, Hofstra University, 114 Hofstra University, Hempstead, NY 11549, (3)Archbishop Molloy High School,, 8353 Manton St, Briarwood, NY 11435

Hofstra University’s Fall 2019 Sedimentation class embarked on a project to corroborate the results of a study initiated by The Nature Conservancy (TNC), in partnership with Northwell Health, to use medical imaging to evaluate saltmarsh health. TNC is using computer-aided tomography (CT) to measure saltmarsh response to a dramatic water quality improvement project planned in western Hempstead Bay, NY. Chronic nutrient loading is known to change the way that marsh grasses grow and compromise the integrity of marsh peat. The main source of nutrients to western Hempstead Bay is slated to be “shut off” through treatment upgrades and connection to an ocean outfall. Saltmarsh cores from high marsh and low marsh habitats in four marshes were imaged by CT as a rapid and high-resolution approach to quantify roots, rhizomes, peat, and soil particle densities. Hofstra’s Sedimentation class conducted a traditional sieve analysis of the coarse fraction of the cores to evaluate the CT scan results. Marshes in the study include two that will experience dramatic water quality improvements from the planned water quality restoration project (Lawrence and North Greensedge Marshes); a high nutrient control (Pelham Bay Cove) and a low nutrient control (Bass Creek). We decided as a class to analyze the Lawrence Marsh cores because that site is closest to the water treatment facility (in East Rockaway) and the Bass Creek cores because it is a protected marshland exposed to lower levels of Nitrogen and serving as our low nutrient control. Through this study we have confirmed the presence of higher concentrations of sand where they were suggested in the cores by the CT scans. Further study is aimed to determine the percentage of trace metals that can be detected by use of X-Ray Fluorescence (P-XRF) along with a Scanning Electron Microscope (SEM-EDS) in order to ascertain the elemental composition of sediment samples in sediment core LMHM2 as well as future extruded sediment cores.