Thesis advisor: Gail C. Kineke / This study characterizes the bed of the Connecticut River estuary in terms of grain size and bedforms, and relates these to river discharge, tidal currents, and sediment transport. Over four field excursions, sediment cores were collected, in addition to bathymetry surveys, and water column measurements. A three-dimensional circulation and sediment transport model calculated boundary shear stress over the same time. The bed of the estuary is composed mostly of sand, with small amounts of fine sediments. Deposition of fine sediments is limited by the landward extent of the salt intrusion. Large bedforms are oriented seaward. The critical shear stress for the median grain size is exceeded each tidal cycle. Bedload transport is dominantly seaward during high discharge conditions, but varies during low discharge. Bathymetry surveys from previous studies and this study show consistent bedform fields over 25 years. Bedforms observed in the field reflect typical conditions rather than extreme events. / Thesis (MS) — Boston College, 2015. / Submitted to: Boston College. Graduate School of Arts and Sciences. / Discipline: Earth and Environmental Sciences.

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Thesis advisor: Gail Kineke / Turbidity maxima are areas of elevated suspended-sediment concentration commonly found at the head of the salt intrusion in partially-mixed estuaries. The suspended-sediment distribution in the Connecticut River estuary was examined to determine where turbidity maxima exist and how they form. Areas of enhanced suspended-sediment concentration were found to exist at all phases of the tide near the head of the salt intrusion as well as downstream of this point in deeper parts of the estuarine channel. These areas are locations where peaks in the longitudinal salinity gradient exist, suggesting the presence of a front, or zone of flow convergence. During flood conditions there is a layer of landward-flowing water in the middle of the water column that decelerates upon entering deep parts of the estuary; thus enhancing particle settling. During ebb conditions, stratification and therefore settling from surface waters is enhanced. The combination of processes acting throughout the tidal cycle focuses and, potentially, traps sediment in the deeper parts of the Connecticut River estuary. / Thesis (BS) — Boston College, 2012. / Submitted to: Boston College. College of Arts and Sciences. / Discipline: College Honors Program. / Discipline: Geology & Geophysics Honors Program. / Discipline: Earth and Environmental Sciences.

Thesis. 1977. Sc.D.--Massachusetts Institute of Technology. Dept. of Civil Engineering. / MICROFICHE COPY AVAILABLE IN ARCHIVES AND ENGINEERING. / Vita. / Bibliography: leaves 381-386. / Sc.D.

Tropical Storm Irene’s most extreme rainfall resulted in record-breaking sediment loads from upland tributaries to the Connecticut River. However, was the event exceptional with respect to resultant deposition downstream? Off-river waterbodies to the Lower Connecticut River, such as cut-off meanders and blocked valley lakes, are a particularly important floodplain environment, which have been shown to serve as a focal point for the trapping of sediment and associated contaminants. This study evaluates the relative role of extreme events like Tropical Storm Irene in infilling these off-river environments. To meet this objective we compare the magnitude and composition of resultant sedimentation from Irene to that observed following the 2011 and 2013 spring freshets. Tropical Storm Irene deposits were identified as compositionally distinct, grey layers that were relatively inorganic compared to sediments deposited by the annual spring freshet. Sediment within the Irene deposit was enriched in elemental potassium and depleted in zircon, a finding consistent with being enriched by glacigenic lacustrine and till sediments. Decreased mercury levels in the Irene deposits suggest that this event served to cap highly contaminated, industrial era sediment with a layer of relatively clean, fine-grained silt and clay. Resampling of these waterbodies in Fall 2012 revealed preservation of the 2-3 cm thick Irene deposit as well as 3-4 cm of more recent sediments deposited on top of this event. Sediment contributions from rare events, like Tropical Storm Irene, were found to be less influential than the annual spring freshet in the long-term infilling of waterbodies along the Lower Connecticut River. However, sediments from Irene are compositionally unique and serve to highlight the importance of this event in removing glacially derived fines from the river’s upland catchments.

Under the modern mortality pattern females die at all ages at a lower rate than males. However, this was not always the case. For much of the nineteenth century in the United States and parts of Europe it appears that females died at a higher rate with respect to at least one disease, pulmonary tuberculosis. The purpose of this research is to investigate this question in four towns of the Connecticut River Valley, Massachusetts. First, it is necessary to establish age- and sex-specific mortality rates in the four rural towns in the Connecticut River Valley during the latter half of the 19th century and beginning of the 20th. Secondly, it is necessary to identify those cases in which tuberculosis was the main disease and cause of death. This research seeks to discuss and contribute to the topic of excess female mortality. The four Massachusetts towns of Greenfield, Deerfield, Shelburne, and Montague constitute my research sites. These towns are appropriate for the anthropological pursuit of historical epidemiology due first to the towns’ rural nature at a time when the majority of Americans lived in rural towns, not large urban cities where studies are often focused. Secondly, these towns are of interest because of the extensive data collection that has been conducted previously. Tuberculosis (TB) is an interesting and instructive disease to focus research on. TB has re-emerged in recent decades, and research on the disease may have applied implications and value. TB was the number one killer during the study period, and the nature of the disease is such that it is very sensitive to the social environment. The combination of a rural setting and tuberculosis may give insight into the etiology of a disease that shares a long yet uneven history with humans, and has both biological and cultural significance. Under the traditional mortality pattern females of particular age ranges have greater mortality rates than males. This research discovered that females exceeded males in mortality rates at ages ten to 19 and 30 to 39 and that TB was the root cause of greater female mortality. Interestingly, the sex-specific gap in TB mortality rates was much wider than the gap in overall mortality rates. Thus, while females were dying of one cause, evidence shows that males were dying of another, which may have offset male TB mortality rates.

Active geomorphic features of rivers like sandbars provide habitat for endangered and threatened riparian plant and animal species. However, human development has altered flow and sediment regimes, thus impairing formation of sandbars and islands. Large scale mapping of the fluvial geomorphology in river ecosystems like the Connecticut River is are necessary to understand the dynamics of these features and preserve habitat. Orthophotographs from 2012 from United States Department of Agriculture's Farm Service Agency (FSA), National Agriculture Imagery Program (NAIP) were used to develop a model in ArcGIS Pro to identify fluvial geomorphic features in the Connecticut River and 12 of its major tributaries. This multi-stage image classification model identifies and ranks pixels of proximity and similar color to identify and map sandbars and islands. Locations of sandbars distribution were mapped and analyzed for each river. In the majority of rivers, sandbar area per reach decreases downstream. For the mainstem, sandbar area decreased towards the mouth but with three increases of sandbars due to meandering and major tributary confluences of the White and Deerfield rivers. Dams tend to decrease sandbars downstream but the effect of dams is context specific. Sandbars are stored upstream of the impoundment on the Black River as expected, sandbars appear downstream of a dam on the mainstem if a tributary confluence is present. Conservation of high sandbar area reaches and naturally eroding stream banks are necessary for preservation of endangered species. This spatial model for sandbar mapping can be applied in other river ecosystems across the region.