Repository logo
Log in(current)
Repository logoMIT Open ScholarshipDSpace@MIT
  1. Home
  2. MIT Libraries
  3. MIT Theses
  4. Doctoral Theses
  5. Barrier Island Groundwater Dynamics

Barrier Island Groundwater Dynamics

Thumbnail Image
Download
Name

Housego_rhousego_PhD_CEE_2021_thesis.pdf

Description
Thesis PDF
Size

6.05 MB

Format

Adobe PDF

Checksum (MD5)

98f30de8eb58ed30ef78927b341e571e

Thumbnail Image
Download
Name

toc disclaimer sheets.pdf

Description
Supplementary file
Size

68.61 KB

Format

Adobe PDF

Checksum (MD5)

53c5c860ba5db30472fc21570ac84bd7

Author(s)
Housego, Rachel Mary
Advisor(s)
Raubenheimer, Britt
Date Issued
June 2021
Publisher
Massachusetts Institute of Technology
Abstract
Nearly 1.5 million people inhabit barrier islands along the U.S. Atlantic and Gulf Coasts and coastal groundwater dynamics influence the availability of freshwater, ecosystem health, pollutant transport, and flooding in these densely populated communities. However, groundwater dynamics, including the aquifer head distribution and subsurface salinity structure, in coastal aquifers are affected by multiple environmental forcings, such as waves, tides, storm surges, and precipitation that act on a variety of spatial and temporal scales, making coastal groundwater dynamics complex and difficult to predict. Here, measurements of groundwater heads, salinities, and temperatures collected for 3 years across a 550-m-wide barrier island are used in conjunction with observations of ocean tides, surge, waves, sound level, and rainfall to characterize the dynamics of the surface aquifer. Infiltration from surge, tides, and waves during storms caused up to 2 m increases in the groundwater level under the dune. The head gradients owing to these storm-induced groundwater bulges suggest flows become inland directed on the ocean-side of the island during storms. An upper saline plume (20-30 PSU) was observed above fresher (10 PSU) water up to 30 m inland of the dune face, which was the maximum wave runup location. Differences in inland propagation between tidal- and storm-induced groundwater head fluctuations are explained using analytical theories for intermediate depth aquifers. Additionally, a separate analytical water-table evolution model driven with estimated ocean shoreline water levels (based on the 36-hr-averaged offshore tide, surge, and wave height) and measured precipitation is validated by citizen-science flood reports and predicts the maximum water-table height within 0.1 m of the observed levels across the barrier island.
MIT Department
Massachusetts Institute of Technology. Department of Civil and Environmental Engineering
Terms of Use
In Copyright - Educational Use Permitted
https://rightsstatements.org/page/InC-EDU/1.0/
Copyright retained by author(s)
Persistent DSpace Link
https://hdl.handle.net/1721.1/140363
Repository logo
PrivacyPermissionsAccessibilityContact us
Repository logo
Notify us about copyright concerns.