National Science Foundation and Charles Lamar Family Foundation
Tracing Amite River sediment in the wake of the August 2016 flood
17 months
The Challenge
A heavy rain turned into a deluge in August 2016, ultimately resulting in more than 19 inches of precipitation falling in Baton Rouge and more than 31 inches in portions of adjacent Livingston Parish. This tremendous rainfall during such a short period of time overwhelmed the region’s drainage systems, including the Amite River, and resulted in widespread flooding throughout the lower portion of the drainage basin including the greater Baton Rouge area.
After the flood waters subsided, it was evident that the Amite River had transported large amounts of sediment down river and across the floodplain, as evidenced by piles of sand left in backyards, driveways, and parking lots. However, the sediment’s volume, character and depositional pattern is unknown and can tell us a great deal about how rivers respond to extreme events.
The Approach
With funding from a National Science Foundation Rapid Response Research grant and from the Charles Lamar Family Foundation, Institute researchers started took field measurements, supplemented by satellite data of the changes the flood wrought to the river’s channel and floodplain soon after the floodwaters receded. Researchers focused on locating and quantifying flood deposits on the floodplain, alterations to the channel’s location and shape, and examining the sediment discharged through the river’s mouths into Lake Maurepas and adjacent swamps.
Researchers collected 115 sediment cores and surface grab samples from the Amite River basin in an area stretching from Darlington, La. into Lake Maurepas. Sediment core analysis, field data, and remote sensing imagery were used to improve knowledge about how the river channel and floodplain were changed by the 2016 flood event.
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