Sources of Sediment Loads to the Bay

Assessment
By Chart

Sediments are loose particles of clay, silt, sand and other substances that are suspended in the water and settle to the bottom of a water body.

 

Download This Data          Download This Slide


Importance

Sediments are a problem in the Bay because they can:

  • Smother bottom-dwelling plants and animals, such as oysters and clams.
  • Become suspended in the water column, making the water cloudy so less light is available for underwater bay grasses.
  • Carry high concentrations of certain toxic chemicals that contaminate waterways. 
  • Carry nutrients, particularly phosphorous, which increase nutrient pollution in the Bay.
  • Accumulate in ports and waterways.

Most of the sediment delivered to the Bay comes from:

Learn more about sediment.

Additional Information

Based on long-term average hydrology simulations, it is estimated that 4.8 million tons of sediment were delivered to the Bay’s tidal waters in 2007, compared to 5.9 million tons in 1985.

Loads are simulated based on reported implementation of best management practices (BMPs) that reduce sediment pollution. The simulation removes annual hydrological variations to measure the effectiveness of BMP implementation and converts the numerous BMPs, which have various pollution reduction efficiencies depending on type and location in the watershed, to a common currency of sediment reduction.

Agricultural Land

Approximately 2.9 million tons, or 60 percent of the total sediment load to the Bay, is due to runoff from agricultural areas.

These detrimental loads to the Bay could be reduced by using BMPs that prevent sediment from reaching local waterways that lead to the Bay.

Urban/Suburban Runoff and Legacy Sediment

Approximately 900,000 tons, or 19 percent of the total sediment load to the Bay, is due to runoff from urban and suburban areas and legacy sediment in stream channels from deposits that occurred during the conversion of forest land to agricultural and urban land uses.

These detrimental loads to the Bay could be reduced by using BMPs that prevent any sediment from reaching local waterways that lead to the Bay.

Natural

Approximately 1 million tons, or 21 percent of the total sediment load to the Bay, is due to natural sources such as forests.

Sources Not Accounted For in the Chart

Tidal shoreline erosion is also a significant source of sediments to the Bay, but is not accounted for in the chart.

Reporting Indicator
Contact

For more information contact:Jeff Sweeney at 800-968-7229 ext. 844

Source of Data

Chesapeake Bay Program Phase 4.3 Watershed Model 2007 Simulation

Font SizeSmall Font Standard Font Large Font             Print this Article             Send Comments About This Article
 
Last modified: 09/01/2009
For more information, contact the Chesapeake Bay Program Office:
410 Severn Avenue / Suite 109 / Annapolis, Maryland 21403
Tel: (800) YOUR-BAY / Fax: (410) 267-5777 | Directions to the Bay Program Office
Terms of Use | Privacy Policy