Skip to main content

Thank you for visiting nature.com. You are using a browser version with limited support for CSS. To obtain the best experience, we recommend you use a more up to date browser (or turn off compatibility mode in Internet Explorer). In the meantime, to ensure continued support, we are displaying the site without styles and JavaScript.

  • Letter
  • Published:

Sand as a stable and sustainable resource for nourishing the Mississippi River delta

Abstract

The Mississippi River delta is undergoing a catastrophic drowning, whereby 5,000 km2 of low-lying wetlands have converted to open water over at least the past eight decades1, as a result of many anthropogenic and natural factors1,2,3. Continued net land loss has been thought inevitable due to a decline in the load of total suspended sediment—both sand and mud—carried by the river4. However, sand—which accounts for ~50–70% of modern and ancient Mississippi delta deposits5,6 but comprises only ~20% of the sampled portion of the total load3—could be more important than mud for subaerial delta growth5. Historically, half of the Mississippi River sediment load is supplied by the Missouri River3. Here we analyse suspended sediment load data from two locations downstream from the lowest Missouri River dam to show that the measured sand load in the lower 1,100 km of the Mississippi River has not significantly diminished since dam construction. A one-dimensional numerical model of river morphodynamics predicts that the sand load feeding the delta will decrease only gradually over the next several centuries, with an estimated decline from current values of no more than about 17% within the coming six centuries. We conclude that the lower Mississippi River channel holds a significant reservoir of sand that is available to replenish diminished loads via bed scour and substantially mitigate land loss.

This is a preview of subscription content, access via your institution

Access options

Buy this article

Prices may be subject to local taxes which are calculated during checkout

Figure 1: The Mississippi River drainage basin and the lower Mississippi River.
Figure 2: Sediment transport data from Thebes, Illinois, and Tarbert Landing, Mississippi.
Figure 3: Model results for sediment transport and channel-bed elevation for the lower Mississippi River.
Figure 4: Aerial image of the Mississippi River.

Similar content being viewed by others

References

  1. Walker, H. J., Coleman, J. M., Roberts, H. H. & Tye, R. S. Wetland Loss in Louisiana. Geografiska Annaler 69A, 189–200 (1987).

    Article  Google Scholar 

  2. Morton, R. A. & Bernier, J. C. Recent subsidence-rate reductions in the Mississippi Delta and their geological implications. J. Coast. Res. 26, 555–561 (2010).

    Article  Google Scholar 

  3. Meade, R. H. & Moody, J. A. Causes for the decline of suspended-sediment discharge in the Mississippi River system, 1940–2007. Hydrol. Process 24, 35–49 (2010).

    Google Scholar 

  4. Blum, M. D. & Roberts, H. H. Drowning of the Mississippi delta due to insufficient sediment supply and global sea-level rise. Nature Geosci. 2, 488–491 (2009).

    Article  Google Scholar 

  5. Roberts, H. H., Coleman, J. M., Bentley, S. J. & Walker, N. An embryonic major delta lobe: A new generation of delta studies in the Atchafalaya–Wax Lake Delta system. Gulf Coast Assoc. Geol. Soc. Trans. 53, 690–703 (2003).

    Google Scholar 

  6. Mohrig, D. & Armstrong, C. Building the coastline: Linking study of the modern and ancient depositional environments to predict the response of Mississippi River delta to environmental change. AGU (Fall Meeting Suppl.) abstr. EP43D-1491680 (2012)

  7. American Association of Port Authorities. World Port Rankings (2008); http://www.aapa-ports.org/Industry/content.cfm?ItemNumber=900&navItemNumber=551

  8. State of Louisiana Final Louisiana 2012 Master Plan Report (2012); http://www.coastalmasterplan.louisiana.gov/2012-master-plan/final-master-plan/

  9. Lorenzo-Trueba, J. et al. Exploring the role of organic matter accumulation on delta evolution. J. Geophys. Res. 117, 1–12 (2012).

    Article  Google Scholar 

  10. Wilson, C. A. & Allison, M. A. Sediment dynamics and geomorphology of eroding marsh shorelines in southeastern Louisiana. Estuar. Coast Shelf S. 80, 483–494 (2008).

    Article  Google Scholar 

  11. Nepf, H. M. Ecogeomorphology of Tidal Marshes 137–163 (American Geophysical Union, (2004).

    Google Scholar 

  12. Baumann, R. H., Day, J. W. & Miller, C. A. Mississippi deltaic wetland survival: Sedimentation versus coastal submergence. Science 224, 1093–1095 (1984).

    Article  Google Scholar 

  13. Kenney, M. A. et al. Cost analysis of water and sediment diversions to optimize land building in the Mississippi River delta. Wat. Resour. Res. 49, 3388–3405 (2013).

    Article  Google Scholar 

  14. Kim, W., Mohrig, D., Twilley, R., Paola, C. & Parker, G. Is it feasible to build new land in the Mississippi River Delta? Eos Trans. AGU 90, 373–374 (2009).

    Article  Google Scholar 

  15. Paola, C. et al. Natural processes in delta restoration: Application to the Mississippi Delta. Annu. Rev. Mar. Sci. 3, 67–91 (2011).

    Article  Google Scholar 

  16. Day, G., Dietrich, W. E., Rowland, J. C. & Marshall, A. The depositional web on the floodplain of the Fly River, Papua New Guinea. J. Geophys. Res. 113, 1–19 (2008).

    Article  Google Scholar 

  17. Nittrouer, J. A., Mohrig, D. & Allison, M.A. Punctuated sand transport in the lowermost Mississippi River. J. Geophys. Res. 116, 1–24 (2011).

    Article  Google Scholar 

  18. Nittrouer, J. A., Shaw, J., Lamb, M. P. & Mohrig, D. Spatial and temporal trends for water-flow velocity and bed-material sediment transport in the lower Mississippi River. Geol. Soc. Am. Bull. 124, 400–414 (2012).

    Article  Google Scholar 

  19. Nittrouer, J. A. et al. Mitigating land loss in coastal Louisiana by controlled diversion of Mississippi River sand. Nature Geosci. 5, 534–537 (2012).

    Article  Google Scholar 

  20. Horowitz, A. J., Elrick, K. A. & Smith, J. J. Annual suspended sediment and trace element fluxes in the Mississippi, Columbia, Colorado, and Rio Grande drainage basins. Hydrol. Process 15, 1169–1207 (2001).

    Article  Google Scholar 

  21. Saucier, R. T. Geomorphology and Quaternary Geologic History of the Lower Mississippi Valley (US Army Corps of Engineers, (1994).

    Google Scholar 

  22. Edmonds, D. A. Stability of backwater-influenced river bifurcations: A study of the Mississippi–Atchafalaya system. Geophys. Res. Lett. 39, 1–5 (2012).

    Article  Google Scholar 

  23. Fisk, H. N. Geological Investigation of the Alluvial Valley of the Lower Mississippi River (Mississippi River Commission, (1944).

    Google Scholar 

  24. National Resources Conservation Service. Phase II Sedimentation Assessment for the Upper Missouri River Basin: Assessment Report. Report available at: http://www.msaconline.com/Missouri%20River%20Phase%20II%20%20Report.pdf Prepared by the United States Department of Agriculture, Natural Resources Conservation Service, in consultation with the US Army Corps of Engineers and the US Geological Survey. 51 (2009)

  25. Smith, N. D. & Perez-Arlucea, M. Natural levee deposition during the 2005 flood of the Saskatchewan River. Geomorphology 101, 583–594 (2008).

    Article  Google Scholar 

  26. Nittrouer, J. A., Mohrig, D., Allison, M. A. & Peyret, A. B. The lowermost Mississippi River: A mixed bedrock-alluvial channel. Sedimentology 58, 1914–1934 (2011).

    Article  Google Scholar 

  27. Nittrouer, J. A., Allison, M. A. & Campanella, R. Bedform transport rates for the lowermost Mississippi River. J. Geophys. Res. 113, 1–16 (2008).

    Article  Google Scholar 

  28. Lauer, J. W. & Parker, G. Net local removal of floodplain sediment by river meander migration. Geomorphology 96, 123–149 (2008).

    Article  Google Scholar 

  29. Syvitski, J. P. M. et al. Sinking deltas due to human activities. Nature Geosci. 2, 681–686 (2009).

    Article  Google Scholar 

  30. Kolker, A. S., Allison, M. A. & Hameedj, S. An evaluation of subsidence rates and sea-level variability in the northern Gulf of Mexico. Geophys. Res. Lett. 38, 1–6 (2011).

    Article  Google Scholar 

Download references

Acknowledgements

This research represents a contribution to the Mississippi Wetlands restoration effort of the National Center for Earth-surface Dynamics, a Science and Technology Center of the US National Science Foundation. We thank Gary Parker and Eric Prokocki for help and support. Brandon McElroy is also thanked for his support. We also thank Charlie Hager and Alex Nettles for helping organize the data from Thebes and Tarbert Landing.

Author information

Authors and Affiliations

Authors

Contributions

J.A.N. processed the USGS data, constructed the model and was the lead author of the manuscript; E.V. processed the USGS data, constructed the model and provided significant editorial feedback on the manuscript.

Corresponding author

Correspondence to Jeffrey A. Nittrouer.

Ethics declarations

Competing interests

The authors declare no competing financial interests.

Supplementary information

Supplementary Information

Supplementary Information (PDF 3892 kb)

Rights and permissions

Reprints and permissions

About this article

Check for updates. Verify currency and authenticity via CrossMark

Cite this article

Nittrouer, J., Viparelli, E. Sand as a stable and sustainable resource for nourishing the Mississippi River delta. Nature Geosci 7, 350–354 (2014). https://doi.org/10.1038/ngeo2142

Download citation

  • Received:

  • Accepted:

  • Published:

  • Issue Date:

  • DOI: https://doi.org/10.1038/ngeo2142

This article is cited by

Search

Quick links

Nature Briefing

Sign up for the Nature Briefing newsletter — what matters in science, free to your inbox daily.

Get the most important science stories of the day, free in your inbox. Sign up for Nature Briefing