Watershed Sediment Losses to Lakes Accelerating Despite Agricultural Soil Conservation Efforts

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Abstract

Agricultural soil loss and deposition in aquatic ecosystems is a problem that impairs water quality worldwide and is costly to agriculture and food supplies. In the US, for example, billions of dollars have subsidized soil and water conservation practices in agricultural landscapes over the past decades. We used paleolimnological methods to reconstruct trends in sedimentation related to human-induced landscape change in 32 lakes in the intensively agricultural region of the Midwestern United States. Despite erosion control efforts, we found accelerating increases in sediment deposition from erosion; median erosion loss since 1800 has been 15.4 tons ha-1. Sediment deposition from erosion increased >6-fold, from 149 g m-2 yr-1 in 1850 to 986 g m-2 yr-1 by 2010. Average time to accumulate one mm of sediment decreased from 631 days before European settlement (ca. 1850) to 59 days mm-1 at present. Most of this sediment was deposited in the last 50 years and is related to agricultural intensification rather than land clearance or predominance of agricultural lands. In the face of these intensive agricultural practices, traditional soil conservation programs have not decelerated downstream losses. Despite large erosion control subsidies, erosion and declining water quality continue, thus new approaches are needed to mitigate erosion and water degradation. © 2013 Heathcote et al.

Figures

  • Figure 1. Changing agricultural practices and regional lake sedimentation rates since European settlement, shown as decadal averages across all 32 lakes. (A) Percent land in farms (brown), percent of wetlands drained (light blue), maize yield (t ha21) (yellow), and cumulative USDA financial assistance (inflation adjusted) for soil and water conservation programs in the USA (green). (B) Average regional lake mass accumulation rates for erosional (black) and in-lake (fueled by nutrient enrichment; yellow) derived sediment (g m22 yr21). The time for lakes to add one mm of sediment is also shown (dark blue; days). Error bars represent 61 standard error. Agricultural data were summarized from the United States Department of Agriculture’s Census of Agriculture (1850–2007) and the National Agricultural Statistics Service. Annual maize yield data were fitted to a LOWESS model. doi:10.1371/journal.pone.0053554.g001
  • Table 1. Lake and watershed sizes, maximum 210Pb ages at the bottom of cores (6 SE), historic and modern sediment total (erosional+in-lake) mass accumulation rates (MAR; 6SE) for the sediment cores taken from 32 lakes in this study.
  • Figure 2. Watershed erosion (tons ha21 yr21) versus time for the 32 lakes in this study since 1800. Red line represents average rate of erosion (LOWESS smoothed fit to the data) from the watershed across all 32 lakes in this study, surrounded by the 95% confidence region. Blue lines represent LOWESS smoothed fits for each of the individual lakes and are included to visualize variability among lakes. doi:10.1371/journal.pone.0053554.g002

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CITATION STYLE

APA

Heathcote, A. J., Filstrup, C. T., & Downing, J. A. (2013). Watershed Sediment Losses to Lakes Accelerating Despite Agricultural Soil Conservation Efforts. PLoS ONE, 8(1). https://doi.org/10.1371/journal.pone.0053554

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