Abstract

Nutrient loading from nonpoint source runoff in the Midwest has emerged as one of the largest threats to water quality as the frequency of harmful algal blooms, hypoxic zones, and issues associated with human-resource interactions have risen abruptly over the past several decades. In this study, a saturated buffer ~500 m in length located in the western basin of the Lake Erie watershed was evaluated for its potential to reduce edge of field runoff and nutrient loading. Saturated buffers reduce runoff by routing subsurface tile drainage water into the riparian zone, providing an opportunity for drainage volume as well as nutrient reduction of runoff waters. Over a 12-month study period, controlled drainage was used to redirect nearly 25% of the total tile flow into the riparian zone from a subwatershed in corn/soybean rotation with near complete reductions of dissolved nitrogen and phosphorus from tile inflows averaging 4.7 and 0.08 mg/L, respectively, as well as total reduction of suspended sediments (average 10.4 mg/L). This study provides additional evidence that riparian areas are an important part of nutrient reduction strategies as they can act as both controlled drainage points by raising water tables in fields as well as nutrient sinks which couple to help mitigate nutrient runoff in the region.

Highlights

  • Eutrophication of rivers and lakes as a result of nutrient loading has become one of the most widespread threats to freshwater ecosystems in the eastern United States

  • Organic matter percentages in the riparian were significantly higher than the field area, measuring 5.2% in the first meter of depth compared to 2.9%, respectively

  • Tile flow was observed over 119 days of the year, and while surface flow was not measured, anecdotal observation of surface flow through one obvious lower swale did occur during the highest spring rains, indicating that the remaining 85% of precipitation was not all stored in soils

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Summary

Introduction

Eutrophication of rivers and lakes as a result of nutrient loading has become one of the most widespread threats to freshwater ecosystems in the eastern United States. Excess nutrient loading has manifested on a region wide scale in the formation of harmful algal blooms (HABs) in lakes and slow-moving rivers where a variety of cyanobacteria genera (e.g., Microcystis, Anabaena, Aphanizomenon, Planktothrix, etc.) have negatively affected water clarity, esthetic, human health as a result of consumption or exposure to a variety of bloom produced toxins, as well as other aquatic life through formation of ‘dead zones’ (Braig et al, 2011; Brooks et al, 2016). While HABs in the Great Lakes region are not novel, in recent years they have become increasingly frequent and severe (Michalak et al, 2013; Kane et al, 2014) with wide reaching economic and ecosystem level consequences (Wolf, Georgic & Klaiber, 2017)

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