4.3 Article

Groundwater-surface water interactions and agricultural nutrient transport in a Great Lakes clay plain system

期刊

JOURNAL OF GREAT LAKES RESEARCH
卷 47, 期 1, 页码 145-159

出版社

ELSEVIER SCI LTD
DOI: 10.1016/j.jglr.2020.11.008

关键词

Phosphorus; Nitrogen; Nutrient transport; Groundwater-surface water interactions

资金

  1. Ontario Ministry of Agriculture, Food and Rural Affairs (OMAFRA)
  2. Ontario Agri-Food Innovation Alliance [030319]

向作者/读者索取更多资源

This study conducted in southwestern Ontario, Canada, aimed to investigate the spatial and temporal variations of phosphorus and nitrate in agricultural areas to assess nutrient transport pathways and groundwater-surface water interactions. The results showed that tile drainage played a larger role in phosphorus transport compared to groundwater, and stream water exhibited elevated nutrient concentrations.
Nutrient export from agricultural land to surface waters is a significant environmental concern within the Great Lakes Basin (GLB). A field-based watershed-scale study was completed to investigate spatial and temporal variations of phosphorus and nitrate to assess nutrient transport pathways and groundwater-surface water interactions in an agriculturally dominated clay plain system. This was conducted in the 127 km2 Upper Parkhill Watershed, near Lake Huron in southwestern Ontario, Canada. Data collection occurred from June 2018 to May 2019 via continuous sensor deployment and discrete sampling of stream water, groundwater, hyporheic zone, and tile drainage water. Samples were analyzed for various nutrient species (total, total dissolved, soluble reactive, and particulate phosphorus, and nitrate-N) to examine the hydrological dynamics of principal transport pathways of agriculturallyderived nutrients. Total phosphorus and nitrate concentrations in stream water ranged from 0.007 to 0.324 mg/L and 0.32 to 13.13 mg NO3-N/L, respectively. Tile drainage water total phosphorous concentrations varied from 0.006 to 0.066 mg/L. Groundwater total dissolved phosphorus concentrations ranged from <0.003 to 0.085 mg/L. Transport of phosphorus through tile drainage was observed to be greater than through groundwater over the study period. No distinct relationship was observed between nutrient concentrations in the hyporheic zone and the vertical hydraulic gradient within this zone in the studied stream reach. Preliminary correlations were discerned between water quality observations and recognized land management practices. Given the elevated stream nutrient concentrations, these results are consequential for the continual improvement of strategies and programs devised to conserve water resources within the GLB. (C) 2020 International Association for Great Lakes Research. Published by Elsevier B.V. All rights reserved.

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