Marmots do not drink coffee: Human urine contributions to the nitrogen budget of a popular national park destination

Author:

Baron Jill S.1ORCID,Weinmann Tim1,Acharya Varun Kirk2,Charlton Caitlin3,Nydick Koren R.4,Esser Scott4

Affiliation:

1. U.S. Geological Survey Fort Collins Science Center Fort Collins Colorado USA

2. Sleeping Bear Dunes National Lakeshore National Park Service Empire Michigan USA

3. Graduate Degree Program in Ecology Colorado State University Fort Collins Colorado USA

4. Rocky Mountain National Park National Park Service Estes Park Colorado USA

Abstract

AbstractReactive nitrogen (Nr) concentrations are higher than expected for mountain lakes in Rocky Mountain National Park, and for many years, high Nr concentrations have been attributed to atmospheric Nr deposition from regional and more distant emission sources, including combustion of fossil fuels and agricultural activities. Here, we estimated the contribution from a very local source, that of human urine, related to intensive use by visitors in Loch Vale Watershed (LVWS). Not only does urine convey hormones, pharmaceuticals, antibiotic‐resistant bacteria, and antibiotic‐resistant genes to the environment, but it also contributes Nr, which contributes to loss of biodiversity and eutrophication. Using caffeine as a specific marker for human urine, we compared the calculated maximum potential input of urine with that from wet atmospheric Nr deposition. The maximum potential input is a worst‐case scenario. Nearly 30,000 and 45,000 people hiked the 4.0 km to the Loch, the lowest lake in LVWS, in June–September 2019 and 2020, respectively. Informal trails and informal latrine sites were mapped, and the contribution of human urine was calculated based on several assumptions, including that each visitor voided their bladder on the ground once per visit somewhere in Loch Vale. The resulting Nr input from urine in Loch Vale for the summer months of June through September was 0.02 kg Nr ha−1, and prorated to a full year, the 2019 potential contribution of human waste was 0.06 kg ha−1 year−1. These values are compared with June–September 1.2 kg Nr ha−1 from wet atmospheric deposition or annual measured 2019 deposition of 2.5 kg Nr ha−1 year−1, to indicate a contribution of 2% Nr to the waters of Loch Vale from local human urine. Most Nr in this alpine and subalpine watershed is still attributable to emissions and subsequent wet atmospheric deposition, but a 2% contribution from human waste is not insignificant. In the very broadest sense, our results document an ecological disturbance from an unprecedented level of human activity in a protected and designated wilderness area. Local solutions to this local problem could include greater outreach to visitors of public lands about the consequences of their activities and installation of latrines.

Funder

U.S. Geological Survey

Publisher

Wiley

Subject

Ecology,Ecology, Evolution, Behavior and Systematics

Reference42 articles.

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2. Hindcasting Nitrogen Deposition To Determine An Ecological Critical Load

3. Long‐term ecosystem and biogeochemical research in Loch Vale watershed, Rocky Mountain National Park, Colorado

4. Ecosystem Responses to Nitrogen Deposition in the Colorado Front Range

5. Baron J. S. T.Weinmann andV. K.Acharya.2023.“Soil and Surface Water Nitrogen and Caffeine Data from 2019 and 2019–2020 Trail Counts of Hikers in Loch Vale Watershed Rocky Mountain National Park.”USGS Data Release.https://doi.org/10.5066/P95IOUKH.

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