Persistent Nitrate in Alpine Waters with Changing Atmospheric Deposition and Warming Trends.
Sydney C Clark1,2, Rebecca T Barnes3, Isabella A Oleksy4
1Department of Earth, Environmental, and Planetary Sciences, Brown University, Providence, Rhode Island 02912, United States.
Environmental Science & Technology
|October 12, 2021
Summary
Elevated nitrate in alpine lakes persists due to atmospheric deposition and catchment nitrification. Microbially produced nitrate is increasingly significant, linked to rising ammonium deposition in these sensitive ecosystems.
Area of Science:
- Environmental Chemistry
- Isotope Hydrology
- Alpine Ecology
Background:
- High-elevation lakes in the Colorado Front Range show persistent elevated nitrate levels.
- Atmospheric nitrate deposition has declined since 2000, making the nitrate source elusive.
- Shifts in nitrogen sources from glacial melt and atmospheric ammonium complicate nitrate origin.
Purpose of the Study:
- To constrain the provenance of elevated nitrate in alpine lakes.
- To investigate nitrate sources during the summer open-water season.
- To understand the role of different nitrogen inputs in alpine aquatic systems.
Main Methods:
- Analysis of complete nitrate isotopic composition (δ15N, δ18O, Δ17O).
- Sampling of nitrate-bearing source waters from two alpine ecosystems (2017-2018).
- Comparison with historical surface water samples from the mid-1990s to present.
Main Results:
- A consistent contribution (13-23%) of uncycled atmospheric nitrate was observed throughout the summer.
- Nitrification within the catchment, utilizing soil organic matter and ammonium deposition, likely contributes up to 87% of nitrate.
- Historical data reveal an increasing importance of microbially produced nitrate over time.
Conclusions:
- Both atmospheric deposition and catchment nitrification are significant nitrate sources in alpine lakes.
- Increasing ammonium deposition is linked to a greater role of microbially produced nitrate.
- Understanding these nitrogen sources is crucial for managing alpine aquatic ecosystems.
Related Concept Videos
2° Amines to N-Nitrosamines: Reaction with NaNO2
4.7K
Secondary amines react with nitrous acid to form N-nitrosamines, as depicted in Figure 1. Nitrous acid, a weak and unstable acid, is formed in situ from an aqueous solution of sodium nitrite and strong acids, such as hydrochloric acid or sulfuric acid, in cold conditions. In the presence of an acid, the nitrous acid gets protonated. The subsequent loss of water results in the formation of the electrophile known as nitrosonium ion.
4.7K
Primary Production
24.2K
The total amount of energy acquired by primary producers in an ecosystem is called gross primary production (GPP). However, of this energy, producers use some for metabolic processes, and some is lost as heat, decreasing the amount of energy available to the next trophic level. The remaining usable amount of energy is called the net primary productivity (NPP). In terrestrial ecosystems, NPP is driven by climate, while light penetration and nutrient availability drive NPP in aquatic ecosystems.
24.2K
The Nitrogen Cycle
56.3K
Nitrogen atoms, present in all proteins and DNA, are recycled between abiotic and biotic components of the ecosystem. However, the primary form of nitrogen on Earth is nitrogen gas, which cannot be used by most animals and plants. Thus, nitrogen gas must first be converted into a usable form by nitrogen-fixing bacteria before it can be cycled through other living organisms. The use of nitrogen-containing fertilizers and animal waste products in human agriculture has greatly influenced the...
56.3K
1° Amines to Diazonium or Aryldiazonium Salts: Diazotization with NaNO2 Overview
3.5K
Nitrous acid and nitric acids are two types of acids containing nitrogen, among which nitrous acid is weaker than nitric acid. Nitrous acid with a pKa value of 3.37 ionizes in water to give a nitrite ion and the hydronium ion.
The nitrous acid is unstable. Hence, it is formed in situ from a solution of sodium nitrite and cold aqueous acids such as hydrochloric or sulfuric acid. In an acidic solution, the –OH group of nitrous acid undergoes protonation to give oxonium ion, followed by...
The nitrous acid is unstable. Hence, it is formed in situ from a solution of sodium nitrite and cold aqueous acids such as hydrochloric or sulfuric acid. In an acidic solution, the –OH group of nitrous acid undergoes protonation to give oxonium ion, followed by...
3.5K
Overview of Nitrogen Metabolism
9.8K
Nitrogen is a very important element for life because it is a major constituent of proteins and nucleic acids. It is a macronutrient, and in nature, it is recycled from organic compounds and stored in the form of ammonia, ammonium ions, nitrate, nitrite, or nitrogen gas by many metabolic processes. Many of these metabolic processes are carried out only by prokaryotes.
The largest pool of nitrogen available in the terrestrial ecosystem is gaseous nitrogen (N2) from the air, but this...
The largest pool of nitrogen available in the terrestrial ecosystem is gaseous nitrogen (N2) from the air, but this...
9.8K
Metabolism of Chemolithotrophs
325
Chemolithotrophs are microorganisms that obtain energy by oxidizing inorganic molecules such as hydrogen gas (H₂), ammonia (NH₃), reduced sulfur compounds (H₂S, S²⁻), and ferrous iron (Fe²⁺). Unlike heterotrophic organisms that rely on organic carbon, chemolithotrophs transfer electrons from these inorganic donors to the electron transport chain (ETC), generating a proton motive force (PMF) that drives ATP synthesis through oxidative phosphorylation.
325


