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Published on: October 21, 2016
Quantifying Carbon Cycling across the Groundwater-Stream-Atmosphere Continuum Using High-Resolution Time Series of
Chuan Wang1,2,3, Matthias S Brennwald3, Yueqing Xie1,2
1Key Laboratory of Surficial Geochemistry, Ministry of Education, School of Earth Sciences and Engineering, Nanjing University, Nanjing 210023, China.
Groundwater significantly impacts stream carbon emissions, supplying CO2 and methane. High-resolution dissolved gas analysis reveals dynamic carbon cycling across the groundwater-stream-atmosphere continuum (GSAC).
Area of Science:
- Environmental Science
- Geochemistry
- Biogeochemistry
Background:
- Quantifying carbon cycling across the groundwater-stream-atmosphere continuum (GSAC) is vital for global carbon budgets.
- Coupled carbon exchange and turnover in the GSAC present significant quantification challenges.
Purpose of the Study:
- To disentangle carbon cycling processes within a representative GSAC transect.
- To quantify carbon exchange and turnover with high spatiotemporal resolution.
Main Methods:
- Obtained high-resolution time series of dissolved gases (He, Ar, Kr, O2, CO2, CH4).
- Employed numerical simulations to analyze gas concentrations and carbon dynamics.
- Investigated diurnal variations in stream metabolism and carbonate precipitation/dissolution.
Main Results:
- Groundwater contributes approximately 60% of stream CO2 and 30% of stream CH4 inputs.
- Stream CO2 and CH4 emissions to the atmosphere are supported by these groundwater inputs.
- Diurnal variations in stream metabolism drive significant carbonate precipitation and dissolution cycles.
Conclusions:
- Dissolved gases serve as effective tracers for discerning and quantifying GSAC carbon cycling.
- High-resolution time series are crucial for understanding the diurnal variability of biogeochemical processes.
- This study provides a mechanistic understanding of carbon cycling across the GSAC.
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