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Updated: Feb 13, 2026

Design and Use of a Full Flow Sampling System FFS for the Quantification of Methane Emissions
Published on: June 12, 2016
Scale-dependent processes drive spatially discontinuous methane emissions from small cascade reservoirs
Dongfeng Li1, Yuewei Zhang2, Xiaofeng Wang1
1Chongqing Key Laboratory of Carbon Cycling and Carbon Regulation in Mountain Ecosystems, School of Geography and Tourism, Chongqing Normal University, Chongqing 401331, China; Chongqing Field Scientific Observation and Research Station for Surface Ecological Processes in the Three Gorges Reservoir Area, Chongqing 405400, China.
Small cascade reservoirs are significant methane (CH4) hotspots, with emissions driven by reservoir size rather than location. Ebullition dominates CH4 release, showing a downstream "cascading efficiency" effect impacting climate assessments.
Area of Science:
- Environmental Science
- Geochemistry
- Hydrology
Background:
- River damming fundamentally alters aquatic ecosystems, yet methane (CH4) emissions from cascade reservoirs are poorly understood.
- Previous studies on large river-reservoir systems show longitudinal patterns in CH4 flux, often decreasing downstream.
- Small cascade systems present unique biogeochemical dynamics due to their physical configuration and material transport.
Purpose of the Study:
- To investigate the spatio-temporal patterns and controlling factors of CH4 dynamics in small cascade reservoirs.
- To quantify CH4 emission fluxes and identify dominant emission pathways.
- To assess the relationship between reservoir scale, organic carbon retention, and methanogenic potential.
Main Methods:
- Conducted annual investigations of CH4 dynamics across 15 small cascade reservoirs.
- Measured monthly CH4 fluxes (ebullition and diffusion) in each reservoir.
- Analyzed the ratio of methanogenic (mcrA) to aerobic (pmoA) genes in sediments.
- Calculated CH4 release efficiency relative to organic carbon stock.
Main Results:
- Small cascade reservoirs are significant CH4 hotspots with a mean flux of 2.73 ± 2.70 mmol m-2 d-1.
- CH4 fluxes showed spatial discontinuity, primarily governed by reservoir scale, not longitudinal position.
- Larger reservoirs exhibited higher CH4 fluxes due to enhanced organic matter retention and increased methanogenic potential.
- Ebullition was the dominant pathway (~70.5%), sensitive to reservoir size, while diffusion was scale-independent.
- A downstream increase in CH4 release efficiency, termed
Conclusions:
- Small cascade reservoirs create a unique, spatially discontinuous yet highly efficient CH4 emission regime.
- Reservoir scale is a key factor controlling CH4 hotspots and emission pathways.
- Accurate climate impact assessment requires accounting for scale-dependent emissions and downstream efficiency gains in global inventories.
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