Radon‐traced pore‐water as a potential source of CO2 and CH4 to receding black and clear water environments in the Amazon Basin
Abstract Groundwater is a primary source of dissolved CO2 and CH4 in Amazonian headwaters, yet in higher order rivers, a groundwater/pore‐water source is difficult to constrain due to the high spatial and temporal heterogeneity of pore‐water exchange. Here, we report coupled, high resolution measure...
Main Authors: | , , , , , , |
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Format: | Article |
Language: | English |
Published: |
Wiley
2018-10-01
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Series: | Limnology and Oceanography Letters |
Online Access: | https://doi.org/10.1002/lol2.10089 |