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Carbon source/sink function of a subtropical, eutrophic lake determined from an overall mass balance and a gas exchange and carbon burial balance

Carbon source/sink function of a subtropical, eutrophic lake determined from an overall mass balance and a gas exchange and carbon burial balance
Carbon source/sink function of a subtropical, eutrophic lake determined from an overall mass balance and a gas exchange and carbon burial balance
Although studies on carbon burial in lake sediments have shown that lakes are disproportionately important carbon sinks, many studies on gaseous carbon exchange across the water–air interface have demonstrated that lakes are supersaturated with CO2 and CH4 causing a net release of CO2 and CH4 to the atmosphere. In order to more accurately estimate the net carbon source/sink function of lake ecosystems, a more comprehensive carbon budget is needed, especially for gaseous carbon exchange across the water–air interface. Using two methods, overall mass balance and gas exchange and carbon burial balance, we assessed the carbon source/sink function of Lake Donghu, a subtropical, eutrophic lake, from April 2003 to March 2004. With the overall mass balance calculations, total carbon input was 14 905 t, total carbon output was 4950 t, and net carbon budget was +9955 t, suggesting that Lake Donghu was a great carbon sink. For the gas exchange and carbon burial balance, gaseous carbon (CO2 and CH4) emission across the water–air interface totaled 752 t while carbon burial in the lake sediment was 9477 t. The ratio of carbon emission into the atmosphere to carbon burial into the sediment was only 0.08. This low ratio indicates that Lake Donghu is a great carbon sink. Results showed good agreement between the two methods with both showing Lake Donghu to be a great carbon sink. This results from the high primary production of Lake Donghu, substantive allochthonous carbon inputs and intensive anthropogenic activity. Gaseous carbon emission accounted for about 15% of the total carbon output, indicating that the total output would be underestimated without including gaseous carbon exchange.

Due to high primary production, substantive allochthonous carbon inputs and intensive anthropogenic acitivity, subtropical, eutrophic Lake Donghu is a great carbon sink.

carbon budget, overall mass balance, gas exchange, carbon burial, lake donghu
0269-7491
559-568
Yang, Hong
2ea2c94c-8d28-4555-98f9-59b615b0cee7
Xing, Yangping
ab1dc613-403f-4216-9f3e-fc7b06ac776f
Xie, Ping
bf059083-ccc2-464c-9f1f-83ace6e26e04
Ni, Leyi
51f18d39-bd71-41bd-8266-35e1e5e634cc
Rong, Kewen
efe0f096-3846-4781-8745-22193f0e61cd
Yang, Hong
2ea2c94c-8d28-4555-98f9-59b615b0cee7
Xing, Yangping
ab1dc613-403f-4216-9f3e-fc7b06ac776f
Xie, Ping
bf059083-ccc2-464c-9f1f-83ace6e26e04
Ni, Leyi
51f18d39-bd71-41bd-8266-35e1e5e634cc
Rong, Kewen
efe0f096-3846-4781-8745-22193f0e61cd

Yang, Hong, Xing, Yangping, Xie, Ping, Ni, Leyi and Rong, Kewen (2008) Carbon source/sink function of a subtropical, eutrophic lake determined from an overall mass balance and a gas exchange and carbon burial balance. Environmental Pollution, 151 (3), 559-568. (doi:10.1016/j.envpol.2007.04.006). (PMID:17664033)

Record type: Article

Abstract

Although studies on carbon burial in lake sediments have shown that lakes are disproportionately important carbon sinks, many studies on gaseous carbon exchange across the water–air interface have demonstrated that lakes are supersaturated with CO2 and CH4 causing a net release of CO2 and CH4 to the atmosphere. In order to more accurately estimate the net carbon source/sink function of lake ecosystems, a more comprehensive carbon budget is needed, especially for gaseous carbon exchange across the water–air interface. Using two methods, overall mass balance and gas exchange and carbon burial balance, we assessed the carbon source/sink function of Lake Donghu, a subtropical, eutrophic lake, from April 2003 to March 2004. With the overall mass balance calculations, total carbon input was 14 905 t, total carbon output was 4950 t, and net carbon budget was +9955 t, suggesting that Lake Donghu was a great carbon sink. For the gas exchange and carbon burial balance, gaseous carbon (CO2 and CH4) emission across the water–air interface totaled 752 t while carbon burial in the lake sediment was 9477 t. The ratio of carbon emission into the atmosphere to carbon burial into the sediment was only 0.08. This low ratio indicates that Lake Donghu is a great carbon sink. Results showed good agreement between the two methods with both showing Lake Donghu to be a great carbon sink. This results from the high primary production of Lake Donghu, substantive allochthonous carbon inputs and intensive anthropogenic activity. Gaseous carbon emission accounted for about 15% of the total carbon output, indicating that the total output would be underestimated without including gaseous carbon exchange.

Due to high primary production, substantive allochthonous carbon inputs and intensive anthropogenic acitivity, subtropical, eutrophic Lake Donghu is a great carbon sink.

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More information

Published date: February 2008
Keywords: carbon budget, overall mass balance, gas exchange, carbon burial, lake donghu

Identifiers

Local EPrints ID: 153553
URI: http://eprints.soton.ac.uk/id/eprint/153553
ISSN: 0269-7491
PURE UUID: 7d5e6dbe-ffef-4658-ba9f-32d2ac1b99f6

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Date deposited: 11 May 2011 09:05
Last modified: 14 Mar 2024 01:31

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Contributors

Author: Hong Yang
Author: Yangping Xing
Author: Ping Xie
Author: Leyi Ni
Author: Kewen Rong

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