The Buffer Capability of the Ocean to Increasing Atmospheric CO2

Xu Yongfu

doi:10.1007/BF02677083

Impact Factor: 5.8

Volume 9 Issue 4

Oct. 1992

Article Contents

Article > ADVANCES IN ATMOSPHERIC SCIENCES > 1992 > 9(4): 501-510

The Buffer Capability of the Ocean to Increasing Atmospheric CO2

Xu Yongfu

1.
Institute of Atmospheric Physics, Academia Sinica, Beijing 100029

Xu Yongfu

doi: 10.1007/BF02677083

Abstract
References
Related papers
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Abstract:
The CO2-seawaler system and the method for calculating the partial pressure of CO2 (pCO3) in seawater are stu-died. The buffer capability of the ocean to increasing atmospheric CO2, is expressed in terms of the differential buffer factor and buffer index. Dissolutions of aragonite and calcite have a significant influence on the differential buffer factor. The trend of change in the buffer factor is obtained by a box model.
References

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Manuscript History

Manuscript received: 10 October 1992

Manuscript revised: 10 October 1992

通讯作者: 陈斌, bchen63@163.com

1.
沈阳化工大学材料科学与工程学院沈阳 110142

The Buffer Capability of the Ocean to Increasing Atmospheric CO2

Xu Yongfu

1. Institute of Atmospheric Physics, Academia Sinica, Beijing 100029

Manuscript received: 1992-10-10
Manuscript revised: 1992-10-10

Abstract: The CO2-seawaler system and the method for calculating the partial pressure of CO2 (pCO3) in seawater are stu-died. The buffer capability of the ocean to increasing atmospheric CO2, is expressed in terms of the differential buffer factor and buffer index. Dissolutions of aragonite and calcite have a significant influence on the differential buffer factor. The trend of change in the buffer factor is obtained by a box model.