东海中北部海域秋季表层海水中无机碳与海气界面碳的迁移
Dissolved inorganic carbon and air-sea carbon exchange flux in the central and northern East China Sea in autumn
查看参考文献36篇
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文摘
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基于2010年11月对长江口外东海中北部海域的综合调查,系统研究了该海域的无机碳体系参数的分布特征、海?气界面二氧化碳通量及其影响因素。研究结果表明,该海域秋季溶解无机碳(DIC)高值区主要出现在调查海域东北部及长江口附近海域,而调查海域南部DIC含量较少且变化平缓,其主要是受台湾东部流向东北方向的黑潮支流及长江冲淡水的影响;表层海水CO_2分压(pCO_2)值变化范围为40.8 ~ 63.5 Pa,呈现沿黑潮支流流入方向由东南向西北逐渐增高的趋势。秋季表层海水pCO_2与温度(T)、盐度(S)有较好的负相关性,说明海水温度升高和盐度增加,pCO_2降低,反之亦然。另外,通过估算得出,秋季CO_2海-气交换通量为2.69~33.66 mmol/(m~2·d),平均值为(14.35 ± 7.06 )mmol/(m~2·d),其在长江口邻近海域相对较大,而在调查海域南部相对较小; 2010年秋季水体向大气释放CO_2的量(以碳计)为(2.35 ± 1.16)×10~4 t/d,是大气CO_2较强的源,说明东海中北部海域秋季总体上是CO_2的源。 |
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其他语种文摘
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Based on the comprehensive survey in the central and northern East China Sea near the Yangtze River estuary in November 2010, the distribution of the dissolved inorganic carbon system and air-sea exchange flux of carbon dioxide and its influencing factors were examined in this paper. High DIC was found in the northeast of the investigated area and Yangtze River estuary, whereas DIC content was small and changed gently in the south of the investigated area. The investigated area was mainly affected by the Kuroshio Branch Current which flows from the east part of Taiwan to northeast and Changjiang River Diluted Water.The pCO_2 ranged from 40.8 ~ 63.5 Pa with an increasing trend from southeast area to northwest area along the KBCNT. The pCO_2 in the surface water negatively correlated with temperature and salinity, suggesting that with the increase of the temperature and salinity, the pCO_2 decreased, and vice versa. In addition, according to calculation, the net sea-to-air CO_2 exchange flux in autumn at each station was obtained. It varied from 2.69 to 33.66 mmol/(m~2·d) with an average of (14.35 ± 7.06) mmol/(m~2·d). The carbon flux near the Yangtze River Estuary was higher than that in the south part of the investigated area. Overall, the central and northern East China Sea emitted 2.35×10~4 ± 1.16×10~4 tons of carbon to the atmosphere per day which was a relatively strong source of atmospheric CO_2 in autumn. |
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来源
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海洋科学
,2012,36(10):26-32 【核心库】
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关键词
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海-气界面碳通量
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海水无机碳
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东海中北部海域
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地址
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中国科学院海洋研究所, 中国科学院海洋生态与环境科学重点实验室, 山东, 青岛, 266071
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语种
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中文 |
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ISSN
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1000-3096 |
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学科
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海洋学 |
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基金
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国家973计划
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中国科学院战略性先导科技专项
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国家自然科学基金
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文献收藏号
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CSCD:4733141
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参考文献 共
36
共2页
|
|
1.
Battle M. Global carbon sinks and their variability inferred from atmospheric O_2 and δ13C.
Science,2000,287:2467-2470
|
CSCD被引
52
次
|
|
|
|
|
2.
Tsunogai S. Is there a "continental shelf pump" for the absorption of atmospheric CO_2?.
Tellus. B,1999,51:701-712
|
CSCD被引
52
次
|
|
|
|
|
3.
Smyth T J. Integration of radiative transfer into satellite models of ocean primary production.
Journal of Geophysical Research,2005,110:1-11
|
CSCD被引
2
次
|
|
|
|
|
4.
谭燕. 夏季东海西部表层海水中的pCO_2及海-气界面通量.
海洋与湖沼,2004,35:239-244
|
CSCD被引
22
次
|
|
|
|
|
5.
Andersson A J. Shallow-water oceans: a source or sink of atmospheric CO_2?.
Frontiers in Ecology and the Environment,2004,2(7):348-353
|
CSCD被引
6
次
|
|
|
|
|
6.
Thomas H. Enhanced open ocean storage of CO_2 from shelf sea pumping.
Science,2004,304:1005-1008
|
CSCD被引
29
次
|
|
|
|
|
7.
Borges A V. Do we have enough pieces of the jigsaw to integrate CO_2 fluxes in the coastal ocean?.
Estuaries and Coasts,2005,28(1):3-27
|
CSCD被引
13
次
|
|
|
|
|
8.
Cai W J. Comment on "enhanced open ocean storage of CO_2 from shelf sea pumping".
Science,2004,306:1477
|
CSCD被引
17
次
|
|
|
|
|
9.
Nitishinsky M. Inorganic carbon and nutrient fluxes on the Arctic Shelf.
Continental Shelf Research,2007,27(10/11):1584-1599
|
CSCD被引
5
次
|
|
|
|
|
10.
Li X G. Dissolved inorganic carbon and CO_2 fluxes in Jiaozhou Bay.
Acta oceanologic sinica,2004,23(2):279-285
|
CSCD被引
3
次
|
|
|
|
|
11.
Li X G. Role of the Jiaozhou Bay as a source/sink of CO_2 over a seasonal cycle.
Scientic marina,2007,71(3):441-450
|
CSCD被引
9
次
|
|
|
|
|
12.
Chou W C. The carbonate system in the East China Sea in winter.
Marine Chemistry,2010
|
CSCD被引
1
次
|
|
|
|
|
13.
Abril G. Excess atmospheric carbon dioxide transported by rivers into the Scheldt estuary.
Earth and Planetary Sciences,2000,330:761-768
|
CSCD被引
7
次
|
|
|
|
|
14.
高学鲁. 长江口及杭州湾邻近海域夏季表层海水中的溶解无机碳.
海洋科学,2008,4:61-67
|
CSCD被引
1
次
|
|
|
|
|
15.
Ichikawa H. The current system in the Yellow and East China Seas.
Journal of Oceanography,2002,58:77-92
|
CSCD被引
47
次
|
|
|
|
|
16.
宋金明.
中国近海与湖泊碳的生物地球化学,2008:1-533
|
CSCD被引
13
次
|
|
|
|
|
17.
Song Jinming.
Biogeochemical processes of biogenic elements in China Marginal Seas,2010:1-662
|
CSCD被引
25
次
|
|
|
|
|
18.
Weiss R F. Carbon dioxide in water and seawater: the solubility of a non-ideal gas.
Marine Chemistry,1974,2:203-215
|
CSCD被引
92
次
|
|
|
|
|
19.
Mehrbach C. Measurement of the apparent dissociation constants of carbonic acid in seawater at atmospheric pressure.
Limnology and Oceanography,1973,18:897-907
|
CSCD被引
47
次
|
|
|
|
|
20.
Dickson A G. Thermodynamics of the dissociation of boric acid in synthetic seawater from 273.15 to 318.15 K.
Deep Sea Research,1990,37:755-766
|
CSCD被引
28
次
|
|
|
|
|
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