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Wang Yalu, Yuan Huamao, Song Jinming, Li Xuegang, Li Ning, Qu Baoxiao, Kang Xuming, Wang Qidong, Xing Jianwei, Liang Xianmeng. Benthic exchange rates of dissolved silicate at the sediment-water interface in the Jiaozhou Bay and the impact of relevant environmental factors[J]. Haiyang Xuebao, 2016, 38(12): 55-65. doi: 10.3969/j.issn.0253-4193.2016.12.006
Citation: Wang Yalu, Yuan Huamao, Song Jinming, Li Xuegang, Li Ning, Qu Baoxiao, Kang Xuming, Wang Qidong, Xing Jianwei, Liang Xianmeng. Benthic exchange rates of dissolved silicate at the sediment-water interface in the Jiaozhou Bay and the impact of relevant environmental factors[J]. Haiyang Xuebao, 2016, 38(12): 55-65. doi: 10.3969/j.issn.0253-4193.2016.12.006

Benthic exchange rates of dissolved silicate at the sediment-water interface in the Jiaozhou Bay and the impact of relevant environmental factors

doi: 10.3969/j.issn.0253-4193.2016.12.006
  • Received Date: 2016-03-25
  • The benthic exchange rates of dissolved silicate (DSi) at the sediment-water interface in Jiaozhou Bay were measured by intact sediment cores incubation. Further, the impacts of environmental factors on the exchange rate were also discussed. Silicate transported from sediment to overlying water, and the exchange rate ranged from 947 to 4 889 μmol/(m2·d) with a mean of 1 819 μmol/(m2·d). Total organic carbon (TOC) and chlorophyll a(Chl a) in surface sediment which were relative with the biological activity were the dominant factors controlling the exchange rate of DSi. Moreover, water ratio(φ), biogenic silicate(BSi), clay content of sediment and DSi in the pore water also had important effects on the exchange process. As a result, the exchange of DSi at the sediment-water interface in Jiaozhou Bay was a consequence of dissolution-dilution process which was dominantly controlled by biological activity. Grain diameter of sediment and DSi in bottom water, however, were not relatively important when compared with those factors.
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