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黄海硅的分布与收支研究
引用本文:刘军,臧家业,张丽君,孙涛,于志刚,冉祥滨.黄海硅的分布与收支研究[J].中国环境科学,2016,36(1):157-166.
作者姓名:刘军  臧家业  张丽君  孙涛  于志刚  冉祥滨
作者单位:1. 中国海洋大学, 海洋化学理论与工程技术教育部重点实验室, 山东 青岛 266100; 2. 国家海洋局第一海洋研究所, 海洋生态研究中心, 山东 青岛 266061; 3. 青岛大学化学科学与工程学院, 山东 青岛 266071
基金项目:国家自然科学基金(41106072,41376093);中央级公益性科研院所基本科研业务费专项资金(2012G19)
摘    要:基于2012年在黄海的综合调查,对黄海水体和沉积物中溶解硅和生物硅的含量和分布及主要影响因素进行了分析,并结合历史数据建立了黄海硅收支与循环的模型.结果表明,黄海水体溶解硅和生物硅在秋季均高于春季,生物硅占活性硅的22%,陆源输入、初级生产和底界面扩散对硅的含量和分布的影响较为突出.收支表明,底界面扩散是黄海水体溶解硅的主要来源,占外部输入的48%,其次是东海的输入,占32%,河流贡献为9%,地下水贡献为6%,地表径流(非河流部分)贡献为3%,渤海贡献为1.5%,大气仅贡献0.5%;黄海水体溶解硅的支出主要是通过生物的吸收与随后的沉积埋藏和向东海的输出,其比例分别为72%和27%,黄海向渤海输出比例仅为1.0%;黄海沉积物是水体溶解硅的源,同时黄海体系还具有潜在汇的特性;黄海硅的净埋藏量约为55×109mol/a,占当年生物硅总量的7.2%,高于全球海洋的平均比值(3%),是外部输入硅总量的47%.本研究量化了黄海硅循环的主要过程,初步揭示了硅的源-汇特征以及陆地输入对近海硅收支与循环的影响.

关 键 词:黄海    生物硅  收支  

Distribution,fluxes and budget of silicon in the Yellow Sea
LIU Jun,ZANG Jia-ye,ZHANG Li-jun,SUN Tao,YU Zhi-gang,RAN Xiang-bin.Distribution,fluxes and budget of silicon in the Yellow Sea[J].China Environmental Science,2016,36(1):157-166.
Authors:LIU Jun  ZANG Jia-ye  ZHANG Li-jun  SUN Tao  YU Zhi-gang  RAN Xiang-bin
Institution:1. Key Laboratory of Marine Chemistry Theory and Technology, Ministry of Education, Ocean University of China, Qingdao 266100, China; 2. Research Center for Marine Ecology, First Institute of Oceanography, State Oceanic Administration, Qingdao 266061, China; 3. College of Chemical Science and Engineering, Qingdao University, Qingdao 266071, China
Abstract:Based on the comprehensive investigation in the Yellow Sea in 2012, Si concentrations and distributions in the water column and sediment were analyzed; and a budget model of Si in the Yellow Sea was established. The results show that both dissolved silica (DSi) and biogenic silica (BSi) in the water column are higher in Fall than in Spring. BSi accounts for 22% of total reactive Si. DSi and BSi in the water column are largely affected by terrestrial inputs, phytoplankton production and diffusion at the water-sediment interface. Si budget indicates that the major process contributed to the primary production in the water column is the benthic flux, accounting for 48% of total input loading, followed by water exchange from the East China Sea, representing for 32%. Riverine input, groundwater discharge, surface runoff (excluding riverine input) and Bohai Sea input contribute 9%, 6%, 3%, and 1.5% of total Si input, respectively, while the atmospheric deposition holds only 0.5%. The dominant removal of DSi from water column in the Yellow Sea is diatom uptake then sedimentation and export to the East China Sea, accounting for 72% and 27%, respectively, while output to Bohai Sea contributes only 1.0%. Net burial of BSi is about 55×109mol/a, representing 7.2% of primary production and accounting for 47% of exogenetic Si inputs into the Yellow Sea. This study quantifies the main processes of Si cycling, and reveals the source-sink characteristics and the influence of terrestrial loadings on the Si budget in the Yellow Sea.
Keywords:Yellow Sea (Huanghai Sea)  silicon  biogenic silica  flux and budget  
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