其他题名Exchange fluxes of nutrients across sediment-water interface in the Muping Marine Ranch and its adjacent waters in autumn
高天赐; 高学鲁
; 邢前国; 赵建民发表期刊海洋环境科学
ISSN1007-6336
2020-05-26
卷号39期号:03页码:387-392
关键词牟平海洋牧场营养盐沉积物-水界面交换通量
产权排序(1) 中国科学院烟台海岸带研究所; (2) 中国科学院大学
作者部门海岸带信息集成与综合管理实验室
英文摘要In this research,the surface sediment samples were collected from the Muping Marine Ranch and its adjacent area in November 2017.The exchange fluxes of nutrients across the sediment-water interface were estimated by a laboratory incubation method.In addition,the effects of dissolved oxygen and temperature on the fluxes were also studied.The results indicated that the average exchange fluxes of NO2-N,NO3-N,NH4-N and PO4-P across sediment-water interface were 1.01,-181.91,-268.41 and-45.69 μmol/（m2·d）,respectively.The sediments acted as a "source" of NO2-N and a "sink" of NO3-N,NH4-N and PO4-P.Both dissolved oxygen and temperature had obvious influence on the fluxes.The results showed that the fluxes of NO2-N,NH4-N and PO4-P were higher in the aerobic situation than in the anoxic situation,while that of NO3-N showed the opposite trend; the fluxes of NO2-N,NO3-N and NH4-N were higher at a higher temperature,but that of PO4-P was opposite to them.
中文摘要本研究于2017年11月在牟平海洋牧场及其邻近海域采集表层沉积物样品,通过实验室模拟培养法估算了该季节沉积物-水界面营养盐的交换通量,并研究了溶解氧与温度对交换通量的影响。结果表明,目标海域沉积物水界面NO_2-N、NO_3-N、NH_4-N、PO_4-P的交换通量平均值分别为1.01、-181.91、-268.41、-45.69μmol/(m~2·d),沉积物表现为NO_2-N的"源",NO_3-N、NH_4-N、PO_4-P的"汇"。溶解氧及温度均对交换通量有较大影响,富氧条件下NO_2-N、NH_4-N、PO_4-P交换通量大于贫氧条件,NO_3-N反之;温度升高,NO_2-N、NO_3-N、NH_4-N的交换通量增大,PO_4-P反之。
文章类型期刊论文
资助机构中国科学院战略性先导科技专项(XDA23050303)
收录类别CSCD
语种中文
引用统计
文献类型期刊论文
条目标识符http://ir.yic.ac.cnhttp://ir.yic.ac.cn/handle/133337/25171
专题中科院海岸带环境过程与生态修复重点实验室
海岸带生物学与生物资源利用重点实验室_海岸带生物学与生物资源保护实验室
中科院海岸带环境过程与生态修复重点实验室_海岸带信息集成与战略规划研究中心
作者单位1.中国科学院烟台海岸带研究所;
2.中国科学院大学
推荐引用方式
GB/T 7714高天赐,高学鲁,邢前国,等. 秋季牟平海洋牧场及其邻近海域沉积物-水界面营养盐交换通量[J]. 海洋环境科学,2020,39(03):387-392.
APA高天赐,高学鲁,邢前国,&赵建民.(2020).秋季牟平海洋牧场及其邻近海域沉积物-水界面营养盐交换通量.海洋环境科学,39(03),387-392.
MLA高天赐,et al."秋季牟平海洋牧场及其邻近海域沉积物-水界面营养盐交换通量".海洋环境科学 39.03(2020):387-392.
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