globalchange  > 气候变化与战略
CSCD记录号: CSCD:5110382
论文题名:
渤海湾百年来沉积物Li/Ba 和Rb/Sr 协同变化的地球化学特征与环境指示作用
其他题名: Geochemical covariation characteristics of Li/Ba and Rb/Sr and their environmental indication in recent hundred years of the Bohai Bay
作者: 宋金明1; 徐亚岩2; 段丽琴1
刊名: 海洋科学
ISSN: 1000-3096
出版年: 2014
卷: 38, 期:1, 页码:1026-1038
语种: 中文
中文关键词: Li/Ba 和Rb/Sr ; 环境变化指示 ; 柱状沉积物 ; 渤海湾
英文关键词: Li/Ba and Rb/Sr ; environmental change indication ; core sediments ; the Bohai Bay
WOS学科分类: OCEANOGRAPHY
WOS研究方向: Oceanography
中文摘要: 通过对渤海湾两根柱状沉积物中Li、Rb、Sr、Ba 以及Li/Ba 和Rb/Sr 的系统研究, 阐明了百年来沉积物中Li、Rb、Sr、Ba 的垂直变化特征, 发现了在不同年代沉积物中Li/Ba 和Rb/Sr 具有的协同变化规律, 揭示了沉积物Li/Ba 和Rb/Sr 作为近海区域性环境演变可能的指示作用。结果表明, 在0~20 cm沉积层间, Li、Rb 在A2和A6柱中均有随深度增加而增加的趋势, Sr 和Ba 随着深度的增加而降低; 近百年来, 渤海湾沉积物A2和A6柱中Li/Ba 和Rb/Sr 垂直变化表现出惊人的协同变化特征, Li/Ba 和Rb/Sr 在近河口的A2柱中, 基本呈现随深度的增加而增加的趋势, 而在远离河口区域的A6柱中, 其结果是0~15 cm 段(1963~2008年), Li/Ba 和Rb/Sr随深度的增加而增加, 15 cm以下(1900~1963年)则基本稳定, 在海洋过程作用下该区域沉积物Li/Ba 和Rb/Sr变化发生在45 a 时间段内; 沉积物中Li/Ba反映沉积物从河流进入海湾沉积过程中的变化, Rb/Sr反映来源沉积物的化学风化历史并指示来源区的气候环境变迁过程。A2沉积柱的20~22 cm(20世纪30年代)和10~12 cm(20世纪60年代), Li/Ba 出现极小值, 与1939年和1963年的海河流域大洪水相契合, 在0~12 cm 段, 两柱样Rb/Sr随着深度的降低有明显减小的趋势, 对应20世纪70年代初至2008年这一区域百年来气温升高并持续高温的时段。
英文摘要: Based on the researches on Li, Rb, Sr and Ba concentrations and Li/Ba and Rb/Sr in two sediment cores of the Bohai Bay, the vertical variations of Li, Rb, Sr and Ba concentrations in recent hundred years were studied, the covariation patterns of Li/Ba and Rb/Sr were found, and the environmental change indications of Li/Ba and Rb/Sr to the coastal waters were revealed in this paper. The results suggested that the Li and Rb concentrations increased with depth during 0~20 m in core A2 and A6, whereas the Sr and Ba concentrations decreased with depth. Surprisedly, the vertical distributions of Li/Ba and Rb/Sr displayed covariation characteristic in recent one hundred years, that was, Li/Ba and Rb/Sr increased with depth in core A2 near the Haihe Estuary whereas those in core A6 off the estuary increased with depth during 0~15 cm (corresponding to 1963~2008 years) and then remained stable below 15 cm (corresponding to 1900~1963 years). In conclusion, the changes of Li/Ba and Rb/Sr affected by marine processes mainly occurred in recent 45 years. Li/Ba mainly reflected the deposition process change of riverine sediments entering the Bohai Bay; however, Rb/Sr dominantly reflected the chemical weathering history of original sediments and indicated climate change of source region. In core A2, the minimum value of Li/Ba appeared in 20~22 cm (corresponding to 1930s) and 10~20 cm (corresponding to 1960s), according with the floods of the Haihe River in the years of 1939 and 1963. Rb/Sr decreased with depth during 0~12 cm in both cores, according with the temperature increase during early-1970s to 2008.
资源类型: 期刊论文
标识符: http://119.78.100.158/handle/2HF3EXSE/147883
Appears in Collections:气候变化与战略

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作者单位: 1.中国科学院海洋研究所, 青岛, 山东 266071, 中国
2.中国水产科学研究院东海水产研究所, 上海 200090, 中国

Recommended Citation:
宋金明,徐亚岩,段丽琴. 渤海湾百年来沉积物Li/Ba 和Rb/Sr 协同变化的地球化学特征与环境指示作用[J]. 海洋科学,2014-01-01,38(1):1026-1038
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