海洋学报(中文版)
海洋學報(中文版)
해양학보(중문판)
ACTA OCEANOLOGICA SINICA
2014年
5期
98-106
,共9页
方引%陈颖军%林田%田崇国%潘晓辉%唐建辉
方引%陳穎軍%林田%田崇國%潘曉輝%唐建輝
방인%진영군%림전%전숭국%반효휘%당건휘
黑碳%沉积记录%柱状沉积物%泥质区%渤海
黑碳%沉積記錄%柱狀沉積物%泥質區%渤海
흑탄%침적기록%주상침적물%니질구%발해
black carbon%sedimentary record%core sediment%mud area%Bohai Sea
在渤海泥质沉积区采集柱状沉积物样品,分析其黑碳含量和沉积通量,结合210 Pb年龄测定,探讨百年尺度黑碳沉积通量的时间序列变化对区域人类活动的响应。结果表明:(1)研究区黑碳含量和沉积通量分别为0.24~0.49 mg/g [平均为(0.32±0.07) mg/g]和0.026~0.053 mg/(cm2· a)[平均为(0.040±0.008) mg/(cm2· a)],黑碳含量与我国东海内陆架等海区相当,但远低于美国港湾和瑞典大陆架等污染较严重地区;(2)黑碳通量在20世纪50年代-70年代中期和90年代初-90年代末出现两个明显的峰值,分别对应于两个阶段的生物质燃烧量和煤炭、石油等化石燃料燃烧量的急剧增加;而20世纪70年代末-80年代末较低的黑碳通量以及21世纪初黑碳通量下降的趋势则分别与黄河改道事件、我国能源利用技术提高及污染控制减排措施逐步实施等有关;(3)通过比较本文结果以及国内外其它海域和湖泊的研究资料,证明黑碳沉积记录可以作为一个良好的地球化学指标,用于评估人类活动对生态环境的影响历史。
在渤海泥質沉積區採集柱狀沉積物樣品,分析其黑碳含量和沉積通量,結閤210 Pb年齡測定,探討百年呎度黑碳沉積通量的時間序列變化對區域人類活動的響應。結果錶明:(1)研究區黑碳含量和沉積通量分彆為0.24~0.49 mg/g [平均為(0.32±0.07) mg/g]和0.026~0.053 mg/(cm2· a)[平均為(0.040±0.008) mg/(cm2· a)],黑碳含量與我國東海內陸架等海區相噹,但遠低于美國港灣和瑞典大陸架等汙染較嚴重地區;(2)黑碳通量在20世紀50年代-70年代中期和90年代初-90年代末齣現兩箇明顯的峰值,分彆對應于兩箇階段的生物質燃燒量和煤炭、石油等化石燃料燃燒量的急劇增加;而20世紀70年代末-80年代末較低的黑碳通量以及21世紀初黑碳通量下降的趨勢則分彆與黃河改道事件、我國能源利用技術提高及汙染控製減排措施逐步實施等有關;(3)通過比較本文結果以及國內外其它海域和湖泊的研究資料,證明黑碳沉積記錄可以作為一箇良好的地毬化學指標,用于評估人類活動對生態環境的影響歷史。
재발해니질침적구채집주상침적물양품,분석기흑탄함량화침적통량,결합210 Pb년령측정,탐토백년척도흑탄침적통량적시간서렬변화대구역인류활동적향응。결과표명:(1)연구구흑탄함량화침적통량분별위0.24~0.49 mg/g [평균위(0.32±0.07) mg/g]화0.026~0.053 mg/(cm2· a)[평균위(0.040±0.008) mg/(cm2· a)],흑탄함량여아국동해내륙가등해구상당,단원저우미국항만화서전대륙가등오염교엄중지구;(2)흑탄통량재20세기50년대-70년대중기화90년대초-90년대말출현량개명현적봉치,분별대응우량개계단적생물질연소량화매탄、석유등화석연료연소량적급극증가;이20세기70년대말-80년대말교저적흑탄통량이급21세기초흑탄통량하강적추세칙분별여황하개도사건、아국능원이용기술제고급오염공제감배조시축보실시등유관;(3)통과비교본문결과이급국내외기타해역화호박적연구자료,증명흑탄침적기록가이작위일개량호적지구화학지표,용우평고인류활동대생태배경적영향역사。
Core sediment samples collected from the mud area of Bohai Sea (BS) were analyzed for the concentration and depositional flux of black carbon (BC) .By combining with 210 Pb radionuclide dating ,the relationship between centennial scale variation of BC depositional flux and human activities adjacent to the BS w as discussed .T he results showed that :(1) the concentration and flux of BC ranged from 0.24 to 0.49 mg/g and from 0.026 to 0.053 mg/(cm2 · a) ,with mean values of (0.32 ± 0.07) mg/g and (0.040 ± 0.008) mg/(cm2 · a) ,respectively .BC con-centration was equivalent to those in other China seas (like the East China Sea) ,but significantly lower than the heavily polluted areas ,such as America bays and Swedish continental shelf ;(2) BC flux peaked around 1950s to mid-1970s and early 1990s to late 1990s ,which each could be attributed to the sharply increased biomass burning and fossil fuels (coal and oil) combustion .However ,the lower value and the decreasing trend of BC flux occurred in the period of late 1970s to late 1980s and the initial period of the 21st century could be explained by the diversion of the Huanghe River and the utilization of clean technology for energy consumption as well as pollution control strategies ,respectively ;(3) By comparing the present results and other studies in various seas and lakes around the world ,it was confirmed that BC sedimentary record in core sediment could be used as a good geochemical indicator to reveal the influence history of anthropogenic activities on regional ecological environment .