极地研究
極地研究
겁지연구
CHINESE JOURNAL OF POLAR RESEARCH
2014年
1期
79-88
,共10页
汪卫国%方建勇%陈莉莉%吴日升%余兴光
汪衛國%方建勇%陳莉莉%吳日升%餘興光
왕위국%방건용%진리리%오일승%여흥광
楚科奇海%悬浮体%分布%颗粒组分%海洋环流
楚科奇海%懸浮體%分佈%顆粒組分%海洋環流
초과기해%현부체%분포%과립조분%해양배류
Chukchi Sea%suspended particles%distribution%composition%marine currents
对中国第四次北极科学考察在楚科奇海获取的悬浮体样品进行悬浮体及其颗粒组分特征的分析,旨在了解楚科奇海悬浮体分布、成因特征以及其沉积学意义。研究发现,楚科奇海中部悬浮体浓度最低,而在靠近白令海峡的南部海域和中北部海域,中下层海水中发现两个悬浮体浓度高值区。楚科奇海阿拉斯加沿岸和巴罗峡谷底层海水中,悬浮体浓度相对较高。扫描电镜分析结果显示,楚科奇海南部和中北部中下层海水中的悬浮体,主要以硅藻为主,但这两个海域的硅藻优势种明显不同。阿拉斯加沿岸和巴罗峡谷中的悬浮体,以生物碎屑为主。结合楚科奇海温度、盐度资料,楚科奇海南部和中北部高浓度悬浮体分别受经白令海峡夏季入侵的太平洋海水和楚科奇海冬季残留水的控制,而阿拉斯加沿岸和巴罗峡谷中下层的悬浮体,则受阿拉斯加沿岸流的控制。
對中國第四次北極科學攷察在楚科奇海穫取的懸浮體樣品進行懸浮體及其顆粒組分特徵的分析,旨在瞭解楚科奇海懸浮體分佈、成因特徵以及其沉積學意義。研究髮現,楚科奇海中部懸浮體濃度最低,而在靠近白令海峽的南部海域和中北部海域,中下層海水中髮現兩箇懸浮體濃度高值區。楚科奇海阿拉斯加沿岸和巴囉峽穀底層海水中,懸浮體濃度相對較高。掃描電鏡分析結果顯示,楚科奇海南部和中北部中下層海水中的懸浮體,主要以硅藻為主,但這兩箇海域的硅藻優勢種明顯不同。阿拉斯加沿岸和巴囉峽穀中的懸浮體,以生物碎屑為主。結閤楚科奇海溫度、鹽度資料,楚科奇海南部和中北部高濃度懸浮體分彆受經白令海峽夏季入侵的太平洋海水和楚科奇海鼕季殘留水的控製,而阿拉斯加沿岸和巴囉峽穀中下層的懸浮體,則受阿拉斯加沿岸流的控製。
대중국제사차북겁과학고찰재초과기해획취적현부체양품진행현부체급기과립조분특정적분석,지재료해초과기해현부체분포、성인특정이급기침적학의의。연구발현,초과기해중부현부체농도최저,이재고근백령해협적남부해역화중북부해역,중하층해수중발현량개현부체농도고치구。초과기해아랍사가연안화파라협곡저층해수중,현부체농도상대교고。소묘전경분석결과현시,초과기해남부화중북부중하층해수중적현부체,주요이규조위주,단저량개해역적규조우세충명현불동。아랍사가연안화파라협곡중적현부체,이생물쇄설위주。결합초과기해온도、염도자료,초과기해남부화중북부고농도현부체분별수경백령해협하계입침적태평양해수화초과기해동계잔류수적공제,이아랍사가연안화파라협곡중하층적현부체,칙수아랍사가연안류적공제。
The content and composition of suspended particles(SP)were measured in samples obtained in Chukchi Sea (CS)during the 4th Chinese Arctic Research Expedition,2010,as an attempt to understand the distribution and origin of the suspended matter there,which is essential for research into sedimentology,paleoclimate and environ-mental change.The results show that the SP content is lowest in the central CS,highest in the middle and bottom water column of the southern and central-northern CS,and the content along the Alaskan coast and in Barrow Can-yon is relatively higher.SEM analysis of the SP shows that the SP in the southern and central-northern CS is mainly composed of diatoms;however,the dominant species in the two areas are different.The SP along the Alaskan coast and in Barrow Canyon is mainly composed of bio-skeletal clasts.Combined with the distribution of temperature and salinity,the higher SP content in the southern CS is controlled by the summer Pacific Water via the Bering Strait. The higher SP content in the central-northern CS is controlled by the Pacific Water,which reaches this area in win-ter.The SP in the middle and bottom water column along the Alaska coastal line and in Barrow Canyon is controlled by the Alaska Coastal Water.