全部 标题 作者
关键词 摘要

OALib Journal期刊
ISSN: 2333-9721
费用:99美元

查看量下载量

相关文章

更多...

象山近海表层沉积物特征及成因
Characteristics and Sedimentary Origin of the Surface Sediment in the Xiangshan Offshore Area

DOI: 10.12677/AMS.2023.102014, PP. 130-135

Keywords: 表层沉积物,粒度分析,成因,象山近海
Surface Sediment
, Grain Size, Provenance, Xiangshan Offshore Sea Area

Full-Text   Cite this paper   Add to My Lib

Abstract:

根据象山近海沉积物现场地质采样和粒度分析成果,对其特征和成因进行了探讨。结果表明,研究区表层沉积类型以粘土质粉砂为主,砂、粉砂和粘土粒级含量分别为5%~10%、65%~75%和20%~25%,平均粒径大多数在6.00 φ~7.00 φ (0.016~0.008 mm)之间,分选较差。沉积物由近岸到外海呈现粗–细–粗的总体分布格局,西北近岸海域沉积物类型变化稍大,东南侧外部海域沉积物较为统一。频率曲线呈弱正偏态到常态,峰态较宽平的单峰型为主,峰值在4 φ~7 φ之间。概率曲线可分2~4段。沉积动力分区图显示水动力条件较弱。粒级–标准差曲线识别出四个峰值区,6 μm和29 μm附近峰值突出,说明研究区沉积物主要来源于长江入海物质向南输运沉积;460 μm和1 μm附近峰值较弱,分别代表本地海岸岛屿侵蚀物质和外海物质漂移的影响。
According to the data of grain size and characteristics of the surficial sediments in the Xiangshan offshore sea area, the type, distribution pattern and possible origin of the surface sediments are discussed. Surface sedi-ments are mainly clayey silt, in which the sand, silt and clay particles portions weight 5%~10%, 65%~75% and 20%~25%, respectively. With mean diameter of about 6.00 Φ~7.00 Φ (0.016 mm~0.008 mm, fine silt), stand deviation coefficient of about 1.60 Φ~2.10 Φ, frequency analysis displays poor sorting and weak-positive skewness with one-dominant peak value (4 Φ~7 Φ) curve. Probability distribution may be discerned 2~4 sections represented as rolling, skip and suspended sediment transportationpatterns. The Pejrup ternary diagram for sedimentary environment classi-fication shows a weak dynamics condition. Distinguished the environmental sensitive groups from the sediments by particle size standard deviation method, the dominant deposits is silt which is widespread in subaqueous delta and adjacent sea areas transported by modern coastal currents systems, while the coarse sandy and fine muddy components show the influence of local lands-islands erosion and marine transportation.

References

[1]  高抒. 中国东部陆架全新世沉积体系: 过程-产物关系研究进展评述[J]. 沉积学报, 2013, 31(5): 845-855.
[2]  梁娟. 浙江近岸海域近现代沉积作用与全新世沉积环境演化[D]: [博士学位论文]. 武汉: 中国地质大学, 2019.
[3]  Liu, J.P., Xu, K.H., Li, A.C., et al. (2007) Flux and Fate of Yangtze River Sediment Delivered to the East China Sea. Geomorphology, 85, 208-224.
https://doi.org/10.1016/j.geomorph.2006.03.023
[4]  李家彪. 东海区域地质[M]. 北京: 海洋出版社, 2008.
[5]  宁波市海洋环境监测中心. 韭山列岛海洋自然保护区建设总体规划[R]. 2007.
[6]  郭志刚, 杨作升, 范德江. 东海陆架北部表层细粒级沉积物的级配及意义[J]. 青岛海洋大学学报, 2002, 32(5): 741-747.
[7]  刘升发, 刘焱光, 朱爱美, 等. 东海内陆架表层沉积物粒度及其净输运模式[J]. 海洋地质与第四纪地质, 2009, 29(1): 1-6.
[8]  中华人民共和国国家技术监督检验检疫总局、中国国家标准化管理委员会. GB/T12763-2007海洋调查规范[S]. 北京: 中国标准出版社, 2007.
[9]  张富元, 冯秀丽, 章伟艳, 等. 南海表层沉积物的沉降法和激光法粒度分析结果对比和校正[J]. 沉积学报, 2011, 29(4): 767-775.
[10]  章伟艳, 张霄宇, 金海燕, 等. 长江口-杭州湾及其邻近海域沉积动力环境及物源分析[J]. 地理学报, 2013, 68(5): 640-650.
[11]  周鸿权, 孙昭晨, 李伯根, 等. 浙江象山港海域悬沙浓度分布变化及其水动力影响分析[J]. 海洋通报, 2014, 33(6): 694-702.
[12]  肖尚斌, 李安春. 东海内陆架泥质区沉积物的环境敏感粒度组分[J]. 沉积学报, 2005, 23(1): 122-129.

Full-Text

Contact Us

service@oalib.com

QQ:3279437679

WhatsApp +8615387084133