海洋地质与第四纪地质2018，Vol.38Issue(1)：108-117,10.DOI:10.16562/j.cnki.0256-1492.2018.01.011
曹娥江沉积物黏土矿物与磁性特征及其指示意义
Magnetic properties and clay mineralogy of the surface sediments of Cao'e River basin and implications
摘要
Abstract
The Cao'e River is located in the Qiantang River estuary.The sedimentation and provenance of the river were complicated under the effect of the Qiantang River tide before the estuary sluice was built in December 2008.XRD and environmental magnetism are adopted as means to study clay mineralogy of the surface sediments and their spatial distribution in this paper,with emphasis on the sources of clay minerals in the mainstream and the influence of estuary sluice on sedimentation after construction.Results show that the clay mineral assemblages in tributaries are rather similar to those in topsoil sediments,in which the 1.4nm clay minerals are dominated by vermiculite and 1.4nm mixed layer clays.In the mainstream,however,the contents of 1.4nm clay minerals vary at different river sections.For examples,vermiculite dominates the 1.4nm clay minerals in the upper reach before the Shangpu gate,chlorite in the lower reaches of the New Sanjiang gate,and two 1.4nm clay minerals (chlorite and vermiculite) in the section between the Shangpu gate and the New Sanjiang gate.With regard to the magnetic properties of the sediments,they are similar among topsoil,tributaries and the upper reach sediments of the Shangpu gate.The magnetic properties of sediments' in the lower reaches of the New Sanjiang Gate is similar to that offshore.Magnetic properties of sediments between the Shangpu gate and New Sanjiang gate vary in between.The study of sediment source shows that the sediments of the mainstream above the Shangpu gate comes from tributaries and topsoils;sediments of the lower reaches of the New Sanjiang Gate from the Yangtze River,Hangzhou Bay and Qiantang River;and the sediments between the Shangpu gate and New Sanjiang gate from tributaries and topsoils with strong influence of materials from the outside of the River.关键词
曹娥江流域/表层沉积物/黏土矿物/物源/河口大闸Key words
the Cao'e River Basin/surface sediments/clay mineral/provenance/estuary sluice分类
资源环境引用本文复制引用
何姗姗,师育新,戴雪荣,许锐,刘朝..曹娥江沉积物黏土矿物与磁性特征及其指示意义[J].海洋地质与第四纪地质,2018,38(1):108-117,10.基金项目
国家自然科学基金项目“钱塘江流域河流沉积物1.4nm黏土矿物及其物源示踪研究”(41371214) （41371214）
