首页> 外文期刊>Palaeogeography, Palaeoclimatology, Palaeoecology: An International Journal for the Geo-Sciences >Changing environmental conditions in recent past - Reading through the study of geochemical characteristics, magnetic parameters and sedimentation rate of mudflats, central west coast of India
【24h】

Changing environmental conditions in recent past - Reading through the study of geochemical characteristics, magnetic parameters and sedimentation rate of mudflats, central west coast of India

机译:最近发生的环境条件变化-通过研究印度中西部海岸滩涂的地球化学特征,磁参数和沉积速率来进行研究

获取原文
获取原文并翻译 | 示例
       

摘要

Geochemical (sediment components, major and trace metals), magnetic related parameters (concentration, mineralogy and grain size) and radionuclide (210Pb) analyses were carried out on sediment cores collected from mudflat regions of central west coast of India viz, Kolamb creek (Malvan), Mandovi estuary (Panaji) and Tadri creek (Gokarn), in order to study the variations in sediment characteristics with time. The changes in spatial and temporal (depth) distributions of sediment composition were observed to be mainly controlled by the catchment area geology, geomorphology and anthropogenic activities. The sedimentation rate in the study area varied from 0.13 to 2 cm/yr. The rate was extremely low at the lower half of the cores (0.13- 0.31 cm/yr, before ~1980) as compared to the near surface (1.21-2 cm/yr, after ~1980) with two clear phases of sedimentation rates. The higher sedimentation rate in the upper portions of the cores was found to correspond to increased deposition of finer sediment components, metals and magnetic minerals which in turn were found to be mainly controlled by geology and/or human activities. The results of the present study reveal variations in sediment properties with time and support the use of geochemical in addition to magnetic susceptibility parameters on mudflats to understand changing environmental conditions of recent past.
机译:对从印度中西部海岸,科拉姆布克里克(Malvan) ),曼多维河口(Panaji)和塔德里克里克(Gokarn),以研究沉积物特征随时间的变化。观察到沉积物组成的时空(深度)分布变化主要受集水区的地质,地貌和人为活动控制。研究区的沉积速率从0.13到2 cm / yr不等。与下表面(1.21-2 cm / yr,〜1980年之后)相比,在下半部岩心(0.13-0.31 cm / yr,〜1980年之前)的沉积速率极低,且沉降速率有两个清晰的阶段。发现在岩心上部的较高沉积速率对应于较细的沉积物成分,金属和磁性矿物的沉积增加,而沉积物,金属和磁性矿物又被发现主要受地质和/或人类活动控制。本研究的结果揭示了沉积物特性随时间的变化,并支持在泥滩上使用磁化参数以及磁化率参数来了解近代环境条件的变化。

著录项

相似文献

  • 外文文献
  • 中文文献
  • 专利
获取原文

客服邮箱:kefu@zhangqiaokeyan.com

京公网安备:11010802029741号 ICP备案号:京ICP备15016152号-6 六维联合信息科技 (北京) 有限公司©版权所有
  • 客服微信

  • 服务号