引用本文:
【打印本页】   【下载PDF全文】   View/Add Comment  Download reader   Close
←前一篇|后一篇→ 过刊浏览    高级检索
本文已被:浏览 1388次   下载 1100 本文二维码信息
码上扫一扫!
分享到: 微信 更多
洪湖垦殖剖面的地球化学特征
杨汉东, 蔡述明
中国科学院测量与地球物理研究所 武汉 430077
摘要:
于1988-1990年在洪湖设6个剖面站位,对洪湖地区不同时期的垦殖剖面进行地球化学分析,并通过对沉积物层序间的21个元素的聚类分析,探讨垦殖剖面中元素的分布,地下水及垦殖对元素迁移的影响和再沉积作用与垦殖土壤的关系,指出由于湖泊区域性干演和垦殖过程的变化,导致沉积层序发生变化。这是人类垦殖活动对沼泽化湖泊产生影响的典型例证。
关键词:  垦殖  地球化学  地下水  沉积物
DOI:
分类号:
基金项目:国家自然科学基金资助项目,49070060号
THE GEOCHEMICAL CHARACTERISTICS OF CULTIVATION PROFILES IN LAKE HONGHU
Yang Handong, Cai Shuming
Institute of Geodesy and Gcophysics, Academia Sinica, Wuhan 430077
Abstract:
Chemical analysis of cultivation profiles taken in Lake Honghu from 1988 to 1990 showed that:

(1) Owing to luxuriant aquatic plant growth, some elements such as C, N and Ca are enriched in the surface sediment. The concentrations of nutrient elements reduce in the process of cultivation.

(2) Because of the high and frequent removal of the groundwater level in cultivation area, many elements such as Ca, Mg, Fe and Mn are removed. The loss of Ca is nearly 80%.

(3) In the evolution of the lake, Changes in cultivation and in dry and wet processes of the lake have altered the sedimentation processes, the order of sediment layers and the distribution of elements.

Key words:  Cultivation, Geochemistry, Groundwater, Sediment
Copyright ©  Editorial Office for Oceanologia et Limnologia Sinica    Copyright©2008 All Rights Reserved
Supervised by: China Association for Science and Technology   Sponsored by: Chinese Society for Oceanology and Limnology, Institute of Oceanology and Limnology, CAS.
Address: 7 Nanhai Road, Qingdao, China.    Postcode: 266071    Tel: 0532-82898753  E-mail: liuxiujuan@qdio.ac.cn  
Technical support: Beijing E-Tiller Co.,Ltd.