南四湖的形成與水環(huán)境演變

Through high-resolution research of sedimental chronology and the sediment environmentalindexes, such as graininess, minerals, magnetic parameters, pigment content, organic carbon andchronology in Ds-core and Ws-core in Nansihu Lake, the authors analyze the formation cause of theNansihu Lake and its water environmental changes. Historical documents are also analyzed here inorder to reach the conclusion. Researches indicate that the Nansihu Lake came into being about 2500aBP and its evolution succession can be divided into four stages. In this evolution process, severalscattered lakes merge into one large lake in the east of China. This process is distinctively affected bythe overflow of the Yellow River, the excavation of the Grand Canal and other human activities.

作 者： 張祖陸 沈吉 劉恩峰 Sun Qingyi Jiang Luguang WANG Lin   作者單位： 張祖陸,Jiang Luguang,WANG Lin(Department of Geography, Shandong Normal University, Jinan 250014, China)

沈吉,劉恩峰(Nanjing Institute of Geography & Limnology, CAS, Nanjing 210008, China)

Sun Qingyi(Office of Water Resources Management Committee of Jining City, Jining 272119, China) 

刊 名： 地理學(xué)報(bào)(英文版)  ISTIC SCI 英文刊名： JOURNAL OF GEOGRAPHICAL SCIENCES  年，卷(期)： 2003 13(2)  分類號(hào)： X144  關(guān)鍵詞： Nansihu Lake   lake sediment study   water environment evolution   migration and overflowof the Yellow River   excavation of the Grand Canal  

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