Identification Marks of Paleo-flood Events and the Preliminary Application of Micro-morphology in It

Q3 Environmental Science 干旱区研究 Pub Date : 2010-04-09 DOI:10.3724/SP.J.1148.2009.00340
Dai XiaoGuo, Zhang Xiaochun, Pang Jiangli
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Abstract

Paleo-flood hydrology study is a hot field in global change study.It is the key for studying paleo-flood events how to look for and identify the paleo-flood slack-water deposits effectively and accurately.In this paper,the effects of paleontology,archeology,sedimentology and geochemistry in studying paleo-flood events are summarized at first,and then the micro-morphological features of paleo-flood deposits and other strata are compared and analyzed based on the theory of micro-morphology.The results show that the grain characteristics,mineral composition,pores and micro-configuration in paleo-flood deposits are obviously different from those in other strata:(1) The grains in the paleo-flood slack-water deposits are fine,well-sorted and subrounded or rounded;(2) Mineral composition in the paleo-flood deposits is similar to that in other strata,but the contents of unstable minerals are relatively low in paleo-flood deposits;(3) Soil in paleo-flood deposits is dominated by clay,and the clay content is second only to that in paleosol;(4) The pores are irregular,and the pore walls are coarse.These reveal that the micro-morphology can be used to research and identify the paleo-flood events.
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古洪水事件的识别标志及其微形态学的初步应用
古洪水水文研究是全球变化研究的热点。如何有效、准确地寻找和识别古洪水淡水沉积是研究古洪水事件的关键。本文首先总结了古生物学、考古学、沉积学和地球化学在古洪水事件研究中的作用,然后基于微形态学理论对古洪水沉积物和其他地层的微形态特征进行了比较分析。结果表明,古洪水沉积物的颗粒特征、矿物组成、孔隙和微构型与其他地层明显不同:(1)古洪水散水沉积物颗粒细,分选良好,呈亚圆状或圆形;(2)古洪水沉积物的矿物组成与其他地层相似,但不稳定矿物含量相对较低粘土含量仅次于古土壤;(4)孔隙不规则,孔壁粗大。这表明微形态可以用于研究和识别古洪水事件。
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干旱区研究
干旱区研究 Environmental Science-Water Science and Technology
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2.50
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4294
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