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中国网纹红土研究进展

Research Advance of Vermiculated Red Soil in China

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【作者】 王芳周尚哲康建成郑琰明周凌云

【Author】 WANG Fang~(1,2),ZHOU Shang-zhe~1,KANG Jian-cheng~2,ZHENG Yan-ming~(1,2),ZHOU Ling-yun~1(1.College of Geographical Science,South China Normal University,Guangzhou 510631,China;2.Research Center of Urban Ecology and Environment,Shanghai Normal University,Shanghai 200234,China)

【机构】 华南师范大学地理科学学院上海师范大学城市生态与环境研究中心华南师范大学地理科学学院 广州510631上海200234广州510631

【摘要】 综述了近年来网纹红土研究的事实成果,结果表明:网纹红土的强酸、富铝化特征明显;其形成是百万年以来的事,发育盛期在中更新世;其形成过程是先红土化,再网纹化,成因有风成和水成的说法;关于对网纹化机制、红土化是否仍在进行、网纹红土对古气候事件的指示意义等问题仍存在争议。

【Abstract】 The studies of vermiculated red soil in recent years are summarized,The results show that the strong acid and laterized characteristics of vermiculated red soil are obvious;its formed time is in millions years,and the main period is in Middle Pleistocene;its formation includes laterite weathering and reticulation forming,and the causes of formation are considered of wind-cause and water-cause;but the questions such as the mechanism of reticulation forming,laterization in presentday and the indication of vermiculated red soil for ancient environmental are on the debate.

  • 【文献出处】 烟台师范学院学报(自然科学版) , 编辑部邮箱 ,2006年01期
  • 【分类号】P642.132
  • 【被引频次】31
  • 【下载频次】753
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