南京周家山下蜀黄土色度特征及其意义

刘峰, 王昊, 秦艺帆, 任少芳, 郑祥民. 南京周家山下蜀黄土色度特征及其意义[J]. 海洋地质与第四纪地质, 2015, 35(5): 143-151. doi: 10.16562/j.cnki.0256-1492.2015.05.017
引用本文: 刘峰, 王昊, 秦艺帆, 任少芳, 郑祥民. 南京周家山下蜀黄土色度特征及其意义[J]. 海洋地质与第四纪地质, 2015, 35(5): 143-151. doi: 10.16562/j.cnki.0256-1492.2015.05.017
LIU Feng, WANG Hao, QIN Yifan, REN Shaofang, ZHENG Xiangmin. CHROMA CHARACTERISTICS OF THE ZHOUJIASHAN XIASHU LOESS PROFILE IN NANJING AND ITS SIGNIFICANCE[J]. Marine Geology & Quaternary Geology, 2015, 35(5): 143-151. doi: 10.16562/j.cnki.0256-1492.2015.05.017
Citation: LIU Feng, WANG Hao, QIN Yifan, REN Shaofang, ZHENG Xiangmin. CHROMA CHARACTERISTICS OF THE ZHOUJIASHAN XIASHU LOESS PROFILE IN NANJING AND ITS SIGNIFICANCE[J]. Marine Geology & Quaternary Geology, 2015, 35(5): 143-151. doi: 10.16562/j.cnki.0256-1492.2015.05.017

南京周家山下蜀黄土色度特征及其意义

  • 基金项目:

    国家自然科学基金项目(41371032,J)

详细信息
    作者简介: 刘峰(1991-),男,硕士,研究方向为第四纪环境演变,E-mail:13162570993@163.com
    通讯作者: 王昊, hgoodspeed2008@163.com
  • 中图分类号: P532

CHROMA CHARACTERISTICS OF THE ZHOUJIASHAN XIASHU LOESS PROFILE IN NANJING AND ITS SIGNIFICANCE

More Information
  • 对南京周家山下蜀黄土-古土壤的研究发现,色度参数与其他参数对应关系良好,如亮度(L*)值与有机质含量明显正相关;红度(a*)值与氧化铁含量也有着显著相关性。与西北黄土相比,下蜀黄土经历了较强的风化作用。在其他指标不能很好地记录气候变化和土壤发育的情况下,色度参数可以发展成为一种可靠且简便的古环境研究的潜在替代性指标。在周家山地区,L*值受到土壤中有机质含量的影响较大,碳酸盐由于发生了较强的淋溶而对L*值影响不大。a*值受土壤中Fe元素含量的直接影响,对环境变化的响应更为敏感。黄度(b*)值在本区域对气候响应程度有限。
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收稿日期:  2014-11-12
修回日期:  2015-03-14

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