地震地质 ›› 2018, Vol. 40 ›› Issue (4): 920-934.DOI: 10.3969/j.issn.0253-4967.2018.04.014

• 新技术应用 • 上一篇    下一篇

探索第四纪钻探岩心沉积物颜色测量新方法

何付兵1,2, 徐锡伟1, 郑桂森3, 孙永华2, 张巍2, 李莉2, 李瑞杰2   

  1. 1 中国地震局地质研究所, 北京 100029;
    2 北京市地质调查研究院, 北京 100195;
    3 北京市地质矿产勘查开发局, 北京 100195
  • 收稿日期:2017-08-21 修回日期:2018-01-13 出版日期:2018-08-20 发布日期:2018-09-26
  • 作者简介:何付兵,男,1980年生,2010年于中国地质大学(北京)获构造地质学专业硕士学位,主要从事北京区域地质研究,E-mail:hefubing14@126.com。
  • 基金资助:
    国家自然科学基金(91214201)和北京市优秀人才培养资助项目"北京平原区第四纪沉积物颜色特征定量研究及其古气候意义"共同资助

A NEW METHOD FOR COLOR MEASUREMENT OF QUATERNARY DRILLING CORE DEPOSITS

HE Fu-bing1,2, XU Xi-wei1, ZHENG Gui-sen3, SUN Yong-hua2, ZHANG Wei2, LI Li2, LI Rui-jie2   

  1. 1 Institute of Geology, China Earthquake Administration, Beijing 100029, China;
    2 Beijing Institute of Geological Survey, Beijing 100095, China;
    3 Beijing Geology Prospecting & Developing Bureau, Beijing 100095, China
  • Received:2017-08-21 Revised:2018-01-13 Online:2018-08-20 Published:2018-09-26

摘要: 文中提出1种基于数字图像分析法测量第四纪沉积物颜色的新方法,其操作简单快捷,可节省测试成本和时间,提高沉积物颜色研究效率。为论证该方法的可行性,对其测量成果同传统色度测量方法进行了对比。结果表明:1)传统沉积物颜色测量方法和数字图像颜色测量方法都受沉积物颗粒粒级制约。细砂及其以细颗粒可开展沉积物颜色研究,中砂、粗砂误差较大。同传统测量方法相比,数字图像法可减小粗碎屑沉积物颜色继承色干扰;2)碎屑沉积物粒级和含水量影响数字图像法沉积物颜色数值。一般来说,数字图像法获得的湿色数值低于使用分光测色仪所获得的干色数值,且颜色数值变化幅度更大,色度/亮度曲线表现出更大波状起伏;3)同传统沉积物颜色测量方法相比,数字图像法颜色测量红度、黄度具有较好一致性,而亮度受光照不均一影响,产生一定误差。采用沉积物数字图像提取沉积物颜色信息一定程度上可替代室内实测方法,用于建立更加复杂的沉积环境下较为完整的沉积物颜色序列,为第四纪地层划分、古气候研究、古土壤识别和古地震事件识别提供数据资料,拓展色度学在地质方向的应用。

关键词: 钻孔岩心, 第四纪沉积物, 色度测量, 数字图像分析, 地学应用

Abstract: In this paper, a method for measuring the color of Quaternary sediments based on digital image analysis is proposed, which has the advantages of simple and quick operation, and improving the research efficiency of sediment color. In order to demonstrate the feasibility of this method, the measurement results are compared with the traditional colorimetric measurement methods. The results show that:1) Both the traditional sediment color measurement method and the digital image color measurement method are controlled by sediment grain size. Sediment color research can be carried out on fine sand or finer sediments, but for medium grained sand and coarse sand, the error will be larger. Compared with the traditional measurement methods, digital image method can reduce the inherited color interference of coarse clastic sediments; 2) The particle size and water content of clastic sediments affect the numerical value of digital image sediment color. Generally, the wet-color values obtained by the digital image method are lower than the dry-color values obtained by using a spectrophotometer, and the color value variation is large, and the undulation of chromaticity/brightness curve is greater; 3) Compared with the traditional sediment color measurement method, digital image method has good consistency of color measurement of redness and yellowness, but the brightness is affected by uneven illumination, resulting in some error. Sediment digital image extraction of sediment color information can replace the indoor measurement method to a certain extent, and can be used to establish a more complete sediment color sequence under more complex sedimentary environment, so as to provide information for the Quaternary stratigraphic division, paleoclimate research, paleosol recognition and paleoearthquake event identification, thus expanding the application of colorimetric results to the geological direction.

Key words: core drilling, Quaternary sediments, colorimetric measurement, digital image analysis, geo-application

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