沉积物色度在古环境重建中的应用
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摘要
随着对全球环境演变研究的不断深入,涉及千年、百年、十年和年际时间尺度的研究已经越来越受到学者们的重视,提高时间尺度上的分辨率进行古环境重建成为一种趋势。为了在高分辨率的时间尺度上进行古环境的重建,色度作为一个环境代用指标逐渐开始被应用。本文回顾了国内外利用色度指标对湖泊沉积物、黄土-古土壤、深海沉积物和海岸带沉积物进行古气候重建的内容,论述了色度在沉积物示踪、冰川进退、天文周期和青藏高原的隆升与西风的流通等研究方面的指代作用,以及在古地震这个新的研究领域中的应用,并对色度指标在今后地质学中的应用进行了展望。
Global environmental evolution studies involving millennia, centuries, decades, and interannual time scales have received increasing attention from scholars. Improved resolution of these time scales for paleo-environmental reconstruction has become increasingly popular, especially paleo-environmental reconstruction performed using high-resolution data. For reconstructing the paleo-environment using high-resolution data, many researchers are opting to use chromaticity an environmental proxy. This paper reviews the use of chromaticity for paleoclimate reconstruction of lake sediments, ancient loess soils, deep-sea sediments and coastal sediments. The paper also discusses the role of chromaticity in sediment tracing, determining advancement and retreat of glaciers, astronomical cycles, uplift of Qinghai-Tibet Plateau, circulation of Westerlies, and its application in the new research field of paleo-earthquakes. Lastly, the paper explores the application of chromaticity in geology.
Global environmental evolution studies involving millennia, centuries, decades, and interannual time scales have received increasing attention from scholars. Improved resolution of these time scales for paleo-environmental reconstruction has become increasingly popular, especially paleo-environmental reconstruction performed using high-resolution data. For reconstructing the paleo-environment using high-resolution data, many researchers are opting to use chromaticity an environmental proxy. This paper reviews the use of chromaticity for paleoclimate reconstruction of lake sediments, ancient loess soils, deep-sea sediments and coastal sediments. The paper also discusses the role of chromaticity in sediment tracing, determining advancement and retreat of glaciers, astronomical cycles, uplift of Qinghai-Tibet Plateau, circulation of Westerlies, and its application in the new research field of paleo-earthquakes. Lastly, the paper explores the application of chromaticity in geology.
引文
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[8]陈杰,杨太保,曾彪,等.中国帕米尔地区黄土上部色度变化特征及古气候意义.沉积学报,2018,36(2):333-342.
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[16]杨胜利,安芷生.青土颜色和气候定性至半定量关系研究.中国科学,2001(B12):175-181.
[17] Long X, Ji J, Barron V, et al. Climatic thresholds for pedogenic iron oxides under aerobic conditions:processes and their significance in paleoclimate reconstruction. Quaternary Science Reviews, 2016,150:264-277.
[18]杨胜利,方小敏,李吉均,等.表土颜色和气候定性至半定量关系研究.中国科学:地球科学,2001,13(s1):175-181.
[19]朱正芳,汤顺青.色度学及其进展.物理,1996,25(6):342-347.
[20] Malacara D. Color vision and colorimetry:theory and applications.Washington:SPIE, 2011.
[21] Munsell A H. Munsell book of color. 1950.
[22] Broadbent A D. A critical review of the development of the CIE1931 RGB color:matching functions. Color Research&Application, 2004,29(4):267-272.
[23]顾磊,吴晟,李宝锋,等.基于数字图像分析的沉积物色度测量方法及其古环境应用.兰州大学学报:自然科学版,2010,46(s1):48-53.
[24]汤顺青.波长范围对色度学计算精度的影响.光学技术,1998(2):58-60.
[25]郭凌华.对标准色度学系统颜色空间的理解.包装工程,2003,24(2):13-14.
[26]胡维生.颜色物理和CIE标准色度系统·物理,1982,11(4):202-208.
[27]荆其诚,焦书兰,喻柏林,等.色度学.北京:科学出版社,1979.
[28]李宝锋.沉积物色度数据的转化方法.科协论坛,2012(9):99-100.
[29]刘浩学.CIE均匀颜色空间与色差公式的应用.北京印刷学院学报,2003,11(3):3-8.
[30]王苏民,张振克.中国湖泊沉积与环境演变研究的新进展.科学通报,1999,44(6):579-587.
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