黄土高原地区泥沙来源复合指纹示踪研究进展
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摘要
[目的]为把握复合指纹示踪方法发展动态,为黄土高原泥沙来源研究提供建议。[方法]综述了复合指纹示踪方法的理论基础,对各指纹因子(物理示踪剂、核素、地化元素、磁性、有机质、碳氮稳定同位素、孢粉、生物标志物)的发展进程、模型算法、不确定分析等进行了详细论述。[结果]黄土高原地区在利用指纹因子的时空差异性来研究侵蚀区泥沙的来源,定量描述侵蚀过程的发展等方面已取得一系列成果。[结论]复合指纹示踪泥沙来源技术在黄土高原地区以探讨指纹因子应用研究为主,在混合模型矫正、多方法比较、指纹因子守恒等方面还需要进一步加强研究。
[Objective] This study aims to review the development of composite fingerprinting technique and provide support for the study of sediment sources in the Loess Plateau. [Methods] The theoretical basis of composite fingerprint tracing technique was reviewed. The development process, model algorithm and uncertainty analysis of various fingerprint factors(physical tracers, radionuclides, geochemical tracers, mineral magnetics, properties of organic matter, stable isotopes of organic carbon and nitrogen, plant pollen and biomarkers) were discussed in detail. [Results] A series achievements have been made in studying the sources of sediment and quantitatively describing the development of erosion process in the Loess Plateau by using the spatial and temporal differences of fingerprint factors. [Conclusion] Most existing studies on the Loess Plateau focused on the application of sediment tracing methods. Further studies are needed in the area of mix model correction, methods comparison and fingerprint factor conservation in the future.
[Objective] This study aims to review the development of composite fingerprinting technique and provide support for the study of sediment sources in the Loess Plateau. [Methods] The theoretical basis of composite fingerprint tracing technique was reviewed. The development process, model algorithm and uncertainty analysis of various fingerprint factors(physical tracers, radionuclides, geochemical tracers, mineral magnetics, properties of organic matter, stable isotopes of organic carbon and nitrogen, plant pollen and biomarkers) were discussed in detail. [Results] A series achievements have been made in studying the sources of sediment and quantitatively describing the development of erosion process in the Loess Plateau by using the spatial and temporal differences of fingerprint factors. [Conclusion] Most existing studies on the Loess Plateau focused on the application of sediment tracing methods. Further studies are needed in the area of mix model correction, methods comparison and fingerprint factor conservation in the future.
引文
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