摘要
黄土是第四纪时期的重要堆积物,其对于古环境的恢复具有极重大的意义。黄土磁化率对古降水量的推算,以及建立古气候复元的定量模型等都已成为可行。同时,对现代土壤环境与降尘等环境因素的研究是磁化率应用性研究的新领域。
The Chinese loess is important Quaternary sediment. The information from the loess is important to understand Quaternary paleoenvironment. It is possible to use the magnetic susceptibility of the loess to propose quantitative models for restoring paleoenvironment on the basis of paleoprecipitation. At the same time, the research of the modem soil and aeolian dust is the new field about the applied study of magnetic susceptibility.
出处
《现代生物医学进展》
CAS
2006年第4期80-81,共2页
Progress in Modern Biomedicine
关键词
黄土
磁化率
环境意义
The loess
Magnetic susceptibility
The paleoenvironmental influence
