首页> 外文期刊>Catena: An Interdisciplinary Journal of Soil Science Hydrology-Geomorphology Focusing on Geoecology and Landscape Evolution >210Pb geochronology of sediment accumulation rates in Mexico City Metropolitan Zone as recorded at Espejo de los Lirios lake sediments.
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210Pb geochronology of sediment accumulation rates in Mexico City Metropolitan Zone as recorded at Espejo de los Lirios lake sediments.

机译:根据Espejo de los Lirios湖沉积物记录的墨西哥城大都会区210Pb沉积物累积速率的年代学。

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摘要

A sedimentary sequence from the Espejo de los Lirios lake in the Metropolitan Zone of Mexico City (MZMC) was analysed in detail for 210Pb and 137Cs activities, allowing to assess the evolution of the accretion rates in the lake during the last ~84+or-4 years. The core revealed the deposition of contemporaneously indigenous lake sediments to the site interspersed with eroded bedrock from the catchment, evidencing episodic increases in sediment accretion which varied from 0.14 to 0.93 cm year-1. Increasing trends in sedimentation rates were found to be closely related to demographic expansion of the Metropolitan Zone of Mexico City and explained on the basis of the erosive processes produced as a result of deforestation created as a consequence of the urban and industrial development of the MZMC..
机译:详细分析了墨西哥城都会区(MZMC)的Espejo de los Lirios湖的沉积序列的210Pb和137Cs活性,从而可以评估在最后一个〜84 +或-期间湖中吸积率的演变。 4年岩心显示,当时流域的原生湖沉积物散布在流域受侵蚀的基岩所散布的地方,表明第一年沉积物积聚量呈周期性增加,范围从0.14到0.93 cm不等。人们发现,沉积速率的增加趋势与墨西哥城大都会区的人口增长密切相关,并以MZMC的城市和工业发展所造成的森林砍伐所产生的侵蚀过程为依据进行了解释。 。

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