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[Objective] Many strata emerge in the high-quality tea producing area in Qionglai Mountains,which belongs to Mesozoic Cretaceous(K),Mingshan Fm(E1-2mn)and Dayi conglomerate Team(N)of Cenozoic Tertiary System as well as Quaternary System(Q).Analysis on the migrating features of soil heavy metal from each stratum to tea leaves showed that the enrichment ability of elements was Cu>Cd>Zn>Ni>Hg>As>Cr>Pb.By comparing the soil background values with the soil base values of Sichuan hilly area and Chengdu economic region,it could be concluded that Cd,Hg,Mo,Pb and Se were enriched,and other metal elements existed at a level close to that of the comparing areas.The pH was a little acidic,and high quality tea cultivation could be developed here at present.With the increase of human activities,the environment of study area tends to deteriorate.Therefore,land planning and use should be reasonable.The government should control the environment nearby and prevent pollution.
[Objective] Many strata emerge in the high-quality tea producing area in Qionglai Mountains, which belongs to Mesozoic Cretaceous (K), Mingshan Fm (E1-2mn) and Dayi conglomerate Team (N) of Cenozoic Tertiary System as well as Quaternary System (Q). Analysis on the migrating features of soil heavy metal from each stratum to tea leaves showed that the enrichment ability of elements was Cu> Cd> Zn> Ni> Hg> As> Cr> Pb.By comparing the soil background values with the soil base values of Sichuan hilly area and Chengdu economic region, it could be that that Cd, Hg, Mo, Pb and Se were enriched, and other metal elements existed at a level close to that of the comparing areas. The pH was a little acidic, and high quality tea cultivation could be developed here at present.With the increase of human activities, the environment of study area tends to deteriorate.Therefore, land planning and use should be reasonable. The government should control the environment nearby and prevent pollution.