Distribution and accumulation of trace elements in rhizosphere and non-rhizosphere soils on a karst plateau after vegetation restoration
Distribution and accumulation of trace elements in rhizosphere and non-rhizosphere soils on a karst plateau after vegetation restoration
复制标题
喀斯特高原植被恢复后根际与非根际土壤微量元素的分布与积累
DOI:
10.1007/s11104-017-3363-1
复制
发表时间:
2017
期刊:
影响因子:
4.9
通讯作者:
Li Changlan
中科院分区:
文献类型:
--
作者:
Peng Xudong;Dai Quanhou;Ding Guijie;Zhu Chao;Li Changlan
AimsThe restoration of vegetation in the rocky desertified areas of karst plateaus is a major problem for present-day ecological studies. The aim of this study was to determine the effects of vegetation restoration on the distribution and accumulation of trace elements in rhizosphere and non-rhizosphere soils.MethodsFour representative areas containing the plantsCoriaria nepalensisWall.,Pinus armandiiFranch.,Elaeagnus pungensThunb., andCotoneaster hissaricusPojark. were selected within a vegetation restoration area in the Karst Plateau of Caohai County, Guizhou Province, China. Soils were sampled using a grid method to measure the total contents of the trace elements iron (Fe), manganese (Mn), copper (Cu), and zinc (Zn) in rhizosphere and non-rhizosphere soils.ResultsThe representative area containingElaeagnusdisplayed the greatest amount of accumulation in the rhizosphere of both total and available trace elements, except for total Zn. Representative areas of the rhizosphere with other types of vegetation showed accumulation of only some of the trace elements studied. All types of vegetation were associated with the bioenrichment of available trace elements in both rhizosphere and non-rhizosphere soils, except for available Cu in areas associated withCotoneaster.ConclusionsRepresentative areas containingPinusdisplayed the greatest degree of bioenrichment for both total and available trace elements in both rhizosphere and non-rhizosphere soils.