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岩溶区原始林土壤微量元素含量与有效特征

杨霖 杨程 朱同彬 谢银财 秦兴华 罗柳玲 朱梓弘 孟磊 何秋香

中国岩溶2018,Vol.37Issue(1):59-66,8.
中国岩溶2018,Vol.37Issue(1):59-66,8.DOI:10.11932/karst2017y01

岩溶区原始林土壤微量元素含量与有效特征

Contents and availability of trace elements in soils of natural forests in karst region

杨霖 1杨程 2朱同彬 3谢银财 3秦兴华 3罗柳玲 3朱梓弘 3孟磊 1何秋香1

作者信息

  • 1. 海南大学热带农林学院,海口570228
  • 2. 江苏省地质调查研究院,南京210018
  • 3. 中国地质科学院岩溶地质研究所/自然资源部、广西岩溶动力学重点实验室,广西桂林541004
  • 折叠

摘要

Abstract

Soil under undisturbed natural forests were sampled to investigate total and available contents of four trace elements (Cu,Fe,Mn and Zn) from four nature reserves including Maolan in Guizhou,Mengyuan and Green Stone Forest in Yunnan,and Exianling in Hainan,all of which were characterized by typical karst landform.The results showed total content of Cu,Fe,Mn and Zn reached to 0.03~0.08g · kg-1,35.6~ 57.4 g · kg-1,0.74~5.83 g · kg-1 and 0.13~1.03g · kg-1,respectively,which were significantly higher the average national background values.The available content of Cu,Fe,Mn and Zn in study areas were 1.09~3.51 mg · kg-1,11.6~62.9 mg · kg-1,48.3~173 mg · kg-1 and 4.17~37.6 mg · kg-1,respectively.According to the evaluation standard for trace elements in soil,available contents of all four elements were at relatively high level.The average activation ratios of Cu,Fe,Mn and Zn in soils under the natural forest were 5.48%,0.10%,6.44% and 4.19%,respectively,indicating high supply level for Cu,Mn and Zn but low supply level for Fe.Total availability index of trace element (Et) in soil was ranked as Maolan (21.0) >Green Stone Forest (12.8) ≈Mengyuan (12.7) >Exianling (5.15).In addition,Et was significantly positively correlated with total N and organic carbon contents.

关键词

岩溶区/原始林/微量元素/有效性

Key words

karst area/natural forest/trace elements/availability

分类

农业科技

引用本文复制引用

杨霖,杨程,朱同彬,谢银财,秦兴华,罗柳玲,朱梓弘,孟磊,何秋香..岩溶区原始林土壤微量元素含量与有效特征[J].中国岩溶,2018,37(1):59-66,8.

基金项目

国家重点研发计划项目(2016YFC0502503) (2016YFC0502503)

中国地质科学院基本科研业务费专项经费资助(YYWF201637,201724) (YYWF201637,201724)

中国岩溶

OA北大核心CSCDCSTPCD

1001-4810

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