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广西岩溶区灌木林地凋落物—土壤碳、氮、磷化学计量特征

岳祥飞 李衍青 刘鹏

中国岩溶2023,Vol.42Issue(5):1106-1116,11.
中国岩溶2023,Vol.42Issue(5):1106-1116,11.DOI:10.11932/karst2023y032

广西岩溶区灌木林地凋落物—土壤碳、氮、磷化学计量特征

Stoichiometric characteristics of C,N and P in soil and litter of shrublands in karst areas of Guangxi

岳祥飞 1李衍青 2刘鹏3

作者信息

  • 1. 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/联合国教科文组织国际岩溶研究中心,广西桂林 541004||岩溶动力系统与全球变化国际联合研究中心,广西桂林 541004||广西平果喀斯特生态系统国家野外科学观测研究站,广西平果 531406
  • 2. 广西师范大学环境与资源学院,广西桂林 541004
  • 3. 广西大学林学院,广西南宁 530001
  • 折叠

摘要

Abstract

This study was conducted at seven typical karst areas(Longlin,Lingyun,Donglan,Hechi,Luocheng,Rongshui and Guilin)of Guangxi,China.These areas present subtropical monsoon climate,with annual temperatures averaging from 19.27 ℃ to 20.73 ℃,and the annual rainfall averaging from 1,149.2 mm to 1,931.3 mm.This study focused on the stoichiometric characteristics and the influencing factors of organic carbon(C),nitrogen(N)and phosphorus(P)in soil and litter of typical karst areas.By field sampling and laboratory experiment,the stoichiometric characteristics of soil organic C,N,and P,and litter C,N and P of 63 shrub quadrats in the seven typical karst areas were investigated.Besides,the correlation between the variation in stoichiometric characteristics of soil and environmental factors were analyzed. The research findings show that:(1)the mean content of C,N and P in 0-40 cm soil was 31.90 g·kg-1,3.95 g·kg1 and 2.65 g·kg-1,and the coefficient of variation was 40.13%,41.46%and 65.24%,respectively.The mean value of C/N,C/P and N/P was 8.10,14.82 and 7.80,and the coefficient of variation was 14.88%,48.78%and 41.33%,respectively.The values of C/N,C/P and N/P in 0-20 cm soil were slightly higher than those in 20-40 cm.There were significant differences in soil C/N,C/P and N/P between 0-20 cm and 20-40 cm(P>0.05).(2)There were significant correlations among the contents of soil C,N and P(P<0.01).The stoichiometric characteristics of soil nutrients elements were significantly affected by litter N and P(PP<0.05)which was negatively correlated with the C/N ratio of litter.There was a moderately negative correlation between mean annual precipitation and soil C and P.However,the mean annual temperature was negatively correlated with soil C,C/N and C/P,which was positively correlated with soil N. The soil C,N and P of typical karst shrubland in Guangxi presents high spatial heterogeneity,with the characteristics of low C and high P,and the litter is characterized by low C,high P,low C/P and low N/P.Litter N and P is the important factor affecting the stoichiometric characteristics of soil nutrients in shrubland of the karst area.The increase of mean annual temperature will promote the increase of soil N and decrease soil C/N,and the increase of mean annual precipitation will reduce soil C and P.Our research results have great significance for the theoretical improvement of the stoichiometric study on soil ecology,vegetation restoration in degraded karst ecosystem and the response of karst ecosystem to climate change in Southwest China.

关键词

岩溶区/化学计量/土壤/凋落物/灌木林

Key words

karst area/stoichiometric characteristics/soil/litter/shrubland

分类

农业科技

引用本文复制引用

岳祥飞,李衍青,刘鹏..广西岩溶区灌木林地凋落物—土壤碳、氮、磷化学计量特征[J].中国岩溶,2023,42(5):1106-1116,11.

基金项目

广西自然科学基金面上项目(2018GXNSFAA138172) (2018GXNSFAA138172)

广西创新驱动发展专项资金项目(桂科AA20161004) (桂科AA20161004)

中国地质科学院基本科研业务费专项经费资助(2002372017007) (2002372017007)

中国地质调查局地质调查项目(DD20230081) (DD20230081)

中国岩溶

OA北大核心CSCDCSTPCD

1001-4810

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