黄土高原次生林演替过程土壤氮矿化特征及其影响因素
作者:
作者单位:

作者简介:

通讯作者:

中图分类号:

基金项目:

陕西省自然科学基础研究计划项目(2024JC-YBMS-224);榆林市科技计划项目(2023-CXY-212);国家级大学生创新创业训练计划项目(202310719001)


The soil nitrogen mineralization and its influencing factors during secondary forest succession in the Loess Plateau
Author:
Affiliation:

Fund Project:

The Shaanxi Natural Science Basic Research Program(2024JC-YBMS-224);Yulin Science and Technology Planning Project(2023-CXY-212);National innovation and entrepreneurship training program for college students (202310719001)

  • 摘要
  • |
  • 图/表
  • |
  • 访问统计
  • |
  • 参考文献
  • |
  • 相似文献
  • |
  • 引证文献
  • |
  • 文章评论
    摘要:

    土壤氮矿化速率限制着森林土壤有效氮素供给能力,但目前关于黄土高原次生林演替过程土壤氮矿化特征的认识还不清楚。选择黄土高原黄龙山次生林区草本阶段、灌木阶段、先锋乔木群落阶段、混交森林群落阶段和顶级森林群落阶段等5个演替阶段的9种群落类型,测定了其林下土壤氮矿化速率,并分析了土壤理化性质、凋落物养分特征和土壤酶活性及其对氮矿化的影响。结果表明:随着演替进展,土壤有机碳和氮不断积累,土壤硝态氮和铵态氮含量逐渐增加,凋落物养分和土壤酶活性也发生了显著变化。土壤硝化速率从草本群落阶段到顶级森林群落阶段显著增加了71.73%;土壤氨化速率一直为负值且持续负向增加;土壤净矿化速率从草本群落阶段的(0.16±0.06) mg kg-1 d-1逐渐增加到混交森林阶段的(0.31±0.08)mg kg-1 d-1,但从混交林群落到顶级森林群落阶段有所下降。土壤理化性质(路径系数-0.530)和酶活性(路径系数-0.268)对氮矿化速率有显著的直接作用;凋落物养分对氮矿化速率的影响来自于其直接作用(路径系数-0.283)和通过调控土壤理化性质、酶活性产生的间接影响(路径系数-0.315)。结果有助于认识黄土高原植被演替过程中土壤氮循环过程,对森林可持续经营也有一定的意义。

    Abstract:

    The rate of soil nitrogen mineralization can determine the supply capacity of available nitrogen in forest soil, but it is not yet fully understood in the succession process of secondary forests on the Loess Plateau. This study selected nine plant communities from five succession stages (herbaceous community stage, shrub community stage, pioneer forests community stage, mixed forest stage and climax forest community stage) in the secondary succession forest area of Huanglong Mountain area on the Loess Plateau as sample lands. The soil nitrogen mineralization rate was measured, and the soil physicochemical properties, litter nutrient characteristics, soil enzyme activities and their impact on nitrogen mineralization were analyzed. The results revealed a continuous accumulation of soil organic carbon and nitrogen with the progression of succession, and the soil nitrate and ammonium nitrogen contents also gradually increased. Litter nutrients and soil enzyme activities changed significantly along with succession. The soil nitrification rate increased by 71.73% from the herbaceous community stage to climax forest community stage, while the ammonification rate remained negative and continued to increase negatively with succession. The soil net mineralization rate increased from (0.16±0.06) mg kg-1 d-1 in the herbaceous community stage to (0.31±0.08) mg kg-1 d-1 in the mixed forest stage, but decreased from the mixed forest to the climax forest community stage. Soil physicochemical properties (path coefficient -0.530) and enzyme activities (path coefficient-0.268) influenced the rate of nitrogen mineralization directly. The effect of litter nutrients on the nitrogen mineralization rate stemmed from both direct influence (path coefficient -0.283) and indirect effect through the regulation of soil physicochemical properties and enzyme activities (path coefficient -0.315). These results can contribute to our understanding of the soil nitrogen cycle during vegetation succession on the Loess Plateau, and help with the sustainable forest management.

    参考文献
    相似文献
    引证文献
引用本文

刘冲,朱运,邓健,徐莉萍,张丹,王晨枫,欧阳洪梁,李江文.黄土高原次生林演替过程土壤氮矿化特征及其影响因素.生态学报,2024,44(14):6346~6356

复制
分享
文章指标
  • 点击次数:
  • 下载次数:
  • HTML阅读次数:
  • 引用次数: