外源添加对黄河流域典型湿地土壤矿化及硝化的影响

朱文会; 杨欣桐; 王夏晖; 卢然; 刘瑞平; 陈茜

doi:10.11949/0438-1157.20200097

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外源添加对黄河流域典型湿地土壤矿化及硝化的影响

能源和环境工程 | 更新时间：2026-07-24

- 外源添加对黄河流域典型湿地土壤矿化及硝化的影响
- Effects of exogenous addition on soil mineralization and nitrification of typical wetlands in the Yellow River Basin
- 化工学报 2020年71卷第11期页码：5278-5285
- 作者机构：
  
  生态环境部环境规划院土壤环境保护中心，重金属污染防治研究中心，北京 100012
- 作者简介：
  
  朱文会（1988—），男，硕士研究生，工程师，zhuwh@caep.org.cn
  王夏晖（1975—），男，博士，研究员，728389776@qq.com
- 基金信息：
  
  国家重点研发计划项目(2018YFC1800200;2018YFC1800205)
- DOI：10.11949/0438-1157.20200097
  中图分类号： X 53
- 收稿：2020-02-03，
  
  修回：2020-06-03，
  
  网络首发：2020-11-03，
  
  纸质出版：2020-11-05
- 稿件说明：
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朱文会, 杨欣桐, 王夏晖, 卢然, 刘瑞平, 陈茜. 外源添加对黄河流域典型湿地土壤矿化及硝化的影响[J]. 化工学报, 2020, 71(11): 5278-5285

ZHU Wenhui, YANG Xintong, WANG Xiahui, LU Ran, LIU Ruiping, CHEN Xi. Effects of exogenous addition on soil mineralization and nitrification of typical wetlands in the Yellow River Basin[J]. CIESC Journal, 2020, 71(11): 5278-5285
朱文会, 杨欣桐, 王夏晖, 卢然, 刘瑞平, 陈茜. 外源添加对黄河流域典型湿地土壤矿化及硝化的影响[J]. 化工学报, 2020, 71(11): 5278-5285 DOI： 10.11949/0438-1157.20200097.

ZHU Wenhui, YANG Xintong, WANG Xiahui, LU Ran, LIU Ruiping, CHEN Xi. Effects of exogenous addition on soil mineralization and nitrification of typical wetlands in the Yellow River Basin[J]. CIESC Journal, 2020, 71(11): 5278-5285 DOI： 10.11949/0438-1157.20200097.

摘要

以黄河上游若尔盖湿地（A土）、中游包头南海湿地（B土）、下游黄河三角洲湿地（C土）为研究对象，分别选用NH

和葡萄糖作为外加氮源和碳源，采用28 d恒温培养法，研究了外源添加对黄河流域典型湿地土壤日平均碳矿化速率（

average

）、净氮矿化速率（NN

min

）、净硝化速率（NN

nitri

）的影响。结果表明，湿地类型对土壤碳、氮矿化及硝化速率影响显著，土壤理化性质差异是主要影响因素。外源碳添加对不同类型湿地

average

均显著提高，且对A土促进作用最显著；外源氮添加对

average

影响不显著。外源碳、氮添加水平对不同类型湿地NN

min

的影响存在显著差异。低水平碳源添加显著抑制C土NN

min

，但对A土和B土NN

min

影响不显著；高水平碳

源添加对不同类型湿地NN

min

均表现出显著的抑制作用。低水平氮源添加对不同类型湿地NN

min

影响不显著；高氮添加显著抑制B土、C土NN

min

，但对A土NN

min

影响不显著。外源碳、氮添加对不同类型湿地NN

nitri

的影响不显著。

Abstract

Taking Zoige Wetland (soil A) in the upper reaches of the Yellow River

Baotou Nanhai Wetland (soil B) in the middle reaches

and the Yellow River Delta Wetland (soil C) in the lower reaches as the research objects

and glucose were used as external nitrogen and carbon sources

respectively

and a 28 d constant temperature cultivation method was used. The effects of exogenous addition on daily average carbon mineralization rate (

average

)

net nitrogen mineralization rate (NN

min

)

and net nitrification rate (NN

nitri

) of typical wetland soil in the Yellow River Basin were studied. The results show that wetland types have significant effects on soil carbon and nitrogen mineralization and nitrification rates

and differences in soil physical and chemical properties are the main influencing factors. Carbon addition significantly increased

average

of different wetland soils and the most significant promotion was exerted on soil A. However

nitrogen addition had no significant effect on

average

. Addition level had significant influence on NN

min

. Low level carbon addition significantly inhibited NN

min

of soil C while had no significant effect on that of soil A or soil B. High level carbon addition significantly prevented NN

min

of different wetland soils. Low level nitrogen addition had no significant effect on NN

min

. High level nitrogen addition significantly inhibited NN

min

of soil B and soil C

while had no significant effect on soil A. Exogenous addition had no significant effect on NN

nitri

关键词

Keywords

references

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