| 注册
首页|期刊导航|生态学报|森林土壤融化期异养呼吸和微生物碳变化特征

森林土壤融化期异养呼吸和微生物碳变化特征

吴浩浩 徐星凯 段存涛 李团胜 CHENG WeiGuo

生态学报2017,Vol.37Issue(8):2729-2742,14.
生态学报2017,Vol.37Issue(8):2729-2742,14.DOI:10.5846/stxb201511162320

森林土壤融化期异养呼吸和微生物碳变化特征

Changes in heterotrophic respiration and microbial biomass carbon of forest soils during thaw

吴浩浩 1徐星凯 2段存涛 1李团胜 2CHENG WeiGuo1

作者信息

  • 1. 中国科学院大气物理研究所大气边界层物理和大气化学国家重点实验室,北京100029
  • 2. 中国科学院大学地球科学学院大气化学与环境科学系,北京100049
  • 折叠

摘要

Abstract

Packed soil core incubation experiment was made to study the effects of external carbon (C) (glucose,6.4 g C/ m2) addition on microbial respiration and microbial biomass C (MBC) in soils of a mature broadleaf and Korean pine mixed forest (BKPF) and an adjacent white birch forest (WBF) during thaw under different soil moisture levels (55% and 80% water-filled pore space) and nitrogen (N) supply (NH4C1 and KNO3,4.5 g N/m2).The results showed that,without C and N addition,cumulative CO2 flux from the WBF soil was significantly higher than that from the BKPF soil during the incubation period.With increasing soil moisture,the cumulative CO2 flux and microbial metabolic quotient (qco2) decreased in the WBF soil but increased in the BKPF soil without C and N addition(P < 0.05).The glucose-induced cumulative CO2 fluxes from the two forest soils ranged from 9.61 to 13.49 g CO2-C/m2,which was greater than the dose of added C in the form of glucose.The glucose-induced MBC in the two forest soils ranged from 3.65 to 27.18 g C/m2,while glucose addition had little impact on soil dissolved organic C pool.Hence,the extra C released upon addition of glucose may result from the decomposition of soil native organic C.Without N addition and under the two soil moisture levels,the glucose-induced cumulative CO2 flux from the BKPF soil was significantly higher than that from the WBF soil during thaw (P < 0.001).With increasing soil moisture,the glucose-induced cumulative CO2 fluxes from the two forest soils were significantly increased (P < 0.001).The addition of KNO3 alone significantly increased the glucose-induced cumulative CO2 flux (P < 0.01) and the glucose-induced MBC (P < 0.001) in the WBF soil under two soil moisture levels (P < 0.001).Addition of NH4 C1 alone significantly increased the glucose-induced MBC in the BKPF soil with low moisture level.Based on the results from the previously reported non-freezing experiments and the results of the present study,it can be concluded that freezing treatment significantly affects the stimulating effects of glucose on soil microbial respiration and MBC under temperate forests.Regardless of whether freezing occurred or not,the responses of soil microbial respiration and MBC to the addition of extraneous C as glucose in temperate forests depend on vegetation type,soil moisture,and the amount and type of N added.

关键词

微生物呼吸/微生物碳/葡萄糖/外源氮/溶解性有机碳/激发效应/冻土融化

Key words

microbial respiration/microbial biomass carbon/glucose/nitrogen supply/dissolved organic carbon/stimulating effect/thawing of frozen soil

引用本文复制引用

吴浩浩,徐星凯,段存涛,李团胜,CHENG WeiGuo..森林土壤融化期异养呼吸和微生物碳变化特征[J].生态学报,2017,37(8):2729-2742,14.

基金项目

国家自然科学基金(41175133,21228701,41275166,41321064,41575154) (41175133,21228701,41275166,41321064,41575154)

生态学报

OA北大核心CHSSCDCSCDCSTPCD

1000-0933

访问量2
|
下载量0
段落导航相关论文