JEB logo

Journal of Environmental Biology

pISSN: 0254-8704 ; eISSN: 2394-0379 ; CODEN: JEBIDP

About Journal
    Home
    Obituary: Dr. R. C. Dalela
    Editorial Board
    Reviewer Panel
    Publication Policies
    Guidelines for Editors
    Guidelines for Reviewers
    Abstracting and Indexing
    Subscription and Payments
    Contact Journal
    About Triveni Enterprises
 
Read Journal
    Current Issue
    Journal Archives
 
For Authors
    Guidelines for Authors
    Terms and Conditions
    Author Resources
    Fees and Payments
    Track Paper Status
 

Google Search the Journal web-site:


    Abstract - Issue Jan 2015, 36 (1)                                     Back


nstantaneous and historical temperature effects on a-pinene

Responses of microbial respiration to nitrogen addition in two

alpine soils in the Qinghai-Tibetan Plateau

 

 

Y.H. Gao1,2*, G. Ma3, X.Y. Zeng4, S.Q. Xu3 and D.X. Wang3

1Key Laboratory of Mountain Environment Evolution and Regulation, Institute of Mountain Hazards and Environment, Chinese Academy of Sciences, Chengdu-610041, P.R. China

2Institute of Environment Sciences, University of Quebec, Montrea-H3C3P8, Canada

3College of Resources and Environment, Gansu Agricultural University, Lanzhou-730070, P.R. China

4Department of Landscape Architecture, Sichuan College of Architectural Technology, Deyang-618000, P.R. China

*Corresponding Author E-mail: yhgao@imde.ac.cn

 

 

 

Publication Data

Paper received:

31 August 2013

 

Revised received:

17 February 2014

 

Accepted:

24 July 2014

 

Abstract

An incubation experiment was conducted to examine the effects of nitrogen (N) application on microbial respiration in alpine meadow and alpine shrub soils from eastern of Qinghai-Tibetan Plateau. Four different levels of nitrogen fertilization were selected in this study: control (CK, 0 mg N g-1), low (LN, 0.04 mg N g-1), medium (MN, 0.16 mg N g-1), high (HN, 0.4 mg N g-1). The results showed that microbial respiration was higher in alpine shrub than in alpine meadow soil, regardless of the rate of N application. Total microbial respiration over the course of incubation period decreased in both soils with HN and MN treatments relative to control, but no significant differences were observed in soils with LN treatments. There was significantly positive correlation between total microbial respiration and dissolved organic carbon concentration in both soils. The results indicated that DOC may be a useful indicator of microbial respiration rate in alpine soils and the increasing N inputs could drive a negative feedback to global warming effects of carbon dioxide emitted to the atmosphere in alpine soils. ?  

 

 Key words

 

Alpine shrub soil, Carbon cycle, Fertilization, Microbial CO2, Nitrogen deposition 

 

 

Copyright ? 2015 Triveni Enterprises. All rights reserved. No part of the Journal can be reproduced in any form without prior permission. Responsibility regarding the authenticity of the data, and the acceptability of the conclusions enforced or derived, rest completely with the author(s).