Literature DB >> 23721610

Turnover of organic carbon and nitrogen in soil assessed from δ13C and δ15N changes under pasture and cropping practices and estimates of greenhouse gas emissions.

Ram C Dalal1, Craig M Thornton, Bruce A Cowie.   

Abstract

The continuing clearance of native vegetation for pasture, and especially cropping, is a concern due to declines in soil organic C (SOC) and N, deteriorating soil health, and adverse environment impact such as increased emissions of major greenhouse gases (CO2, N2O and CH4). There is a need to quantify the rates of SOC and N budget changes, and the impact on greenhouse gas emissions from land use change in semi-arid subtropical regions where such data are scarce, so as to assist in developing appropriate management practices. We quantified the turnover rate of SOC from changes in δ(13)C following the conversion of C3 native vegetation to C4 perennial pasture and mixed C3/C4 cereal cropping (wheat/sorghum), as well as δ(15)N changes following the conversion of legume native vegetation to non-legume systems over 23 years. Perennial pasture (Cenchrus ciliaris cv. Biloela) maintained SOC but lost total N by more than 20% in the top 0-0.3m depth of soil, resulting in reduced animal productivity from the grazed pasture. Annual cropping depleted both SOC and total soil N by 34% and 38%, respectively, and resulted in decreasing cereal crop yields. Most of these losses of SOC and total N occurred from the >250 μm fraction of soil. Moreover, this fraction had almost a magnitude higher turnover rates than the 250-53 μm and <53 μm fractions. Loss of SOC during the cropping period contributed two-orders of magnitude more CO2-e to the atmosphere than the pasture system. Even then, the pasture system is not considered as a benchmark of agricultural sustainability because of its decreasing productivity in this semi-arid subtropical environment. Introduction of legumes (for N2 fixation) into perennial pastures may arrest the productivity decline of this system. Restoration of SOC in the cropped system will require land use change to perennial ecosystems such as legume-grass pastures or native vegetation.
Copyright © 2013 Elsevier B.V. All rights reserved.

Entities:  

Keywords:  C turnover; Greenhouse gases; Soil nitrogen; Soil organic carbon; δ(13)C; δ(15)N

Year:  2013        PMID: 23721610     DOI: 10.1016/j.scitotenv.2013.04.101

Source DB:  PubMed          Journal:  Sci Total Environ        ISSN: 0048-9697            Impact factor:   7.963


  3 in total

1.  Soil organic carbon dynamics under long-term fertilization in a black soil of China: Evidence from stable C isotopes.

Authors:  Xiaolin Dou; Ping He; Ping Zhu; Wei Zhou
Journal:  Sci Rep       Date:  2016-02-22       Impact factor: 4.379

2.  Response of Soil Properties and Microbial Communities to Agriculture: Implications for Primary Productivity and Soil Health Indicators.

Authors:  Pankaj Trivedi; Manuel Delgado-Baquerizo; Ian C Anderson; Brajesh K Singh
Journal:  Front Plant Sci       Date:  2016-07-12       Impact factor: 5.753

3.  Functional Links between Biomass Production and Decomposition of Vetiver (Chrysopogon zizanioides) Grass in Three Australian Soils.

Authors:  Bezaye Tessema; Brian Wilson; Heiko Daniel; Paul Kristiansen; Jeff A Baldock
Journal:  Plants (Basel)       Date:  2022-03-15
  3 in total

北京卡尤迪生物科技股份有限公司 © 2022-2023.