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

被引:28
|
作者
Dalal, Ram C. [1 ,3 ]
Thornton, Craig M. [2 ]
Cowie, Bruce A. [2 ]
机构
[1] Dept Sci Informat Technol Innovat & Arts, Dutton Pk, Qld 4102, Australia
[2] Dept Nat Resources & Mines, Rockhampton, Qld 4700, Australia
[3] Univ Queensland, Sch Agr & Food Sci, Brisbane, Qld 4072, Australia
关键词
Soil organic carbon; Soil nitrogen; delta C-13; delta N-15; C turnover; Greenhouse gases; C-13; NATURAL-ABUNDANCE; LONG-TERM TRENDS; LAND-USE CHANGE; CONTINUOUS CULTIVATION; SOUTHERN QUEENSLAND; FOREST SOIL; MATTER; DYNAMICS; FRACTIONS; FERTILITY;
D O I
10.1016/j.scitotenv.2013.04.101
中图分类号
X [环境科学、安全科学];
学科分类号
08 ; 0830 ;
摘要
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 delta C-13 following the conversion of C-3 native vegetation to C-4 perennial pasture and mixed C-3/C-4 cereal cropping (wheat/sorghum), as well as delta N-15 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 0-0.3 m 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 mu m fraction of soil. Moreover, this fraction had almost a magnitude higher turnover rates than the 250-53 mu m and <53 mu m 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 N-2 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. (C) 2013 Elsevier B.V. All rights reserved.
引用
收藏
页码:26 / 35
页数:10
相关论文
共 50 条
  • [1] Soil organic matter decomposition and turnover in a tropical Ultisol:: Evidence from δ13C, δ15N and geochemistry
    Krull, ES
    Bestland, EA
    Gates, WP
    [J]. RADIOCARBON, 2002, 44 (01) : 93 - 112
  • [2] Dynamics of physically-separated soil organic carbon pools assessed from δ13C changes under 25 years of cropping systems
    Dou, Xiaolin
    Cheng, Xiaoli
    He, Ping
    Zhu, Ping
    Zhou, Wei
    Wang, Ligang
    [J]. SOIL & TILLAGE RESEARCH, 2017, 174 : 6 - 13
  • [3] Isotopic composition of carbon (δ13C) and nitrogen (δ15N) in foliage and soil as a function of tree species
    Menyailo O.V.
    Makarov M.I.
    Cheng C.-H.
    [J]. Doklady Biological Sciences, 2014, 456 (1) : 209 - 211
  • [4] Effects of land-use change on soil organic carbon and nitrogen in density fractions and soil δ13C and δ15N in semiarid grasslands
    Qiu, Liping
    Wei, Xiaorong
    Ma, Tiane
    Wei, Yanchun
    Horton, Robert
    Zhang, Xingchang
    Cheng, Jimin
    [J]. PLANT AND SOIL, 2015, 390 (1-2) : 419 - 430
  • [5] Effects of land-use change on soil organic carbon and nitrogen in density fractions and soil δ13C and δ15N in semiarid grasslands
    Liping Qiu
    Xiaorong Wei
    Tiane Ma
    Yanchun Wei
    Robert Horton
    Xingchang Zhang
    Jimin Cheng
    [J]. Plant and Soil, 2015, 390 : 419 - 430
  • [6] Natural abundance of 13C and 15N in earthworms from different cropping treatments
    Briones, MJI
    Bol, R
    [J]. PEDOBIOLOGIA, 2003, 47 (5-6) : 560 - 567
  • [7] The use of 13C and 15N based isotopic techniques for assessing soil C and N changes under conservation agriculture
    Ismaili, Kenza
    Ismaili, Mohammed
    Ibijbijen, Jamal
    [J]. EUROPEAN JOURNAL OF AGRONOMY, 2015, 64 : 1 - 7
  • [8] 13C and 15N NMR spectroscopy as a tool in soil organic matter studies
    Kogel-Knabner, I
    [J]. GEODERMA, 1997, 80 (3-4) : 243 - 270
  • [9] C and N allocation in soil under ryegrass and alfalfa estimated by 13C and 15N labelling
    Andreas Schmitt
    Johanna Pausch
    Yakov Kuzyakov
    [J]. Plant and Soil, 2013, 368 : 581 - 590
  • [10] C and N allocation in soil under ryegrass and alfalfa estimated by 13C and 15N labelling
    Schmitt, Andreas
    Pausch, Johanna
    Kuzyakov, Yakov
    [J]. PLANT AND SOIL, 2013, 368 (1-2) : 581 - 590