Impact of agricultural management practices on soil organic carbon: simulation of Australian wheat systems

被引:68
|
作者
Zhao, Gang [1 ,2 ]
Bryan, Brett A. [2 ]
King, Darran [2 ]
Luo, Zhongkui [3 ]
Wang, Enli [3 ]
Song, Xiaodong [2 ,4 ]
Yu, Qiang [1 ,5 ]
机构
[1] Chinese Acad Sci, Inst Geog Sci & Nat Resources Res, Key Lab Water Cycle & Related Land Surface Proc, Beijing 100101, Peoples R China
[2] CSIRO Ecosyst Sci, Urrbrae, SA 5064, Australia
[3] CSIRO Land & Water, Canberra, ACT 2601, Australia
[4] Zhejiang Univ, Coll Environm & Nat Resources, Hangzhou 310058, Zhejiang, Peoples R China
[5] Univ Technol Sydney, Sch Environm, Sydney, NSW 2007, Australia
基金
美国国家科学基金会;
关键词
agricultural management practice; APSIM; Australia; carbon sequestration; climate change; crop model; soil organic carbon; wheat; GLOBAL CLIMATE-CHANGE; CONSERVATION TILLAGE; PROJECTED CHANGES; SPATIAL-ANALYSIS; MINERAL SOIL; MATTER POOLS; LARGE-SCALE; SEQUESTRATION; TEMPERATURE; NITROGEN;
D O I
10.1111/gcb.12145
中图分类号
X176 [生物多样性保护];
学科分类号
090705 ;
摘要
Quantifying soil organic carbon (SOC) dynamics at a high spatial and temporal resolution in response to different agricultural management practices and environmental conditions can help identify practices that both sequester carbon in the soil and sustain agricultural productivity. Using an agricultural systems model (the Agricultural Production Systems sIMulator), we conducted a high spatial resolution and long-term (122years) simulation study to identify the key management practices and environmental variables influencing SOC dynamics in a continuous wheat cropping system in Australia's 96million ha cereal-growing regions. Agricultural practices included five nitrogen application rates (0200kgNha1 in 50kgNha1 increments), five residue removal rates (0100% in 25% increments), and five residue incorporation rates (0100% in 25% increments). We found that the change in SOC during the 122-year simulation was influenced by the management practices of residue removal (linearly negative) and fertilization (nonlinearly positive) and the environmental variables of initial SOC content (linearly negative) and temperature (nonlinearly negative). The effects of fertilization were strongest at rates up to 50kgNha1, and the effects of temperature were strongest where mean annual temperatures exceeded 19 degrees C. Reducing residue removal and increasing fertilization increased SOC in most areas except Queensland where high rates of SOC decomposition caused by high temperature and soil moisture negated these benefits. Management practices were particularly effective in increasing SOC in south-west Western Australia an area with low initial SOC. The results can help target agricultural management practices for increasing SOC in the context of local environmental conditions, enabling farmers to contribute to climate change mitigation and sustaining agricultural production.
引用
收藏
页码:1585 / 1597
页数:13
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