Agro-C: A biogeophysical model for simulating the carbon budget of agroecosystems

被引:108
作者
Huang, Yao [1 ,6 ]
Yu, Yongqiang [1 ]
Zhang, Wen [1 ]
Sun, Wenjuan [1 ]
Liu, Shiliang [2 ]
Jiang, Jun [3 ]
Wu, Jinshui [4 ]
Yu, Wantai [5 ]
Wang, Yu [6 ]
Yang, Zhaofang [6 ]
机构
[1] Chinese Acad Sci, Inst Atmospher Phys, LAPC, Beijing 100029, Peoples R China
[2] Beijing Normal Univ, Sch Environm, Beijing 100075, Peoples R China
[3] Chinese Acad Sci, Inst Soil Sci, Nanjing 210008, Peoples R China
[4] Chinese Acad Sci, Inst Subtrop Agroecol, Changsha 410125, Peoples R China
[5] Chinese Acad Sci, Inst Appl Ecol, Shenyang 110016, Peoples R China
[6] Nanjing Agr Univ, Coll Resource & Environm Sci, Nanjing 210095, Peoples R China
基金
中国国家自然科学基金;
关键词
Agro-C model; Agroecosystem; Net primary production; Soil organic carbon; Net CO2 exchange; Carbon budget; SOIL ORGANIC-CARBON; CROPGRO-SOYBEAN MODEL; CLIMATE-CHANGE; TERRESTRIAL BIOSPHERE; GROWING-SEASON; SCALING-UP; NITROGEN; RICE; CO2; RESPIRATION;
D O I
10.1016/j.agrformet.2008.07.013
中图分类号
S3 [农学(农艺学)];
学科分类号
0901 ;
摘要
We developed a biogeophysical model called Agro-C to assess the regional carbon budgets of agroecosystems on a large scale. The model consists of two submodels, Crop-C and Soil-C. Crop-C simulates crop photosynthesis, autotrophic respiration and net primary production (NPP). Soil-C simulates soil heterotrophic respiration via the decomposition of both input organic carbon and soil organic carbon (SOC). Changes in SOC are determined by balancing the loss of soil carbon with the sequestration of input organic carbon. The model also simulates the net ecosystem exchange (NEE) between cropland and the atmosphere. Agro-C was validated against independent datasets from the literature, multi-year agricultural statistics, and field measurements in China. These datasets covered areas with a range of climates, soils, crop rotations and agricultural practices. Model validation showed that Crop-C simulated NPP quite well for rice, wheat and maize, and reasonably well for cotton, while it did not simulate NPP well for soybean and rapeseed. Changes in SOC at different sites could be properly simulated, although there was a systematic negative bias. Observed seasonal fluctuations of NEE in a winter wheat-maize rotation system were well captured by Agro-C, but a discrepancy existed at a daily timescale. These systematic biases and errors may result from imperfect inputs, insufficient knowledge and inappropriate simplifications during model development. We conclude that the Agro-C can simulate crop NPP and changes in SOC under various conditions of climate, soil, and agricultural practices in general, making it possible to extrapolate the model to a wider domain. Agro-C also has the potential for modeling net CO2 exchange between cropland and the atmosphere. Further improvements of Agro-C should focus on the enhancement of its descriptive power for key processes, as well as on parameterization, re-calibration and validation using spatiotemporal datasets across a wider domain so that it can be more applicable to broader regions. (c) 2008 Elsevier B.V. All rights reserved.
引用
收藏
页码:106 / 129
页数:24
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