农田生态系统碳循环模型研究概述
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摘要
陆地生态系统的碳循环过程中最活跃的碳库是农田生态系统。农田生态系统碳循环模型是研究碳循环的重要方法之一。简要介绍了碳素在不同碳库之间迁移转化的规律,阐述了农田生态系统碳循环模型的发展历程以及国内外主要的碳循环模型,并对未来农田生态系统碳循环模型研究趋势进行了展望,以期为减少农业面源污染、温室气体排放和研究全球气候变化提供科学依据。
The most active carbon pool in terrestrial ecosystems carbon cycle is the farmland ecosystem. The carbon cycle model of farmland ecosystem is one of the important methods to study carbon cycle. The law of migration and transformation of carbon between different carbon pools briefly were introduced, the development process of the carbon cycle model of farmland ecosystem was explained, the main carbon cycle modes at home and abroad were reviewed, the research trend of carbon cycle model of farmland ecosystem in the future is prospected. This will provide a scientific basis for reducing agricultural source pollution, greenhouse gas emissions, and studying global climate change.
The most active carbon pool in terrestrial ecosystems carbon cycle is the farmland ecosystem. The carbon cycle model of farmland ecosystem is one of the important methods to study carbon cycle. The law of migration and transformation of carbon between different carbon pools briefly were introduced, the development process of the carbon cycle model of farmland ecosystem was explained, the main carbon cycle modes at home and abroad were reviewed, the research trend of carbon cycle model of farmland ecosystem in the future is prospected. This will provide a scientific basis for reducing agricultural source pollution, greenhouse gas emissions, and studying global climate change.
引文
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[36]王晓凤.DAISY模型在高产农田水、氮优化管理中的应用[D].北京:中国农业大学,2007.
[37]邱建军,王立刚,唐华俊,等.东北三省耕地土壤有机碳储量变化的模拟研究[J].中国农业科学,2004(8):1166-1171.
[38]王瑞利.基于多模型的森林-草原交错带碳动态模拟研究[D].呼和浩特:内蒙古农业大学,2017.
[39]张欢.华东沿海滩涂围垦区土壤有机碳动态及其模型预测[D].南京:南京大学,2017.
[41]张娜,于贵瑞,赵士洞,等.基于遥感和地面数据的景观尺度生态系统生产力的模拟[J].应用生态学报,2003(5):643-652.
[42]赵风华,王秋凤,王建林,等.小麦和玉米叶片光合-蒸腾日变化耦合机理[J].生态学报,2011,31(24):7526-7532.
[2]周文婷,黄毅斌,王义祥,等.农业生态系统碳循环[J].草业科学,2013,30(11):1725-1731.
[3]陈新芳,居为民,陈镜明,等.陆地生态系统碳水循环的相互作用及其模拟[J].生态学杂志,2009,28(8):1630-1639.
[4]毛留喜,孙艳玲,延晓冬.陆地生态系统碳循环模型研究概述[J].应用生态学报,2006(11):2189-2195.
[5]姚桃峰,王润元,王燕.中国小麦生长模拟模型研究概述[J].干旱气象,2009,7(1):66-72.
[6]PIAO S,FANG J,CIAIS P,et al.The carbon balance of terrestrial ecosystems in China[J].Nature,2009,458(23):1009-1013.
[7]REICHSTEIN M,BAHN M,CIAIS P,et al.Climate extremes and the carbon cycle[J].Nature,2013,500(2725):287-295.
[8]XIA J Y,CHEN J Q,PIAO S L,et al.Terrestrial carbon cycle affected by non-uniform climate warming[J].Nature geoscience,2014,7:173-180.
[9]POULTER B,FRANK D,CIAIS P,et al.Contribution of semiarid ecosystems to interannual variability of the global carbon cycle[J].Nature,2014,509(7502):600-608.
[10]CARVALHAIS N,FORKEL M,KHOMIK M,et al.Global covariation of carbon turnover times with climate in terrestrial ecosystems[J].Nature,2014,514(7521):213-217.
[11]GISLASON S R,OELKERS E H.Carbon storage in basalt[J].Science,2014,344(6182):373-374.
[12]DAVIS S J,CALDEIRA K.Consumption-based accounting of CO2emissions[J].Proceedings of the national academy of sciences of the United States of America,2010,107(12):5687-5692.
[13]王平,沈润平.基于CLM模型的植被覆盖变化对黄土高原气温和降水的影响研究[J].科学技术与工程,2013,13(20):5754-5760.
[14]FAO.FAO Statis tical Yearbook 2013:World Food and Agriculture[M].Rome:Fao Inter-Departmental Working Group,2013.
[15]赵荣钦,刘英,丁明磊,等.河南省农田生态系统碳源/汇研究[J].河南农业科学,2010(7):40-44.
[16]田志会,刘瑞涵.基于京津冀一体化的农田生态系统碳足迹年际变化规律研究[J].农业资源与环境学报,2018,35(2):167-173.
[17]张启霞.甘肃省定西市作物秸秆资源利用与低碳农业发展研究[D].成都:四川师范大学,2014.
[18]张赛,王龙昌.全球变化背景下农田生态系统碳循环研究[J].农机化研究,2013,35(1):4-9.
[19]孙振钧,周东兴.生态学研究方法[M].北京:科学出版社,2010.
[20]万盛,宋新山,秦天玲,等.农田生态系统碳循环模型研究综述[J].农田水利,2017(4):58-61,66.
[21]杨靖民,杨靖一,姜旭,等.作物模型研究进展[J].吉林农业大学学报,2012,34(5):553-561.
[22]张海清,刘琪璟,陆佩玲,等.陆地生态系统碳循环模型概述[J].中国科技信息,2005(13):25-19.
[23]王文佳,冯浩.国外主要作物模型研究进展与存在问题[J].节水灌溉,2012(8):63-68,73.
[24]MALDONADO I I.Determination of genetic coefficients of three spring wheat varieties under a Mediterranean environment applying the DSSAT model[J].Chilean journal of agricultural research,2015,75(4):412-424.
[25]L魷PEZCRUZ I L,ROJANOAGUILAR A,SALAZARMORENO R,et al.Global sensitivity analysis of crop growth sucros model applied to husk tomato[J].Revista fitotecnia mexicana,2014,37(3):279-288.
[26]MISHRA S K,SHEKH A M,PANDEY V,et al.Sensitivity analysis of four wheat cultivars to varying photoperiod and temperature at different phenological stages using WOFOSTmodel[J].Journal of agrometeorology,2015,17(1):74-79.
[27]LU X H,BAI H,LIU H Y.Validate the DSSAT model on winter wheat under conservation tillage treatments in the West Henan,China[J].Agricultural research in the arid Areas,2014,28(3):64-70.
[28]SUBASH N,SHAMIM M,SINGH V K.Applicability of APSIMto capture the effectiveness of irrigation management decisions in ricebased cropping sequence in the Upper-Gangetic Plains of India[J].Paddy and water environment,2015,13(4):325-335.
[29]高懋芳,邱建军,李长生,等.应用Manure-DNDC模型模拟畜禽养殖氮素污染[J].农业工程学报,2012,28(9):183-189,294.
[30]周少平.基于APSIM模型的黄土高原玉米-小麦-大豆轮作系统产量、土壤水分动态[D].兰州:兰州大学,2008.
[31]刘志娟,杨晓光,王静,等.APSIM玉米模型在东北地区的适应性[J].作物学报,2012,38(4):740-746.
[32]龙军,毛艳玲,张黎明,等.农田土壤有机碳演变模型的研究进展[J].中国农学通报,2012,28(5):232-239.
[33]XU W,CHEN X,LUO G,et al.Using the CENTURY model to assess the impact of land reclamation and management practices in oasis agriculture on the dynamics of soil organic carbon in the arid region of North-western China[J].Ecological complexity,2011,8(1):30-37.
[34]GUO L,FALLOON P,COLEMAN K,et al.Application of the Roth C model to the results of long term experiments on typical upland soils in Northern China[J].Soil use and management,2007,23(1):63-70.
[35]杨轩,谭广洋,沈禹颖.秸秆还田对旱作冬小麦后茬土壤水分的影响及其APSIM模拟[J].干旱区研究,2013,30(4):609-614.
[36]王晓凤.DAISY模型在高产农田水、氮优化管理中的应用[D].北京:中国农业大学,2007.
[37]邱建军,王立刚,唐华俊,等.东北三省耕地土壤有机碳储量变化的模拟研究[J].中国农业科学,2004(8):1166-1171.
[38]王瑞利.基于多模型的森林-草原交错带碳动态模拟研究[D].呼和浩特:内蒙古农业大学,2017.
[39]张欢.华东沿海滩涂围垦区土壤有机碳动态及其模型预测[D].南京:南京大学,2017.
[41]张娜,于贵瑞,赵士洞,等.基于遥感和地面数据的景观尺度生态系统生产力的模拟[J].应用生态学报,2003(5):643-652.
[42]赵风华,王秋凤,王建林,等.小麦和玉米叶片光合-蒸腾日变化耦合机理[J].生态学报,2011,31(24):7526-7532.