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首页> 外文期刊>Biogeosciences >Quantifying methane emissions from rice fields in the Taihu Lake region, China by coupling a detailed soil database with biogeochemical model
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Quantifying methane emissions from rice fields in the Taihu Lake region, China by coupling a detailed soil database with biogeochemical model

机译:通过将详细的土壤数据库与生物地球化学模型相结合来量化中国太湖地区稻田的甲烷排放

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As China has approximately 22% of the world's ricepaddies, the regional quantification of CH4 emissions from thesepaddies is important in determining their contribution to the globalgreenhouse gas effect. This paper reports the use of a biogeochemical model(DeNitrification and DeComposition or DNDC) for quantifying CH4emissions from rice fields in the Taihu Lake region of China. For thisapplication, the DNDC model was linked to a 1:50 000 soil database derivedfrom 1107 paddy soil profiles compiled during the Second National SoilSurvey of China in the 1980s–1990s. The simulated results showed that the2.3 Mha of paddy rice fields in the Taihu Lake region emitted the equivalentof 5.7 Tg C from 1982–2000, with the average CH4 flux ranging from 114to 138 kg C ha−1 y−1. As for soil subgroups, the highest emissionrate (660 kg C ha−1 y−1) was linked to gleyed paddy soilsaccounting for about 4.4% of the total area of paddy soils. The lowestemission rate (91 kg C ha−1 y−1) was associated with degleyedpaddy soils accounting for about 18% of the total area of paddy soils.The most common soil in the area was hydromorphic paddy soils, whichaccounted for about 53% of the total area of paddy soils with a CH4flux of 106 kg C ha−1 y−1. On a regional basis, the annualaveraged CH4 flux in the Taihu Lake plain soil region and alluvialplain soil region were higher than that in the low mountainous and hillysoil region and the polder soil region. The model simulation was conductedwith two databases using polygons or counties as the basic units. Thecounty-based database contained soil information coarser than the polygonsystem built based on the 1:50 000 soil database. The modeled results withthe two databases found similar spatial patterns of CH4 emissions inthe Taihu Lake region. However, discrepancies exist between the results from thetwo methods. The total CH4 emissions generated from the polygon-baseddatabase is 2.6 times the minimum CH4 emissions generated from thecounty-based database, and is 0.98 times the maximum CH4 emissionsgenerated from the county-based database. The average value of the relativedeviation ranged from −20% to 98% for most counties, which indicatesthat a more precise soil database is necessary to better simulate CH4emissions from rice fields in the Taihu Lake region using the DNDC model.
机译:由于中国约占全球稻田的22%,因此这些稻田CH 4 排放的区域量化对于确定其对全球温室气体效应的贡献非常重要。本文报道了使用生物地球化学模型(脱硝化和分解或DNDC)来量化中国太湖地区稻田CH 4 的排放量。对于此应用程序,DNDC模型与一个1:50 000土壤数据库相链接,该数据库来自1980年代至1990年代第二次中国全国土壤调查期间编制的1107个稻田土壤剖面。模拟结果表明,从1982〜2000年,太湖地区2.3 Mha的稻田排放了相当于5.7 Tg C的碳,平均CH 4 通量范围为114〜138 kg C ha <。 sup> -1 y -1 。至于土壤亚类,最高的排放率(660 kg C ha −1 y -1 )与水稻田土壤相关,约占水稻田总面积的4.4%。 。最低的排放率(91 kg C ha -1 y -1 )与去稻田土壤有关,约占稻田土壤总面积的18%。该地区为水溶水稻土,约占CH 4 通量为106 kg C ha -1 y 的水稻土总面积的53%。 -1 。从区域上看,太湖平原土壤区和冲积平原区的年均CH 4 通量高于低山丘陵区和田区的年均CH 4 通量。使用两个以多边形或县为基本单位的数据库进行模型仿真。基于县的数据库包含的土壤信息要比基于1:50 000土壤数据库建立的多边形系统更粗糙。通过两个数据库的模拟结果,发现太湖地区CH 4 排放的空间格局相似。但是,两种方法的结果之间存在差异。基于多边形的数据库生成的总CH 4 排放量是基于县数据库的最小CH 4 排放量的2.6倍,是最大的CH 排放量的0.98倍从基于县的数据库生成的4 排放量。大多数县的相对偏差平均值在-20%到98%之间,这表明使用更精确的土壤数据库来更好地模拟太湖地区稻田CH 4 的排放量是必要的。 DNDC模型。

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