首页> 外文期刊>Biogeosciences >Quantifying methane emissions from rice paddies in Northeast China by integrating remote sensing mapping with a biogeochemical model
【24h】

Quantifying methane emissions from rice paddies in Northeast China by integrating remote sensing mapping with a biogeochemical model

机译:通过将遥感绘图与生物地球化学模型相结合来量化东北稻田的甲烷排放量

获取原文
           

摘要

The Sanjiang Plain located in Northeastern China is one of the major riceproducing regions in the country. However, differing from the majority riceregions in Southern China, the Sanjinag Plain possesses a much coolerclimate. Could the rice paddies in this domain be an important source ofglobal methane? To answer this question, methane (CH4) emissions fromthe region were calculated by integrating remote sensing mapping with aprocess-based biogeochemistry model, Denitrification and Decomposition orDNDC. To quantify regional CH4 emissions from the plain, the model wasfirst tested against a two-year dataset of CH4 fluxes measured at atypical rice field within the domain. A sensitivity test was conducted tofind out the most sensitive factors affecting CH4 emissions in theregion. Based on the understanding gained from the validation andsensitivity tests, a geographic information system (GIS) database wasconstructed to hold the spatially differentiated input information to driveDNDC for its regional simulations. The GIS database included a rice mapderived from the Landsat TM images acquired in 2006, which provided crucialinformation about the spatial distribution of the rice fields within thedomain of 10.93 million ha. The modeled results showed that the total1.44 million ha of rice paddies in the plain emitted 0.48–0.58 Tg CH4-Cin 2006 with spatially differentiated annual emission rates ranging between38.6–943.9 kg CH4-C ha?1, which are comparable with that observed inSouthern China. The modeled data indicated that the high SOC contents, longcrop season and high rice biomass enhanced CH4 production in the coolpaddies. The modeled results proved that the northern wetland agroecosystemscould make important contributions to global greenhouse gas inventory.
机译:位于中国东北的三江平原是中国主要的水稻生产地区之一。但是,与中国南方的大部分稻米地区不同,桑基纳格平原气候凉爽得多。这个领域的稻田能否成为全球甲烷的重要来源?为了回答这个问题,该地区的甲烷(CH 4 )排放量是通过将遥感制图与基于过程的生物地球化学模型(反硝化和分解或DNDC)相集成而计算得出的。为了量化平原地区CH 4 的排放量,首先对该模型在非典型稻田中测量的CH 4 通量的两年数据集进行了测试。进行敏感性测试以找出影响该区域CH 4 排放的最敏感因素。基于从验证和敏感性测试中获得的理解,构建了一个地理信息系统(GIS)数据库,以保存空间差异化的输入信息,以驱动DNDC进行区域模拟。 GIS数据库包括从2006年获得的Landsat TM影像中提取的水稻图,它提供了有关1093万公顷范围内稻田空间分布的重要信息。模拟结果表明,2006年平原地区水稻总排放量为144万公顷,Tg CH 4 -Cin为0.48–0.58 Tg,空间差异年排放量介于38.6–943.9 kg CH 4 -C ha ?1 ,与中国南方地区的观测值相当。建模数据表明,较高的SOC含量,较长的作物生长季节和较高的水稻生物量可提高稻田CH 4 的产量。模型结果证明,北部湿地农业生态系统应该为全球温室气体清单做出重要贡献。

著录项

相似文献

  • 外文文献
  • 中文文献
  • 专利
获取原文

客服邮箱:kefu@zhangqiaokeyan.com

京公网安备:11010802029741号 ICP备案号:京ICP备15016152号-6 六维联合信息科技 (北京) 有限公司©版权所有
  • 客服微信

  • 服务号