首页> 外文期刊>Geoderma: An International Journal of Soil Science >Spatially explicit estimation of soil denitrification rates and land use effects in the riparian buffer zone of the large Guanting reservoir
【24h】

Spatially explicit estimation of soil denitrification rates and land use effects in the riparian buffer zone of the large Guanting reservoir

机译:官厅大型水库河岸缓冲带土壤反硝化速率和土地利用效应的空间显式估计

获取原文
获取原文并翻译 | 示例
           

摘要

An important function of riparian ecosystems, usually characterized as nitrate-loaded wetland environments, is nitrogen removal by denitrification. Riparian buffer zones around large dams and water reservoirs are also recognized as hotspots for emission of nitrogen (N-2) and nitrous oxide (N2O), the latter being a strong greenhouse gas. Research has proven that land use has an important effect on soil denitrification. A spatial landscape-scale approach for analyzing denitrification processes and land use effects can therefore be considered important for an adequate assessment and management of NO3- losses and N2O emissions in riparian ecosystems.In this study, we couple a soil denitrification process model with remote sensing data and techniques to analyze the spatial and temporal dynamics of soil denitrification in the riparian area of the Guanting reservoir, an important water supply of Beijing, China. SPOT-5 and Landsat TM5 satellite data were used to interpret the spatial land surface information and derive model parameters. A laboratory-scale anaerobic incubation experiment was used to estimate the soil denitrification model parameters for the different soil types. Modeling results were compared and validated with data from a nearby experimental N2O emission research site. The overall average soil denitrification rate (SDR) of the Guanting riparian basin was 32.45 mg N m(-2) d(-1) during the simulation period from March to September 2007, with a maximum of 370.49 mg N m(-2) d(-1) appeared in August and the minimum of 0.02 mg N m(-2) d(-1) in March. Bottomland and wetlands had large SDR's, with an average daily rate of 80.20 and 136 mg N m(-2) d(-1) respectively. Forest, grassland and shrub showed lower values, with average daily rates of 25.21,18.77 and 16.59 mg N m(-2) d(-1) respectively. The modeling results also indicated that farmland and orchards had a relative high SDR (34.09 and 33.25 mg N m(-2) d(-1) respectively), with large fluctuations observed between June and August due to agricultural practices. As soil denitrification rates and N-2 and N2O emissions showed to be strongly correlated to the different land use practices, this could be taken into consideration when planning best management strategies for non-point source pollution control and greenhouse gas mitigation.
机译:河岸生态系统的一个重要功能(通常以负载硝酸盐的湿地环境为特征)是通过反硝化去除氮。大型水坝和水库周围的河岸缓冲区也被认为是排放氮(N-2)和一氧化二氮(N2O)的热点,后者是强温室气体。研究证明,土地利用对土壤反硝化具有重要影响。因此,空间景观尺度分析反硝化过程和土地利用影响的方法被认为对于充分评估和管理河岸生态系统中NO3损失和N2O排放至关重要。在这项研究中,我们将土壤反硝化过程模型与遥感相结合。数据和技术来分析官厅水库河岸地区土壤反硝化的时空动态,官厅水库是北京的重要供水。 SPOT-5和Landsat TM5卫星数据被用来解释空间地表信息并推导出模型参数。实验室规模的厌氧培养实验用于估算不同土壤类型的土壤反硝化模型参数。对建模结果进行了比较,并用附近的N2O实验研究站点的数据进行了验证。在2007年3月至2007年9月的模拟期内,官厅河岸盆地的总体平均土壤反硝化率(SDR)为32.45 mg N m(-2)d(-1),最大为370.49 mg N m(-2) d(-1)出现在8月,最小0.02 mg N m(-2)d(-1)出现在3月。海底和湿地的SDR较大,平均日发病率分别为80.20和136 mg N m(-2)d(-1)。森林,草地和灌木的价值较低,分别为25.21、18.77和16.59 mg N m(-2)d(-1)。模拟结果还表明,农田和果园具有较高的特别提款权(分别为34.09和33.25 mg N m(-2)d(-1)),由于农业实践,在6月至8月之间观察到较大的波动。由于土壤反硝化率以及N-2和N2O排放与不同的土地利用方式密切相关,因此在规划非点源污染控制和减缓温室气体的最佳管理策略时,可以考虑到这一点。

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