首页> 外文期刊>Biogeosciences >Regulation of carbon dioxide and methane in small agricultural reservoirs: optimizing potential for greenhouse gas uptake
【24h】

Regulation of carbon dioxide and methane in small agricultural reservoirs: optimizing potential for greenhouse gas uptake

机译:小农业储层中二氧化碳和甲烷的调节:优化温室气体吸收潜力

获取原文
获取外文期刊封面目录资料

摘要

Small farm reservoirs are abundant in many agricultural regions across the globe and have the potential to be large contributing sources of carbon dioxide (CO2) and methane (CH4) to agricultural landscapes. Compared to natural ponds, these artificial waterbodies remain overlooked in both agricultural greenhouse gas (GHG) inventories and inland water global carbon (C) budgets. Improved understanding of the environmental controls of C emissions from farm reservoirs is required to address and manage their potential importance in agricultural GHG budgets. Here, we conducted a regional-scale survey (~ 235 000 km2) to measure CO2 and CH4 surface concentrations and diffusive fluxes across 101 small farm reservoirs in Canada's largest agricultural area. A combination of abiotic, biotic, hydromorphologic, and landscape variables were modelled using generalized additive models (GAMs) to identify regulatory mechanisms. We found that CO2 concentration was estimated by a combination of internal metabolism and groundwater-derived alkalinity (66.5 % deviance explained), while multiple lines of evidence support a positive association between eutrophication and CH4 production (74.1 % deviance explained). Fluxes ranged from ?21 to 466 and 0.14 to 92 mmol m?2 d?1 for CO2 and CH4, respectively, with CH4 contributing an average of 74 % of CO2-equivalent (CO2-e) emissions based on a 100-year radiative forcing. Approximately 8 % of farm reservoirs were found to be net CO2-e sinks. From our models, we show that the GHG impact of farm reservoirs can be greatly minimized with overall improvements in water quality and consideration to position and hydrology within the landscape.
机译:小农场水库在全球各地的许多农业区域都丰富,有可能成为农业景观的大量贡献二氧化碳(CO2)和甲烷(CH4)。与天然池塘相比,这些人造水平仍然忽视了农业温室气体(GHG)库存和内陆水全球碳(C)预算。需要改善对农用水库的C减排环境控制的理解,需要解决并管理其在农业温室气体预算中的潜在重要性。在这里,我们进行了区域规模调查(〜235 000平方公里),以测量加拿大最大农业区的101个小型农用水库的二氧化碳和CH4表面浓度和扩散势量。使用广义添加剂模型(Gams)进行非生物,生物形态,水性形态和景观变量的组合,以确定调节机制。我们发现通过内部代谢和地下水衍生的碱度(解释的66.5%偏差)的组合估计CO 2浓度,而多种证据支持富营养化和CH4生产之间的阳性关联(解释74.1%的偏差)。对于CO 2和CH 4,CH4分别为CO 2和CH 4的助熔剂的范围为21至466和0.14至92mmolM≤2d?1,CH 4有助于基于100年辐射的100年的CO 2等同(CO2-E)排放量的74%强迫。大约8%的农用水库被发现是净CO2-E水槽。从我们的模型来看,我们表明,农用水库的温室气体影响力可以大大尽量减少水质的整体改善,并考虑景观内的位置和水文。

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