Ecology & Biodiversity, Department of Biology, Utrecht University, P.O. Box 800.84, 3508 TB Utrecht, The Netherlands.
Environ Pollut. 2012 Jun;165:67-76. doi: 10.1016/j.envpol.2012.02.008. Epub 2012 Mar 8.
This paper presents a spatially explicit model for simulating the fate of nitrogen (N) in soil and groundwater and nitrous oxide (N(2)O) production in groundwater with a 1 km resolution at the European scale. The results show large heterogeneity of nitrate outflow from groundwater to surface water and production of N(2)O. This heterogeneity is the result of variability in agricultural and hydrological systems. Large parts of Europe have no groundwater aquifers and short travel times from soil to surface water. In these regions no groundwater denitrification and N(2)O production is expected. Predicted N leaching (16% of the N inputs) and N(2)O emissions (0.014% of N leaching) are much less than the IPCC default leaching rate and combined emission factor for groundwater and riparian zones, respectively.
本文提出了一个空间显式模型,用于模拟氮(N)在土壤和地下水中的归宿以及在欧洲范围内以 1 公里分辨率在地下水中产生的氧化亚氮(N2O)。结果表明,硝酸盐从地下水向地表水的流出和 N2O 的产生存在很大的异质性。这种异质性是农业和水文系统变化的结果。欧洲的大部分地区没有地下水含水层,从土壤到地表水的迁移时间很短。在这些地区,预计不会发生地下水反硝化和 N2O 的产生。预测的 N 淋失(占 N 输入的 16%)和 N2O 排放(N 淋失的 0.014%)均远低于《政府间气候变化专门委员会》默认的地下水和河岸带的淋失率和综合排放系数。