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高浓度CO_2处理后土壤N_2O排放特征 被引量:2
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作者 徐仲均 王迎红 +4 位作者 徐星凯 pascal boeckx Oswald Van Cleemput 朱建国 王跃思 《农业环境科学学报》 CAS CSCD 北大核心 2008年第5期1866-1869,共4页
土壤被认为是大气氧化亚氮(N_2O)的重要生物排放源。随着大气CO_2浓度升高,土壤N_2O排放规律可能发生改变。无锡FACE(Free-air CO_2 Enrichment)基地至2003年已运行2年,分别采集Ambien(t背景大气CO_2浓度处理)和FACE(背景大气CO_2浓度+2... 土壤被认为是大气氧化亚氮(N_2O)的重要生物排放源。随着大气CO_2浓度升高,土壤N_2O排放规律可能发生改变。无锡FACE(Free-air CO_2 Enrichment)基地至2003年已运行2年,分别采集Ambien(t背景大气CO_2浓度处理)和FACE(背景大气CO_2浓度+200mmol·mol-1处理)农田土壤,调节含水量至40%WFPS,在25℃室内有氧预培养7d后,按250μgN·g-1添加NH4NO3,将含水量调节至80%WFPS,在25℃进行有氧培养7d。在此培养期间,定期测定施肥后土壤N_2O和CO_2排放速率,探讨来自田间Ambient和FACE土壤N_2O排放差异及其可能的影响因素。结果表明,所有土壤N_2O和CO_2排放速率均随培养时间延长而迅速递减,来自Ambient处理的土壤N_2O和CO_2排放速率均高于来自FACE处理的土壤相应排放量,且土壤N_2O与CO_2排放速率存在显著正相关。通过比较培养前后土壤交换态NH_(4+)和NO_(3-)含量的变化,显示培养过程中可能存在相当量的微生物氮固持,有必要加强相关研究。 展开更多
关键词 氧化亚氮 大气CO2升高 土壤
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Hydrological Controls on Nutrient Exportation from Old-Growth Evergreen Rainforests and <i>Eucalyptus nitens</i>Plantation in Headwater Catchments at Southern Chile
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作者 Carlos E. Oyarzun Pedro Hervé-Fernández +2 位作者 Dries Huygens pascal boeckx Niko E. C. Verhoest 《Open Journal of Modern Hydrology》 2015年第2期19-31,共13页
Soil cover disturbances have a direct effect on biogeochemistry, potentially enhancing nutrient loss, land degradation and associated changes in ecosystem services and livelihood support. The objective of this study w... Soil cover disturbances have a direct effect on biogeochemistry, potentially enhancing nutrient loss, land degradation and associated changes in ecosystem services and livelihood support. The objective of this study was to assess how canopy affected throughfall chemistry and how hydrology affected stream nutrient load responses in two watersheds dominated by native old-growth evergreen rainforest (NF) and exotic plantation of Eucalyptus nitens (EP), located at the Coastal mountain range of southern Chile (40&deg;S). We measured nitrogen (NO3-N, NH4-N, Organic-N, Total-N) and total phosphorus (Total-P) at catchment discharge, and δ18O in throughfall precipitation and stream discharge in both catchments, in order to separate throughfall (or new water) contributions during storm events. It was hypothesized that all nutrients showed an increase in concentration as discharge increased (or enhanced hydrological access), in EP;but not in NF. Our results indicated that Organic-N, Total-N and Total-P concentrations were positively related to discharge. However, NO3<sup style="margin-left:-7px;">--N showed a negative correlation with catchment discharge. Organic-N and Total-P showed a flush during storm events;the opposite was observed for NO3<sup style="margin-left:-7px;">--N. However, this behavior suggested that NO3<sup style="margin-left:-7px;">--N was being retained by charged particles or soil micro biota, whether Organic-N was flushed as it was more concentrated in big pore water that was not tightly attached, compared with NO3<sup style="margin-left:-7px;">--N. 展开更多
关键词 Native RAINFORESTS Exotic Plantations Nutrient Fluxes HYDROLOGICAL CONTROLS HEADWATER Catchments
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