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不同水肥条件下黄河三角洲盐土的N2O排放速率

张金凤1,2**,李增嘉3   

  1. 1中山大学环境科学与工程学院,广州 510275;2福建师范大学地理科学学院,福州 350007;3山东农业大学农学院作物生物学国家重点实验室,山东泰安 271018)
  • 出版日期:2013-07-10 发布日期:2013-07-10

Nitrous oxide emission rates of saline soils in Yellow River Delta of China under different water and N amendment conditions.

ZHANG Jin-feng1, 2**, LI Zeng-jia3   

  1. (1School of Environmental Science and Engineering, Sun YatSen University, Guangzhou 510275, China; 2College of Geographical Sciences, Fujian Normal University, Fuzhou 350007, China; 3State Key Laboratory of Crop Biology, College of Agronomy, Shandong Agricultural University, Taian 271018, Shandong, China)
  • Online:2013-07-10 Published:2013-07-10

摘要: 用室内培养法测定了不同水肥处理下的盐土N2O排放速率。未加氮肥时,从中盐土(ECe = 6.4 mS·cm-1)到极盐土(ECe=126.5 mS·cm-1),在各水分条件下(50% WHC,80% WHC和4 cm深水面),盐土排放N2O的速率都非常低,经常在检测限以下。添加硝酸铵 (0.4 mg N·g-1soil)后,沙质中盐土排放速率在50% WHC时为41.0 μg N2O·kg-1soil
·d-1,在4 cm深水面时为364.6 μg N2O·kg-1soil·d-1,与以往类似处理的非盐土相当。沙质重盐土和极盐土排放速率分别为中盐土的43%~65%和23%~48%。相反,壤质盐土排放速率极低(0.91~37.1 μg N2O·kg-1 soil·d-1)。盐土高的N2O生产潜力及对氮和质地的强烈依赖性表明盐影响N2O排放主要来源于碳、氮供给限制,而较少受微生物因素的直接影响。

关键词: 叶经济谱, 植物功能型, 功能性状

Abstract: A laboratory incubation was conducted to investigate the N2O emission rates of saline soils collected from the Yellow River Delta of China under different water and N treatments. For the soils with the salinity from ECe = 6.4 mS·cm-1 to ECe = 126.5 mS·cm-1, their N2O emission rates under different water conditions (50% WHC, 80% WHC, and 4 cm water depth) and without N amendment were very low, often below the detection limit. After applying 0.4 mg N·g-1 soil of NH4NO3, the N2O emission rate of sandy moderately saline soil at 50% WHC and at 4 cm water depth was 41.0 μg N2O·kg-1 soil·d-1 and 364.6 μg N2O·kg-1 soil·d-1, respectively, being comparable to that of non-saline soils under the similar conditions, and the N2O emission rate of sandy strongly and extremely saline soils was 43%-65% and 23%-48% of that of sandy moderately saline soil, respectively. By contrast, the N2O emission rate of Namended loamy saline soils was very low, from 0.91 to 37.1 μg N2O·kg-1 soil·d-1. The  high potential of N2O production and its strong dependence on nitrogen amendment and soil texture in saline soils suggested that the effects of soil salinity on N2O emission were mainly controlled by the limitation of C and N supply rather than the microbial factors.

Key words: leaf economics spectrum, plant functional type, functional trait.