Zhang Rui, Yang Xiao-Di, Geng Jin-Ju, Hong Yu-Ning, Gu Xue-Yuan, Wang Xiao-Rong, Wang Rui, Zhu Jian-Guo
School of Chemistry and Environmental Science, Nanjing Normal University, Nanjing 210097, China
Huan Jing Ke Xue. 2009 Sep 15;30(9):2694-700.
Phosphine, a trace gas, has been proved to commonly exist in environment. Under free air carbon dioxide enrichment (FACE) condition, the phosphine fluxes were investigated on the function of different nitrogen fertilizer application, NN (normal N, 250 kg/hm2) and LN (low N, 125 kg/hm2). Results showed that phosphine fluxes and concentrations in flourishing stages, both tillering stage and elongation stage, were higher than in slowly growing stages. The highest phosphine flux of (155.2 +/- 22.71) ng/(m2 x h) was observed in tillering stage in NN zone of the FACE area. The highest average phosphine flux of (41.72 +/- 7.006) ng/(m2 x h) was observed in NN zone of FACE area, while the lowest average phosphine flux of (- 1.485 +/- 6.229) ng/(m2 x h) could be detected in LN zone of the ambient area. CO2 enrichment can obviously improve the phospine emission. The nitrogen fertilizing level doesn't play an important role in phosphine emission. Both net fluxes and concentrations of phosphine had obviously positive correlation with temperature. A one-day phosphine flux and concentration experiment was carried out in ripening stage. The result showed that light was the prominent factor influencing phosphine concentration in daytime.
磷化氢作为一种痕量气体,已被证明在环境中普遍存在。在自由空气二氧化碳富集(FACE)条件下,研究了不同氮肥施用量(正常施氮量NN为250 kg/hm²和低施氮量LN为125 kg/hm²)对磷化氢通量的影响。结果表明,在分蘖期和拔节期等生长旺盛阶段,磷化氢通量和浓度高于生长缓慢阶段。在FACE试验区NN区的分蘖期观测到最高磷化氢通量为(155.2±22.71) ng/(m²·h)。在FACE试验区NN区观测到最高平均磷化氢通量为(41.72±7.006) ng/(m²·h),而在对照区LN区可检测到最低平均磷化氢通量为(-1.485±6.229) ng/(m²·h)。二氧化碳富集能明显提高磷化氢排放。氮肥施用量对磷化氢排放不起重要作用。磷化氢的净通量和浓度均与温度呈明显正相关。在成熟期进行了为期一天的磷化氢通量和浓度试验。结果表明,光照是影响白天磷化氢浓度的主要因素。