Chen Ji-Ji, Song He, Cao Wen-Chao, Wang Yi-Ran, Wang Jing-Guo
College of Resource and Environment, China Agriculture University, Beijing 100193, China.
College of Agronomy, Anhui Agricultural University, Hefei 230036, China.
Huan Jing Ke Xue. 2018 Aug 8;39(8):3826-3834. doi: 10.13227/j.hjkx.201801017.
To explore the sources of peak nitrous oxide (NO) flushes in solar greenhouse vegetable field, an experiment was conducted with two conventional vegetable soils under different initial volume fractions of oxygen (O) (0%, 1%, 3%, 5%, and 10%). A robotized incubation system was employed to analyze the gas kinetics[O, NO, nitric oxide (NO), nitrogen (N), and carbon dioxide (CO)] every 6 or 8 h and calculate the NO/(NO+NO+N) index. Sodium chlorate (NaClO) was used to inhibit the oxidation of NO to further explore the relationship between NO and nitrite (NO). A parallel off-line incubation in triplicates was conducted under similar conditions to measure the dynamic changes in inorganic nitrogen content[ammonia (NH), nitrate (NO), and NO]. The results showed that NO production under anaerobic condition was significantly higher than that under aerobic condition. The peak value of NO in the soil collected from a straw-added plot (DIS) was significantly higher than that in the soil from non-straw added plot (DI) (<0.01) when the volume fraction of oxygen was ≤ 1%. Oxygen can directly affect NO production by delaying or inhibiting NO reduction, with significant increase in NO production rate under oxygen-depleted condition. However, the Nproduction rate decreased significantly with increase in initial oxygen volume fraction (<0.01). When the initial volume fraction of oxygen was between 1% and 5%, a continuous accumulation of NO was observed during the incubation period, resulting in the significantly higher NO/(NO+NO+N) index than that in either anaerobic or 10% of oxygen treatments. Furthermore, a linear correlation was observed between NO and NO at 5% and 10% of oxygen with the addition of NaClO ( ≥ 0.85). Incomplete denitrification and nitrifier denitrification from NO induction co-occurred in the range of 1% and 5% volume fractions of oxygen, significantly increasing the soil NO production and NO/(NO+NO+N) index. In addition, NO production under anaerobic condition was significantly higher than that under aerobic condition (<0.01).
为探究日光温室菜地氧化亚氮(NO)排放峰值的来源,在两种常规蔬菜土壤中设置了不同初始氧(O)体积分数(0%、1%、3%、5%和10%)进行试验。采用自动化培养系统,每6或8小时分析一次气体动力学[O、NO、一氧化氮(NO)、氮(N)和二氧化碳(CO)],并计算NO/(NO+NO+N)指数。使用氯酸钠(NaClO)抑制NO的氧化,以进一步探究NO与亚硝酸盐(NO)之间的关系。在相似条件下进行了三次平行离线培养,以测量无机氮含量[氨(NH)、硝酸盐(NO)和NO]的动态变化。结果表明,厌氧条件下的NO产生量显著高于好氧条件。当氧体积分数≤1%时,添加秸秆地块(DIS)土壤中的NO峰值显著高于未添加秸秆地块(DI)土壤中的NO峰值(<0.01)。氧气可通过延迟或抑制NO还原直接影响NO产生,缺氧条件下NO产生速率显著增加。然而,随着初始氧体积分数的增加,N产生速率显著降低(<0.01)。当初始氧体积分数在1%至5%之间时,培养期间观察到NO持续积累,导致NO/(NO+NO+N)指数显著高于厌氧或10%氧处理。此外,添加NaClO后,在5%和10%氧条件下,NO与NO之间存在线性相关性(≥0.85)。在1%至5%氧体积分数范围内,同时发生了由NO诱导的不完全反硝化和硝化细菌反硝化,显著增加了土壤NO产生量和NO/(NO+NO+N)指数。此外,厌氧条件下的NO产生量显著高于好氧条件(<0.01)。