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Ammonia flux and dry deposition velocity from near-surface concentration gradient measurements over a grass surface in North Carolina

机译:北卡罗莱纳州草地表面近地表浓度梯度测量得出的氨通量和干沉降速度

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Atmospheric ammonia concentrations were measured during fall 2001, winter, spring, and summer 2002 over natural surfaces in North Carolina where animal farms and waste storage and treatment lagoons (which are known to emit ammonia) at two heights (2 and 6 m) above the surface employing an arrangement of two Thermo Environmental Instruments, Inc. Model 17C chemiluminescent nitrogen oxides (NO_X)―ammonia (NH_3) analyzers along with a solenoid for each analyzer to alternate measurements between the two elevations. Simultaneously, mean winds and temperatures are also measured at the same two heights. The micrometeorological gradient method is used in conjunction with the Monin-Obukhov similarity theory, to estimate the vertical flux and dry deposition velocity of ammonia under different meteorological conditions. Diurnal and seasonal variations of ammonia flux and dry deposition velocity were investigated under a wide range of wind and atmospheric stability conditions yielding hourly variation of NH_3 fluxes and deposition during each seasonal campaign. Fall average NH_3 concentrations were generally the highest with daytime concentrations of 7.60 +- 6.54 μg m~(-3) at 2 m, while nighttime NH_3 concentrations were 7.25 +- 6.14 μg m~(-3) at 2 m. The winter season had the lowest overall concentrations collected during each seasonal campaign with averages of 1.73 +- 2.00 μg m~(-3) (2m) during daytime and 1.37 +- 1.50 μg m~(-3) (2 m) during nighttime. Deposition and emission occur, both on daily and seasonal scales. Summer measurements yielded the largest average daytime deposition velocity of 3.94 +- 2.79 cm s~(-1), whereas winter measurements gave the lowest daytime velocities with an average of 2.41 +- 1.92 cm s~(-1). The largest nighttime deposition velocities were estimated during the summer season with an average of 0.76 +- 1.69 cm s~(-1), whereas fall nighttime deposition velocities were considerably lower at 0.07 +- 0.17 cm s~(-1). Regression relationships between the ammonia deposition velocity and the friction velocity are obtained for different stability conditions.
机译:在2001年秋季,冬季,春季和2002年夏季在北卡罗来纳州的自然表面上测量了大气中的氨浓度,那里的动物农场以及废物储存和处理泻湖(已知会排放出氨水)位于海拔两个高度(2和6 m)上。使用两个Thermo Environmental Instruments,Inc.布置的表面。型号为17C的化学发光氮氧化物(NO_X)-氨(NH_3)分析仪以及每个分析仪的螺线管,用于在两个标高之间交替测量。同时,在相同的两个高度也测量平均风和温度。结合Monin-Obukhov相似性理论,采用微气象梯度法,估算了不同气象条件下氨的垂直通量和干沉降速度。在广泛的风和大气稳定条件下,研究了氨通量和干沉降速度的每日和季节性变化,从而在每个季节性运动期间产生了每小时NH_3通量和沉降的每小时变化。秋季平均NH_3浓度最高,白天为2 m时为7.60±6.54μgm〜(-3),而夜间NH_3浓度为2 m时为7.25±6.14μgm〜(-3)。冬季是每个季节运动中收集的最低总浓度,白天平均为1.73 +-2.00μgm〜(-3)(2m),夜间平均为1.37 +-1.50μgm〜(-3)(2 m) 。沉积和排放均在每日和季节性范围内发生。夏季测量得出的最大日间平均沉积速度为3.94±2.79 cm s〜(-1),而冬季测量得出的日间速度最低,平均为2.41±1.92 cm s〜(-1)。夏季最大的夜间沉积速度估计为平均0.76±1.69 cm s〜(-1),而秋季夜间沉积速度则低得多,为0.07±0.17 cm s〜(-1)。对于不同的稳定性条件,获得了氨沉积速度与摩擦速度之间的回归关系。

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