Measurement of the oxygen dissociation fraction in RF low pressure oxygen/argon plasma using optical emission spectrometry is presented. The oxygen dissociation fraction and its evolutions as functions of operational ...Measurement of the oxygen dissociation fraction in RF low pressure oxygen/argon plasma using optical emission spectrometry is presented. The oxygen dissociation fraction and its evolutions as functions of operational parameters were determined using argon as the actinometer. At a pressure of 30 Pa, the oxygen dissociation fraction decreased from 13.4% to 9.5% as the input power increased from 10 W to 70 W. At an input power of 50 W, the oxygen dissociation fraction decreased from 12.3% to 7.7% when the gas pressure increased from 10 Pa to 40 Pa. The influences of operational parameters on the generation of atomic oxygen were also discussed.展开更多
利用HIDEN公司HPR40溶解气体质谱分析仪,通过实验探索和实际应用,建立了连续走航高频率同时测定海水中O_2、Ar和CO_2等多种气体的分析方法。通过选择硅树脂膜的循环水取样器、进样流量为220 m L/min、进样平衡温度低于海水2℃等实验条件...利用HIDEN公司HPR40溶解气体质谱分析仪,通过实验探索和实际应用,建立了连续走航高频率同时测定海水中O_2、Ar和CO_2等多种气体的分析方法。通过选择硅树脂膜的循环水取样器、进样流量为220 m L/min、进样平衡温度低于海水2℃等实验条件,建立了船载连续走航系统,实现了利用膜进样质谱仪(MIMS)连续走航测定表层海水O_2/Ar比值和p CO_2。所用仪器稳定性良好,连续测定12 h大气鼓泡48 h后的海水样品获得O_2、Ar和CO_2的精密度分别为1.57%、3.75%和2.21%,O_2/Ar的精密度为2.61%;该方法的重复性好,10 d内绘制7条CO_2工作曲线斜率的相对标准偏差RSD=4.18%。应用该方法在南海北部陆坡19.8°N^20.8°N,114.7°E^115°E断面进行调查并取得了很好的效果,结果表明:该调查断面的生物氧过饱和量Δ(O_2/Ar)为0.56%±1.02%,其变化范围为-2.52%至3.34%,调查断面的pCO_2值为361.53±40.46μatm。该方法具有直接、快速、高时空分辨率测定多种溶解气体的优点,为认识多组分气体的高分辨时空分布格局,深入开展我国陆架边缘海生物过饱和氧、海洋群落净生产力和pCO_2动力学研究提供了新方法。展开更多
群落净生产力(Net Community Production,NCP)代表了总初级生产力与群落呼吸的差值,是衡量生物活动对上层海洋碳循环影响的重要指标。O_(2)/Ar比值消除了物理过程对海水中溶解氧(O_(2))饱和度的影响,因此基于生物氧饱和度(ΔO_(2)/Ar)...群落净生产力(Net Community Production,NCP)代表了总初级生产力与群落呼吸的差值,是衡量生物活动对上层海洋碳循环影响的重要指标。O_(2)/Ar比值消除了物理过程对海水中溶解氧(O_(2))饱和度的影响,因此基于生物氧饱和度(ΔO_(2)/Ar)可以估算海洋混合层群落净生产力。本研究于2015年10月,首次利用膜进样质谱法走航获取了黄东海表层海水中高分辨率O_(2)/Ar数据,并估算了其NCP,探讨了其分布特征及影响因素。本航次观测到的Δ(O_(2)/Ar)范围为-30.21%~44.38%,平均值为(0.32±8.29)%,低值主要出现在长江口北侧,而长江口(11.75±13.75)%和浙闽沿岸(5.42±5.21)%的Δ(O_(2)/Ar)明显高于南黄海(-2.62±5.96)%和东海陆架区(-0.79±5.02)%。南黄海和东海陆架区平均NCP为(-9.24±23.15)和(-4.04±18.68)mmol·m^(-2)·d^(-1),总体表现为异养状态,而长江口和浙闽近岸NCP均值分别为(24.49±35.74)和(10.85±12.17)mmol·m^(-2)·d^(-1)。东、黄海NCP的空间分布格局主要受到陆源输入和水团混合的影响,营养盐和光照也是秋季影响NCP分布的重要因素。本研究有助于深入认识高度动态的东、黄海碳循环过程及控制机制。展开更多
基金supported by the Beijing Municipal Education Commission of China(No.KM201010015005)Beijing Key Laboratory of Printing & Packaging Materials and Technology of Beijing Institute of Graphic Communication of China(No.KF201005)
文摘Measurement of the oxygen dissociation fraction in RF low pressure oxygen/argon plasma using optical emission spectrometry is presented. The oxygen dissociation fraction and its evolutions as functions of operational parameters were determined using argon as the actinometer. At a pressure of 30 Pa, the oxygen dissociation fraction decreased from 13.4% to 9.5% as the input power increased from 10 W to 70 W. At an input power of 50 W, the oxygen dissociation fraction decreased from 12.3% to 7.7% when the gas pressure increased from 10 Pa to 40 Pa. The influences of operational parameters on the generation of atomic oxygen were also discussed.
文摘群落净生产力(Net Community Production,NCP)代表了总初级生产力与群落呼吸的差值,是衡量生物活动对上层海洋碳循环影响的重要指标。O_(2)/Ar比值消除了物理过程对海水中溶解氧(O_(2))饱和度的影响,因此基于生物氧饱和度(ΔO_(2)/Ar)可以估算海洋混合层群落净生产力。本研究于2015年10月,首次利用膜进样质谱法走航获取了黄东海表层海水中高分辨率O_(2)/Ar数据,并估算了其NCP,探讨了其分布特征及影响因素。本航次观测到的Δ(O_(2)/Ar)范围为-30.21%~44.38%,平均值为(0.32±8.29)%,低值主要出现在长江口北侧,而长江口(11.75±13.75)%和浙闽沿岸(5.42±5.21)%的Δ(O_(2)/Ar)明显高于南黄海(-2.62±5.96)%和东海陆架区(-0.79±5.02)%。南黄海和东海陆架区平均NCP为(-9.24±23.15)和(-4.04±18.68)mmol·m^(-2)·d^(-1),总体表现为异养状态,而长江口和浙闽近岸NCP均值分别为(24.49±35.74)和(10.85±12.17)mmol·m^(-2)·d^(-1)。东、黄海NCP的空间分布格局主要受到陆源输入和水团混合的影响,营养盐和光照也是秋季影响NCP分布的重要因素。本研究有助于深入认识高度动态的东、黄海碳循环过程及控制机制。
