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The relationship of N2O distributions with the Arctic vortex breakup is first analyzed with a probability distribution function (PDF) analysis. The N2O concentration shows different distributions between the early and late vortex breakup years. In the early breakup years, the N2O concentration shows low values and large dispersions after the vortex breakup, which is related to the inhomogeneity in the vertical advection in the middle and high latitude lower stratosphere. The horizontal diffusion coefficient (Kyy) shows a larger value accordingly. In the late breakup years, the N2O concentration shows high values and more uniform distributions than in the early years after the vortex breakup, with a smaller vertical advection and Kyy after the vortex breakup. It is found that the N2O distributions are largely affected by the Arctic vortex breakup time but the dynamically defined vortex breakup time is not the only factor. 相似文献
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The localization of nitric oxide synthases (NOS) is dealed with in the developing gonads of amphioxus Branchiostoma belcheri tsingtauense. It was found by NADPH-diaphorase staining that (1) NOS activity was present in the nuclear membranes of germinal vesicles during the entire period ofoocyte development; (2) NOS was localized in both the nuclear membranes and the perinuclear region of cytoplasm in the vitellogenetic oocytes; (3) NOS was relocated in the cortical layer in the mature egg; (4) NOS activity was present in spermatocytes, but not in the spermatogonia in the middle of October; (5) NOS was detected in both spermatozoa and spermatids as well as spermatocytes during the breeding season. This is the first report on the distribution pattern of NOS in the developing gonads in protochordates. These results suggest a role for NOS in the functioning of the nuclear membranes and yolk synthesis during oogenesis and in cell division and differentiation during spermatogenesis. 相似文献
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龙凤山大气近地层O3浓度变化及与其它因素的关系 总被引:16,自引:0,他引:16
研究首次在龙凤山区域大气本底站测得的地面O3浓度及其变化的资料表明,中国东北农村地面大气O3浓度总体水平不很高,但在少数特殊的天气条件下,时均浓度可超过国家二级标准。O3浓度存在明显的季节和日变化,其月平均浓度1995年1月最低(27.5ppb),1994年11月最高(43.2ppb)。O3日变化幅度夏季的晴天最大(28ppb),冬季的阴天最小(8ppb)。气象要素(尤其是风速、气温和相对湿度等)和NOx与地面O3浓度有较密切的关系。用多变量分析法探讨了地面O3各指标随气象因子和NOx共同变化的规律,并拟合了寒冷和温暖期里与地面O3日最高浓度、日最低浓度及日变化幅度有关的方程。 相似文献
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Experiments on the effects of nitric oxide (NO) and iron on the growth of marine microalgae Skeletonema costatum were conducted. The results are as follows: exogenous NO could increase the growth rate of marine algae and raise the biomass remarkably under iron-deficient conditions. But it was a complicated process that the phytoplankton growth was influenced by NO and iron, which was controlled by the NO concentration, the nutrition level of the culture medium and the iron concentration, etc. Meanwhile, the iron concentration in the medium also has a direct influence on the growth and NO release capacity of the algae. Therefore, the effects of NO and iron on the growth of marine phytoplankton were mutual. 相似文献
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影响SO2和NOx气相化学转化率的敏感因子分析 总被引:4,自引:0,他引:4
在一个已建立的简化的气相化学模式基础上,本文估算了SO2和NOX的气相化学转化率,进一步研究了影响转化率的敏感因子。结果表明:在典型的大气污染状况和晴天无云的条件下,白天SO2和NOX的平均转化率分别为1.5%/h和13.8/h,大气温度,太阳高度,水汽混合比以及云厚,云量,云中液态水含量等云物理参数都会对转化率产生不同程度的影响。 相似文献
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Quick measurement of CH<Subscript>4</Subscript>, CO<Subscript>2</Subscript> and N<Subscript>2</Subscript>O emissions from a short-plant ecosystem 总被引:43,自引:0,他引:43
Combining improved injector, gas line and valve-driving models, a gas chromatograph (GC) equipped with Hydrogen Flame Ionization Detector (FID) and Electron Capture Detector (ECD), can measure CH4, CO2, and N2O simultaneously in an air sample in four minutes. Test results show that the system has high sensitivity, resolution, and precision; the linear response range of the system meets the requirement of flux measurements in situ. The system is suitable for monitoring fluxes of the main greenhouse gases in a short-plant field since it is easy to use, efficacious, and constant and reliable in collecting data. 相似文献
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Effects of Irrigation on Nitrous Oxide, Methane and Carbon Dioxide Fluxes in an Inner Mongolian Steppe 总被引:2,自引:0,他引:2
LIU Chunyan Jirko HOLST Nicolas BRUGGEMANN Klaus BUTTERBACH-BAHL YAO Zhisheng HAN Shenghui HAN Xingguo ZHENG Xunhua 《大气科学进展》2008,25(5):748-756
Increased precipitation during the vegetation periods was observed in and further predicted for Inner Mongolia. The changes in the associated soil moisture may affect the biosphere-atmosphere exchange of greenhouse gases. Therefore, we set up an irrigation experiment with one watered (W) and one unwatered plot (UW) at a winter-grazed Leymus chinensis-steppe site in the Xilin River catchment, Inner Mongolia. UW only received the natural precipitation of 2005 (129 mm), whereas W was additionally watered after the precipitation data of 1998 (in total 427 mm). In the 3-hour resolution, we determined nitrous oxide (N20), methane (CH4) and carbon dioxide (CO2) fluxes at both plots between May and September 2005, using a fully automated, chamber-based measuring system. N20 fluxes in the steppe were very low, with mean emissions (±s.e.) of 0.9-4-0.5 and 0.7-4-0.5 μg N m^-2 h^-1 at W and UW, respectively. The steppe soil always served as a CH4 sink, with mean fluxes of -24.1-4-3.9 and -31.1-4- 5.3 μg C m^-2 h^-1 at W and UW. Nighttime mean CO2 emissions were 82.6±8.7 and 26.3±1.7 mg C m^-2 h^-1 at W and UW, respectively, coinciding with an almost doubled aboveground plant biomass at W. Our results indicate that the ecosystem CO2 respiration responded sensitively to increased water input during the vegetation period, whereas the effects on CH4 and N2O fluxes were weak, most likely due to the high evapotranspiration and the lack of substrate for N2O producing processes. Based on our results, we hypothesize that with the gradual increase of summertime precipitation in Inner Mongolia, ecosystem CO2 respiration will be enhanced and CH4 uptake by the steppe soils will be lightly inhibited. 相似文献
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三种主要的温室气体-CO2、CHR和N2O-在大气中日益升高的浓度总共占所预期的全球变暖效应的约70%,但是对于其中的任何一种气体来说,生产-消耗预算都是不平衡的。积雪可覆盖北半球陆地面积的44% ̄53%,并且在高山及亚高山区,可以有好几米深的积雪厚度持续半年多。大多数微量气体预算假定:当土壤被积雪覆盖或土壤温度降至约0℃时,微量气体交换便会停止。因此,通常认为高山及亚高山区土壤是大气CO2的总汇 相似文献
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