城市区域大气环境与各天气状况下的辐射特征

以低纬高原城市昆明为研究对象，分析了各种天气状况下城市内，外不同波长辐射的分布特征，变化规律及其差异，得出１．造成城内外差异的主要原因午前是大气污染状况，而在污染程度较小的午后，则是天气状况；２．各波长辐射日总量对午前总量的分配率受大气环境和天气状况的影响，城内外差异十分显著；３．红外和紫外辐射的百分率值均大于大气上界的百分率值，而可见光则反之；各辐射百分率城内外差值午前午后显相反分布。     

细水雾幕衰减热辐射的数值模拟研究

针对现有防火分隔技术的不足,以细水雾幕作为新的防火分隔技术,开展了不同细水雾幕雾特性对衰减热辐射影响的数值模拟研究。通过建立长通道模型,在火源和被保护物体中间设置细水雾幕系统,测量有无细水雾幕及不同细水雾特性条件下被保护侧温度及热辐射强度值,来定性定量研究细水雾幕衰减热辐射的效率。模拟结果表明:细水雾幕可以很好的降低被保护侧空间的温度和热辐射强度;衰减热辐射效率随雾滴粒径的减小,喷雾流量的增大,喷头排数增加而增大;另外,其衰减热辐射效率与喷头布置方式有关,上喷方式明显优于下喷方式。研究结果将对现有防火分隔技术的改善提供帮助和技术支持。     

Characteristics of soil fauna community in the decomposition of Deyeuxia arundinacea litters北大核心CSCD

This study aimed to understand the soil fauna characteristics during the litter decomposition process of perennial herb Deyeuxia arundinacea. The litters were put in 6-, 30-, and 260-mesh litterbags to investigate their mass loss and the dynamics of soil faunal community during Aug. 2013 to Jul. 2014. Faster decomposition rate of Deyeuxia arundinacea in different meshes was found in the early period than in mid- and end-periods. Among different mesh sizes, 6-mesh had the fastest decomposition rate, followed by 30-mesh and 260-mesh. A total of 2218 individuals of soil fauna were obtained in different meshes, with 958, 737 and 523 individuals in 30-, 260- and 6-mesh respectively. Oribatida and Poduridae were the dominant groups, accounting for 73.22% of total individuals. The soil animal individual and group densities shared a very similar trend among the decomposition bags of three aperture sizes, all with obvious characteristics of seasonal dynamic distribution. During the 12 months of decomposition, the density of soil animal groups did not show significant difference between the 6 mesh and 260 mesh decomposition bags except for May. Correlation analysis showed that the group density was highly significantly correlated with average monthly temperature and rainfall, and the individual density significantly correlated with the average monthly temperature. The results indicated that the structure and diversity of soil fauna community of Deyeuxia arundinacea are influenced by hydrothermal conditions. The findings help in understanding the effect of soil fauna to perennial herb litter decomposition.     

Hydrogen peroxide (H2O2) requirement for the oxidation of crude oil in contaminated soils by a modified Fenton's reagent

The oxidation of soil organic matter (SOM) and total petroleum hydrocarbon were investigated in two soils at eight different hydrogen peroxide (H₂O₂) concentrations to determine the optimal H₂O₂ dosage for the efficient remediation of soils contaminated by crude oil with minimal SOM removal. In our study, H₂O₂ concentrations up to 1100 mM increased the SOM destruction up to 10%–15% in the two soils while no improvement of the crude oil removal efficiencies was observed. The results indicate that the destruction of SOM significantly limits the oxidation of crude oil because SOM might consume H₂O₂ more effectively than crude oil at H₂O₂ concentrations above 1100 mM. In addition, H₂O₂ concentrations higher than 1100 mM were not expected for both soils because of the extremely rapid H₂O₂ decomposition, and low H₂O₂ utilization, of both soils.     

Trends of the sunshine duration and diffuse radiation percentage on sunny days in urban agglomerations of China during 1960–2005

The long-term observational data of sunshine duration (SD) and diffuse radiation percentage (defined as diffuse solar radiation/total solar radiation, DRP) on sunny days during 1960–2005 were analyzed in 7 urban agglomerations and the whole of China. The results show that the sunny sunshine duration (SSD) has decreased significantly except at a few stations over northwestern China in the past 46 years. An obvious decrease of the SSD is found in eastern China, with the trend coefficients lower than − 0.8. Accompanied by the SSD decline, the sunny diffuse radiation percentage (SDRP) in most stations shows obvious increasing trends during the 46 years. The averaged SDRP over China has increased 2.33% per decade, while the averaged SSD shows a decrease of − 0.13 hr/day per decade. The correlation coefficient between SDRP and SSD is − 0.88. SSD decreased over urban agglomerations (small to large city clusters) in the past 46 years, especially in large cities and medium cities, due to the strong anthropogenic activities and air pollution represented by aerosol option depth (AOD) and tropospheric column NO₂ (TroNO₂). On the regional scale, SSD has an opposite trend from SDRP during 1960 to 2005, and the variation trends of regional mean values of SSD and SDRP in southeastern China are more pronounced than those in northwestern China.     

废旧金属回收熔炼辐射安全管理研究

介绍了一起废旧金属熔炼导致的放射性污染事件,以及环保部门在事件中采取的措施.反思了废旧金属回收熔炼辐射安全监管存在的问题,指出相关的法律法规不够明确,对熔炼企业辐射监测的监管力度不足,废金属进出口的放射性管理存在漏洞,熔炼企业缺乏辐射安全意识和手段,提出了完善标准体系,强化口岸监测,实施分级管理,加强企业辐射安全管理等对策措施.     

城区中全户内变电站电磁辐射环境影响分析研究

全户内变电站是将主变压器、电容器组、GIS及配电柜等电气设备布置于户内,此类变电站能有效减少电磁波往外辐射,减少对周围环境的电磁辐射影响。某市110 kV广场变电站为典型的城区中全户内变电站,通过电磁环境监测,得出变电站站界工频电场强度测量值范围为1.96 V/m~22.7 V/m,磁感应强度测量值范围为0.03μT~0.22μT,变电站主变一侧围墙外70 m范围内工频电场强度为1.91 V/m~12.8 V/m,磁感应强度为0.02μT~0.22μT。变电站围墙外20 m处0.5 MHz频率下无线电干扰值为35.40 dB(μV/m)。测量结果表明,全户内变电站围墙外的工频电、磁场强度和无线电干扰值远远低于中国环境标准中推荐的居民区的场强限值,即电场4 kV/m,磁感应强度0.1 mT,无线电干扰46 dB(μV/m)。该变电站围墙外的电磁辐射已接近环境本底水平,对周边环境的影响很小。     

Soil organic carbon decomposition and carbon pools in temperate and sub-tropical forests in China

Decomposition of soil organic carbon (SOC) is a critical component of the global carbon cycle, and accurate estimates of SOC decomposition are important for forest carbon modeling and ultimately for decision making relative to carbon sequestration and mitigation of global climate change. We determined the major pools of SOC in four sites representing major forest types in China: temperate forests at Changbai Mountain (CBM) and Qilian Mountain (QLM), and sub-tropical forests at Yujiang (YJ) and Liping (LP) counties. A 90-day laboratory incubation was conducted to measure CO(2) evolution from forest soils from each site, and data from the incubation study were fitted to a three-pool first-order model that separated mineralizable soil organic carbon into active (C(a)), slow (C(s)) and resistant (C(r)) carbon pools. Results indicate that: (1) the rate of SOC decomposition in the sub-tropical zone was faster than that in the temperature zone, (2) The C(a) pool comprised approximately 1-3% of SOC with an average mean residence time (MRT) of 219 days. The C(s) pool comprised approximately 25-65% with an average MRT of 78 yr. The C(r) pool accounted for approximately 35-80% of SOC, (3) The YJ site in the sub-tropical zone had the greatest C(a) pool and the lowest MRT, while the QLM in the temperature zone had the greatest MRT for both the C(a) and C(s) pools. The results suggest a higher capacity for long-term C sequestration as SOC in temperature forests than in sub-tropical forests.     

SNOW AND ICE ALBEDO MEASURED WITH TWO TYPES OF PYRANOMETERS1

ABSTRACT: In order to obtain total short-wave albedos of snow and ice, both incident and reflected solar radiation were measured over a frozen lake surface using two different types of radiation measurement devices: a Kipp and Zonen thermopile pyranometer with a spectral sensitivity of 300 to 2800 nm and a LI-COR photovoltaic pyranometer with a spectral sensitivity of 400 to 1100 am. The spectral response of the LI-COR pyranometers limits its use as a short-wave radiation measurement device. Therefore, two equations were developed to adjust both the daily incident radiation data and the daily reflected radiation data measured by the LI-COR instrument to total short-wave radiation values, i.e., to the waveband of 300 to 2800 nm (visible to near-infrared spectrum). The LI-COR data were then adjusted, and a total short-wave adjusted albedo was calculated with a modeling efficiency of 0.97.