紫外吸收光谱法监测硫化氢浓度的实验研究

紫外吸收光谱法是利用不同气体在紫外波段对光具有选择吸收的特性来测量排放烟气中的气体成分和浓度。基于这种方法设计出一套能够实时、在线监测硫化氢的实验装置。在常温常压状态下,通过对测量的一次光谱进行分析,计算出硫化氢的标准吸收截面,选择合适的数据处理方法,减小浓度计算时的误差,可得出硫化氢的实时浓度值。     

九龙山南方铁杉群落物种多样性及乔木种种间联结性

采用物种丰富度指数、Shannon-Weiner指数、Simpson指数、Pielou均匀度指数研究南方铁杉(Tsuga tchekiangensis)群落物种多样性.同时在2×2联列表基础上,应用x2检验、联结系数AC、种间共同出现的百分率PC研究南方铁杉群落19个乔木种群的种间联结性.结果表明:(1)物种丰富度的大小均表现为灌木层大于乔木层,乔木层中物种丰富度为乔木中层>乔木下层>乔木上层.(2)乔木层、乔木层上层和乔木层中层的Shannon-Weiner指数、Simpson指数、Pielou均匀度指数在1 300～1 500 m随海拔升高而增大,在1 500～1 620 m随海拔升高而减小,物种随海拔梯度变化呈现"中间高度膨胀"现象;乔木下层和灌木层则表现为相反规律.(3)x2统计度量值表明,在162个种对中,147对联结关系未达到显著水平,种间的独立性较大;共同出现的百分率PC表明多数种对之间联结程度不显著,南方铁杉、猴头杜鹃(Rhododendron simoarum)、木荷(Schima superba)三者联结是比较紧密的;联结系数AC表明,南方铁杉与厚皮香(Temstroemia gymnanthe)、多脉冬青(Ilexpolyneura)、红花油茶(Camellia chekiang-oleosa)、浙江樟(Cinnamomum chekiangense)、青冈栎(Cyclobalanopsis glauc)等种对存在显著负联结,表明这几个树种对南方铁杉的生长存在重要影响,在营造林工林时应重点加于考虑.     

有机污染物在包气带中迁移转化试验研究

采集一定浓度的有机物废水 ,在试验室内进行了静态吸附、静态降解和动态土柱试验 ,对COD在包气带中迁移转化规律进行研究 ,提出了描述COD在包气带中迁移转化规律的数学模型。结果表明 :包气带对COD的吸附过程是线性的 ,可用亨利吸附模式s =Kdc +s0 表示 ,吸附系数Kd=0 .0 6 93;包气带对COD的降解曲线基本符合一级动力学方程c =c0 e-k1 t,降解系数k1=0 .0 4 99d-1;弥散试验测得弥散系数D =0 .0 0 2 4 2m2 /d。COD在包气带中的迁移转化过程是弥散、吸附、降解等多种作用共同作用的结果。     

What has caused regional income inequality in China? Effects of 10 socioeconomic factors on per capita income

This study analyzes the driving factors behind regional income inequality to provide an important reference for China and other developing countries and to support the formulation of more effective regional development policies. The study used data from 625 county-level administrative units in China in 2017 and conducted a total factor analysis of China's regional income based on 10 economic dimensions using spatially explicit regression methods. The results show that commerce, population footprint, industrialization, and investment are the main factors that affected a Chinese region’s income, but different factors have different degrees of influence in different regions. The impact of economic institutions (developing an institutionally diverse market economy) on income cannot be ignored. Based on our findings, China should give local governments more autonomy, so they can formulate strategies that account for local constraints and opportunities, thereby increasing their chances of decreasing regional income inequality.

     

关于环保、水利行业地表水水质监测工作的比较研究

立足于现实水利部和生态环境部的水资源水环境管理工作,对比两个部门在水质监测、评价工作中的差异,探讨两个部门在水质监测、水质评价工作中的侧重点,研究结果可为水资源的合理开发利用提供一定的决策基础。     

Spatial distribution pattern of degree–day factors of glaciers on the Qinghai–Tibetan Plateau

Glaciers have a very obvious feedback effect on the global water cycle and environmental change. The Qinghai–Tibetan Plateau, also known as the “Water Towers of Asia,” provides an important source of freshwater resources derived from glacial meltwater. Changes in glaciers on the Qinghai–Tibetan Plateau are the most important aspect of the research related to global climate change. Because only a few input parameters are available, the degree–day factor model of glacier mass balance has been widely used on the Qinghai–Tibetan Plateau. Study of the spatial distribution pattern of degree–day factors for glaciers on the Qinghai–Tibetan Plateau and the factors that influence glaciers is important scientifically. The study of degree–day factors is important to the calculation of the glacial grid mass balance on the Qinghai–Tibetan Plateau, and this data can be used in the analysis of the response of glaciers experiencing climate change and for predicting future glacial trends. Through an analysis of the degree–day factors related to 24 glaciers on the Qinghai–Tibetan Plateau, one can conclude that the mean value of glacial degree–day factors on the Qinghai–Tibetan Plateau is 8.14 mm day^?1 °C^?1. The glacial degree–day factor shows a longitudinal zonality with values ranging from high to low from east to west, a latitudinal zonality with values ranging from high to low from south to north, and a vertical zonal regularity along with the change of elevation. The spatial distribution pattern of glacial degree–day factors in the Tibetan Plateau is related to the fact that the climate environment across the Qinghai–Tibetan Plateau is mainly affected by the Indian monsoon, the eastern monsoon, and the westerly winds. The climate gradually changes from cold-humid to warm-humid from northwest to southeast. The single-unit glacier of Qinghai–Tibetan Plateau—the Renlongba Glacier—is located in the southeastern portion of the Qinghai–Tibetan Plateau in a warm and humid climate; its degree–day factor is slightly large, averaging at 6.12 mm day^?1 °C^?1. Mountainous barriers exist in the eastern and western parts of the Renlongba Glacier. On the east side, the degree–day factor is small (5.63 mm day^?1 °C^?1) because of large mountains block weather systems. The glacial tongue is affected by valley wind, contributing to glacial ablation, so the degree–day factor is large on the tongue, averaging at 6.56 mm day^?1 °C^?1. The degree–day factor on the west side of the Renlongba Glacier increases gradually increasing radiation and elevation, presenting a vertical zonal feature. In general, the climate of the Qinghai–Tibetan Plateau is mainly affected by the Indian and eastern monsoons and by westerly winds. In dry and cold climatic conditions, the glacial degree–day factor in the Tibetan Plateau is small, while at warm and humid climate conditions, it is large, with latitudinal, longitudinal, and vertical zonality. In addition, the degree–day factor is also affected by blocking, topography, and other local microclimatic conditions.     

Remediation mechanisms of mercapto-grafted palygorskite for cadmium pollutant in paddy soil

The immobilization agent was the key factor that determined the success of remediation of heavy metal polluted soil. In this study, mercapto-grafted palygorskite (MP) as a novel and efficient immobilization agent was utilized for the remediation of Cd-polluted paddy soil in pot trials, and the remediation mechanisms were investigated in the aspect of soil chemistry and plant physiology with different rice cultivars as model plants. Mercapto-grafted palygorskite at applied doses of 0.1–0.3% could reduce Cd contents of brown rice and straws of different cultivars significantly. Both reduced DTPA-extractable Cd contents in rhizosphere and non-rhizosphere soil and decreasing Cd contents in iron plaques on rice root surfaces confirmed that MP was an efficient immobilization agent for Cd pollutant in paddy soil. In the aspect of soil chemistry, the pH values of rhizosphere and non-rhizosphere soils had no statistical changes in the MP treatment groups, but their zeta potentials decreased obviously, indicating that MP could enhance the fixation or sorption of Cd on soil compositions. In the aspect of antioxidant system, MP could increase POD activity of rice roots significantly to alleviate the stress of Cd to roots, and resulted in the decrease of T-AOC, SOD, and CAT activities of rice roots of the selected cultivars. MP had no inhabitation or enhancement effects on TSH of rice roots but enhance the contents of MTs and NPT to binding Cd to complete detoxification process. MP as a novel and efficient immobilization agent could complete the remediation effects through soil chemistry and plant physiological mechanisms.

     

On the forming mechanism of the cleaning airflow of pulse-jet fabric filters

To reveal the formation mechanism of a pulse-jet airflow’s cleaning effect in a filter bag, a theoretical model is built by using the theory of the gas jet and unitary adiabatic flow according to given specifications and dimensions of the bags and resistance characteristics of the cloth and dust layer. It is about the relationship between cleaning system structure and operating parameters. The model follows the principle that the flow and kinetic energy of jet flow injected into a filter bag should be consistent with the flow of cleaning airflow in the bag and the pressure drop flowing through the filter cloth and dust layer. The purpose of the model is to achieve the peak pressure of cleaning airflow, which dominates the effect of the pulse-jet cleaning process. The cleaning system structure includes air pressure in the nozzle, structure and size of nozzle, exit velocity of nozzle, jet distance, and diameter of jet cross section. Based on the condition of the cleaning system structure and operating parameters established by using the theoretical model, Fluent software is applied to carry out a numerical simulation of the jet airflow field at the nozzle’s outlet, jet airflow field between nozzle and bag top, and cleaning airflow field in the filter bag. Experimental results are used to verify the reliability of the theoretical model. They are obtained in a pilot-scale test filter with a single bag, with length 2 m and in general full-scale dimensions of the cleaning system. The results show that when any rectification measure is not installed at the bag opening, the cross-sectional area covered by the jet gas is hardly sufficient to cover the entire area of the bag opening. A large portion of the gases injected into the filter bag will overflow reversely upward from the edge due to pressure differences between the upper area and lower area inside the bag opening. This led to a serious shortage of the cleaning airflow and ar limited increase in static pressure. When a venturi-type rectifier tube is installed at the bag opening, the jet flow is converted to funnel flow for which the cross-section velocity distribution is more uniform at the throat of the rectifier tube due to the guided effects of the upper tapered pipe. Then it is transited to stressful flow below the bag opening via rectified effects of the lower dilated pipe. The results show that the gap between the static pressure of gas in the bag and the expected value is significantly reduced. The theoretical value of the nozzle diameter is enlarged to compensate for two aspects of adverse effects of cleaning airflow and energy. This is because the flow is not a purely free-form jet from the nozzle to the entrance of the rectifier tube and because the gas suffers from local resistance while flowing through the rectifier tube. The numerical simulation and experiment show that the peak pressure of cleaning airflow in the filter bag is able to reach the expected value. The results confirm that the mechanism of the pulse-jet cleaning airflow and the calculation method of the pulse-jet cleaning system structure and operating parameters offered in this study are correct. The study results provide a scientific basis for designing the system of pulse-jet fabric filters.

Implications: Pulse-jet cleaned fabric filters are commonly used for air pollution control in many industries. Pulse-jet cleaning is widely used for this purpose as it enables frequent cleaning while the filter is operating. However, the theoretical system of the forming mechanism of the pulse-jet cleaning has not formed so far. This indicates the theoretical model plays an important role in designing effective pulse-jet cleaned fabric filters.     

生产企业及周边环境中全氟化合物的污染特征

生产企业作为全氟化合物(perfluorinated compounds,PFCs)的直接来源地,现今被认为是PFCs污染的主要来源之一,同时其对周边环境具有更加直接而重大的影响。我国对生产企业周边环境中PFCs污染特性研究的报道较缺乏,补充丰富各地生产企业周边环境的PFCs污染特征,可为PFCs点源分析和污染溯源提供依据。以湖北省孝昌县某化工有限公司为典型生产企业,采集7个采样点的水体和土壤样品,分析典型地区环境介质中PFCs的污染现状与特征。结果显示,11种目标PFCs污染物在水体中有7种、土壤中有6种不同程度地检出,环境水体中PFCs的总浓度介于4.70~40.22μg·L-1,土壤中PFCs的总浓度介于58.22~2 075.60 ng·g-1之间。全氟辛基磺酸(PFOS)为典型行业周边水体和土壤中最主要的PFCs污染物,其次是水体中的全氟己基磺酸钾(PFHx S)、全氟丁烷磺酸钾(PFBS)和土壤中的全氟辛酸(PFOA)、全氟己基磺酸钾(PFHx S)。PFCs检出浓度的大小与采样点距典型企业的距离极其相关,距离与污染物总量之间呈显著负相关性,但周边环境中PFCs的种类和构成比,不受与点源之间距离的影响。     

Characterization and speciation of mercury in mosses and lichens from the high-altitude Tibetan Plateau

The accumulation and species of mercury (Hg) in mosses and lichens collected from high-altitude Tibetan Plateau were studied. The altitudes of the sampling sites spanned from 1983 to 5147 m, and a total of 130 mosses and 52 lichens were analyzed. The total mercury (THg) contents in mosses and lichens were in the ranges of 13.1–273.0 and 20.2–345.9 ng/g, respectively. The average ratios of methylmercury (MeHg) in THg in mosses and lichens were 2.4 % (0.3–11.1 %) and 2.7 % (0.4–9.6 %), respectively, which were higher than those values reported in other regions. The contents of THg in both mosses and lichens were not correlated with the THg in soils (p > 0.05). The lipid contents displayed a significantly positive correlation with concentrations of MeHg in mosses (r = 0.461, p < 0.01, n = 90), but not in lichens. The correlations between Hg contents in mosses and the altitudes, latitudes and longitudes of sampling sites indicated the mountain trapping and spatial deposition of Hg in the Tibetan Plateau.