Cooperative analysis of infrastructure perfection and residents’ living standards in poverty-stricken counties in Qinghai Province

Environment, Development and Sustainability - The western region of China has always been the main battlefield for poverty alleviation. It is essential to explore the interaction mechanism between...     

湿法回收砷碱渣中锑的工艺研究

本研究先以水浸实现砷碱渣中的砷锑分离,再对水浸渣进行盐酸浸出,得到了可作为工业原料氯化锑溶液.研究结果表明,在液固比为6∶1,温度40℃,浸出时间40 min的条件下,可使水浸过程中锑的浸出率低于3%,砷的浸出率达到99%;盐酸浸出中,控制酸浓度为1∶1,液固比10∶1,温度60℃,浸出时间30 min,能使锑的浸出率达到88%以上.经过水浸和盐酸浸出,锑的直接回收率为85.36%.     

水体表面微层中酞酸酯的光降解研究

研究了水体表面微层中酞酸酯化合物光降解的动力学,指出光催化降解符合一级动力学过程,实验证明：催化剂ＴｉＯ２为２ｇ．ｌ＾－１,ｐＨ为６,并有Ｈ２Ｏ２存在时,是ＤＢＰ,ＤＥＨＰ光降解的最佳条件,溶解氧增加有利于光降解,实际表面微层水样的光催化降解速率比模拟水样快。     

云南墨江金矿床成矿作用探讨

云南墨江金矿床位于“三江”褶皱带哀牢山板块结合带北段的墨江 -九甲断裂带中。矿体分布于金厂超基性岩体西侧的金厂组烂山段含火山物质的硅质岩、变余粉砂岩和板岩中 ,矿体由含金石英脉、含金硅质岩组成 ,金矿体受层位和岩性控制。在矿区还分布晚于金矿化形成的镍矿体。金镍矿体共同存在于同一矿区 ,矿区围岩蚀变种类多 ,与金矿化有关的围岩蚀变主要有硅化、黄铁矿化等。矿体的空间分布与穿插关系表明 ,金成矿作用开始于晚三叠世以前。含金硅质岩具有沉积作用形成的地质特征 ,其稀土元素、氧、硅同位素地球化学特征与热水沉积作用形成的硅质岩一致 ;含金石英脉的矿物组成、结构和构造特征、稀土元素、硅同位素、微量元素组成与含金硅质岩相似 ,可能与硅质岩具有相似物质来源或形成作用。金矿石中金与镍、铬等元素的相关性很低。推断金矿床成矿作用可能开始于中石炭世含金硅质岩的热水沉积作用 ,在早三叠世以前 ,成矿热液通过充填和交代作用在硅质岩和上部的岩石中形成含金石英脉。后来的区域变质作用、超基性岩自变质作用及镍矿化作用可能使金矿体的金含量提高 ,但没有产生具有工业意义的独立金矿化。     

有机膨润土吸附对硝基苯酚的性能及其在水处理中的应用初探

分别用溴化十六烷基三甲铵（ＣＴＭＡＢ）和氯化十六烷基吡啶（ＣＰＣ）改性膨润土，研究了制备有机膨润土的适宜条件及其对吸附对对硝基苯酚性能的影响。２５℃时，ＣＴＭＢ－膨润土和ＣＰＣ－膨润土对对硝基苯酚的饱和吸附量分别为４７５ｍｇ／ｇ，远大于原土的饱和吸附量（１２５ｍｇ／ｇ）。ｐＨ〉７时，有机膨润土吸附处理对硝基苯酚的去除率都在８５％以上，比原土的去除率（８．６％）大９倍，通过Ｘ－衍射、红外光谱分析、比     

Performance, microbial community and inhibition kinetics of long-term Cu2+ stress on an air-lift nitritation reactor with self-recirculation

Biological nitrogen removal process could be affected due to the presence of heavy metals owing to their toxicity and accumulation in the sludge.In this study,the impact of Cu~(2+)shock on a long-term nitritation operation was investigated in an air-lift reactor with selfrecirculation.Both the dynamics of microbial community and inhibition kinetics under Cu~(2+) stress were ascertained.The results showed that Cu~(2+) exerted severe inhibition on nitritation performance of an air-lift reactor(ALR) at 25 mg/L.The corresponding NH_4~+-N removal efficiency decreased to below 50%,which was mainly due to the variation of microbial community structure,especially the inhibition of nitrifiers like Nitrosomonas(the relative abundance decreased from 30% to 1% after Cu~(2+)inhibition).Kinetic parameters were obtained and compared after fitting the Haldane model.The long-term Cu~(2+) stress on the ALR aggravated the ammonium affinity and the resistance to substrate self-inhibition of the nitritation sludge,but reduced the resistance to Cu~(2+) inhibition.Furthermore,Cu~(2+)acted as uncompetitive inhibitor on nitritation process.Our results provide new insights into the nitritation characteristics under long-term Cu~(2+) stress.     

桂林市酸雨污染特征及防治对策研究

为促进桂林市酸雨污染防控,利用2013—2017年桂林市3个监测站点采集的共1 147个降雨样品,分析了降雨pH、电导率和水溶性离子成分,结合气态污染物的变化特征和气象因素影响分析,探讨了桂林市酸雨污染成因,并提出了桂林市酸雨污染防治对策建议.结果表明:①2013—2017年桂林市降雨的pH年均值范围为4.85~5.23.酸雨频率范围为42.5%~74.9%,2017年酸雨频率达74.9%.虽然近年来桂林市环境空气质量明显改善,但是酸雨污染却没有明显减轻,反而在2015年后出现恶化.降雨的离子组成中,SO₄2-和NO₃-是主要的阴离子成分,分别占总离子当量浓度的28.19%和10.82%;Ca2+和NH₄+是主要的阳离子成分,分别占总离子当量浓度的23.46%和17.64%.酸中和效应分析显示,Ca2+和NH₄+为降雨中主要的中和物质.②降雨中碱性离子当量浓度的降幅比酸性离子当量浓度的降幅大,这是导致桂林市近年酸雨恶化的重要因素;此外,来自西部和东南部方向的气流对应了较高的降雨酸度和总离子当量浓度,因此污染物的远距离传输对降雨酸度和离子当量浓度也有一定影响.研究显示,桂林市SO₂和NO_x排放的持续管控将有利于酸雨污染防治,但桂林市目前实施的削减大气粗颗粒物和NH₃排放的大气污染控制策略对于降雨酸度的影响还需要开展进一步评估.      

Preface

正Air pollution as well as climate change and their possible effects on the environment,ecosystems and human health,are pressing challenges.Nowadays,it is clear that sustainable societal development cannot remain solely wealth-oriented,but must take into account the present and future environmental issues.However,this approach is possible only if scientifically sound knowledge in all environmental areas becomes available to our societies and decision makers,which requires a firm     

2007—2014年北京地区PM2.5质量浓度变化特征

为更好地解析北京地区ρ(PM_2.5)的长期变化特征及气流轨迹聚类分析结果,对2007年8月—2014年7月在中国环境科学研究院实测的ρ(PM_2.5)数据进行了统计分析,分析其年际、季节和月际变化特征;通过计算PM_2.5的AQI分指数,分析了污染等级的时间变化特征;结合后向气流轨迹,对ρ(PM_2.5)年际、季节变化与气团来源的关系进行了分析.结果表明:北京地区2008—2013年ρ(PM_2.5)年均值分别为111.5、95.8、94.8、80.5、75.2、81.3 μg/m3,整体呈逐年下降趋势,但污染水平依然较高;ρ(PM_2.5)由高到低的季节次序为秋季、冬季、春季、夏季,平均值分别为111.6、94.8、77.2、70.5 μg/m3,PM_2.5重污染时段主要出现在秋冬季节,并且冬季ρ(PM_2.5)近年来逐渐呈上升趋势;ρ(PM_2.5)月均值呈单峰型变化,11月最高(为125.3 μg/m3),7月最低(为76.4 μg/m3);轨迹聚类分析发现,途经山西省北部和河北省南部的气流轨迹中ρ(PM_2.5)较高,而来自北方及西北方向的气团相对较清洁,ρ(PM_2.5)较低.北京地区近些年实施的大气污染减排措施对于控制PM_2.5污染取得了一定效果,但针对秋冬季节重污染过程的控制力度仍需要加强,同时也要注意区域污染传输对北京地区ρ(PM_2.5)的影响.      

The gap report of global climate change mitigation,finance, and governance after the United States declared its withdrawal from the Paris Agreement

On 1 June 2017, the US President Donald Trump officially announced the withdrawal from the Paris Agreement, thus the study on the reasons of withdrawal, the potential impacts, and coping strategies has become a focus among policy circles and of the international community. Based on the self-developed US Policy Assessment Model, this paper systematically evaluates the three potential “major deficits” in terms of mitigation, climate finance, and global climate governance, as a result of the US withdrawal from the Paris Agreement and puts forward policy suggestions for coping with such transformations accordingly. The study shows that the United States ’withdrawal from the Paris Agreement will affect the existence and implementation of successive climate policies and result in an additional 8.8–13.4% increase in the global emissions reduction deficit. The United States’ withdrawal will also deteriorate the existing climate finance mechanism. The Green Climate Fund (GCF)’s funding gap will increase by US$2 billion, while the gap of long-term climate finance will increase by about US$5 billion a year. Either the China–EU or the “BASIC plus” mechanism could fill the governance deficit caused by the United States and the lack of political momentum may continue for a while in the future.