北京大气中主要温室气体近10年变化趋势   总被引：16，自引：0，他引：16  

刘强  王跃思  王明星  李晶  刘广仁 《大气科学》2005,29(2):267-271

对1993～2002年10年间北京市大气中三种主要温室气体的监测数据进行分析,研究二氧化碳、甲烷和氧化亚氮这三种温室气体浓度的变化趋势,并初步探讨了造成这种变化的原因.分析结果表明:北京市大气二氧化碳浓度总体是上升趋势,且后5年增长较快;大气甲烷浓度前5年缓慢上升,后5年转为下降,总体已是下降趋势;与大气二氧化碳变化趋势相似,大气氧化亚氮总体也是上升趋势,后5年增长较快.  相似文献   

Phase Equilibria Constraints on Relations of Ore-bearing Intrusionswith Flood Basalts in the Panxi Region, Southwestern China     

ZHANG Zhaochong  HAO Yanli  AI Yu  LI Ying  ZHAO Li 《《地质学报》英文版》2009,83(2)

There are two types of temporally and spatially associated intrusions within the Emeishan large igneous province (LIP); namely, small uitramafic subvolcanic sills that host magmatic Cu-Ni-Platinum Group Element (PGE)-bearing sulfide deposits and large mafic layered intrusions that host giant Ti-V magnetite deposits in the Panxi region. However, except for their coeval ages, the genetic relations between the ore-bearing intrusions and extrusive rocks are poorly understood. Phase equilibria analysis (Q-PI-OI-Opx-Cpx system) has been carried out to elucidate whether ore-bearing Panzhihua, Xinjie and Limahe intrusions are co-magmatic with the picrites and flood basalts (including high-Ti, low-Ti and alkali basalts), respectively. In this system, the parental magma can be classified as silica-undersaturated olivine basalt and silica-saturated tholeiite. The equivalents of the parental magma of the Xinjie and Limahe peridotites and picrites and iow-Ti basalts are silica-undersaturated, whereas the Limahe gabbro-diorites and high-Ti basalts are silica-saturated. In contrast, the Panzhihua intrusion appears to be alkali character. Phase equilibria relations clearly show that the magmas that formed the Panzhihua intrusion and high-Ti basalts cannot be co-magmatic as there is no way to derive one liquid from another by fractional crystallization. On the other hand, the Panzhihua intrusion appears to be related to Permian alkali intrusions in the region, but does not appear to be related to the alkali basalts recognized in the Longzhoushan lava stratigraphy. Comparably, the Limabe intrusion appears to be a genetic relation to the picrites, whereas the Xinjie intrusion may be genetically related to be low-Ti basaits. Additionally, the gabbro-diorites and peridotites of the Limahe intrusion are not co-magmatic, and the former appears to be derived liquid from high-Ti basalts.  相似文献   

Environmental Issues Pertaining to the Kwale Mineral Sands Project,Kenya's South Coast—Reply     

J. Schwarz 《Marine Georesources & Geotechnology》2013,31(2):145-149

Tiomin Resources Inc. (“Tiomin”), the proponent of the Kwale Mineral Sands Project in Kenya, presents a response to the article authored by J. O. Z. Abuodha and P. O. Hayombe, entitled “Protracted Environmental Issues on a Proposed Titanium Minerals Development in Kenya's South Coast”, published in Volume 24, Number 2, April–June 2006. This article contains a series of inaccuracies, some grossly misleading and many statements relate to outdated information. Tiomin is greatly concerned at the publication of such a misleading report and is obliged to state the facts correctly. This response seeks to identify the misrepresentation of statements and/or facts in the article and present a correct and accurate perspective on the environmental issues of the project.  相似文献   

A Review of Study on Fe-C Interaction and Their Adsorption Properties to Soil Heavy Metal     

Zhao Zhuanjun  Yang Yanyan  Pang Yu  Zhao Lifang  Guan Yuli  Zhang Zhaohu 《地球科学进展》2017,32(8):867-874

Nowadays, the Fe-C coprecipitate mechanism is recognized by more and more scholars and becomes the hot topic in the environmental science. On the basis of discussing the interaction between iron oxide and organic matter, and the adsorption research progress of Fe-C complexes on heavy metals, the immobilization potential of Fe-C complexes on heavy metals in polluted soil were illustrated. The surface properties and physical characterizations of iron oxide are changed regularly with the interaction of organic matter, which lead to the higher adsorption capacity of Fe-C complexes in contrast to single iron oxide. Besides, the influences of pH values, organic matter types and surface properties of iron oxides on the adsorption capacity of Fe-C complexes on heavy metals were discussed. The excellent adsorption performance of Fe-C complexes in certain conditions will provide important theoretical basis for contaminated soil remediation.  相似文献   

Global Warming Potential in an Intensive Vegetable Cropping System as Affected by Crop Rotation and Nitrogen Rate   总被引：3，自引：0，他引：3       下载免费PDF全文

Ju Min  Kouping Lu  Haijun Sun  Longlong Xia  Hailin Zhang  Weiming Shi 《洁净——土壤、空气、水》2016,44(7):766-774

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贵州某地玄武岩型氧化铜矿选矿试验研究     

狄永宁  余红林  王莉 《贵州地质》2009,26(1)

对贵州某地的玄武岩型氧化铜矿进行了可选性试验研究.对氧化矿采用的硫化浮选方法经试验不适合本矿,故采用离析浮选.采用离析、一次粗选的试验指标为:铜精矿品位26.70%,铜回收率84.36%.  相似文献   

纳米TiO2分离富集ICP-MS法测定河口环境样品中重金属研究     

黄霄红  卢豪良 《亚热带资源与环境学报》2013,(2):35-40

建立了以纳米二氧化钛（TiO2）作为吸附剂填充微柱,电感耦合等离子体质谱（ICP-MS）法测试Cu^2＋,Cd^2＋,Pb^2＋和Ni^2＋离子的分析方法．考察了不同pH值、洗脱液浓度、样品流速、体积和外源干扰离子的影响,实验结果表明在pH值8～10范围内待测离子可被TiO2定量吸附,2．0molL^-1HNO3可将吸附在微柱上的待测物完全洗脱,优化条件下本方法对溶液中Cu^2＋,Cd^2＋,Ph^2＋和M^2＋离子检出限分别为：0．02,0．01,0．01,0．02μgL～,相对标准偏差小于2％（n=7）,富集系数50倍．对水系沉积物标准物质（GBW07310）的测定值与标准值相一致,方法具有简便、快速,灵敏度高,重现性好的优点,可满足河口水体与沉积物样品中痕量金属元素定量分析的要求．  相似文献   

Preparation of Nano‐Lepidocrocite and an Investigation of Its Ability to Remove a Metal Complex Dye     

Mohsen Sheydaei  Soheil Aber 《洁净——土壤、空气、水》2013,41(9):890-898

Lepidocrocite (γ‐FeOOH) nanoparticles were synthesized from iron(II) sulfate solution and characterized using X‐ray diffraction (XRD), transmission electron microscopy (TEM), Fourier transform‐IR (FT‐IR), nitrogen adsorption, and point of zero charge pH (pH_PZC) analyses. TEM, XRD, and FT‐IR analyses proved the synthesis of nano‐lepidocrocite. Surface area and pH_PZC of the synthesized lepidocrocite were 68.1 m² g^?1 and 4.8, respectively. Utilization of the synthesized lepidocrocite in the adsorption of Lanacron brown S‐GL (LBS‐GL) from aqueous solutions was investigated, and the effect of lepidocrocite dosage, pH, temperature, and contact time on this process were optimized and modeled using response surface methodology approach. The lepidocrocite dosage of 0.015 g, pH 3.5, temperature of 38°C, and contact time of 100 min were determined as optimum adsorption conditions. Isotherm and kinetics of the adsorption process were analyzed at the optimum conditions. The equilibrium data were fitted well to the Langmuir isotherm model. The maximum monolayer adsorption capacity was 528.21 mg g^?1. The adsorption process was described by the pseudo‐second‐order kinetic model. Furthermore, the effect of pH on the desorption of LBS‐GL was investigated. High LBS‐GL desorption efficiency was achieved at a high pH value.  相似文献   

Possible link between new coronavirus variants and atmospheric lightning and seawater intrusion          下载免费PDF全文

Jianping Huang  Yingjie Zhao  Danfeng Wang 《大气和海洋科学快报》2022,15(1):100135

自新型冠状病毒肺炎暴发一年多以来,已经对全球产生深远影响.新型冠状病毒肺炎变异毒株的出现使当前疫情发展充满了不确定性.从这方面出发,我们讨论病毒变异与大气因素之间的联系.根据固氮过程和硝酸盐在人体中的转化过程,我们提出了新型冠状病毒肺炎变异毒株的出现或许和闪电以及海水入侵有联系.我们的研究对新型冠状病毒肺炎变异毒株可能的产生原因提供新的观点.  相似文献   

陈家岭钒矿选矿工艺试验     

李麟  尹进喜  冯艳华 《陕西地质》2012,30(1):82-88

采用钙法氧化焙烧——酸浸的方法从钒矿石中浸出钒,克服了钠化焙烧过程中产生的H2S、Cl2,实验了矿石物料粒度、氧化钙添加量、焙烧温度、焙烧时间、漫出温度、浸出时间、酸的浓度、浸出液固比对浸出率的影响,获得了88％的浸出率。实验表明,焙烧温度、酸的浓度、浸出温度、浸出时间、液固比是影响钒浸出率的重要因素。  相似文献