岩石吸留烃气相色谱快速检测技术及其应用研究

在油气勘探有机地化实验室中 ,岩石中全烃制备分析方法主要有“岩石氯仿抽提物及气相色谱分析技术”、“岩石热解气相色谱分析技术”等 ,而这些技术都存在操作烦琐、不适合钻井现场分析等缺陷 ,而新开发的岩石吸留烃气相色谱快速检测技术 ,就是利用气相色谱仪特点研制出解吸装置及技术 ,省去了实验室中繁杂的烃类制备过程 ,直接进岩样测定岩石中吸留烃C3—C4 0单体烃化合物。本方法不仅适合实验室岩石中全烃分析 ,更适合现场分析 ,在柴达木盆地某深探井现场地化录井及识别真假油显示的实际应用效果好 ,是油气地球化学勘探的一种新方法。     

原油中芳烃及其碳稳定同位素组成特征

芳烃作为原油的主要组分之一,蕴含丰富的地球化学信息,常用原油中芳烃的分布及其碳稳定同位素组成来评价原油的有机质来源和热成熟度等指标。为了补充油品化学指纹的基础鉴别指标和数据,找出适用于油样鉴别的芳烃地球化学指标以及碳稳定同位素组成,本文主要测定了来自不同地区七种原油芳香烃组分的相对含量以及碳稳定同位素组成,并计算分析了甲基萘比值（MNR）、二甲基萘比值（DNR）、三甲基萘比值（TNR）、甲基菲比值（MPR）、甲基菲指数（MPI1）和甲基菲分馏系数（MPDF）等常见的芳烃特征比值。从原油中芳烃组分相对含量分布来看,七种原油均显示出了各自的特点;从原油芳烃的特征比值来看,成熟度参数（MNR、TNR1、TNR2、MPR、MPI1、MPDF1和MPDF2）均反映出所有原油的高成熟度,其它芳烃参数如DNR1、DNR2和TNR4等比值反映原油的母质来源及生物降解等信息,由芳烃特征比值的单因素方差分析（ANOVA）结果可知,与成熟度参数MNR和MPI1相比,DNR1、DNR2和TNR4在不同原油间的差异更加明显;从原油芳烃碳稳定同位素组成来看,不同地区原油间差别较大,其中巴西原油最富集13C,阿曼原油和委内瑞拉原油最亏损13C,二甲基萘和菲的碳稳定同位素组成在不同油样间的差异最明显。将显著性差异大的芳烃参数与芳烃δ13C值联用,结果表明,该方法可以更加有效区分七种原油。最后使用主成分分析方法分析原油芳烃碳稳定同位素组成,七种原油显示出各自不同的碳稳定同位素组成特征和明显的区分效果,利用不同油样芳烃的碳稳定同位素组成差异可实现对油样来源的鉴别。     

The dri thermal/optical reflectance carbon analysis system: description,evaluation and applications in U.S. Air quality studies

The thermal/optical reflectance method of carbon analysis developed by Huntzicker et al. (in Particulate Carbon, Atmospheric Life Cycle, edited by Wolff G. T. and Klimisch R. L., pp. 79–88, Plenum Press, New York, 1982) has been adapted by several laboratories for the quantification of organic and elemental carbon on quartz-fiber filter deposits. While the principle used by these laboratories is identical to that of Huntzicker et al., the details differ with respect to calibration standards, analysis time, temperature ramping and volatilization/combustion temperatures. This paper reports a variation on this method which has been applied to over 27,000 samples taken in more than a dozen urban and regional air quality studies in the U.S.A. In this variation, a 0.5 cm² punch from a dozen urban and regional air quality studies in 120, 250, 450 and 550°C in a pure helium atmosphere, then to combustion at temperatures of 550, 700 and 800°C in a 2% oxygen and 98% helium atmosphere. The carbon which evolves at each temperature is converted to methane and quantified with a flame ionization detector. The seven separate carbon fractions facilitate evaluation of the method and increase the information content concerning the samples.The reflectance from the deposit side of the filter punch is monitored throughout the analysis. This reflectance usually decreases during volatilization in the helium atmosphere owing to the pyrolysis of organic material. When oxygen is added, the reflectance increases as the light-absorbing carbon is combusted and removed. Organic carbon is defined as that which evolves prior to re-attainment of the original reflectance, and elemental carbon is defined as that which evolves after the original reflectance has been attained. By this definition, “organic carbon” is actually organic carbon that does not absorb light at the wavelength used (632.8 nm) and “elemental carbon” is light-absorbing organic and elemental carbon. Assumptions underlying the procedure are discussed, as well as comparisons with other methods and recommendations for further work.     

硝酸盐电子受体反硝化同时除磷试验分析

经研究发现AAA SBR系统中的活性污泥可以利用硝酸盐作为电子受体进行缺氧吸磷并同时发生反硝化脱氮。试验利用“双泥”系统进一步探讨了污水生物反硝化同时除磷的可能性,结果表明 :“双泥”系统的“双重”吸磷以及内碳源反硝化除磷方式可以使生物处理出水磷酸盐浓度趋近于零,TP≤ 0 2 3mg L、NH3 N≤ 0 5mg L、TN≤ 8mg L、CODCr≤2 5mg L。     

山东半岛南部近海表层沉积物中脂类生物标志物的组成及形态分析

分析了山东半岛南部近海表层沉积物中游离态和碱不稳定结合态脂类物质的组成,结果显示:脂肪酸呈现以16∶0为主峰的单峰形分布趋势,具明显偶碳优势,海源为其主要来源,脂肪酸主要以结合态形式存在,不同类别的脂肪酸形态分布略有差异,脂肪酸的结构和来源是影响脂肪酸形态分布的重要因素;同样以海源为主的甾醇则主要以游离态形式存在,但陆源甾醇的结合态比重相对较高;烷烃呈现以C29烷烃为主峰的单峰形分布趋势,陆源输入是其主要来源;烷烃主要以游离态形式存在,且UCM(不可分辨成分)峰仅出现在游离态烷烃的气相色谱图中。     

济阳坳陷石炭二叠系烃源岩有机地球化学特征

济阳坳陷石炭二叠系烃源岩主要为煤和暗色泥岩。本文从有机质丰度、有机质类型及成熟度三方面对烃源岩有机地球化学特征做了详细分析。分析结果如下:有机质丰度普遍较高,煤的TOC含量在50%以上,暗色泥岩TOC含量在0 6%～1 5%之间;有机质母质类型较差,属以Ⅲ型干酪根为主的气源岩;整个济阳坳陷的C P地层处于成熟 高成熟阶段,Ro值在0 6%～1%的范围内。分析表明,区内C P煤岩总体上为较好 好的烃源岩,暗色泥岩基本上为中等 较好烃源岩。     

我国环境空气颗粒物质量基准研究框架及研究体系的构建

空气颗粒物来源广泛、组成复杂,我国目前尚未有一套基于完整科学理论和足量实测数据支持的颗粒物基准体系,导致其来源、暴露水平、健康和环境风险信息量不足,相关标准制、修订的依据不足. 解析了美国环境空气质量管理的模式,并追踪了美国基准文件的发布历程和世界卫生组织导则值的发布和修订历程. 辨析了环境空气颗粒物质量基准与标准的内涵,分析了空气颗粒物质量基准研究对环境空气质量标准制/修订的支撑作用. 综合国外环境基准体系框架构成和已有研究成果,结合国内空气颗粒物质量基准研究现状和存在的问题,基于“污染源—环境空气浓度—暴露水平与剂量—健康/环境效应与风险”的各环节研究方法与目标,提出了“2-4-4”基准研究框架体系,即颗粒物质量基准研究包括空气颗粒物人体健康基准和空气颗粒物环境效应基准两部分,其中人体健康基准包括颗粒物污染特征与来源解析、个体暴露、剂量-效应关系及人体健康效应四部分,空气颗粒物环境效应基准包括颗粒物对生态系统、能见度、建筑物和材料、气候的影响四部分. 建议我国应开展大气污染健康影响前瞻性队列研究和对生态环境影响研究,采用多种方法,包括近期发展的暴露组学方法,系统研究空气颗粒物特别是PM_2.5载带的有毒有害组分对公众健康的危害和风险;基于我国人群或区域调查结果,建立我国空气颗粒物特别是PM_2.5环境质量基准体系,定期发布质量基准文件.      

原水碳源分子量分布及DPB效能对酸化时间的响应

采用超滤-纳滤膜法对污水中碳源分子量(MW)进行切割试验,并测定各区间总有机碳(TOC)浓度以了解污水碳源组成特性;同时采用污水酸化技术,研究在不同酸化时间,碳源分子量分布的变化及对厌氧-膜好氧-反硝化(A2N)工艺中反硝化聚磷菌(DPB)用碳和净污效能的影响.结果表明,试验原水TOC为(58.3±2.83) mg /L,其中颗粒有机碳(POC)为(38.05±1.65)mg /L,占65.27%,剩余溶解有机碳(DOC)在分子量0.5kDa以上区间呈现“W”型分布,其中 MW>100kDa、10k~5kDa、1k~0.5kDa、MW<0.5kDa区间碳源分别占36.20%、12.05%、13.68%和29.83%.在不同酸化时间下,POC含量与DOC分布存在显著差异,在12h内酸化,可以有效将POC转化为DOC,且在14mg/L左右趋于平衡;DOC在大于0.5kDa区间上的分布呈现随时间而整体后移的趋势,在8h时碳源质量最优,其中MW<1kDa的小分子有机物高达17.30mg/L;此时,DPB污泥在厌氧池与缺氧池中的碳源利用率分别为 83.48%、79.59%,比0h时分别提高了23.56%、18.03%;TN、TP去除率分别提高了14.63%、16.98%.     

在线表征萘二次有机气溶胶硝基多环芳烃

硝基多环芳烃(NPAHs)广泛存在于大气气溶胶中,是棕色碳的重要组成部分.萘和其他多环芳烃是NPAHs的重要前体物.为研究NO₂对NPAHs形成的影响,本文利用气溶胶激光飞行时间质谱仪(ALTOFMS)在线测定不同NO₂浓度下萘光氧化形成的二次有机气溶胶(SOA)的NPAHs组分.实验结果表明,NO₂对NPAHs的产生和萘SOA的形成有促进作用.通过ALTOFMS在线检测、模糊C均值(FCM)聚类分析,结合离线电喷雾电离质谱验证,测得萘酚和羰基化合物是不存在NO₂时萘SOA粒子主要成分,而通过OH-萘加合物和萘酚硝化产生的硝基萘、二硝基萘、硝基萘酚和二硝基萘酚及其衍生物是NO₂存在时萘SOA粒子的主要组分.这为城市大气高浓度NO_x背景下,研究NPAHs的化学组分和形成机理提供了实验依据.     

“碳达峰和碳中和”的科学内涵及我国的政策措施

中国提出的"碳达峰和碳中和"目标是基于统筹国际国内两个大局的战略考量,基于科学论证的国家战略需求提出的,实现这一目标挑战和机遇并存。我国的承诺为全球高质量绿色复苏注入了强心剂和新活力,但实现该目标比发达国家面临更大挑战。它将倒逼我国社会经济结构进行重大调整,对科技创新提出了新要求,会给经济高质量发展、建设美丽中国带来机遇。建议切实贯彻我国"十四五"规划纲要提出的"碳强度控制为主,碳排放总量控制为辅的双控目标",充分考虑将碳排放总量控制目标考核和现有污染减排考核体系相结合,增强"十四五"的行动力。尽快制定碳中和目标下的科技创新规划和实施方案。统筹考虑短期经济复苏、中期结构调整、长期低碳转型,布局低碳/脱碳技术,提升未来绿色产业竞争力。     

一株高效异养硝化菌的分离、鉴定及其氨氮去除特性

以丁二酸钠为唯一C源,从垃圾渗滤液活性污泥中富集、分离及筛选出一株高效的异养硝化菌,通过形态观察、生理生化特征及16S rDNA序列分析,对分离菌株进行了鉴定,同时对其硝化功能和氨氮去除特性进行了研究.结果表明,分离到的异养硝化菌为假单胞菌属(Pseudomonas sp.),命名为XS76,其GenBank登录号为(JQ934897).该菌经过24h培养,有约60%的氨氮转化为胞内氮,35%左右的氨氮被去除,仅有少量硝酸盐氮的积累,没有羟胺和亚硝酸盐氮的积累.碳源、有机氮源、C/N比、温度等因素均对氨氮去除有较大的影响,在接种量为4%、丁二酸钠为碳源、硫酸铵为氮源、C/N 15、转速180~200r/min、pH 6~9及温度为34℃,氨氮负荷为420 mg/L时处理效果最佳, 96 h氨氮去除率可达99.20%.显示了高效的氨氮去除效果,具有潜在的实际废水应用价值.     

酸雨对广西典型碳酸盐岩地区碳源效应研究

选取广西两个典型碳酸盐岩地区桂林(代表灰岩地区)与柳州(代表白云岩地区)作为研究区域,研究酸雨与岩石表面反应,并计算出由酸雨对碳酸盐岩的化学风化过程中形成CO2成为碳源的量。利用溶蚀试片溶蚀速率以及GIS技术得到研究区由酸雨产生的CO2源为41.066×108 g/a,其中桂林市区速率为33.349×108 g/a,柳州市区速率为7.717×108 g/a。单位面积源桂林与柳州分别为66.967×105 g/a.km2和42.777×105 g/a.km2,虽然低于两地的单位面积汇分别为273.891×105 g/a.km2与43.660×105 g/a.km2,但已不容忽略。柳州市区CO2源的释放速率比桂林市区慢的原因主要有二:桂林市区碳酸盐岩的代表面积为柳州市区2.77倍;由于柳州酸雨总体强度比桂林低,导致碳酸盐岩的溶蚀速率较低。     

Dynamic equity carbon permit allocation scheme to limit global warming to two degrees

Significant international collaboration is required to limit global temperature increase to below 2 °C above pre-industrial levels. Equity is the foundation of cooperation, and therefore, this study proposed a new dynamic carbon permit allocation scheme based on four principles: equality, historical responsibility, capability, and future development opportunities. Decision makers could have different preferences for allocating carbon permits, therefore, four equity rules or indicators (equality, responsibility, capacity, and sovereignty) were assigned different weights. Based on the global carbon budget of the 2 °C target, emission permits were calculated and relevant economic implications analyzed using the Global Change Assessment Model. Results indicated that developed countries should reduce emissions immediately, while allowances for developing regions could permit an initial increase in emissions until peaking. Applying different weights to the indicators resulted in multifarious regional allowances. Developed regions would benefit from the “preferring sovereignty” scenario and most developing countries would benefit under the “preferring responsibility” and “preferring capacity” scenarios. Compared with the Intended Nationally Determined Contributions submitted to the United Nations Framework Convention on Climate Change, this study found that in the short term, developed countries might insist on sovereignty as the preferred indicator. However, preferring sovereignty would place substantial mitigation pressures on developing countries in the long term. Therefore, in addressing global climate change, a dynamic choice in the weighting distribution for different indicators might be conducive to international agreement. Furthermore, a market-based trading instrument could help all participants both mitigate global climate change by reducing regional and global costs and facilitate mitigation capital flow from developed to less developed regions.     

Diaphorobacter sp.PDB3菌好氧反硝化脱氮特性

研究了Diaphorobactersp.PDB3菌在发酵罐内好氧反硝化特性.经过分析比较确定柠檬酸钠是好氧反硝化最佳碳源,采用响应面法对影响好氧反硝化的条件（温度、pH值、发酵罐转速、碳氮比）进行优化,构建出好氧反硝化数学模型.本模型预测值与实测值相关性非常好,预测PDB3菌发酵罐内好氧反硝化最佳条件：pH值、碳氮比、温度、转速分别为7.3、8.1、30.1℃、299.9r/min,最佳好氧反硝化比速率为2.25h^-1.验证实验表明,PDB3菌在发酵罐内好氧反硝化比速率为2.12h^-1,误差仅为5.8%.通过氮平衡分析表明,29.0%的总氮去除量转化为胞内氮,氮损失占总氮去除量的67.3%,细胞主要通过好氧反硝化作用和细胞同化作用脱氮.荧光定量PCR分析测定好氧反硝化过程中脱氮基因（napA,nirS,cnorB,nosZ）的表达水平以进一步解释脱氮特征,为Diaphorobacter sp.PDB3菌的实际应用提供一定的理论依据.     

生物滴滤池反硝化脱氮试验研究

采用一套内部填充多孔蜂窝陶瓷填料的生物滴滤池,研究了在不同温度下3种不同类型的碳源(甲醇、醋酸钠和葡萄糖)以及不同的C N对于系统反硝化效果的影响。结果表明,不同碳源对于系统的反硝化能力有很大的影响,采用甲醇和葡萄糖不会引起亚硝酸盐的积累,而醋酸钠会引起明显的亚硝酸盐积累,在硝酸盐基本消耗完的时候达到最大的积累值(初始硝酸盐总量的2 0 % )。不同碳源的最佳操作温度有所不同,3种碳源在4 0℃下都具有较好的反硝化效果。     

Potential carbon sequestration in China’s forests

Forests are believed to be a major sink for atmospheric carbon dioxide. There are 158.94 million hectares (Mha) of forests in China, accounting for 16.5% of its land area. These extensive forests may play a vital role in the global carbon (C) cycle as well as making a large contribution to the country’s economic and environmental well-being. Currently there is a trend towards increased development in the forests. Hence, accounting for the role and potential of the forests in the global carbon budget is very important.In this paper, we attempt to estimate the carbon emissions and sequestration by Chinese forests in 1990 and make projections for the following 60 years based on three scenarios, i.e. “baseline”, “trend” and “planning”. A computer model F-CARBON 1.0, which takes into account the different biomass density and growth rates for the forests in different age classes, the life time for biomass oxidation and decomposition, and the change in soil carbon between harvesting and reforestation, was developed by the authors and used to make the calculations and projections. Climate change is not modelled in this exercise.We calculate that forests in China annually accumulate 118.1 Mt C in growth of trees and 18.4 Mt in forest soils, and release 38.9 Mt, resulting in a net sequestration of 97.6 Mt C, corresponding to 16.8% of the national CO₂ emissions in 1990. From 1990 to 2050, soil carbon accumulation was projected to increase slightly while carbon emissions increases by 73, 77 and 84%, and net carbon sequestration increases by −21, 52 and 90% for baseline, trend and planning scenarios, respectively. Carbon sequestration by China’s forests under the planning scenario in 2000, 2010, 2030 and 2050 is approximately 20, 48, 111 and 142% higher than projected by the baseline scenario, and 8, 18, 34 and 26% higher than by the trend scenario, respectively. Over 9 Gt C is projected to accumulate in China’s forests from 1990 to 2050 under the planning scenario, and this is 73 and 23% larger than projected for the baseline and trend scenarios, respectively. During the period 2008–2012, Chinese forests are likely to have a net uptake of 667, 565 and 452 Mt C, respectively, for the planning, trend and baseline scenarios. We conclude that China’s forests have a large potential for carbon sequestration through forest development. Sensitivity analysis showed that the biggest uncertainty in the projection by the F-CARBON model came from the release coefficient of soil carbon between periods after harvesting and before reforestation.     

Starch/polyvinyl alcohol blended materials used as solid carbon source for tertiary denitrification of secondary effluent

Starch/polyvinyl alcohol （PVA） blended materials for using as a solid carbon source （SCS） were prepared by blending PVA and gelatinized starch in an aqueous solution system, in which PVA served as framework material and starch as carbon source. The optimization of starch content and temperature effects were investigated. It was indicated that higher denitrification efficiency could be achieved with more starch in the materials. The average specific denitrification rates were 0.93, 0.66, 0.37 and 0.36 mg/（g·day） corresponding to starch content of 70%, 60%, 40% and 30% respectively at 37℃. The denitrification rates increased when operating temperature was raised from 23℃ to 30℃ and then 37℃. The mechanism of carbon release was analyzed incorporating the experimental results of abiotic release in deionized water. The organic carbon was mainly hydrolyzed by microbes, and the biological release efficiencies were at the range of 89.2% to 96.0%. A long-term experiment with a continuous flow reactor with SCS material containing 70% starch was conducted to gain some experience for practical application. When the influent nitrate concentration was in the range of 35.2 to 39.1 mg/L, hydraulic retention time of 4 hr, and operating temperature of 30℃, a nitrogen removal efficiency up to 94.6% and denitrification rate of 0.217 kg/（m3.day） was achieved. The starch-based materials developed in this study can be used as a solid carbon source for tertiary nitrogen removal from secondary effluent.     

腐植酸和黑炭的提取及其对菲和芘的吸附行为

从河水沉积物中提取腐植酸和黑炭,通过元素分析仪、总有机碳仪、扫描电子显微镜和Zeta电位仪对其进行表征分析。研究了多环芳烃（PAHs）的代表物质菲和芘分别在腐植酸和黑炭上的分配行为并测定其分配系数,以及Ca2+浓度对菲、芘吸附的影响。结果表明:河水沉积物中提取的腐植酸和黑炭的主要元素组成是碳和氧,两者含有较多的芳香烃组分;水生植物是腐植酸和黑炭来源的主要贡献者;腐植酸呈发泡絮状结构,黑炭具有微孔结构;黑炭颗粒表面带有的负电荷明显少于腐植酸,其分子间的斥力作用较小。基于以上结果,认为黑炭的吸附能力高于腐植酸。菲和芘在腐植酸上分配系数的对数值（lg K_d）分别为3.55和4.55,在黑炭上分配系数的对数值（lg K_d）分别为4.57和5.35,这说明单位质量腐植酸和黑炭上芘的吸取量高于菲;菲和芘在腐植酸和黑炭上的吸附量随着Ca2+浓度的增加而呈先增加后减少的趋势。     

Search for biochemical fossils on earth and non-biological organic molecules on Jupiter,Saturn and Titan

Recognizable remnants of ancient biochemicals may survive under mild/moderate geological environments. Acyclic isoprenoid hydrocarbons, cyclic hydrocarbons with terpenoid carbon skeletons (e.g. hopanes) and vanadyl and nickel porphyrins have been isolated from organic matter, including petroleum, in Phanerozoic sedimentary rocks. Remnants of lignin have also been found. Usually, carbohydrates do not survive long; they degrade and/or react with other organic substances to form macromolecular matter. Proteins, e.g. apparently those in dinosaur bone collagen, break down relatively rapidly. Life arose during the Precambrian and potential biochemical fossils, e.g. n-alkanes, 2,5-dimethylfuran have been isolated from Precambrian kerogens. Traces of hydrocarbons, NH₃, PH₃ occur on Jupiter and Saturn. Hydrocarbons, N₂ and HCN, the latter a key intermediary in the laboratory abiological syntheses of amino acids and nucleic acid bases, are present on Titan where life could not have evolved. Precursor abiological organic molecules of some complexity may have been synthesized on Titan and the Jovian planets.     

毒死蜱降解细菌XZ-3的分离及降解特性研究

从某农药厂排污口的污泥中采样,经驯化富集后筛选到1株能高效降解毒死蜱的细菌XZ-3,经过对其形态、生理生化特征及16S rDNA的分析,鉴定该菌株为节杆菌属（Arthrobactersp.）.测定了不同碳源、pH、温度及毒死蜱浓度对细菌降解能力和生长量的影响,以培养液在波长400 nm下的光密度值表示细菌生长量,液体介质中毒死蜱的提取采用漩涡振荡提取法,提取溶剂为石油醚,毒死蜱的测定采用紫外分光光度法.结果表明,该菌株24 h内对100 mg·L^-1毒死蜱的降解率高达86.8%;在外加碳源浓度为0.3%时降解率最大;细菌的生长量随着外加碳源浓度的升高而增加;pH在偏酸和偏碱性的条件下降解率较大,pH 9.0时达到最大,细菌的生长量在pH 8.0～10.0偏碱性的条件下较大;在毒死蜱浓度为100　mg·L^-1时降解率最大,该菌具有较强的抗药性,当毒死蜱浓度达到1?000　mg·L^-1时仍能生长,细菌的生长量在800　mg·L^-1时达到最大,绝对去除量随毒死蜱浓度的提高而增加;细菌的生长和降解需要适宜的温度,30℃培养时,降解率和生长量最大.本研究提出了细菌XZ-3生长和降解毒死蜱的最佳培养条件,可为农药污染治理及生产污水处理提供理论依据.