纳米氢氧化铝三相泡沫制备研究*

为更好地解决煤矿采空区煤炭自燃问题,以十二烷基硫酸钠为主体进行发泡剂复配,通过泡沫性能测试实验,研制出高性能发泡剂。以纳米氢氧化铝作为固相颗粒,制备出发泡倍数高、稳定性强的纳米氢氧化铝三相泡沫,使用锥形量热仪研究其高温阻燃能力和消烟性能。实验结果表明:当纳米氢氧化铝的质量分数从0提高到1%时,泡沫体积从500 mL增长至830 mL;当质量分数从3%提高到4%时,泡沫析液半衰期由15 min提升至42 min,且能在完全析液后保留三维网状结构。在高温阻燃和消烟能力方面,纳米氢氧化铝三相泡沫的加入将点燃时间从24 s延长至87 s,持续燃烧时间从835 s缩短至325 s,热释放速率高峰值从97.2 kW/m2降低至49.8 kW/m2,烟气生成速率峰值从0.064 m2/s降低至0.012 m2/s,对CO,CO2释放速率也有一定抑制作用。     

顺层或逆层岩质急倾斜边坡坡角的确定

为了解当岩体具有急倾斜构造和水平裂隙发育时,由该岩体形成顺层和逆层边坡情况下,不同坡角对该边坡稳定性的影响,使用基于颗粒流理论的PFC3D进行了模拟。利用PFC3D中的JSET和Bonds模拟了非连续性和连续性的岩体构造形式。构建了坡角为40°、50°、60°、70°和80°的顺层和逆层边坡,并对边坡稳定性进行了模拟。模拟结果表明,岩层的重力作用在逆层时有利于岩体外倾,顺层时抑制外倾。相同坡角时顺层较逆层更为稳定。大变形裂隙区的出现位置与岩体构造有很大关系。提出的修建边坡坡角建议为顺层时坡角不应大于60°,逆层时坡角不应大于50°。     

蓝藻胞外聚合物对供水管网水质的影响

针对游离态蓝藻胞外聚合物（EPS）在常规水处理工艺中不易去除、残留蓝藻EPS极易进入供水管网的特性,研究了蓝藻EPS对供水管网水质变化及生物稳定性的影响.针对管道使用时限分析了不同管道内部产生附膜条件下,蓝藻EPS对供水管网中余氯、浑浊度、生物稳定性、有机组分等主要水质指标变化规律的影响.结果表明,蓝藻EPS加快了管网余氯衰减速度,导致管网水质浑浊度在12~24h后即超出生活饮用水卫生标准上限,并使管网水质生物稳定性降低,BDOC在72h内增加37.2~39.5%,AOC增加365~393%,总活菌数升高18~20倍.阐明了蓝藻水华爆发时期净水厂出厂水残留蓝藻EPS在管网余氯存在前提下,仍然能够作为微生物营养基质和代谢能量,而促进管道内细菌生长繁殖,增加微生物代谢活性,刺激微生物胞外有机组分分泌释放,导致管网水质二次污染.     

不同植被带生态恢复过程土壤团聚体及其稳定性——以黄土高原为例

为分析黄土高原不同植被带植被恢复对土壤团聚体分布特征及其稳定性的影响,以黄土高原从北到南不同纬度梯度分布的3个典型植被类型区域（草原带、森林草原带和森林带）为研究对象,对不同植被类型和恢复年限下的土壤团聚体分布及其稳定性进行了研究.结果表明：不同植被带对土壤团聚体分布及其稳定性影响显著,大于0.25mm团聚体含量（WR_0.25）、水稳性团聚体平均重量直径（E_WMD）、水稳性团聚体几何平均直径（E_GMD）和有机质含量（SOM）整体上均表现为：森林带 > 森林草原带 > 草原带.不同植被带下不同恢复类型对土壤团聚体及其稳定性影响不一,森林草原带表现为灌木 > 草地 > 乔木,森林带则表现为乔木 > 草地.随植被恢复年限增大,各种恢复类型WR_0.25、E_GMD、SOM整体呈逐渐增加趋势,团聚体结构破坏率（PAD）和可蚀性因子（K）呈现相反的变化趋势;分形维数（D）无显著差异.冗余分析表明,植被带对土壤团聚体及其稳定性的影响最大,其次是恢复年限,恢复类型与植被带和恢复年限具有较强的交互作用.本研究有利于加强对区域生态恢复过程机理的认识.     

Efficient low-temperature soot combustion by bimetallic Ag–Cu/SBA-15 catalysts

In this study, the effects of copper(Cu) additive on the catalytic performance of Ag/SBA-15 in complete soot combustion were investigated. The soot combustion performance of bimetallic Ag–Cu/SBA-15 catalysts was higher than that of monometallic Ag and Cu catalysts. The optimum catalytic performance was acquired with the 5 Ag_1-Cu_(0.1)/SBA-15 catalyst, on which the soot combustion starts at T_(ig)= 225°C with a T_(50)= 285°C. The temperature for 50% of soot combustion was lower than that of conventional Ag-based catalysts to more than 50°C(Aneggi et al., 2009). Physicochemical characterizations of the catalysts indicated that addition of Cu into Ag could form smaller bimetallic Ag–Cu nanolloy particles, downsizing the mean particle size from 3.7 nm in monometallic catalyst to 2.6 nm in bimetallic Ag–Cu catalyst. Further experiments revealed that Ag and Cu species elicited synergistic effects, subsequently increasing the content of surface active oxygen species. As a result, the structure modifications of Ag by the addition of Cu strongly intensified the catalytic performance.     

CRITICAL DATA REQUIREMENTS FOR PREDICTION OF EROSION AND SEDIMENTATION IN MOUNTAIN DRAINAGE BASINS1

ABSTRACT: The potential for understanding and, where necessary, managing sedimentation in humid mountain drainage basins increases with awareness of the conditions that lead to shallow landsliding, debris flows, and catastrophic sedimentation in stream channels. Progress in understanding has involved: improved recognition of source areas and the potential for downstream effects of slope failure; improved understanding of hydrological conditions required for failure; and a general theory of slope stability in shallow colluvium, including the role of plants, fires, timber harvest, and other disturbances. The theory acknowledges spatial variability in topographic and geotechnical terrain characteristics, the stochastic nature of climatic triggering events such as forest fires and rainstorms, and the integrating nature of channel networks in modulating the cumulative effects of transient processes within a basin. Anthropogenic fire regimes, road effects, and timber harvest can readily be included. Continued application and modification of the theory over an expanded geographical range require improvements in field data and their systematic storage in spatial databases. Improvements in digital topographic data for mountain basins, systematic network-wide surveys of channel conditions, and new technology for rapid documentation of soil depths in landslide source areas would enhance the prediction of mass failure, its consequences for channel habitat, and the basin-wide or regional distribution of hillslope and channel conditions. Computations of the probabilities of transient effects throughout basins could then form the basis of ecological risk analyses. Large-scale spatial data sets of a few critical variables are required before this next level of understanding can be developed and applied to sedimentation impacts on ecosystems and other resources.     

大气CO2浓度升高对农田土壤颗粒组成及其碳周转的影响

采集FACE(Free Air CO2 Enrichment)平台下运行3年的水稻(Oryza sativaL.)/小麦(Triticum aestivumL.)轮作土壤(0~15cm耕作层土壤),利用超声波分散-湿筛分法对烘干土样进行颗粒分级,分析土壤各粒级及其碳、氮的分布特征,研究大气CO2浓度升高对土壤碳周转的影响。结果表明:高浓度大气CO2条件下稻/麦轮作3年后,土壤颗粒组成较对照发生了改变,>53μm粒级的质量分数减小27%(p<0.05),约占土壤总质量20%;53~25μm粒级的质量分数增大35%(p<0.05),约占土壤总质量25%;<25μm无明显变化,约占土壤总质量55%,三种粒级之间质量分数呈显著差异(p<0.05)。FACE条件下,不同粒级土壤颗粒碳质量分数在两个氮水平下平均为:>53μm(30.60g·kg-1),<25μm(13.08g·kg-1),25~53μm(12.85g·kg-1),氮质量分数分别为2.42g·kg-1,1.33g·kg-1,1.12g·kg-1。>53μm粒级的土壤颗粒碳、氮质量分数均极显著高于其它两个粒级(p<0.001)。FACE条件下土壤总碳、氮质量分数高于对照,增幅分别为6.2%和6.7%。从各粒级土壤颗粒碳、氮质量分数变化分析,新增碳、氮主要进入>53μm粒级中,表明该粒级土壤颗粒对土壤碳氮循环(转化和保存)起着重要作用。该研究结果表明高浓度大气CO2条件下,稻/麦轮作农田土壤将成为大气CO2的汇,这将为预测我国未来农田土壤碳的变化趋势提供科学依据。     

优良籼型恢复系转基因植株的获得及其遗传稳定性

报道了用基因枪转化法将雪花莲凝集素基因(gna)转移到优良籼型杂交稻恢复系蜀恢527中．PCR、PCR Southern blotting和Southern blotting等分子检测证明，外源基因以多拷贝单位点方式整合到受体基因组中并稳定遗传到转基因第三代(T2)．转基因第一代植株(TO)在株高和结实率上与相应的组培、种子实生苗植株相比，发生明显的不可遗传的变异，随着繁殖代数的增加，转基因植株恢复到与对照植株一致．Western blotting表明，目的基因在转基因植株中正确表达．蛋白活性分析显示，外源基因在转基因植株中合成的蛋白具有凝血生物活性，含量占可溶性总蛋白的0．1％左右．本文还对转基因技术在杂交稻育种中的应用进行了讨沦．图4表2参18     

Temporary natural resource cartels

We analyze the behavior of a nonrenewable resource cartel that anticipates being forced, at some date in the future, to break up into an oligopolistic market in which its members will then have to compete as rivals. Under reasonable assumptions about the value function of the individual firms in the oligopolistic equilibrium that follows the breakup, we show that the cartel will then produce more over the same interval of time than it would if there were no threat of dissolution, and that its rate of extraction is a decreasing function of the cartel's life; that there are circumstances under which the cartel will attach a negative marginal value to the resource stocks, in which case the rate of depletion will be increasing over time during the cartel phase; that, for a given date of dissolution, the equilibrium stocks allocated to the post-cartel phase will increase as a function of the total initial stocks, whereas those allocated to the cartel phase will increase at first, but begin decreasing beyond some level of the total initial stocks.     

湿解产物与堆肥在土壤中的稳定性和腐熟度比较分析

研究了不同培养阶段湿解产物与土壤混合物(HTS)的物质变化特征、稳定性和腐熟度,并与堆肥和土壤混合物(CS)及自然土壤进行了对比。结果表明:在培养过程中,所有HTS和CS的参数变化趋势相似,HTS的温度变化接近于CS的温度变化,稍高于自然土壤的温度,低于环境温度;pH值变化不大,基本稳定在7.6左右;在培养初期,水溶性有机碳比有机态氮w(WSC)/w(Norg)小于0.55,种子发芽系数(GI)高于80%;培养14d后,w(C)/w(N)降低至小于20,w(NH4 -N)/w(NO3--N)渐渐趋于稳定至小于0.16,GI基本高于100%;49d后,HTS的CO2释放率接近CS和自然土壤的CO2释放率;种子发芽系数的变化表明,湿解产物中含有更丰富的营养元素,可以促进植物根系的生长;相关性分析显示,w(WSC)/w(Norg)、w(NH4 -N)/w(NO3--N)和GI可以作为湿解产物腐熟度的评价指标。综合各项参数表明,湿解产物在土壤中会很快达到稳定,可以安全应用。