峨眉山景区旅游商品的开发与营销模式

通过对旅游商品定义的综述,界定了旅游商品的定义、范围和功能,同时对峨眉山景区旅游商品的开发、需求、购买力等抽取420份问卷作为样本,分析了峨眉山旅游商品的需求现状,并以旅游者需求现状为依据,对峨眉山旅游商品的开发和营销提出了“4P＋4C＋4R”营销策略,以期对其它景区的旅游商品开发和营销具有一定的借鉴意义。     

化学解耦联剂对活性污泥产率的控制作用

采用3,3',4',5-四氯水杨酰苯胺(TCS)作为代谢解耦联剂添加到活性污泥工艺中,进行连续曝气分批培养实验.结果表明:在TCS总投加量相同的情况下,采用一次性大剂量投加的污泥减量化效果好于分次小剂量投加.每d投加 12 mg TCS,污泥产量比对照下降了33%,而每2 d一次性投加24 mg TCS,污泥产量比对照下降了55%.污泥的CODCr去除能力有所下降,当一次性投加12 mg时,CODCr去除率比对照下降了12%,但出水氨氮及总氮质量浓度均未受影响.污泥的SVI有所上升,但沉降性能未见有明显变化.      

活化后钾改性正硅酸锂吸附CO2的性能评价及动力学研究

制备了钾改性正硅酸锂(K-Li4SiO4),并对其进行了自活化,考察了活化后K-Li4SiO4吸附剂在不同温度和CO2浓度气氛中吸附CO2的性能及动力学行为。总体而言,吸附剂的CO2吸附能力随着温度的升高、CO2浓度的增加而提升。在700℃、100%体积分数CO2气氛中吸附剂的吸附量最大,可达7.9 mmol/g,吸附剂的利用率为95.2%。利用双指数模型能够很好地描述吸附剂在各个温度以及各个CO2浓度气氛下的CO2吸附过程。吸附活化能随着CO2气氛浓度的升高而降低,CO2体积分数为20%,50%,100%时的吸附活化能分别为26448,14035,6178 J/mol。     

高压微波络合消解石墨炉原子吸收分光光度法测定环境空气中锡

用有机滤膜采集空气中颗粒物样品,用HNO3-HCl-HClO4-EDTA微波络合消解后制成样品溶液。用石墨炉原子吸收分光光度法可确定样品溶液中锡的浓度。该方法具有消解完全,无损失,灵敏度高,准确度、精密度好等特点。     

磷酸活化植物基活性炭对水溶液中铅的吸附

以棉秆与互花米草为原料,采用磷酸活化法制备了低成本的植物基活性炭,通过静态实验研究了其对重金属铅的吸附性能。结果表明,在活化温度为500℃、活化时间为2 h条件下,制备的棉秆和互花米草活性炭比表面积为1 570m2/g和856 m2/g,含氧酸官能团含量分别为1.43 mmol/g和1.27 mmol/g。在25℃下,两种活性炭对重金属铅的Langmuir最大吸附量分别为119 mg/g和111 mg/g,吸附最佳pH为4.3,吸附平衡符合Freundlich方程,离子交换在吸附过程中发挥了重要作用。     

Concentration and characterization of plutonium in soils of Hubei in central China

To study the Pu concentration and isotope ratio distributions present in China, the ^239+240Pu total activities and ²⁴⁰Pu/²³⁹Pu atom ratios in core soil samples from Hubei Province in central China were investigated using Accelerator Mass Spectrometry (AMS). The activities ranged from 0.019 to 0.502 mBq g⁻¹ and the ^239+240Pu inventories of 45 and ∼55 Bq m⁻² agree well with that expected from global fallout. The ²⁴⁰Pu/²³⁹Pu atom ratios in the soil ranged from 0.172 to 0.220. The ratios are similar to typical global fallout values. Hence, any close-in fallout contribution from the Chinese nuclear weapons tests, mainly conducted in the 1970s, must have either been negligible or had a similar ²⁴⁰Pu/²³⁹Pu ratio to that of global fallout. The top 10 cm layer of the soil contributes ∼90% of the total inventory and the maximum concentrations appeared in the 2-4 cm or 4-6 cm layers. It is suggested that climatic conditions and organic content are the two main factors that affect the vertical migration of plutonium in soil.     

可见光响应型CuO/BiVO4的光催化活性研究

采用浸渍法制备了CuO/BiVO4光催化剂,通过X射线衍射(XRD)、热重/差示扫描量热(TG/DSC)和傅立叶红外光谱(FTIR)对其进行了表征,并在可见光照射下考察了其光催化氧化亚甲基蓝(MB)的动力学特性。结果表明,Cu的掺杂并未改变BiVO4的晶型结构;Cu(NO3)2/BiVO4在热处理(30～300℃)过程中,NO3-已经完全分解,Cu最终以CuO的形式存在于CuO/BiVO4光催化剂体系中;掺杂不同量Cu的CuO/BiVO4中的Cu2+/Bi+(摩尔比)实测值与理论值相近,该系列光催化剂的合成过程具有较高的可信度;在可见光照射下,CuO/BiVO4光催化降解MB反应符合表观一级反应动力学特征;当Cu2+/Bi+为0.050时,反应动力学速率常数(k)达到最高值(0.4334h-1),此时的k比单体BiVO4作用下的提高了1.04倍;由于异质结的存在,CuO/BiVO4与单体BiVO4相比,电子和空穴的利用率大大增加,使得CuO/BiVO4的光催化活性较单体BiVO4有了大幅度提高。     

4A沸石去除水中Pb2＋的研究

在静态条件下,研究了4A沸石对废水中Pb2＋的吸附性能,并探讨了影响吸附的因素。实验表明：当温度为30℃,废水pH为5～6,0．01g4A沸石对100mg／LPb2＋溶液10mL吸附20min,Pb2＋的去除率可达到99％以上。在实验研究条件下,4A沸石对Pb2＋的吸附符合Langmuir和Freundlich等温吸附方程,相关系数为0．9819和0．9998。经计算,4A沸石对Pb2＋的饱和吸附量为125mg／g。4A沸石吸附水中Pb2＋达到吸附平衡的时间较短;溶液pH值的变化对吸附效果影响不显著;温度从室温略微升高,Pb2＋的去除率略有增大。吸附在4A沸石上的Pb“可回收利用,处理后的4A沸石可以再生,且重复使用性能较好。     

Characterization of plutonium in deep-sea sediments of the Sulu and South China Seas

Anthropogenic Pu isotopes are important geochemical tracers for sediment studies. Their distributions and sources in the water columns as well as the sediments of the North Pacific have been intensively studied; however, information about Pu in the Southeast Asian seas is limited. To study the isotopic composition of Pu, and thus to identify its sources, we collected sediment core samples in the South China Sea and the Sulu Sea during the KH-96-5 Cruise of the R/V Hakuho Maru. We analysed the activities of ^239+240Pu and the atom ratios of ²⁴⁰Pu/²³⁹Pu using isotope dilution sector-field inductively coupled plasma mass spectrometry (SF-ICP-MS). The ²⁴⁰Pu/²³⁹Pu atom ratios in the sediments of both areas (inventory weighted mean: 0.251 for the South China Sea and 0.280 for the Sulu Sea) were higher than the global fallout value (0.178 ± 0.019), suggesting the existence of Pu from the Pacific Proving Grounds in the North Pacific. Low inventories of ^239+240Pu in sediments were observed in the South China Sea (3.75 Bq/m²) and the Sulu Sea (1.38 Bq/m²). Most of the Pu input is still present in the water column. Scavenging and benthic mixing processes were considered to be the main processes controlling the distribution of Pu in the deep-sea sediments of both study areas.     

磷酸微波活化多孔生物质炭对亚甲基蓝的吸附特性

以甘蔗渣为原料,采用微波辅助H3PO4活化法制备富含含氧酸官能团的中孔生物质炭。通过扫描电子显微镜SEM、傅立叶变换红外光谱FT-IR等技术对生物质炭物理化学性质进行表征,并通过静态实验法,探讨炭样对亚甲基蓝的吸附行为及热力学性质。结果表明,H3PO4活化制备蔗渣生物质炭的适宜条件为浸渍比1：1,烘干时间10h,活化功率900W,活化时间22min,在此条件下制得的生物质炭得率为39．2％,碘值为817mg／g,亚甲基蓝值为229mg／g,为国家一级品标准的1．7倍。红外光谱分析表明,炭样表面以羟基、羰基、羧基等酸性官能团为主。静态吸附实验表明,Freundlich方程与Redlich—Peterson方程能较好地描述等温吸附行为,表现为优惠吸附。热力学研究表明,吸附吉布斯自由能（△G0）〈0,说明吸附反应是自发过程,而吸附标准焓变（△H0）〉70KJ／mol,表明亚甲基蓝在制备炭样上的吸附是吸热反应,升温有利于吸附,且化学反应在吸附过程中发挥了重要作用。