相对速率法测氯原子与一系列低碳醇的反应速率常数

在 2 92± 1K温度和 1 0 1× 10 5Pa压力下 ,以丙烷为参照物 ,采用相对速率方法测定了一系列醇与氯原子在气相中的反应速率常数 ,这些醇与氯的反应速率常数分别为 (单位 :10 7m3·mol-1·s-1) :甲醇k1=3 2 9,乙醇k2 =6 14,正丙醇k3=8 97,异丙醇k4 =4 0 0 ,正丁醇k5=11 7,异丁醇k6=12 5 ,叔丁醇k7=2 0 5 ,正戊醇k8=15 8,异戊醇k9=12 3     

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.     

Plutonium isotopes concentration in seawater and bottom sediment off the Pacific coast of Aomori sea area during 1991-2005

A radioactivity survey was launched in 1991 to determine the background levels of ^239+240Pu in the marine environment off a commercial spent nuclear fuel reprocessing plant before full operation of the facility. Particular attention was focused on the ²⁴⁰Pu/²³⁹Pu atom ratio in seawater and bottom sediment to identify the origins of Pu isotopes. The concentration of ^239+240Pu was almost uniform in surface water, decreasing slowly over time. Conversely, the ^239+240Pu concentration varied markedly in the bottom water and was dependent upon the sampling point, with higher concentrations of ^239+240Pu observed in the bottom water sample at sampling points having greater depth. The ²⁴⁰Pu/²³⁹Pu atom ratio in the seawater and sediment samples was higher than that of global fallout Pu, and comparable with the data in the other sea area around Japan which has likely been affected by close-in fallout Pu originating from the Pacific Proving Grounds. The ²⁴⁰Pu/²³⁹Pu atom ratio in bottom sediment samples decreased with sea depth. The land-originated Pu is not considered as the reason of the increasing ^239+240Pu concentration and also decreasing the ²⁴⁰Pu/²³⁹Pu atom ratio with sea depth, and further study is required to clarify it.     

Cs, Pu concentrations and the Pu/Pu atom ratio in a sediment core from the sub-aqueous delta of Yangtze River estuary

A sediment core collected from the sub-aqueous delta of the Yangtze River estuary was subjected to analyses of ¹³⁷Cs and plutonium (Pu) isotopes. The ¹³⁷Cs was measured using γ-spectrometry at the laboratories at the Nanjing University and Pu isotopes were determined with Accelerator Mass Spectrometry (AMS), measurements made at the Australian National University. The results show considerable structure in the depth concentration profiles of the ¹³⁷Cs and ^239+240Pu. The shape of the vertical ¹³⁷Cs distribution in the sediment core was similar to that of the Pu. The maximum ¹³⁷Cs and ^239+240Pu concentrations were 16.21 ± 0.95 mBq/g and 0.716 ± 0.030 mBq/g, respectively, and appear at same depth. The average ²⁴⁰Pu/²³⁹Pu atom ratio was 0.238 ± 0.007 in the sediment core, slightly higher than the average global fallout value. The changes in the ²⁴⁰Pu/²³⁹Pu atom ratios in the sediment core indicate the presence of at least two different Pu sources, i.e., global fallout and another source, most likely close-in fallout from the Pacific Proving Grounds (PPG) in the Marshall Islands, and suggest the possibility that Pu isotopes are useful as a geochronological tool for coastal sediment studies. The ¹³⁷Cs and ^239+240Pu inventories were estimated to be 7100 ± 1200 Bq/m² and 407 ± 27 Bq/m², respectively. Approximately 40% of the ^239+240Pu inventory originated from the PPG close-in fallout and about 50% has derived from land-origin global fallout transported to the estuary by the river. This study confirms that AMS is a useful tool to measure ²⁴⁰Pu/²³⁹Pu atom ratio and can provide valuable information on sedimentary processes in the coastal environment.     

微波消解石墨炉原子吸收法测定空气中的锰(铅)

本文介绍了用微波消解技术消解滤膜以测定空气中的锰（铅）的方法，与传统的稀硝酸浸出法、流酸-灰化法相比，微波消解更加简单、快速、节省、准确、沾污少、环境污染少，回收率高。     

Fe-Mn-Ni-Si四元合金中辐照缺陷对辐照硬化的贡献

目的 研究Fe-Mn-Ni-Si四元合金在350℃下受到离子辐照后产生的辐照缺陷对于辐照硬化的贡献.方法 对辐照前后样品进行纳米压痕测试,获得硬度增量来衡量辐照硬化;再通过三维原子探针及透射电镜等表征手段,获得样品辐照后产生的团簇的数量密度、体积分数、团簇尺寸、位错环密度、位错环尺寸大小等微观结构信息;结合Disper...     

氢化物发生-原子荧光光谱法测定废水中砷探讨

砷是对人体有害的元素,当人体每天的摄入量超过100ug或更高时,对人体就会产生严重的危害,而有些工业废水中合有一定量的砷元素,如果这些工业废水不经处理排放到水中会我们的身体造成很大程度的伤害,所以我对某工厂的工业废水进行检测,检测其排放废水中所含有砷元素的多少。火焰原子荧光和石墨炉原子荧光的检测能力无法满足测定的要求,...     

异丙醇与OH自由基和Cl反应产物的研究

在室温和一个大气压下 ,利用气相色谱和光离子色谱研究了空气中异丙醇与OH自由基和Cl的反应产物 .其主要产物为丙酮、乙醛和甲醛 .对于OH自由基与异丙醇的反应 ,丙酮与乙醛的产率分别大于 81 6%和 6 6% ;对于异丙醇与Cl的反应 ,丙酮和乙醛的产率分别为 78 5± 4 6%和 1 1 7± 1 0 % .结合光氧化反应主要产物 ,对异丙醇的光氧化反应机理进行了初步的探讨     

原子吸收光谱测定重金属影响因素分析

原子吸收光谱分析通常用来测定微量元素,目前常采用石墨炉原子吸收法测定试液中ppb级或更低的痕量和超痕量元素,因此对实验过程中的污染防治就显得尤为重要.文章阐述了在原子吸收光谱测定微量元素的过程中,实验环境、水和试剂的纯度、器皿清洁度、气体(包括燃气、助燃气和惰性保护气体)的纯度以及原子化器等诸多因素均会对测定结果的准确性产生影响.对以上影响因素逐一分析并提出改进建议,以减少分析误差提高测试准确性.     

有机物质的沸点与其结构的关系

本文总结了影响有机化合物沸点的主要因素, 详细地概括了沸点与有机物质结构的关系.尤其是在此基础上找到一种估算沸点的方法,并给出了估算式:Tb=Km·e(W/M). 利用该式,可以更准确地计算出许多有机物质的沸点.