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121.
讨论了IP—1型离子泵测氦仪的工作原理及基本技术特性。通过野外工作,证明仪器具有性能比较稳定、灵敏度较高,便于携带等特点。介绍了仪器在已知铀矿床上开展放射性水化学找矿的试验结果。测量资料表明,在有利的地质、水文地质条件下,水氦异常能较好的指明深部铀矿化范围。  相似文献   
122.
REE mineralogy was characterized at the micrometer scale (using scanning electron microscopy) in the four tectono-metamorphic units of the Beni Mzala window, Sebtide Complex, Internal Rif, Morocco, which sample a HP-LT metamorphic gradient from subgreenschist to blueschist/eclogite facies. These tectonic units are composed of garnet-free metapelites (and associated synmetamorphic veins) from the same homogeneous aluminium-rich and calcium-poor protolith. In that context, mineralogical differences between units are assumed to result from contrasted pressure and temperature histories. Light REE-bearing Al-phosphates of the crandallite group with florencite-rich composition and variable goyazite content are the dominant LREE minerals in the lowest-grade units, Tizgarine (300 °C, 3 kbar as peak conditions) and Boquete de Anjera (350 °C, 10 kbar). In the latter unit, metamorphic florencite is associated with MREE-rich monazite. In the schist of the highest-grade units, Beni Mzala 2 (420–450 °C, 12 kbar) and Beni Mzala 1 (550 °C, 16 kbar), associations of allanite-rich epidote and synchisite (a LREE-fluorocarbonate) are found whereas florencite and monazite are no longer observed. At the wall of the quartz–kyanite veins, retrograde monazite-(Ce) with grain size of 20 to 50 μm is the only LREE-bearing mineral. Th–Pb and U–Pb SIMS data on some of these grains yield ages of 21.3 ± 1.7 Ma and 20.9 ± 2.1 Ma, respectively, consistent with previous K–Ar ages obtained on retrograde clay–mica mixtures in rocks from the same locality. The identification of a stability field for monazite in high-pressure aluminous metapelites with an upper thermal-limit below 450 °C as well as the derivation of meaningful U–Pb and Th–Pb SIMS ages demonstrates the monazite potential for dating HP-LT metapelites. However, since, under these conditions, monazite growth occurs below its admitted closure-temperature, these ages must be interpreted on the basis of monazite textural relationships.  相似文献   
123.
雷翠琼 《云南地质》2007,26(3):360-364
高温燃烧水解-离子选择电极法测定煤中氟,具有灵敏度高、重现性好、干扰少等优点,在测量过程中多注意水解温度、水解时间、氧气通量及试液的pH调节等因素,可以得到更准确、可靠的测量结果。  相似文献   
124.
???????????????????????????????????????????????????????????????????????Ч?????????????????÷??????????1 ns??????0.01 ns??????????????÷?????ù????????????????????????????????????????????????????????????????????????÷??????????IGS?????????????????????????????????  相似文献   
125.
测定石膏及其制品中的氟化物和氯化物,传统分析方法过程复杂,分析速度慢,准确度及灵敏度低。本文采用超声提取技术提取样品中的氟和氯,以Na2CO3-Na HCO3作为淋洗液,色谱柱分离后通过抑制器降低背景电导,用电导检测器进行检测。通过优化样品前处理和离子色谱分离条件,在测定范围内氟和氯的含量与峰面积呈良好的线性关系(相关系数0.9998),方法检测限为0.15 ng/m L(氟)和0.28 ng/m L(氯),加标回收率为95.0%~99.7%,精密度(RSD)均小于5%(n=8)。本方法采用超声提取技术,无需净化处理即可直接分析,半小时内完成前处理,且避免了目标分析物的损失。与离子选择电极法相比,检测限由μg/m L提升至ng/m L级别。  相似文献   
126.
Knowledge of the activity coefficients of solutes under temperature and pressure ranges of interest is generally required for calculations of the physicochemical properties of aqueous multicomponent electrolyte solutions such as seawater. Whilst these activity coefficients are well characterized for the predominant salts individually, fewer data are available for minor components under a sufficiently wide range of conditions and there are significant interactions between some of the chemical species involved which can substantially alter the required activity coefficients in mixtures.For these reasons, accurate thermodynamic predictions for seawater and other multi-electrolyte solutions in moderate or high concentration are more difficult than is often supposed. In particular, progress in this area has been slowed by uncertainty regarding the nature and extent of ion pairing in concentrated strong electrolyte solutions, a problem that has been debated for decades. Zdanovskii's rule, described originally almost a century ago but widely neglected, provides a fundamentally sound method for calculating the properties of mixed electrolyte solutions. Modelling developments are described, which accord with various types of experiment, from our laboratory and from the chemical literature. It has become clear that, when treated in an appropriate way based on solvent activity, linear mixing behaviour of strong electrolyte solutions can be considered the norm. This is an inevitable consequence, first recognized by Guggenheim, of the cancellation of ion pairing and other interactions as, conceptually, one ion replaces another. Stronger solute–solute interactions, described by equilibrium constants, can then easily be coupled in a thermodynamically consistent manner.  相似文献   
127.
近几年,河蟹人工育苗已成为我省沿海种苗培育单位的重要产业 ,随着育苗规模的不断扩大及所带来的可观经济效益,各地又因地制宜发展起地下海水、浓缩海水的育苗生产,为搞清这几种育苗水体的水质特点 ,作者对这几种水体进行了分析检测,以服务于生产 ,为河蟹育苗的健康发展提供科学依据。1工作内容和方法1.1采样点自然海水采于营口市老边区三道沟和盘锦市二界沟;浓缩海水采于营口市青石岭育苗室及营口盐  种型苗水p CD营盐含量Tab .1 pH ,CODandnutritionsaltofeverykindofbreedingwa…  相似文献   
128.
刘倩  刘光学 《地下水》2008,30(3):40-43
快速同时测定排污口样品中阴离子表面活性剂、总氮、总磷、挥发酚、氰化物、硫化物的分析方法。采用连续流动分析法,确定最佳实验方案。经多次试验验证,呈良好线性关系;质量控制样品测定值均在保证值范围内,样品回收率在95.2%~104%之间,RSD小于2%。  相似文献   
129.
Free metal ion concentration is generally considered a useful indicator of a metal’s bioavailability and ecotoxicity to aquatic biota. This article reports the speciation of nickel in mining and municipal effluents from Sudbury (Ontario, Canada), and also in model solutions containing a fully characterized laurentian fulvic acid (LFA) at environmentally relevant concentrations. A column ion exchange technique (IET) using a cation exchange resin (Dowex 50W-X8) was applied to determine free nickel ion concentrations. In model solutions, reasonable correlation was found between the predictions of an equilibrium-based computer speciation code, Windermere Humic Aqueous Model (WHAM) VI, and the results obtained by IET at low nickel-to-fulvic acid ratios. However at higher mole ratios, the WHAM VI predicted higher free nickel ion concentrations than IET. Only three out of six effluent samples showed reasonable agreement between the IET and the WHAM VI results, indicating the need for further development of IET for application to effluent waters.  相似文献   
130.
江岳  杜建国  易丽  罗丽  王富宽  陈志 《地震》2009,29(2):73-80
通过饱水砂岩的三轴压缩实验, 研究了含水层砂岩的破裂过程及其伴随的水化学变化, 并探讨了砂岩在蠕变和剪切破裂过程中地震水化异常现象的形成机理。 用离子色谱仪(IC)和等离子原子发射光谱仪(ICP-OES)测定了不同压力条件下实验溶液的F-、 Cl-、 NO-3、 SO2-4、 Ca2+、 Mg2+、 Na+浓度。 饱水砂岩在差应力作用下, 随着蠕变时间延长和剪切作用的强化实验, 溶液中主要离子的浓度均有不同程度的增大, 仅Mg2+浓度是降低的。 F-和Cl-浓度变化最明显, 在2~12小时的蠕变时间内分别增大约10倍和4倍, 而随剪切作用的强化分别增大约5倍和3倍。 这种变化主要与矿物的溶解和流体包裹体的混入有关。 实验结果表明, F-、 Cl-和Ca2+可作为砂岩含水层地震水化前兆监测的灵敏组分。  相似文献   
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