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1.
陈以良 《广东海洋大学学报》1992,(1)
用比电导法研究两种活性炭自稀水溶液中吸附强电解质硫酸铬和硫酸铜的吸附平衡特性。结果表明,在本文的研究条件下,两种活性炭对硫酸铬和硫酸铜都有吸附作用。同时,活性炭吸附硫酸铜的吸附平衡特性可以用 Freundlich 方程式来描述。研究的结果对固体在溶液中的吸附基础理论以及处理工业废水具有一定的意义。 相似文献
2.
桃山铀矿田桃山断裂及其保矿作用 总被引:2,自引:0,他引:2
桃山铀矿田位于江西省中部,断裂构造发育,既有成矿构造,也有保矿构造,其中斜贯桃山矿田的桃山断裂即是一保矿构造,它形成于车免近时期,走向北东,倾向南东,右行正断,并具铰链断层性质,上盘地块掀斜下落,致使上盘成矿壳层向NW和NE倾斜,由于倾末端的侵蚀深度较小,保矿条件较好,加强这些地带的铀矿勘查和评价具有重要意义。 相似文献
3.
The deposit size frequency (DSF) method has been developed as a generalization of the method that was used in the National Uranium Resource Evaluation (NURE) program to estimate the uranium endowment of the United States. The DSF method overcomes difficulties encountered during the NURE program when geologists were asked to provide subjective estimates of (1) the endowed fraction of an area judged favorable (factorF) for the occurrence of undiscovered uranium deposits and (2) the tons of endowed rock per unit area (factorT) within the endowed fraction of the favorable area. Because the magnitudes of factorsF andT were unfamiliar to nearly all of the geologists, most geologists responded by estimating the number of undiscovered deposits likely to occur within the favorable area and the average size of these deposits. The DSF method combines factorsF andT into a single factor (F·T) that represents the tons of endowed rock per unit area of the undiscovered deposits within the favorable area. FactorF·T, provided by the geologist, is the estimated number of undiscovered deposits per unit area in each of a number of specified deposit-size classes. The number of deposit-size classes and the size interval of each class are based on the data collected from the deposits in known (control) areas. The DSF method affords greater latitude in making subjective estimates than the NURE method and emphasizes more of the everyday experience of exploration geologists. Using the DSF method, new assessments have been made for the young, organic-rich surficial uranium deposits in Washington and idaho and for the solution-collapse breccia pipe uranium deposits in the Grand Canyon region in Arizona and adjacent Utah. 相似文献
4.
Contradictory results are reported for the behaviour of quaternary ammonium compounds (QACs) in sewage treatment plants (STPs). QACs may sorb onto activated sludge. Only little information is available with respect to effects of QACs against bacteria in STPs. Only 5 to 15 % of bacteria present in sewage sludge can be detected by means of culture dependent microbiological methods. The shift of the bacterial populations due to effects of test compounds have not been studied up to now with culture independent methods. The microbial populations shift was studied in situ using culture independent chemotaxonomy profiling ubiquinones and polyamines. Additionally, toxic effects of QACs against bacteria present in the test vessels of the Zahn‐Wellens test (OECD 302 B) were assessed with a toxicity control in the test. The ubiquinone profiles representing changes in Gram‐negative populations mainly showed that the activated sludge was affected only in test vessels containing benzalkonium chloride. According to chemotaxonomy Acinetobacter or/and some members of Pseudomonas spp. have been selected by benzalkonium chloride after some adaptation period (8 to 12 days). 相似文献
5.
华东南中新生代伸展构造时空演化与铀矿化时空分在 总被引:1,自引:0,他引:1
本文运用大陆伸展构造理论,论述了华东南地区中新生代以来伸展构造的分布规律,分析了不同类型伸展构造的时空演化特点。在此基础上,应用华东南地区不同类型铀矿床已有的成矿年龄资料,研究了伸展构造活动与区域铀成矿作用之间的联系,不同类型伸展构造与不同类型铀矿床之间在空间分布和时间演化上的对应关系。认为伸展构造活动产生的有利构造环境是导致铀成矿作用产生的根本原因,伸展构造活动的脉动性及其相应的岩浆作用决定了铀成矿作用的多期多阶段性,不同地区伸展构造活动的先后决定了不同类型铀矿床成矿作用的时序和空间分布。文章最后认为,由于伸展构造活动对区域铀矿化的这种明显控制关系,本区不同类型铀矿化成矿机理具有统一性。 相似文献
6.
A. Bollhöfer A. Eisenhauer N. Frank D. Pech A. Mangini 《International Journal of Earth Sciences》1996,85(3):577-585
Thorium- and uranium isotopes were measured in a diagenetic manganese nodule from the Peru basin applying alpha- and thermal
ionization mass spectrometry (TIMS). Alpha-counting of 62 samples was carried out with a depth resolution of 0.4 mm to gain
a high-resolution230Thexcess profile. In addition, 17 samples were measured with TIMS to obtain precise isotope concentrations and isotope ratios. We
got values of 0.06–0.59 ppb (230Th), 0.43–1.40 ppm (232Th), 0.09–0.49 ppb (234U) and 1.66–8.24 ppm (238U). The uranium activity ratio in the uppermost samples (1–6 mm) and in two further sections in the nodule at 12.5±1.0 mm
and 27.3–33.5 mm comes close to the present ocean water value of 1.144±0.004. In two other sections of the nodule, this ratio
is significantly higher, probably reflecting incorporation of diagenetic uranium. The upper 25 mm section of the Mn nodule
shows a relatively smooth exponential decrease in the230Thexcess concentration (TIMS). The slope of the best fit yields a growth rate of 110 mm/Ma up to 24.5 mm depth. The section from 25
to 30.3 mm depth shows constant230Thexcess concentrations probably due to growth rates even faster than those in the top section of the nodule. From 33 to 50 mm depth,
the growth rate is approximately 60 mm/Ma. Two layers in the nodule with distinct laminations (11–15 and 28–33 mm depth) probably
formed during the transition from isotopic stage 8 to 7 and in stage 5e, respectively. The Mn/Fe ratio shows higher values
during interglacials 5 and 7, and lower ones during glacials 4 and 6. A comparison of our data with data from adjacent sediment
cores suggests (a) a variable supply of hydrothermal Mn to sediments and Mn nodules of the Peru basin or (b) suboxic conditions
at the water sediment interface during periods with lower Mn/Fe ratios. 相似文献
7.
松辽盆地可地浸砂岩型铀矿成矿地质条件 总被引:3,自引:0,他引:3
本文重点讨论了松辽盆地的地质背景、铀源条件、铀矿化异常与岩相古地理以及盆地后期改造的关系,介绍了该盆地后期改造的特征、后期改造的动力条件及铀元素的再分配,探讨了铀矿化异常与复合砂体、氧化还原条件及剥蚀面的关系。在此基础上预测了铀成矿远景地区,选出找矿的重点层位。 相似文献
8.
138矿床是中生代火山-沉积改造型铀矿床。本文对矿床的铀源、矿区地层岩性、岩相古地理及古气候、构造和改造再生等地质条件,以及铀的吸附还原剂,岩石的有效孔隙度、化学成分、酸碱度、氧化还原电位等物理化学条件进行探讨。 相似文献
9.
随着科学技术的发展,壤中氧测量已具备应用于野外找矿的基本条件。本文通过野外壤中氧测量的找矿实例,对方法的理论依据、技术基础做了简要的阐述。介绍了壤中O2测量与壤中Rn,CO2测量配合在找矿中的成功应用,并认为:以积分形式采集数据的壤中氧方法具有方便、稳定的特点。 相似文献
10.
在相山铀矿床田东部地区,采用同位素技术和放射性水化学技术,对铀矿床地下水放射性污染问题从理论实践两方面方面进行研究,获得了当地雨水线的线性回归方程和在铀矿床的勘探开采过程中不会造成明显的地下水放射性污染的结论 相似文献