催化极谱法测定土壤中的痕量镉

采用单扫描极谱法测定土壤中镉含量,确立了1%碘化钾-1.5%酒石酸钾钠-2%三乙醇胺-0.6%盐酸-9%磷酸测定体系.在此测定体系中,镉在滴汞电极上于-0.71V(相对饱和甘汞电极)处产生一灵敏催化极谱波,镉浓度在0.2ng/ml～1μg/ml范围内与极谱峰电流有良好线性关系,检出限为0.1ng/ml.该方法用于土壤样品测定的RSD为0.6%～9.5%,加标回收率为90%～110%.该方法操作简便,用于土壤样品测定的结果满意.     

单扫描极谱法测定瓜子中痕量铅的研究

提出单扫描极谱法测定瓜子中痕量铅的新方法.在6%溴化钾、1%酒石酸钾钠、0.7%盐酸、5%磷酸、2%盐酸羟胺、3%(体积)三乙醇胺混合底液中,以单扫描极谱法对瓜子中痕量铅进行了测定.实验表明,铅在滴汞电极上于-0.47 V(相对饱和甘汞电极)处产生一灵敏催化极谱波,铅浓度在0.2 ng/mL~300 ng/mL范围内与极谱峰电流有良好分段线性关系.检出限为0.16 ng/mL.方法的RSD为2.2%~4.2%,加标回收率为89%~99%.此法仪器试剂简单,操作快速简便,用于实际样品测定,结果满意.     

高钙食品中痕量铅的极谱测定

建立了在0.6%碘化钾-0.8%酒石酸钾钠-0.36 mol/L盐酸-0.14 mol/L磷酸-0.6%三乙醇胺-0.1%抗坏血酸底液条件下,用单扫描极谱法测定高钙食品中痕量铅的方法.试验表明,本法的线性范围为5～800 ng/mL,检出限为1.5 ng/mL,样品加标回收率为95%～107%,相对标准偏差为4.3%～8.5%.     

微波消解GFAAS法测定动物骨中铅和镉

通过考察各种微波消解因素对微波消解效果的影响,以及通过对石墨炉原子吸收光谱法测定条件的优化,建立了用微波消解石墨炉原子吸收光谱法测定动物骨中铅和镉的分析方法.结果表明,最佳微波消解条件为消解压力15 MPa;消解时间5 min.最佳石墨炉测定条件为铅灰化温度800℃,原子化温度1300℃;镉的灰化温度900℃,原子化温度1200℃.方法线性范围为铅1.566~50 ng/mL;镉0.0745~5 ng/mL.方法检出限为铅0.3132 ng/mL;镉0.0149 ng/mL.样品测定的RSD小于5.0%,加标回收率在88.36%~110%之间.     

极谱分析法测定生活固体废弃物中痕量铅

采用浓硫酸炭化、硝酸-高氯酸消解废弃报纸、导购彩报和废弃尼龙麻袋样品,在6%溴化钾、1%酒石酸钾钠、0.7%的盐酸、5%磷酸、2%盐酸羟胺、3%(体积)三乙醇胺混合底液中,以单扫描极谱法测定样品中痕量铅的含量.结果表明,铅在滴汞电极上于-0.47V(相对饱和甘汞电极)处产生一灵敏催化极谱波,极谱峰电流与铅浓度在0.2～300ng/mL范围内有良好的分段线性关系,检出限为0.16ng/ml.该方法的RSD为5.6%～7.1%,加标回收率为89%～105%.本法快速简便,准确度高,用于实际样品测定的结果满意.     

硫磺中铅的快速极谱分析

提出用硫化铵-氨水-过氧化氢分解硫磺试样,在0.63 mol/L醋酸—0.60 mol/L溴化钾—0.14 mol/L盐酸羟胺—0.30 mol/L硫酸铵体系中以单扫描极谱测定微量铅的方法.铅极谱峰电位为—0.48 V(相对饱和甘汞电极).铅浓度在0.2～1μg/mL范围内与峰电流成良好的分段线性关系.检出限为0.16 ng/mL.RSD为3.6%～5.6%.加标回收率为86%～93%.此法操作快速简单,用于硫磺中铅的测定,结果满意.     

二次微分电位溶出法测定食品中镉、锌含量

建立了二次微分电位溶出法测定食品中镉、锌含量的方法.优化了试验条件如pH值、电沉积电位、平衡电位等,线性范围:镉0～16 ng,锌0～800 ng;检出限分别为0.24 ng/mL、0.71 ng/mL,RSD<2.5%(n=7).该法测定食品样品结果与石墨炉原子吸收法一致.     

液相色谱-电喷雾串联质谱法快速测定人体血液中左旋甲基炔诺酮的含量

建立了快速测定人体血液中左旋甲基炔诺酮的液相色谱-串联质谱法.样品加入内标后,经过一个简单的预处理,以电喷雾正离子多反应监测方式进行定性定量分析,并且优化了液相和质谱条件.方法简单快速,一个样品的分析时间仅需10min;方法的检出限为0.2 ng/mL,线性范围为0.625ng/mL~35.0ng/mL,测定结果重复性很好,日内和日间的相对标准偏差均小于3.74%,在添加浓度为1.25ng/mL、5.0ng/mL3、5.0 ng/mL时,回收率分别为(92.1±2.8)%,(95.7±3.4)%,(105.8±3.1)%.通过以与新鲜血液比较,经过冷冻~解冻后的血液样品测量值稳定.结果表明,本方法适合于人体血清中左旋甲基炔诺酮含量的测定.     

原子吸收分光光度法测定资丘木瓜中3种重金属含量

建立了测定资丘木瓜药材中铜、铅和镉三种重金属含量的方法:采用火焰原子吸收光谱法检测铜的含量,以石墨炉原子吸收光谱法检测铅和镉的含量.3种重金属测定的检测限为0.0006μg/mL、0.0030ng/mL、0.0024ng/mL,相对标准偏差(RSD)为2.7%、2.9%、1.2%,回收率为100%¹05%,线性相关系数为0.999和0.992、0.995,均符合要求.经测定3批资丘木瓜药材中铜、铅、镉的含量分别为13.53105%,线性相关系数为0.999和0.992、0.995,均符合要求.经测定3批资丘木瓜药材中铜、铅、镉的含量分别为13.53¹6.24 mg/kg、0.016316.24 mg/kg、0.0163⁰.0232 mg/kg、0.22670.0232 mg/kg、0.2267⁰.3364 mg/kg,结果表明:3批木瓜样品中重金属的含量均符合《药用植物及制剂进出口绿色行业标准》中有关重金属标准的规定.     

微分电位溶出法测定食用油中镉含量

建立了微分电位溶出法测定食用油中镉含量的方法.优化了试验条件如pH值、电沉积电位、平衡电位等,线性范围:镉0～16 ng;检出限0.24 ng/mL,RSD=2.4%(n=7).该法测定食品样品结果与石墨炉原子吸收法一致.     

Markedness and its Interpretation in Language Use

Language markedness is a common phenomenon in languages, and is reflected from hearing, vision and sense, i.e. the variation in the three aspects such as phonology, morphology and semantics. This paper focuses on the interpretation of markedness in language use following the three perspectives, i.e. pragmatic interpretation, psychological interpretation and cognitive interpretation, with an aim to define the function of markedness.     

Lower Paleozoic oil relationships within Williston Basin, Canada

The Williston Basin is a significant petroleum province, containing oil production zones that include the Middle Cambrian to Lower Ordovician, Upper Ordovician, Middle Devonian, Upper Devonian and Mississippian and within the Jurassic and Cretaceous. The oils of the Williston Basin exhibit a wide range of geochemical characteristics defined as "oil families", although the geochemical signature of the Cambrian Deadwood Formation and Lower Ordovician Winnipeg reservoired oils does not match any "oil family". Despite their close stratigraphic proximity, it is evident that the oils of the Lower Palaeozoic within the Williston Basin are distinct. This suggests the presence of a new "oil family" within the Williston Basin. Diagnostic geochemical signatures occur in the gasoline range chromatograms, within saturate fraction gas chromatograms and biomarker fingerprints. However, some of the established criteria and cross-plots that are currently used to segregate oils into distinct genetic families within the basin do not always meet with success, particularly when applied to the Lower Palaeozoic oils of the Deadwood and Winnipeg Formation.     

An Analysis of Catherine＇s Character——Wuthering Heights

Wuthering Heights, Emily Bronte＇s only novel, was published in December of 1847 under the pseudonym Ellis Bell. The book did not gain immediate success, but it is now thought one of the finest novels in the English language. Catherine is the key character of this masterpiece, because everybody and everything center on her though she had a short life. We can understand this masterpiece better if we know Catherine well.     

Characterization of Ordovician carbonate reservoirs, southeastern Saskatchewan, Canada

The discovery of the prolific Ordovician Red River reservoirs in 1995 in southeastern Saskatchewan was the catalyst for extensive exploration activity which resulted in the discovery of more than 15 new Red River pools. The best yields of Red River production to date have been from dolomite reservoirs. Understanding the processes of dolomitization is, therefore, crucial for the prediction of the connectivity, spatial distribution and heterogeneity of dolomite reservoirs.The Red River reservoirs in the Midale area consist of 3～4 thin dolomitized zones, with a total thickness of about 20 m, which occur at the top of the Yeoman Formation. Two types of replacement dolomite were recognized in the Red River reservoir: dolomitized burrow infills and dolomitized host matrix. The spatial distribution of dolomite suggests that burrowing organisms played an important role in facilitating the fluid flow in the backfilled sediments. This resulted in penecontemporaneous dolomitization of burrow infills by normal seawater. The dolomite in the host matrix is interpreted as having occurred at shallow burial by evaporitic seawater during precipitation of Lake Almar anhydrite that immediately overlies the Yeoman Formation. However, the low δ18O values of dolomited burrow infills (-5.9‰～ -7.8‰, PDB) and matrix dolomites (-6.6‰～ -8.1‰, avg. -7.4‰ PDB) compared to the estimated values for the late Ordovician marine dolomite could be attributed to modification and alteration of dolomite at higher temperatures during deeper burial, which could also be responsible for its 87Sr/86Sr ratios (0.7084～0.7088) that are higher than suggested for the late Ordovician seawaters (0.7078～0.7080). The trace amounts of saddle dolomite cement in the Red River carbonates are probably related to "cannibalization" of earlier replacement dolomite during the chemical compaction.     

Features of Women's language

Language is a means of verbal communication. People use language to communicate with each other. In the society, no two speakers are exactly alike in the way of speaking. Some differences are due to age, gender, statue and personality. Above all, gender is one of the obvious reasons. The writer of this paper tries to describe the features of women＇s language from these perspectives： pronunciation, intonation, diction, subjects, grammar and discourse. From the discussion of the features of women＇s language, more attention should be paid to language use in social context. What＇s more, the linguistic phenomena in a speaking community can be understood more thoroughly.     

Design and analysis of generic LBS application developing platform

Location based services is promising due to its novel working style and contents.A software platform is proposed to provide application programs of typical location based services and support new applications developing efficiently. The analysis shows that this scheme is easy implemented, low cost and adapt to all kinds of mobile nework system.     

橡胶颗粒沥青混合料低温抗裂性试验研究

以AC-13级配为基础,将橡胶颗粒代替部分集料掺入混合料中,以低温弯曲试验为评价方法对不同橡胶颗粒掺量下沥青混合料的低温抗裂性进行研究,并引入应变能密度值对混合料的低温抗裂性进行综合评价.试验结果表明:橡胶颗粒沥青混合料试件的破坏微应变均超过2 300,满足冬寒区的技术指标;无论是否掺加橡胶颗粒,随着温度的下降,沥青混合料破坏时的最大弯拉强度增大,弯拉应变降低,劲度模量增大;弯曲应变能密度在胶粒掺量为1%左右时具有较大的弯曲应变能密度值,此时橡胶颗粒沥青混合料具有较好的低温抗裂性.     

A computer generator for randomly layered structures

AcomputergeneratorforrandomlylayeredstructuresYUJia shun1,2,HEZhen hua2(1.TheInstituteofGeologicalandNuclearSciences,NewZealand;2.StateKeyLaboratoryofOilandGasReservoirGeologyandExploitation,ChengduUniversityofTechnology,China)Abstract:Analgorithmisintrod…     

低渗透非均质砂岩油藏启动压力梯度研究

理论推导与室内实验相结合,建立了低渗透非均质砂岩油藏启动压力梯度确定方法。首先借助油藏流场与电场相似的原理,推导了非均质砂岩油藏启动压力梯度计算公式。其次基于稳定流实验方法,建立了非均质砂岩油藏启动压力梯度测试方法。结果表明:低渗透非均质砂岩油藏的启动压力梯度确定遵循两个等效原则。平面非均质油藏的启动压力梯度等于各级渗透率段的启动压力梯度关于长度的加权平均;纵向非均质油藏的启动压力梯度等于各渗透率层的启动压力梯度关于渗透率与渗流面积乘积的加权平均。研究成果可用于有效指导低渗透非均质砂岩油藏的合理井距确定,促进该类油藏的高效开发。     

Quantitative trait loci （QTLs） for quality traits related to protein and starch in wheat

Quality traits in wheat （Triticum aestirum L.） were studied by quantitative trait locus （QTL） analysis in a recombinant inbred line （RIL） population, a set of 131 lines derived from Chuan 35050 × Shannong 483 cross （ChSh）. Grains from RILs were assayed for 21 quality traits related to protein and starch. A total of 35 putative QTLs for 19 traits with a single QTL explaining 7.99-40.52% of phenotypic variations were detected on 10 chromosomes, 1D, 2A, 2D, 3B, 3D, 5A, 6A, 6B, 6D, and 7B. The additive effects of 30 QTLs were positive, contributed by Chuan 35050, the remaining 5 QTLs were negative with the additive effect contributed by Shannong 483. For protein traits, 15 QTLs were obtained and most of them were located on chromosomes 1 D, 3B and 6D, while 20 QTLs for starch traits were detected and most of them were located on chromosomes 3D, 6B and 7B. Only 7 QTLs for protein and starch traits were co-located in three regions on chromosomes 1D, 2A and 2D. These protein and starch trait QTLs showed a distinct distribution pattern in certain regions and chromosomes. Twenty-two QTLs were clustered in 6 regions of 5 chromosomes. Two QTL clusters for protein traits were located on chromosomes 1D and 3B, respectively, three clusters for starch traits on chromosomes 3D, 6B and 7B, and one cluster including protein and starch traits on chromosome 1D.