990 resultados para 890
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论市场经济体制下自然资源的合理利用李法云,范志平(中科院沈阳应用生态研究所)一、计划经济体制下自然资源利用中存在的问题经济社会中的资源配置是指各种生产要素的优化组合,是自然资源与社会资源之间的协调;在计划经济体制下,由于没有形成标志资源稀缺性的合理价...
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新型多功能蔬菜育苗母剂多功能蔬菜育苗母剂是中国科学院沈阳应用生态研究所最新科研成果,并获国家发明专利,现已被列入辽宁省“九五”期间重点推广计划项目,几年来在全国各地应用效果明显,深受广大菜农欢迎。多功能蔬菜育苗母剂可为菜苗提供全面合理的营养,促进苗齐...
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The morphologies and structures for the thin film of blend systems consisting of two asymmetric polystyrene-block-polybutadiene (SB) diblock copolymers induced by annealing in the vapor of different solvents, namely, cyclohexane, benzene, and heptane, which have different selectivity or preferential affinity for a certain block, were investigated by tapping mode atomic force microscopy (AFM) and transmission electron microscopy (TEM). The results revealed that even a slight preferential affinity of good solvent for one block would strongly alter the morphology of the blend thin film.
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Recent advances and key strategies in capillary electrophoresis and microchip CE with electrochemical detection (ECD) and electrochemiluminescence (ECL) detection are reviewed. This article consists of four main parts: CE-ECD; microchip CE-ECD; CE-ECL; and microchip CE-ECL. It is expected that ECD and ECL will become powerful tools for CE microchip systems and will lead to the creation of truly disposable devices. The focus is on papers published in the last two years (from 2005 to 2006).
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Near infrared (NIR) light emitting diodes employing composites of an IR fluorescent dye, CdSe/CdScore/shell semiconductor quantum dots and poly( N-vinylcarbazole) (PVK) have been demonstrated. The device, with a configuration of indium-tin-oxide (ITO)//PEDOT:PSS//PVK:NIR Dye:CdSe/CdS//Al, had a turn-on voltage of 7 V, emitted the NIR light with a maximum at 890 nm and the irradiance intensity of 96 mu W. The electroluminescence efficiency of 0.02% was achieved at a current density of 13 mA cm(-2).
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A chemically modified electrode (CME) constructed by adsorption of aquocobalamin (VB12a) onto a glassy carbon electrode surface was demonstrated to catalyze the electro-oxidation of cysteine, a sulfhydryl-containing compound. The sulfhydryl oxidation occured at 0.54-0.88 V vs. Ag/AgCl depending on pH value (3.0-10.0). The electrocatalytic behavior of cysteine is elucidated with respect to solution pH, operating potential and other variables as well as the CME preparation conditions. When used as the sensing electrode in flow injection amperometric detection, the CME permitted detection of the compound at 0.8 V. The detection limit was 1.7 pmol. The linear response range went up to 1.16 nmol. The stability of the CME was shown by RSD (4.2%) over 10 repeated injections.
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用a-Fe_2O_3研制成的加热式气敏元件功耗大(约1.5W)。常温SnO_2-a-Fe_2O_3气敏元件功耗低(约0.1W),灵敏度高,响应恢复快,稳定,具有一定选择性。 气敏元件制备方法:按62.5%,6.2%和31.3%称取SnO_2,a-Fe_2O_3和硅胶,加水研磨2小时,使其呈浆糊状,点入模具内,放入一对φ0.05mm铂丝电极,晾干,脱模,在860~890℃空气中烧结95分钟。
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由于生长环境的特殊性,红树林及其内生真菌的代谢产物在化学类型和生物活性方面都具有多样性,因此对其代谢产物的研究引起了人们越来越多的关注。本论文以菌丝体生物量、代谢产物量等指标及薄层色谱分析、高效液相色谱分析、抗菌活性测试等筛选手段对来源于我国海南红树植物的九株内生真菌在四种不同液体培养基上的静置发酵产物进行了综合评价,并从中选择了来源于半红树植物黄槿(Hibiscus tiliaceus)的内生真菌G2——赤散囊菌(Eurotium rubrum)进行了30 L规模发酵(采用PDB培养基)和次生代谢产物的研究,对分离得到的部分化合物进行了初步的生物活性评价。此外,本论文还对海南真红树植物红海榄(Rhizophora stylosa Griff.)的化学成分进行了研究,并对分离得到的部分化合物进行了二苯代苦味酰自由基(DPPH)清除活性的评价。 采用常规的硅胶柱层析、Sephadex LH-20柱层析、反相硅胶柱层析、制备薄层层析(pTLC)、重结晶等分离手段,分离纯化得到单体化合物。综合运用现代波谱技术 (IR、UV、MS、1D-NMR 和 2D-NMR) 以及与标准品或文献比对鉴定单体化合物的结构。从G2菌丝体和发酵液的合并提取物中鉴定了45个化合物的结构,其中13个为新化合物,结构类型包括6个苯甲醛类化合物(ER1*~ER6*)、4个蒽醌类化合物(ER15*~ ER18*)和3个含吲哚的二酮哌嗪生物碱类化合物(ER27*~ER29*)。 对以上分离鉴定的部分单体化合物进行了DPPH自由基清除活性、拒食杀虫活性、抗细菌活性以及体外细胞毒活性的初步评价。新化合物ER15*和三个已知化合物ER20、ER39和ER40都表现很强的DPPH自由基清除活性。化合物ER15*还表现较好的拒食杀虫活性,而化合物ER5*和ER18*不但没有杀虫活性,反而能促进幼虫的生长。所测试的化合物只有ER15*和ER18*表现出微弱的抗金黄色葡萄球菌活性。所测试的化合物对A-549、HL-60和P-388细胞株均未表现出有意义的体外细胞毒活性。 从红海榄枝条的提取物中分离鉴定了29个化合物,其中2个为新化合物,包括1个三萜酯(RS1*)和1个黄烷醇类化合物(RS12*);另有1个三萜酯(RS5)和1个黄烷醇类化合物(RS11)作为新的天然产物被分离鉴定。 对从红海榄提取物乙酸乙酯相和正丁醇相分离得到的部分单体化合物进行了DPPH自由基清除活性的研究。黄烷醇类化合物RS16和RS17显示最强的活性。另外,实验结果说明黄烷醇类化合物的DPPH自由基清除活性与其分子中所含的羟基数目有一定关系,而且若芳香环上有多个邻位酚羟基,则该化合物的活性将增强。本论文实验结果为海南红海榄植物资源的利用提供了化学成分及抗氧化活性方面的科学依据。
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在植物生长室中,UV-B辐射明显降低黄瓜幼苗的根系活力,抑制程度随辐射时间的延长而增强.黄瓜和大豆幼苗的叶绿素和可溶性蛋白含量减少与UV-B辐射时间长短呈正相关,但是类胡萝卜素减少幅度不大.UV-B对Chlb的破坏较Chla严重,导致Chla b比值增大.UV-B虽增加大豆幼苗的SOD活性,但降低大豆幼苗的NR活性及其对温度变化的敏感性.分析认为,Chlab比值和SOD 活性升高,有助于植物对UV-B的适应。
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The most novel aspect of this thesis is the combination analysis of the boron isotopes and trace elements. What’s more, it also provides a reliable analytical technique, which is suitable for both boron isotopes and trace elements. Al/Ca values can be used to monitor the clay removal during the sample preparation. It is found that when Al/Ca>100 mol/mol, the measured boron isotopic compositions are always several permil lower than those properly cleaned. B/Ca ratios can be used to calculate the exact boron loaded for each sample. Otherwise, too much loading will lead to too long time for the whole analytical sequence, and too less loading might incur serious blank problem. One other benefit besides those discussed above is that the combination analysis of boron isotopes and trace elements on the same sample allows reconstruction of the marine carbonate system and atmospheric pCO2 without assumption of the other parameter. In the marine carbonate system, with the seawater pH from the foraminiferal 11B, one has to make an assumption on the other variable to obtain the rest four variables. A series studies found that U/Ca and B/Ca are potential proxies for seawater [CO32-]and [HCO3-], respectively. Since they are measured on the same sample with boron isotopes, hence, there is no spatial or temporal ambiguity in the incorporation of the two controlling parameters. With 11B and U/Ca, the reconstructed atmospheric pCO2 variations match the atmospheric pCO2 record from the Vostok ice core within ±20 ppm. The incorporations of U and B into foraminiferal carbonates are controlled by the overall growth rate of individual foraminifers and other possible factors. The reliable application of these proxies still require further calibrations. In a similar fashion, the combination analysis of boron isotopes and Mg/Ca also has great advantages. Mg/Ca has been proved to be a reliable proxy for the surface seawater temperature. With the combination analysis, one can determine the phase between changes in atmospheric pCO2 and surface seawater temperature, thus explore the cause and mechanism of the changes in atmospheric pCO2. .
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The occurrence of Late Cretaceous mafic dykes and their entrained peridotite and granulite xenoliths as well as clinopyroxene xenocrysts in the Qingdao region provide us a precious opportunity to unveil the nature and characteristics of the Late Mesozoic lithospheric mantle and lower crust beneath the Jiaodong region, and the change of the magma sources. These studies are of important and significant for understanding the lithospheric evolution in the eastern North China Craton. There were two periods of magma activities in Late Mesozoic in Qingdao Laoshan region, one was around 107Ma in the Early Cretaceous and the other around 86Ma in the Late Cretaceous according to the whole rock K-Ar age determination. The Early Cretaceous mafic dykes and the Late Cretaceous mafic dyke (i.e. Pishikou mafic dike) have completely different geochemical characteristics. The Early Cretaceous mafic dykes are enriched in LILE, strongly depleted in HFSE (Nb, Ta, Zr, Hf) and characterized by the highly radiogenic Sr and Nd isotopic compositions. These geochemical features indicate that the Early Cretaceous mafic dykes were derived from an enriched lithospheric mantle. In contrast, the Late Cretaceous mafic dyke is enriched in LILE, without HFSE depletion (Nb, Ta, Zr, Hf) and has less radiogenic Nd and Sr isotopic compositions. These geochemical features indicate that the Late Cretaceous mafic dyke was derived from the asthenosphere modified by subducted pelagic sediment contamination. The intrusive age of the Late Cretaceous mafic dyke provides further information for the termination of the lithosphere thinning for the eastern North China Crtaon. Pishikou Late Cretaceous mafic dyke contains abundant peridotitic xenoliths, granulite xenoliths and clinopyroxene xenocrysts. The peridotitic xenoliths can be divided into two types: high Mg# peridotites and low Mg# peridotites, according to their textural and mineral features. The high-Mg# peridotites have high Fo (up to 92.2) olivines and high Cr# (up to 55) spinels. The clinopyroxenes in the high# peridotites are rich in Cr2O3 and poor in Al2O3. The low-Mg# peridotites are typified by low Mg# (Fo <90) in olivines and low Cr# (Cr# <0.14) in spinels. The clinopyroxenes in the low-Mg# peridotites are rich in Al2O3 and Na2O and poor in Cr2O3. These two type peridotites have similar equilibrated temperatures of 950C-1100C. The Clinopyroxenes in the high-Mg# peridotites generally have high and variable REE contents (REE = 5.6-84 ppm) and LREE-enriched chondrite-normalized patterns ((La/Yb)N>1). In contrast, the clinopyroxenes in the low-Mg# peridotites have low REE contents (REE = 12 ppm) and LREE-depleted patterns ((La/Yb)N<1). The textural, mineral and elemental features of the low-Mg# peridotites are similar to those of the low-Mg peridotites from the Junan, representing the newly-accreted lithospheric mantle. However, the mineralogical and petrological features of the high-Mg# peridotites are similar to those of the high-Mg# peridotites from the Junan region, representing samples from the old refractory lithospheric mantle that was strongly and multiply affected by melts of different origins Late Cretaceous mafic dike in the Qingdao region also contains two types of granulite xenoliths according to the mineral constituents: the pyroxene-rich granulites and the plagioclase-rich granulites. Equilibrated temperatures calculated from the cpx-opx geothermometers are in a range of 861C - 910C for the pyroxene-rich granulites and of 847C - 890C for the plagioclase-rich granulites. The equilibrated pressure for the plagioclase-rich granulites is in a range of 9.9-11.7 kbar. Combined with the results of the peridotitic xenoliths, a 40C temperature gap exists between the peridotite and the granulite. The petrological Moho was 33~36 km at depths, broadly consistent with the seismic Moho estimated from the geophysical data. This indicates that there was no obvious crust-mantle transition zone in the Qingdao region in the Late Mesozoic. Pishikou Late Cretaceous mafic dyke entrained lots of clinopyroxene xenocrysts which are characterized by the chemical zoning. According to the zoning features, two types of clinopyroxene xenoliths can be classified, the normal zoning and the revise zoning. The normally-zoned clinopyroxene xenocrysts have LREE-depleted REE patterns in the cores. In contrast, the revisely-zoned clinopyroxenes have LREE-enriched REE patterns in the cores. According to the rim and core compositions of xenocrysts, all the rims are balanced with the host magma. Meanwhile, the origins of the cores were complicated, in which the normally-zoned clinopyroxenes were derived form the lithospheric mantle and some of the reversely-zoned clinopyroxnes were originated from the lower crust. Other revisely-zoned clinopyroxenes had experienced complex geological evolution and need to be further investigated. According to the above results, a simplified lithospheric profile has been established beneath the Qingdao region and a constraint on the nature and characteristics of the lithospheric mantle and lower crust has been made.
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The classical method for preparation of covalently boned cellulose derivative chiral stationary phases (CSP) with diisocyanate as spacer was improved. Diisocyanate was firstly allowed to react with 3-aminopropyltriethoxysilane, and the resulting product was then applied as the spacer reagent to immobilize cellulose derivatives onto silica gel. Influences of the amount and the length of the spacer on the optical resolution ability of the CSP were investigated. Comparing improved procedure to classical diisocyanate method, the cross-linking between the glucose units of the cellulose derivatives was avoided to the most extent. With the improved procedure, regio-nonselective ways could be adopted to prepare covalently bonded CSP, which showed an advantage for the rapid preparation.