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131.
以70%乙醇浸提商陆浆果红色素,采用吸光度值的变化和光谱扫描法研究了光照、温度和pH值对色素稳定性的影响,测定了商陆红色素的还原力、清除DPPH.和OH.的能力.结果表明:商陆红色素在pH3~9较稳定,对光和高温不稳定,因此可以作为冷饮食品的着色剂开发;商陆红色素有一定的还原力和抗氧化性,值得深入研究. 相似文献
132.
稀土光致发光材料的研究现状和应用 总被引:7,自引:1,他引:7
本文就稀土光致发光材料进行了分类 ,对其发光特性作了简要介绍 ,综述了其开发与应用的历史与现状 ,并介绍了其目前在各个领域的应用产品 . 相似文献
133.
以纳米TiO2为催化剂,以砂子为载体,高压汞灯为光源,对粒子元青染料废水进行光催化降解,结果表明,锐钛型TiO2对粒子元青染料有显著的光降解作用,并且讨论了初始pH值,H2O2用量等因素对光催化反应的影响。 相似文献
134.
粉煤灰的酸处理及其对染料脱色效果的影响 总被引:4,自引:0,他引:4
介绍了一种酸处理粉煤灰的方法。用 8mol/L的H2 SO4 处理粉煤灰 ,可较好地改善其表面状况 ,粉煤灰的饱和吸附量明显增大。用处理后的粉煤灰对染料进行脱色试验 ,寻找到了最佳的处理条件 ,取得了较好的脱色效果 相似文献
135.
Carbon isotopic records in paleosols over the Pliocene in Northern China: Implication on vegetation development and Tibetan uplift 总被引:2,自引:0,他引:2
Carbon isotopic composition of pedogenic carbonate can be used to estimate the proportion of C4 and C3 plants. Here we present carbon isotopic data of carbonate in a red earth section at Xifeng, central Loess Plateau. Results
show that C4 vegetation increased in ∼4.4 Ma B.P., stabilized between 4.0 and 3.0 Ma B.P. The character and timing of C4 expansion on the Loess Plateau are similar, but different with other localities, e.g. Pakistan and Africa, implying that
regional climate changes were main factors driving the expansion of C4 plants. This event is comparable in timing with increased aridity evidenced by Xifeng grain size and North Pacific eolian
dust records. Therefore we argue that the Pliocene expansion of C4 plants in northern China might have been caused by the increased aridity, which in turn might be related to rapid uplift
of the Tibetan Plateau. 相似文献
136.
The results of paleogeomagnetics and geochemistry of the coral reef in well Nanyong 2 of Nansha Islands showed that the bottom of the black sedimentary interlayer corresponds to the conversion boundary line between Brunhes Postive Polarity and Matuyama Reversed Polarity (B/M) and the cold/warm (19/20) climatic conversion bounds on δ18O curve, 0.78 Ma ago; and the red sedimentary interlayer corresponds to the ReunionⅠpolarity excursion (reversion) of the geomagnetic field, 2.01—2.04 Ma ago. Comparing with the normal light-coloured coral reef rock, the magnetic susceptibility (c), residual magnetization intensity (Mr) and the content of MnO and Fe2O3 of the black sedimentary layer appeared obviously positive abnormity. The magnetic susceptibility (c), residual magnetization intensity (Mr) and the content of Fe2O3 of the red sedimentary layer also appeared positive abnormity. Combining with the analyzing results of paleontology, we hold that this pair of special and typical sedimentary interlayers was relative to the sudden change of paleoclimate, i.e. the global climatic change and its incidental polarity reversal of the geomagnetic field directly affected the living environment of the paleontological species as well as the dispersion and enrichment of some chemical elements, especially the elements sensitive to redox such as Fe and Mn. For example, the elements Fe and Mn concentrated in the glacial period would be largely oxidized and diluted when the climate warmed up suddenly, and the originally oxidized high valence Fe would be condensed again when the climate cooled suddenly. This is possibly one of the important reasons of appearing and disappearing of the red and black sedimentary events of coral reef in well Nanyong 2. 相似文献
137.
The ecological sequence of Hipparion fauna in the mid-dle reaches of the Yellow River during Neogene
The faunal ecological type and sequence in the Tertiary red clay indicate that Hipparion fauna during the period 7.4-6.1 Ma in the middle reaches of the Yellow River is composed mainly of dorcadoides and mixed types. This represents semiarid veld environment with small fluctuation. The fossil assemblages characterized by the abundance of gaudryi types and even the occurrence of some Hominoid and Chalicotherium indicate an obviously warm and humid period since 5.3 Ma. The fossil assemblages during 3.4 Ma show the typical steppe fauna representing dry climate. It is indicated by the changes of ecological sequence that the climatic conditions in Pliocene are drier than that in late Miocene. The clay-skin content of red clay, which has a synchronous change with faunal features, is a rather good replacing palaeoclimatic index. 相似文献
138.
A mutant strain of E.coli showing strong green fluorescence is obtained during the study of cloning and expression of blue fluorescent protein gene bfp. A recombinant plasmid pHN122 has been isolated. It is demonstrated by enzyme digestion, subcloning and sequence analysis that it contains both of bfp and gfpK79R mutant genes. The results of spectrometric analysis show that GFPK79R expressed by pHN122 is the same as the wild type GFP, but its fluorescent intensity is increased 1.25~2.44-fold. 相似文献
139.
The faunal ecological type and sequence in the Tertiary red clay indicate that Hipparion fauna during the period 7.4–6.1 Ma in the middle reaches of the Yellow River is composed mainly of dorcadoides and mixed
types. This represents semiarid veld environment with small fluctuation. The fossil assemblages characterized by the abundance
of gaudryi types and even the occurrence of some Hominoid and Chalicotherium indicate an obviously warm and humi period since 5.3 Ma. The fossil assemblages during 3.4 Ma show the typical steppe fauna
representing dry climate. It is indicated by the changes of ecological sequence that the climatic conditions in Pliocene are
drier than that in late Miocene. The clay-skin content of red clay, which has a synchronous change with faunal features, is
a rather good replacing palaeoclimatic index. 相似文献
140.
对于基因芯片实验的动力学范围和结果可重复性的研究 总被引:2,自引:0,他引:2
杂交动力学和实验结果的可重复性是基因芯片研究中十分重要的内容,以单基因模拟芯片对DNA芯片的杂交动力学进行了初步的研究:将不同含量的植物cDNA点在玻片上制成DNA芯片,利用体外转录的方法得到植物基因的mRNA,然后通过反转录方法把荧光标记到cDNA上,用不同含量的荧光标记cDNA对芯片进行杂交,根据结果分析了靶基因和探针含量变化对芯片杂交信号产生的影响,利用多基因模拟芯片分析了不同基因的杂交动力学特点;利用12800点的高密度芯片进行了2组不同的表达谱实验,对芯片结果的可重复性做了验证。 相似文献