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high crystallization
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  高结晶度
     Firstly high crystallization Mg-Al carbonic hydrotalcite and alanine-intercalated hydrotalcite were produced by the "urea method" and ion exchange;
     为此,论文首先研究了高结晶度Mg-Al碳酸根型水滑石的合成以及丙氨酸柱撑水滑石的离子交换法制备工艺;
短句来源
     Layered zirconium (proline-N-methylphosphonate-phosphate)(α-ZPMPP) was prepared with high crystallization(interlayer distance is 1.52 nm). The intercalation of n-butylamine into α-ZPMPP was also investigated at room temperature. α-ZPMPP and its intercalation complex were characterized by element analysis, IR, XRD and TG-DSC method.
     以高结晶度制备了层状 (脯氨酸 -N -甲基膦酸 -磷酸氢 )锆 (α-ZPMPP)晶体 (层间距为 1 .5 2 nm ) ,并研究了其常温下对正丁胺的插层性能 ,用元素分析、IR、XRD和 TG-DSC热分析对 α-ZPMPP及其插层复合物进行了表征 .
短句来源
  高的生长
     The high crystallization activation energy for MAP zeolite reveals the reason for seeding while synthesis.
     MAP高的生长活化能以及A型沸石相对低的成核与生长活化能揭示合成MAP沸石时使用晶种的原因.
短句来源
  “high crystallization”译为未确定词的双语例句
     The properties of blue green laser induced crystallization for as deposited Ag 11 In 12 Sb 51 Te 26 phase change thin films irradiation are studied by measuring the reflectivity contrast at 500, 100 and 60 ns pulse duration. The results show that Ag 11 In 12 Sb 51 Te 26 phase change thin films irradiated by blue green laser have high crystallization speed.
     用反射率对比度来衡量晶化程度,分别探讨了脉宽为500ns,100ns,60ns的蓝绿激光(514nm)作用下沉积态Ag11In12Sb51Te26相变薄膜的晶化性能,表明Ag11In12Sb51Te26相变薄膜在蓝绿激光下可具有较高的晶化速度。
短句来源
     The experiment manifested the (VO)_2P_2O_7 catalyst with high crystallization occupied higher selectivity in various VPO catalysts.
     实验结果表明加入助剂后的催化剂和未加助剂时的催化剂的主要活性相相同,都是(VO)_2P_2O_7。
短句来源
     Results show that LS added in dry or wet way to PET produces NPET with 300% high crystallization rate, 30 nm~70 nm of particle size, and about 3%~4% (in number) agglomerations, which are phase separated from PET matrix, and reduce PET toughness.
     LS以干态或湿态加入使PET结晶速率提高3倍左右,无机相以平均30nm~70nm尺度分散于PET基体,有约3%~4%数量的凝聚粒子与基体相分离,使NPET冲击韧性下降。
短句来源
     The experiment manifested the (VO)2P2O7 catalyst with high crystallization occupied higher selectivity in various VPO catalysts.
     实验表明不同晶相的VPO催化剂中以结晶度较高的(VO)_2P_2O_7相催化剂表现出很高的选择性;
短句来源
     The results showed that monocarboxylic acid stearic acid played a role of surfactant, and the product was still orthorhombic Ce2O(CO3)2·H2O with a high crystallization degree.
     实验结果表明在尿素及硝酸铈的混合溶液中分别加入一元羧酸硬脂酸,二元羧酸酒石酸和三元羧酸柠檬酸时,一元羧酸硬脂酸在混合溶液中只起表面活性剂的作用,其产物为斜方晶系的单晶Ce2O(CO3)2.H2O微粉,且表面活性剂硬脂酸的加入使得晶体的晶化程度明显提高;
短句来源
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  相似匹配句对
     High-throughput crystallization in pharmaceutical research and development
     药物研究与开发中的高通量结晶技术
短句来源
     Role of High - temperature Treatment on Crystallization of Turbostratic B - C - N
     高温处理对乱层石墨结构B-C-N晶化的作用
短句来源
     Climbing high
     高高在上
短句来源
     FLYING HIGH
     飞得更高
短句来源
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  high crystallization
A collapsed spherulite appeared in the oligomer-rich fraction at high crystallization temperatures.
      
At high crystallization temperatures, both the DSC and the SEM also provided evidence of a significant rejected linear fraction, which appeared to decorate the sorbitol network on quenching.
      
The orientation is mainly due to the high crystallization rate of PBT, although crystallization and orientation of PBT in the PBT and LCP blends could also be induced by adding LCP.
      
All these formulations, showing a high crystallization rate, and a fast heating rate, can be used as tile glazes and/or tile-glaze components.
      
Two kinds of morphologies have been observed, particularly at high crystallization temperatureTc, on thin sections of the same sheets: a spherulitic one in the centre and a row-like structure on the edges.
      
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The crystallization kinetics of poly (phenylene sulfide) (PPS) and its carbon fibre composites were investigated by dilatometry. An appreciable deviation from the Avrami equation was found for PPS-carbon fiber composites. PPS exhibits a moderate crystallization rate, and possesses a low σσ value, packing density coefficient kc, and a low pre-exponential term G0 of the equation of crystallization kinetics, in compare with polymers such as PE, PMO etc. Go has been found to be the chief factor...

The crystallization kinetics of poly (phenylene sulfide) (PPS) and its carbon fibre composites were investigated by dilatometry. An appreciable deviation from the Avrami equation was found for PPS-carbon fiber composites. PPS exhibits a moderate crystallization rate, and possesses a low σσ value, packing density coefficient kc, and a low pre-exponential term G0 of the equation of crystallization kinetics, in compare with polymers such as PE, PMO etc. Go has been found to be the chief factor for the crystallization rate of polymers. Those polymers which possess a lower ρa/ρc value will probablly show a higher crystallization rate.

用膨胀计法研究了聚苯硫醚及其碳纤维复合材料的结晶动力学行为。发现其碳纤维复合材料对Avrami方程有较明显的偏离。聚苯硫醚具有中等的结晶速率,与PE、PMO等高聚物比较,它的σσ_c值、堆砌系数K_c以及结晶动力学方程中的前置指数G_0值较低。G_0是决定高聚物结晶速率的主要因素,ρ_a/ρ_c(值较小的高聚物有可能出现较高的结晶速率。

Crystallization and orientation of PET films of different crystallization rates have been studied doing various techniques during stretching. It is found that under the same conditions of stretching the extent of crystallization and degree of orientation are higher within the sample of higher crystallization rateThis difference in structural change implies that it is reasonable to ascribe the difference of the two samples in tensile behavior to their crystallization rates.

用多种方法对两个结晶速率不同的PET样品在拉伸过程中的结晶和取向进行了研究。结果表明在同样的拉伸条件下,结晶速率较快的样品的结晶度和取向程度均比另一样品要高得多,这种结构变化上的差别说明把拉伸行为的差别归因于结晶速率的不同是合理的。

Mesozoic volcano-intrusive activities of Tonglu are characterized by multiple eruption-extrusion-intrusion of some magma source. The thermo-baro-geochemical study of magmatic inclusions in minerals reveals that the calc-alkaline magma produced by the partial melting of lower crustal materials had evidently differentiated in the magma reservoir. The depth of magma reservoir is about 10—11 kilometers(value of upper limit). The potential H_2O content of the volcanic magma is in the range of 4 to 6 percent by weight....

Mesozoic volcano-intrusive activities of Tonglu are characterized by multiple eruption-extrusion-intrusion of some magma source. The thermo-baro-geochemical study of magmatic inclusions in minerals reveals that the calc-alkaline magma produced by the partial melting of lower crustal materials had evidently differentiated in the magma reservoir. The depth of magma reservoir is about 10—11 kilometers(value of upper limit). The potential H_2O content of the volcanic magma is in the range of 4 to 6 percent by weight. In the evolution history of volcanic activity, the acidic-intermediate acidic differentiated magma located in the upper part of magmatic reservoir,with higher fo_2(10~(-14.28)-10~(-15.77)·10~5Pa)and lower P_(total)(H_2O)(<100 MPa) erupted and extruded first. The acidic magma erupted earliest out of the surface and formed the rhyolitic, dacite-rhyolitic ash-flow tufts. Then the intermediate-acidic magma located in lower layer extruded out of the surface or near the surface and formed the porphyroclastic dacite of extrusive facies, Owing to the shallow location or outcropping of surface of magma, most of volatile components (water vapour and so on) dissolved in magma escaped outward, and this resulted in higher crystallization temperatures of minerals and lower fco_2, fH_(2O), fH_(2), fN_(2),fH_(2)S. In this course of magma evolution, with the passage of time of volcanic activities, the location of ascending magma in magmatic reservoir became deeper and deeper, the basicity and P_(total) of magma continued to increase, fo_2 decreased progressively, and these resulted in a progressive decrease of crystallization temperatures of minerals(quartz: 1144℃→1112℃→948→896℃; plagioclase: 1144℃→965℃→919℃). The intermediate differentiated magma, which was located in the lower part of magmatic reservoir and had lowest fo_2(10~(-18.89)·10~5Pa) and highest P_(total)(H_2O) (up to 300—320 MPa), intruded upward lastly and formed sub-volcanic stocks and hypabyssal intrusive body of quartz-monzonite—quartz-monzodiorite. Because of their deeper location, the volatile components dissolved in magma were well preserved (the total contents of volatile components dissolved in magma reached 9.52 wt.% and the av erage content of water was about 6.4 wt. %), thus resulting in a decrease in crystaUization temperatures of minerals(plagiocIase: 919℃, quartz: 761—797℃). For each volcanic event, with progressing fractional crystallization of magma , the SiO_2 contents in magma increased, the contents of FeO, MgO, CaO, Na_2O, K_2O, Al_2O_3 decreased and the crystallization temperatures of minerals decreased also. During the fractional crystallization of dacitic and andesitic magma, which did not outcrop out of the surface, their oxygen fugacities decreased to some extent. For the rhyolitic magma, which had erupted out of the surface, owing to a continued supply of atmospheric oxygen in the course of ascending-erupting of magma, the oxygen fugacities increased, on the contrary,to some extent with progressing fractional crystallization of magma.

桐庐中生代火山侵入活动为同源多期喷发-侵出-侵入。矿物中岩浆包裹体温压地球化学研究表明,由下地壳部分熔融产生的钙碱性岩浆,在火山岩浆房内已经发生明显分异。火山岩浆房的深度约为10—11km(上限值)。火山岩浆中含水4—6%(重量%)。在火山活动演化史中,岩浆房上部的酸性分异岩浆,fo_2相对较高,P总(H_2O)较低,先行喷出地表形成流纹质、英安流纹质灰流凝灰岩。层位稍下的中酸性岩浆稍后挤出地表或挤入近地表浅部,形成侵出相碎斑英安岩。岩浆房下部的中性分异岩浆,fo_2最低(10~(-13·29)Pa),P总(H_2O)最高(300—320MPa),最后上侵,形成石英二长岩-石英二长闪长岩等浅成侵入体。

 
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