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The result shows, compared with conventional high-temperature leveling agent, the leveling agent JL can reduce the dyeing rate of the higher rate dye, increase the dyeing rate of the lower rate dye, improve the dye compatibility, migration property, and high temperature dispensability.

结果表明,与常规高温匀染剂相比,高温匀染剂JL能使初始上染速率较高的染料上染速率降低,使初始上染速率较低的染料上染速率提高,改善了染料的配伍性,提高了染料的移染性和高温分散性,且对染品的染色牢度影响不大。

TheJiyang depression located in paleomonsoon climate zone in the period of the sahejieformation sedimentation, the wet and hot climate made ancient lake become deeperwater, enhanced stratification, reduced primary productivity of plankton, decreasingsedimentary velocity of carbonate, increasing sedimentary velocity of clay, fortifiedreductibility on certain degree, and then would be available for development of blackshale, dark shale and oil shale; In the contrast, the cold and dry climate lead ancientlake to shallower water, subdued stratification, increaser primary productivity ofplankton, enhancive sedimentary velocity of aphanitic carbonate, decreasedsedimentary velocity of clay, and then would be available for development calciteshale, calcite laminar shale, calcite mudstone, shaly carbonate rock, even laminarcarbonate or dolomite rock.

济阳坳陷在古近系沙河街组沉积期属于古季风气候带,在湿热的气候条件下古湖水加深,分层性增强,浮游生物的古生产力降低,隐晶碳酸盐的沉淀速率变小,粘土沉积速率加快,还原性一定程度上有所加强,有利于黑页岩、油页岩和暗色泥岩的形成:而相对干冷气候下,古湖水变浅,分层性减弱,浮游生物的古生产力增高,隐晶碳酸盐的沉积速率变大,粘土的沉积速率减慢,有利于钙质页岩、钙质纹层页岩、钙质泥岩、泥灰岩甚至纹层状碳酸盐岩、灰岩的发育。

The results as followed:gaining high yield must keep higher flagleaf and canopyphotosynthetic rate after anthesis,highter flag leaf andcanopy photosyntheticrate would be benefit to keep grain filling rate andform high yield.

在旱地高产大田通过对L21与D27两品种旗叶与群体光合速率、籽粒灌浆速率及产量变化的研究,认为旱地小麦要获得高产必须保持花后高的旗叶与群体光合速率,以有利于籽粒灌浆速率维持,形成高产。

It is shown from the analysis results that the average retrogradation rate of the south coastline of the Laizhou Bay during 1958 to 2004 was 27 m/a,the average retreating rate of the 0 m isobath was in the range of 27 to 65 m/a,and the average cutting rate of beach face was 2.1 cm/a.

结果表明,1958-1984年,莱州湾南岸岸线平均侵蚀后退速率为27 m/a,0 m等深线后退速率为27~65 m/a,岸滩平均蚀低速率为2.1 cm/a.1984-2004年,莱州湾南岸岸线位置基本无变化,岸滩平均蚀低速率为1.04 cm/a,水深5 m以浅的区域表层沉积物变粗。

The method for measuring the velocity distribution graph is established when the photosynthate transports along .

速率范围均匀等分成若干个速率区间,以此为横坐标;测量并计算各速率区间对应运输的同化物或水分的相对百分比 Pi,以此为纵坐标,可得液流中同化物分子和水分子运输的速率分布曲线。

In this paper, based on the triaxial test, it is discovered that the structured loess has special mechanical effect of shearing strain rate, and it is proved that the structured loess also has the phenomena of strain rate softening. The CU shear strength and cohesion c increase at first, then decrease with the increase of strain rate, and a critical rate exists; the angel of internal friction doesn't change visibly with the strain rate.

通过结构性黄土三轴试验研究,发现结构性黄土具有独特的剪应变速率力学效应,"应变速率软化"现象同样存在于结构性黄土中;其CU剪切强度和凝聚力c随剪应变率的增大而呈现先增大后减小的特征,存在临界速率现象,而内摩擦角随剪切速率的增大基本上呈线性减小的趋势。

At present,the rate laws and reaction mechanisms of pyrite oxidation,pyrite and chalcopyrite formation,uraninite and magnetite dissolution in aqueous solutions are mainly studied,and it is discovered that (1)oxidation rate of pyrite controlled by surface reaction assume fractional dependence on Fe3+ and O2 molalities in acid solutions;(2)Pyrite cannot nucleate directly from solutions below 300 ℃,it can only form initially through sulfidation of a FeS precursor. The rate equation of reaction between FeS and H2S to form pyrite is of the second order;(3)Chalcopyrite is formed by reactions of pyrrhotite or pyrite with Cu2+,the former proceeds via a series of mediate metastable phases of Cu-Fe sulfide,whereas the rate equation of the latter is apparently of the first order which is controlled by surface reaction;(4)The nonlinear behavior of magnetite dissolution at acid pH can be represented by a shrinking core model coupling with surface reaction and diffusion transport.

目前主要研究了水溶液中黄铁矿氧化、黄铁矿和黄铜矿形成、晶质铀矿和磁铁矿溶解的速率定律和反应机理,发现:(1)酸性溶液中黄铁矿的氧化速率对Fe3+和O2浓度呈分数依赖并受表面反应的控制;(2)低于300 ℃时黄铁矿不能从溶液中直接成核,而需初始地通过FeS先驱物的硫化生成,FeS与H2S反应形成黄铁矿的速率方程为二级;(3)磁黄铁矿或黄铁矿与Cu2+反应均可形成黄铜矿,前者经历了一系列准稳的Cu-Fe硫化物的中间物,后者的速率方程为表观一级并受表面反应的控制;(4)酸性pH时磁铁矿的非线性溶解行为可采用表面反应扩散输运耦合的收缩核模型来描述。

This res ult provides the theoretical basis for the system of zero order release as well as how to control the release rate and the amount of drug release.

根据该模型还从理论上分析了两种限定条件下药物的释放特征:当DmDf时,释放速率变为常数,达到零级释放,其释放速率与药膜无关,这为零级释放缓释体系如何控制释放速率和药物释放量提供了理论依据:当Dm Df时,药物的释放速率与药膜中的释放系数、溶解度和药物的装填量有关,与包膜过程无关,其释放过程类似于混合药膜缓释体系。

After the oxidative polymerization of DMP,styrene was in-situ polymerized under the initiation of dibenzoyl peroxide and dicumyl peroxide,finally thermodynamically compatible PPO/PS alloy was prepared.When styrene content was 50 wt%,for the synthesized PPO/PS alloy the yield and the weight-average molecular weight were determined to be 95%and 1.7×10~5 for PPO,93%and 2.0×10~5 for PS,respectively.The influence of the concentration of DMP and catalyst,molar ratio of N/Cu, oxygen partial pressure,NaOH concentration and temperature on the initial polymerization rate(R_0) of DMP was studied.It was found that the initial polymerization rate of DMP increased with the concentration of DMP and catalyst. The initial polymerization rate increased with the molar ratio of N/Cu at first and then decreased.

通过测定DMP氧化聚合过程中氧气吸收量随时间的变化,研究了DMP和催化剂浓度、N/Cu摩尔比、氧气分压、氢氧化钠浓度及温度对水介质中DMP氧化聚合初始速率的影响,发现DMP氧化聚合初始速率与氧气分压的0.1次方成正比;DMP氧化聚合初始速率随DMP和催化剂浓度及温度的增加而增加;随氢氧化钠浓度和N/Cu摩尔比的增加DMP氧化聚合初始速率先增加后降低。

When the concentration of sulfur dioxide was fixed, the reaction rate increased separately with increasing oxygen content and water vapor content, when oxygen content was 20%, the reaction rate was the highest, while water vapor content was 444μmol/L, there was an optimum value for the photocatalytic degradation rate of heptene.

庚烯的降解速率随着二氧化硫浓度的增加而增加,最终趋于稳定。在二氧化硫浓度一定时,庚烯的反应速率分别随着氧气和水分子含量的增加而不断增大,氧含量为20%时速率最大;水分子含量为444μmol/L时速率最大。

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