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We dont undrr stand what you are doing if we pay for the samples, promote it free for you and also pay for their frieght, please rethink and ammend your plans for this proposed long term busiess if we must go ahead.

如果既要我方承担样品费,还要免费为其促销甚至承担其运费,那我们这样不是在做亏本买卖吗?为了我们双方的业务关系能够长期发展下去,务必请你方重新考虑样品费的问题。

The 17 of them were tentatively identified as Peonidin3-galactoside, Delphinidin3-galactoside, Cyanidin3-galactoside,Cyanidin3-glucoside,Petunidin3-galactoside ,Petunidin3-glucoside,Cyanidin3-arabinoside,Peonidin3-glucoside, Malvidin3-galactoside,Mal-vidin3-glucoside,Malvidin3-arabinoside,Petunidin3-arabinoside,Delphinidin3- glucoside,Peonidin3-(6''-acetyl)galactoside,Malvidin3-(6''-acetyl)galactoside,Peonidin3-(6''-acetyl)glucoside,Malvidin3-(6''-acetyl)glucoside.

通过制备型高效液相色谱制备2种花色苷单体,经紫外、红外、质谱、核磁共振分析鉴定,样品1主要为锦葵色素3-半乳糖苷,样品2主要为锦葵色素3-葡萄糖苷。

It has been shown in the Al(Na+K+Ca/2) diagram that the Jinla granitoids are all plotted within the area of "S" type of granites, but the samples from Laochang amphibole admellite, Menglinshan biotite admellite and Nanla K-feldspar graniteporphyry are scattered gradually far away from the boundary between "I" and "S" types of granites, implying that the components from the upper mantle gradually decreasing from the Laochang amphibole admellite to the Menglinshan biotite admellite and then to the Nanla K-feldspar granite porphyry.

3上述三类花岗岩样品皆位于S型花岗岩区,但从老厂似斑状角闪二长花岗岩,勐林山似斑状黑云二长花岗岩,到南腊碱长花岗斑岩,样品分布逐渐远离"I"型花岗岩和"S"型花岗岩的分界线,这表明自老厂似斑状角闪二长花岗岩至勐林山似斑状黑云二长花岗岩,到南腊碱长花岗斑岩幔源组分逐渐减少。

This article uses the microwave oven separately to use 700W,336W processing for 3min on pretreatment of three vegetables(celery,greengrocery and green soy bean),andusing the ultrasonic wave extraction process and 70%methyl alcohol to withdraw,then Uses the spectrophotometer method to determine and compare total flavonoid content of the three vegetables in which two samplewere processed by microwave,and the other was fresh.

本文利用微波炉对新鲜的三种常食蔬菜进行处理,分别用700W,336W处理3分钟,采用超声波提取法用70%的甲醇进行提取,然后用分光光度法对三种蔬菜未经微波处理的新鲜样品和经两种微波处理的样品进行总黄酮含量的测定和比较。

Seven molybdenite samples from greisen ore body and quartz vein tungsten ore body associated with black tungsten ore were chosen for Re-Os isotopic dating and model age of (141.4±2.2) Ma~(158.2±2.2) Ma were obtained. The isochrone age of molybdenites from greisen type tungsten-tin ore body is (156.8±3.9) Ma, which indicates that its mineralogenetic epoch is at the Middle Jurassic, corresponds to the second stage of early Yanshanian period. And the model age for the samples from greisen ore body and from quartz vein ore body are (150.7±2.4) Ma~(158.2±2.2) Ma and (141.4±2.2) Ma~(151.0±2.4) Ma respectively, which indicates that the mineralization time of the quartz vein ore body is slightly earlier than that of greisen ore body.

文章选取云英岩型矿体及上部石英脉型钨矿体中与黑钨矿共生的辉钼矿7件,进行Re-Os等时线年龄测定,得到其模式年龄为(141.4±2.2) Ma~(158.2±2.2)Ma,其中云英型钨锡矿体中辉钼矿等时线年龄为(156.8±3.9)Ma,成矿时代为中侏罗世,对应于燕山早期第二阶段;从云英岩矿体中样品模式年龄为(150.7±2.4)Ma~(158.2±2.2)Ma,石英脉型矿体中样品模式年龄为(141.4±2.2)Ma~(151.0±2.4)Ma。

Its excellent slide properties and higher hardness were utilized so that the composite of Co-P- PTFE has already possessed better tribological propetties with no heat treatment. The crystal analysis presents the composite of Co-P-PTFE has the structure of hexagonal system at plating state and its forming process has obviously the trend on a certain direction.

结构分析表明,Co-P-PTFE复合镀层镀态时即以六方密排晶体结构存在,它的形成过程有强烈的择优取向倾象,六方密排钴的(100)面平行于样品表面且衍射峰明显增强,热处理后的样品有部分固溶体形成。

New methods of measurements of specimen thickness and non-elastically scattering mean free path are proposed based on the electron holograph combining with electron dynamic diffraction.

而且,在电子全息照片和电子动力衍射相结合的基础上我们提出了一种测量电镜样品厚度和样品非弹性散射自由程的新方法。

For the sample consisted of plagioclase, clinopyroxene and hornblende, rheological behaviors are controlled by plagioclase and clinopyroxene when the content of hornblende is less than 10%, however, the role of hornblende could become significant for deformation of samples when the content of hornblende is higher than 10%.

由斜长石、单斜辉石和角闪石组成的样品中,当斜长石和单斜辉石含量接近,而角闪石含量低于10%,斜长石和单斜辉石控制了岩石的流变;如果样品中有超过10%的角闪石参与流变,角闪石在变形中所起作用非常显著。

For the sample with major mineral of plagioclase, quartz and hornblende, rheological behaviors are dependent on plagioclase and hornblende when content of quartz is less than 10%, but when plagioclase content is near 70% it will decide the deformation behaviors of the samples. In contrast to that, quartz could completely control the creep of samples when its content is higher than 20%.

由斜长石、石英和角闪石组成的样品,当石英含量小于10%而斜长石和角闪石含量接近时,斜长石和角闪石控制了岩石的流变;当斜长石含量达到70%时,样品变形更接近长石特性;如果石英含量超过20%时,石英在变形中起到主要作用。

Clay minerals in PM〓 collected during dust storm reached 40.3% and hornblende could been found in this kind sample, but in no-dust storm PM〓 just had a percentage of 29% and hematite could been found.

沙尘暴PM〓样品中粘土矿物的含量高达40.3%,含有角闪石没有赤铁矿;非沙尘暴PM〓样品中粘土矿物的含量为29%,没有角闪石却有赤铁矿。

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