助手标题  
全文文献 工具书 数字 学术定义 翻译助手 学术趋势 更多
查询帮助
意见反馈
   no stratification 的翻译结果: 查询用时:0.009秒
图标索引 在分类学科中查询
所有学科
更多类别查询

图标索引 历史查询
 

no stratification
相关语句
  没有分层现象
     The stability of fluids(2.45%) was increased with increasing molecular weight and concentration of dextran. As for the fluid coated with 50% dextran 40000,no stratification appeared after placing at room temperature more than 72 h.
     随葡聚糖相对分子质量和浓度的升高,磁流体(2.45%)的稳定性上升,用50%葡聚糖40000水溶液制备的磁流体,在室温静置72 h以上,没有分层现象
短句来源
  “no stratification”译为未确定词的双语例句
     5. The percent germination of the seeds,which were treated with concentrated sulfuric acid for 0.5 hours to 7 hours,and then infiltrated with water for 30 hours or longer,was lese than 2%,if the seeds had no stratification treatment.
     5、经硫酸处理0.5-7小时,又经水浸30小时 或更长的种子,其发芽率不足2%。
短句来源
     Result: No stratification was found to the production in storage of one year in room temperature.
     结果:成品在室温下贮存一年未见分层。
短句来源
  相似匹配句对
     From No.
     从No.
短句来源
     NO.
     其中NO.
短句来源
     There are no precipition and stratification in storage of 6 months at roomtemperature.
     该饮料颜色鲜艳,酸甜适口,营养丰富,在室温下保存6个月没有沉淀和分层。
短句来源
查询“no stratification”译词为用户自定义的双语例句

    我想查看译文中含有:的双语例句
例句
为了更好的帮助您理解掌握查询词或其译词在地道英语中的实际用法,我们为您准备了出自英文原文的大量英语例句,供您参考。
  no stratification
The solution when there is no rotation-no stratification-neither rotation nor stratification, is deduced and each case is found to differ from the case of rotating stratified fluid in many respects.
      
In contrast to the previous studies on polyacrylate emulsion urethanes, no stratification was detected between 0.65 to 1.14 μm near the F-A and F-S interfaces.
      
Simulated photosynthetic potential for the whole canopy was slightly higher (>amp;lt;10%) using the measured allocation of C and N within the canopy compared with no stratification (i.e., all foliage identical).
      
The farther circular layerings remain incomplete, end at the shell membrane, so that the eisospherite has no stratification.
      
Within those neighborhoods, there is typically no stratification; every household is listed and a random selection is made.
      
更多          


The Wanshouyan Hill,located at about 30km northwestern Sanming City,Fujian Province(seen Fig.1 and Photo 1),is composed of limestone which belongs to Chuanshan Formation and Late Carboniferous period.There are some caves produced by weathering and limestone cavitation in the hill.One of these is named Lingfeng Cave(seen Photo 1 a),and the another Chuanfan Cave(seen Photo 1 b).In September 1999,a great deal of stone wares (about eight hundreds)and many mammalian fossils of the Pleistocene epoch(such as Megatapirus...

The Wanshouyan Hill,located at about 30km northwestern Sanming City,Fujian Province(seen Fig.1 and Photo 1),is composed of limestone which belongs to Chuanshan Formation and Late Carboniferous period.There are some caves produced by weathering and limestone cavitation in the hill.One of these is named Lingfeng Cave(seen Photo 1 a),and the another Chuanfan Cave(seen Photo 1 b).In September 1999,a great deal of stone wares (about eight hundreds)and many mammalian fossils of the Pleistocene epoch(such as Megatapirus augustus,Rhinoceros sinensis,Crocuta crocuta ultima,Cervus sp., Ursus arctos,Rhizomys sp., Macaca sp., Sus scrofa,Muntiacus sp.,Bovidae,Canidae)were discovered in the two above mentioned caves.In addition,a gravel bed which covers an area of about 120m 2 near the cave entrance in Chuanfan Cave was found,About the origin of the gravel bed,some archaeologists believed that it was formed by sedimentation.But others considered it may be a stone ground which had been laid by ancient people in Stone Age.In November 1999,authers made an investigation on the gravel bed and obtained some information about the origin of the gravel bed.Its main characteristics are described briefly as follows: IN GROUND The gravel bed covers an area of about 120m 2 near the cave entrance.It is higher than the ancient landform in the outside cave(about 2 3m).Along the cave wall(about 20~30cm in wide)there is no gravel distributed.The surface of the gravel bed is not level but slight tilte to the east.The inclination is less than 5°.Almost gravels are consisted limestone,and interstitial materials are made of black clay.Gravels occur middle or high degree psephicity,but have not been sorted.It often could be found bigger gravels arranged together with smaller ones.The grain sizes of gravels have a wide difference,the biggest gravels range from 20 to 30 centimetres,but the smallest ones only several centimetres.The arranging orientation of gravels is different,the macro axis of gravels not only points to different direction,but also the surface of gravels tends to various direction. FROM SECTION The gravel bed,30~35 centimetres in thickness (seen Fig.2 and Photo 2),overlays on the brownish yellow clay bed and is overlain by the yellow clay bed (seen Photo 3).The boundaries between them are easily to be determinated.Some small gravels which had not been graded dispersed in the lower and middle parts of the gravel bed.the composition of gravels is mainly limestone and some stalactite.In general,the grain sizes of gravels range from 3 to 5 centimetres and their psephicity is lower or middle.The interstitial materials are composed of black clay,and no stratification could be identified.The top of the gravel bed is composed of bigger gravels which are arranged nearly one by one,and the interstitial materials are black clay,too.The others characteristics are the same as that of the ground.Based on the preliminary studies of sedimentary structures and sedimentogenesis of the gravel bed,it is shown that the lower and middle parts of the gravel bed are originated to sedimentation and its top is not.It is a “man made stone ground”. The stone ground laid by ancient people in Stone Age has not been discovered so far in China.These discoveries (including stone wares,stone ground,mammalian fossils) are of great importance to understanding the origin,evolution,migration and distribution of ancient people,and geographical conditions in ancient times in Fujian Province and South China.

福建三明万寿岩船帆洞遗留有古人类活动遗迹 ,经考古发掘出大量旧石器、哺乳动物化石及一面积逾百平方米的砾石层。详细论述了该砾石层分布特征 ,应用沉积学原理系统分析其沉积特征 ,认为砾石层是经地质作用自然堆积而成 ,但其顶面的砾石不具自然沉积特征 ,应属人工铺就而成。

The study was carried out to know the method of stimulating the germination of Rhus vemiciflua srokes seeds. The following results were obtained:1 Seeds with no sulfuric acid treatment did not germinate regardless of stratification treatment.2 The water content of 1 hour sulfuric acid treated seeds was about 86% after saturated infiltration,while that of the 0.5 hours sulfuric acid treated was 59%.3. Sulfuric acid treatment up to 4.5 hours was safe. The seeds treated with 3 hour sulfuric acid and then 4 week...

The study was carried out to know the method of stimulating the germination of Rhus vemiciflua srokes seeds. The following results were obtained:1 Seeds with no sulfuric acid treatment did not germinate regardless of stratification treatment.2 The water content of 1 hour sulfuric acid treated seeds was about 86% after saturated infiltration,while that of the 0.5 hours sulfuric acid treated was 59%.3. Sulfuric acid treatment up to 4.5 hours was safe. The seeds treated with 3 hour sulfuric acid and then 4 week stratification showed the highest percent germination energy 90%for 10 days.4 week stratification showed the highest percent week because 18% to 28% of seeds treated with 2 hours sulfuric acid and then 5 week stratification were germinating during stratification treatment.5. The percent germination of the seeds,which were treated with concentrated sulfuric acid for 0.5 hours to 7 hours,and then infiltrated with water for 30 hours or longer,was lese than 2%,if the seeds had no stratification treatment. Therefore, Rhus vemiciflua Stokes seed appeared to have two kinds of dormancy; mechanical and physiological .

本文研究了利用浓硫酸刺激漆树种子发芽的方法,取得如下结论:1、没有经硫酸 处理过的种子尽管进行了层积处理也不发芽;2、经过1小时硫酸处理过的种子发 育率约86%,而0.5小时的硫酸处理种子发芽率则为59%;3、硫酸处理时间在4.5 小时以内是安全的,3小时的硫酸处理种子4周的层积显示出10日内90%的最高发 芽力;4、经24小时硫酸处理的种子适合层积时间为4周,为期5周的层积18%-28%的种子在层积过程中就发芽了;5、经硫酸处理0.5-7小时,又经水浸30小时 或更长的种子,其发芽率不足2%。若种子不经层积处理,漆籽显示有两种休眠状 况:机械和生理休眠。

ABSTRACT Objective: To improve the stability of compound streptomycin nasal drops and to establish a method for its quality control. Method: An emulsion was prepared with a compound emulgent. A red chelated compound was formed with Matol ( a production of character reaction of Streptomycin) and Fe3+ after Cod liver oil was extracted with Chloroform. The absorption value (A) was determinate in 550 nm of the wavelength. Result: No stratification was found to the production in storage of one year in room...

ABSTRACT Objective: To improve the stability of compound streptomycin nasal drops and to establish a method for its quality control. Method: An emulsion was prepared with a compound emulgent. A red chelated compound was formed with Matol ( a production of character reaction of Streptomycin) and Fe3+ after Cod liver oil was extracted with Chloroform. The absorption value (A) was determinate in 550 nm of the wavelength. Result: No stratification was found to the production in storage of one year in room temperature. The A value of the blank test of the analysis were 0. 001-0. 003 , the average recoveries for 3 concentration of samples were 78. 8% ( RSD 1. 96% ) ,98.0% (RSD 0. 50% ) ,and 121.7% ( RSD 1.01%),respectively. The RSD of analysis for 2 batches samples were 0. 50% and 0. 45%. Conclusion: This product was stable. The method of analysis is simple and reliable.

目的:改善复方链霉素滴鼻液的稳定性,建立其质量控制方法。方法:采用复合乳化剂改制成乳浊液。用氯仿去除鱼肝油后,利用链霉素的特征反应-麦芽酚反应生成麦芽酚,与Fe3+形成红色络合物,在550 nm处测定A值,求其含量。结果:成品在室温下贮存一年未见分层。链霉素的含量测定研究:空白试验A仅为0.001-0.003,3种不同浓度的回收率平均值(三次)分别为98.3%,98.0%,101.5%(RSD2.39%,0.50%,0.87%)。样品测定两批,每批测定3次,RSD分别为0.50%和 0.45%。结论:复方链霉素滴鼻液稳定,含量测定方法简便可靠。

 
<< 更多相关文摘    
图标索引 相关查询

 


 
CNKI小工具
在英文学术搜索中查有关no stratification的内容
在知识搜索中查有关no stratification的内容
在数字搜索中查有关no stratification的内容
在概念知识元中查有关no stratification的内容
在学术趋势中查有关no stratification的内容
 
 

CNKI主页设CNKI翻译助手为主页 | 收藏CNKI翻译助手 | 广告服务 | 英文学术搜索
版权图标  2008 CNKI-中国知网
京ICP证040431号 互联网出版许可证 新出网证(京)字008号
北京市公安局海淀分局 备案号:110 1081725
版权图标 2008中国知网(cnki) 中国学术期刊(光盘版)电子杂志社