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  rich
     The Studies of Application Platelet Rich Plasma to Bone Tissue Engineering
     富含血小板血浆应用于骨组织工程的研究
短句来源
     LEACHING CHARACTERISTICS OF A TUFF TYPE URANIUM ORE RICH IN FLUORITE
     富含萤石凝灰岩类型铀矿石的浸出特性
短句来源
     Several Important Reactivities of Bacterin of Staphylococcus Areus Contained Rich Protein A
     富含A蛋白的葡萄球菌菌苗的若干重要的反应性
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     Selective Absorption of H_2S from a Gas Stream Containing Rich CO_2
     从富含CO_2的混合气中选择性吸收H_2S
短句来源
     Treatment of 18 Cases of Patients with Digestive System Ulcer Using Shengjiyulou Drinking Rich in Selenium
     富含硒的生肌玉露饮治疗溃疡病18例
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  rich in
     The ores are rich in Ag (5.35~240μg/g), Pb(0.01% -0.16%), Zn(0.26% -2.40%) and Au(0. 02-0. 16μg/g).
     矿石富含Ag(5.35-240μg/g)、Pb(0.01%~0.16%)、Zn(0.26%一2.40%)、Au(0.02~0.16μg/g)。
短句来源
     Garnet is also rich in CaO (7.02%-8.16%), and clinopyroxene rich in Na\-2O (2.35%-2.71%) and Al\-2O\-3 (6.97%-11.29%).
     同时 ,石榴子石富含CaO (7.0 2 %~ 8.16 % ) ,而辉石巨晶富含Na2 O (2 .35 %~ 2 .71% )和Al2 O3(6 .97%~ 11.2 9% )。
短句来源
     Quartz, in whiCh the SiO2 occupies less than 96% and Σ (Al2O3+K2O+Na2O)occupies more than 1. 0 %, is rich in gold.
     SiO2含量低于96%,而Σ(Al2O3+K2O+Na2O)含量高于1.0%的石英为富含金石英;
短句来源
     Diagenesis is obvious at a depth of 1 500 m where sparry calcite (Ⅰ) has been precipitated from water rich in atmospheric CO2 with δ13C in the range of -4‰ and -6‰, and 818O in the range of -5‰ and -6‰.
     成岩作用在埋深1 500 m已很显著,富含大气CO2水中沉淀亮晶方解石(Ⅰ),δ13c为 -4‰-6‰,δ180为-5‰--6‰。
短句来源
     The average nucleotide composition of A+T (56.7%) is higher than that of G+C (43.4%), so the cyt b gene sequences are rich in A and T.
     cyt b基因富含碱基A和T,A+T的平均含量(56.7%)显著高于G+C的含量(43.4%)。
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  rich with
     LHβ gene was rich with GC.
     山羊LHβ基因序列富含GC。
短句来源
     2. Sequences analysis showed, TM1, TM2 and TM3 were rich with A/T base composition and had a number of motifs commonly occuring in MARs, including the A-box,T-box,TATAAA,Drosophila toposiomerase II consensus cleavage site and DNA unwinding sequence.
     2.序列分析表明,TM1、TM2和TM3富含AT序列,并且具有几个MARS序列中常见的DNA结构域,如:A-box、T-box、TATAAA、拓扑异构酶Ⅱ识别切割序列、DNA解旋序列等。
短句来源
     Sichuan Basin is rich with brine, Which contens K,B,I,Br and other useful elements.
     四川盆地卤水分布广泛 ,资源丰富。 卤水普遍富含 K、B、I、Br等有用组分 ,皆为国家短缺矿产。
短句来源
     Objective To observe the effects of amino acids solution rich with alanylglutamine(Ala-Gln)and branched-chain amino acids(BCAA)on traumatized rats.
     目的 观察富含丙氨酰谷氨酰胺 (Ala Gln)和支链氨基酸 (BCAA)的氨基酸注射液 ,对创伤大鼠的营养支持效果。
短句来源
     Petrophysical experiments were carried out to study low resistivity oil and gas reservoirs, which are rich with clay mineral and fine-grain in the freshwater environment reservoirs.
     研究了淡水环境下富含粘土矿物、细颗粒砂岩低电阻率油气层 .
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  “富含”译为未确定词的双语例句
     Study on the Construction of Heterotrophic and High-Containing EPA/DHA Microalgae by Cell Fusion Technique
     利用细胞融合技术构建富含EPA/DHA异养微藻株的研究
短句来源
     The Effect of the Cysteine-rich 61 on the Pathogenesis of Autosomal Dominant Polycystin Kidney Disease
     富含半胱氨酸蛋白61在常染色体显性多囊肾病发病中的作用研究
短句来源
     Expression and Function Analyses of a Gene Family Encoding a Novel Class of Proline-rich Proteins in Rice
     水稻中一个编码富含脯氨酸蛋白基因家族的表达和功能研究
短句来源
     Studies on Starch from Fritillaria and Rhizoma Dioscorea
     富含淀粉中药贝母、山药中淀粉的研究
短句来源
     STUDIES ON THE SYSTEMS RARE EARTH SESQUIOXIDESBERYLLIUM OXIDE, PART II, THE ACTIVITY OF BERYLLIUM OXIDE AND THE STRUCTURAL MODEL OF BeO-RICH MELTS (0-40 mole%LaO_(1.5)) IN THE SYSTEM La_2O_3-BeO
     三价希土氧化物-氧化铍系统的研究Ⅱ、La_2O_3-BeO系统富含BeO熔体(0~40分子%LaO_(1.5))的BeO活度和熔体结构模型
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  rich
The rich world?s reluctance to deal with these issues in an honest and equitable manner provides naught for our comfort.
      
For the multi-resolution properties of the ridgelet function in the direction besides scale and position, DMRN has great capabilities in catching essential features of direction-rich data.
      
tabulaeformis forests of Shidu, Mutianyu, and Yunfengshan are rich in species diversity and have great similarities.
      
involucrata population has a rich genetic diversity, and the differences among populations are significant.
      
In the rainfall-rich year (2003), during the growing season the precipitation was 870.2 mm and the water consumption of potted trees was from 480 to 515 mm.
      
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  rich in
tabulaeformis forests of Shidu, Mutianyu, and Yunfengshan are rich in species diversity and have great similarities.
      
With the aim of controlling the dilution rate and obtaining surfacing beads rich in intermetallic compounds, the effects of surfacing parameters on geometric parameters, dilution rate, composition, and microstructure of the bead are investigated.
      
The exhalative rock occurring in the Xiagou Formation of Lower Cretaceous in Qingxi sag, Jiuxi basin is a sort of a rare lacustrine white smoke type, rich in ferrodolomites and albites.
      
Finally, the oxic environment characterized by red sediment rich in Fe3+ appeared.
      
The results show that PM of 0.1 μm is rich in sulfates.
      
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  - rich
For the multi-resolution properties of the ridgelet function in the direction besides scale and position, DMRN has great capabilities in catching essential features of direction-rich data.
      
In the rainfall-rich year (2003), during the growing season the precipitation was 870.2 mm and the water consumption of potted trees was from 480 to 515 mm.
      
However, electron-deficient boron-rich B-C-N solids have also attracted much interest both theoretically and experimentally.
      
Probing the nuclear symmetry energy with heavy-ion reactions induced by neutron-rich nuclei
      
Heavy-ion reactions induced by neutron-rich nuclei provide a unique means to investigate the equation of state of isospin-asymmetric nuclear matter, especially the density dependence of the nuclear symmetry energy.
      
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  rich with
The attraction causes a significant increase in the concentration of foreign atoms near the carrier (the impurity cloud) and produces around the charge a macroscopic region of radius 50-70 ? rich with the impurity component.
      
Four successive ore formations are apparently fluorite-free and either quartz-rich or barite-rich with minor amounts of sulfides.
      
Waste waters of film processing plants are rich with silver.
      
The introns are extremely AT rich with a pronounced base bias of T >amp;gt; A >amp;gt; G >amp;gt; C in the RNA-like strand.
      
The introns are extremely AT rich with a pronounced base composition bias of T >amp;gt; A >amp;gt; G >amp;gt; C in the mRNA-like strand and group II-like boundary sequences at their 3' and 5' ends having the consensus 5'-GTGTG ..
      
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The roles of the natural development and some properties of the soilsin this area are briefly discussed as follows:The soils are saline and calcareous in nature,in which over 70% of thetotal soluble salts are sodium chloride.Slight to moderate alkalinizationmay be developed,while the total soluble salt contents exceed 0.2%;butgenerally,there is no NaCO_3 present.The ground water table in this areais usally high,and the quantity and constituents of the salts in groundwater are directly varied with and influenced...

The roles of the natural development and some properties of the soilsin this area are briefly discussed as follows:The soils are saline and calcareous in nature,in which over 70% of thetotal soluble salts are sodium chloride.Slight to moderate alkalinizationmay be developed,while the total soluble salt contents exceed 0.2%;butgenerally,there is no NaCO_3 present.The ground water table in this areais usally high,and the quantity and constituents of the salts in groundwater are directly varied with and influenced by that contained in the abovesoils.The saline and alkali properties of soils in this area are originatedfrom the parent materials,through the action of the sea water when theywere deposited.As soon as the sea water ceased to affect,the soils as wellas the ground water are gradurally desalinized by natural leaching and thisprocess will be strengthened by the biological activities.As the desalinization of the soils is proceeded further,the ratio ofNa~+/Ca~(++)+Mg~(++)in the soil solution decreased and the amount of the exchan-geable Na on the soil colloidal complex is finally lowered.It is evident thatdesalinization also introduces the dealkalinization of the soils in this area;there is no hazard of strong alkalinization of the soils taken place throughleaching.

本文简要地说明了江苏省沿海地区盐渍土壤的自然发生过程及盐渍特性转化的规律,文中主要论点,可初步归纳如下:1、本区域的土壤,发育于盐渍性的冲积母质,土层中富含以氯化钠为主的可溶性盐类,并呈一定的“碱性”。土壤碱性表现在两方面:一方面是土壤胶体表面存在有较多的吸附性钠,另方面表现在本身具有较高的pH 值。2、在自然发生过程中,土壤盐渍性为地质过程遗留的影响;随受自然降水淋盐,河沟排水排盐及生物作用的影响,开始“脱盐、脱碱”和肥力积累过程,发育成为本区内现存的各种不同盐渍程度的土壤。3、随着土壤脱盐作用的进行,土壤盐渍的组成在变化;主要是可溶性盐阴离子中钠离子的含量淋失较速,最后降低了土壤溶液中Na~+/Ca~(++)比率。由于这种盐渍组成的改变,土壤胶体上吸收性Na~+也相应的降低,从而导致土壤的脱碱作用。因此本区土壤的脱盐不致引起土壤碱化。4、在自然发生过程中,本区域盐渍土的脱盐过程,一直是在潜水位较高的情况下进行的。在脱盐过程中,潜水位经常在临界水位以内,为本区自然脱盐过程中,最大特点;潜水动能和土壤的脱盐过程,存在着许多内在的联系。在一定地区内,一定盐渍程度、盐渍特性的土壤,则常有和其相适应的矿...

本文简要地说明了江苏省沿海地区盐渍土壤的自然发生过程及盐渍特性转化的规律,文中主要论点,可初步归纳如下:1、本区域的土壤,发育于盐渍性的冲积母质,土层中富含以氯化钠为主的可溶性盐类,并呈一定的“碱性”。土壤碱性表现在两方面:一方面是土壤胶体表面存在有较多的吸附性钠,另方面表现在本身具有较高的pH 值。2、在自然发生过程中,土壤盐渍性为地质过程遗留的影响;随受自然降水淋盐,河沟排水排盐及生物作用的影响,开始“脱盐、脱碱”和肥力积累过程,发育成为本区内现存的各种不同盐渍程度的土壤。3、随着土壤脱盐作用的进行,土壤盐渍的组成在变化;主要是可溶性盐阴离子中钠离子的含量淋失较速,最后降低了土壤溶液中Na~+/Ca~(++)比率。由于这种盐渍组成的改变,土壤胶体上吸收性Na~+也相应的降低,从而导致土壤的脱碱作用。因此本区土壤的脱盐不致引起土壤碱化。4、在自然发生过程中,本区域盐渍土的脱盐过程,一直是在潜水位较高的情况下进行的。在脱盐过程中,潜水位经常在临界水位以内,为本区自然脱盐过程中,最大特点;潜水动能和土壤的脱盐过程,存在着许多内在的联系。在一定地区内,一定盐渍程度、盐渍特性的土壤,则常有和其相适应的矿化潜水类型。在自然发生过程中,随土壤的脱盐和盐渍特性的转化,潜水似亦随之发生相应的淡化和化学性质的变化。二者转化趋势,大致相符。彼此间的关系,是互相依存、互相制约的,在不断运动的过程中,似先有土壤的脱盐,而生导向潜水的淡化;但就土壤脱盐的过程言,本身同时又是潜水淡化的结果。5、在土壤脱盐的过程中,土壤盐分的动能比较复杂,一方面是全区土壤不断地脱盐,另方面是在一定的条件下,又可产生局部地区土壤表层的盐渍化。前者为本区盐渍土壤自然发生过程的实质,后者为临时性现象。此种现象,最终亦必随同潜水的转向淡化而逐渐消除。

To three cultural media composed of montmorillonitic,kaolinitic and illitic type of clay minerals,treatments were made for varying degrees of saturation of exchange- able calcium,magnesium and potassium with constant base exchange capacity.The effect of complementary ions on the availability of exchangeable Cations was judged from the yields as well as their chemical composition of the plants growing on them. The results are summarized as follows. 1.No difference was noticeable among different types of clay...

To three cultural media composed of montmorillonitic,kaolinitic and illitic type of clay minerals,treatments were made for varying degrees of saturation of exchange- able calcium,magnesium and potassium with constant base exchange capacity.The effect of complementary ions on the availability of exchangeable Cations was judged from the yields as well as their chemical composition of the plants growing on them. The results are summarized as follows. 1.No difference was noticeable among different types of clay minerals with respect to the effect of the nature of complementary ions on the availability of the exchangeable cations. 2.As a complementary ion,the higher the degree of saturation of calcium,the lower the availability of the exchangeable magnesium.Similarly,magnesium as a complementary ion has also the same effect on the availability of exchangeable mag- nesium as calcium does on magnesium. 3.The availability of exchangeable potassium increases with the increase of the degree of saturation of calcium functioning as a complementary ion to the exchangeable potassium.But,to the contrary,potassium as a complementary ion affects the availa- bility of exchangeable calcium in the reverse direction.Situation is just about the same between the mutual effect of the exchangeable magnesium and potassium. 4.Results from illitic series of the cultural media showed that with respect to the availability of exchangeable potassium,calcium as a complementary ion is preferable to magnesium,and with respect to the availability of exchangeable calcium,potassium as a complementary ion is superior to magnesium. 5.From the results,it seems that under the conditions of the same base exchange capacity and the same amount of exchangeable potassium content,calcium clay will afford more available potassium as compared with hydrogen clay.This gives a new explanation of the disadvantages of the acid soil and adds to the support for liming an acid soil.According to the author's opinion,the reported deficiency of available calcium supply in some of the alkali soils,in which the total calcium content was known to be sufficient,may be explained from the standpoint of the unfavorable effect of the complementary ion (Na) on calcium. 6.Suggestions are made that rational application of mineral fertilizers should be made according to the status of the exchangeable cations of the soil.It is rather the degree of saturation of the exchangeable cations and the nature and proportion of the complementary ions than the absolute amount of the nutrients as such or the total percentage content of them on the soil weight basis,that will count in order to afford sufficient quantities of available cations for the nutrition of the plants.The unit of fertilization rate (dosage) is,indeed,a relative concept (relative to the base exchange capacity) and not an absolute weight or an ordinary percentage concept. 7.Attempts were made to explain the effect of different complementary ions on the availability of exchangeable cations by the concept of exchange bonding energy of the various cations.The explanation is serviceable in limited cases.More work is yet to be done before a satisfactory theory can be found to fully explain the com- plementary ion effect. 8.It is reasonable to doubt whether some of the antagonistic phenomena between cations observed on the plants growing in soil reported by physiologists are actually physiological problems at all.Might not these be just matters of complementary ion effects in the soil?

在蒙脱石系、高陵石系及水化云母系的培养基里,人为地调节 Ca、Mg、K 三种代换性阳离子的饱和度,把其中任意两个阳离子的饱和度维持不变,而把其余一个阳离子作为陪补离子,调节其饱和度,使其在适当的范围内变化,以观察其对植物生长及其组织的化学组成的影响。试验的主要结果,简要地总结如下:1.陪补离子对代换性阳离子的有效度的影响,无论在高陵石系中或蒙脱石系中,结果都是一致的。这说明它们之间有共同规律可循,和粘粒矿物的种类无关。2.陪补离子钙对代换性镁离子的有效度有不利的影响。反之,陪补离子镁对代换性钙离子的影响也相同。3.作为陪补离子的钙,当其饱和度增大时,代换性钾离子的有效度亦随之而增加。但反之作为陪补离子的钾,当其饱和度增大时,却反降低了代换性钙离子的有效度。4.至于镁离子和钾离子间的相互影响,则情况和钙、钾之间的相互影响同。(见3)5.水化云母系的试验结果表明:对代换性钾离子的有效度而言,作为陪补离子的钙比镁更为理想,而对代换性钙离子的确效度言,则陪补离子钾又比镁更为理想。6.从试验结果看来,在含同量代换性钾及同一盐基代换量的条件下,钙质粘土的钾素供应状况应优于氢质粘土。这对酸性土壤提供了一种新的看法,并对酸土...

在蒙脱石系、高陵石系及水化云母系的培养基里,人为地调节 Ca、Mg、K 三种代换性阳离子的饱和度,把其中任意两个阳离子的饱和度维持不变,而把其余一个阳离子作为陪补离子,调节其饱和度,使其在适当的范围内变化,以观察其对植物生长及其组织的化学组成的影响。试验的主要结果,简要地总结如下:1.陪补离子对代换性阳离子的有效度的影响,无论在高陵石系中或蒙脱石系中,结果都是一致的。这说明它们之间有共同规律可循,和粘粒矿物的种类无关。2.陪补离子钙对代换性镁离子的有效度有不利的影响。反之,陪补离子镁对代换性钙离子的影响也相同。3.作为陪补离子的钙,当其饱和度增大时,代换性钾离子的有效度亦随之而增加。但反之作为陪补离子的钾,当其饱和度增大时,却反降低了代换性钙离子的有效度。4.至于镁离子和钾离子间的相互影响,则情况和钙、钾之间的相互影响同。(见3)5.水化云母系的试验结果表明:对代换性钾离子的有效度而言,作为陪补离子的钙比镁更为理想,而对代换性钙离子的确效度言,则陪补离子钾又比镁更为理想。6.从试验结果看来,在含同量代换性钾及同一盐基代换量的条件下,钙质粘土的钾素供应状况应优于氢质粘土。这对酸性土壤提供了一种新的看法,并对酸土中施用石灰的意义,也多了一种新的认识。 7.在讨论里,作者对某些富含钙质的碱土而反有钙素营养不足的事实,从陪补离子影响的角度试作了解释。并同时提出矿质施肥上的新的施肥原则,要求在施肥时,应对土壤中有关吸收性养料的有效度问题方面作更多的全面考虑——例如,代换性阳离子的饱和度,陪补离子的影响者。8.作者尝试着用代换吸附键能的概念,对陪补离子影响于代换性阳离子的有效度的某些事实,进行了解释,但这些解释目前还不能圆满,它们只是在一定的条件下才成立的假说而已。9.报告中还联系了拮抗作用和陪补离子的影响,指出它们之间有若干相似的意义。

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微生物在关中(土娄)土不同粒径土壤团聚体上有规律性的分布。好气性细菌、嫌气性细菌、好气性自生固氮菌和放线菌等的数量,均以在粒径为2—3毫米土壤团聚体上者为多,在粒径为5—7毫米及0.25—0.5毫米土壤团聚体上者较少。芽孢细菌(或细菌芽孢)的数量在各级土壤团聚体之间变化不大。Bac.subtilis—Bac.mesentericus在芽孢细菌(或细菌芽孢)中的百分含量,有随土壤团聚体的直径減小而有增高的趋势。粒径为2—3毫米的土壤团聚体富含腐殖质及植物的小根。

 
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