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internal buffering
相关语句
  内部缓冲
     Morever, some variations of α CO 2 among samples (from 0.537~0.643) also suggest that CO 2 in the decarbonation process is most likely derived from internal buffering rather than from the deep source. Key word:
     不同样品中αCO2 值有一定变化 (0 .5 37~ 0 .6 43)也进一步表明变质过程中CO2 为内部缓冲 ,并非深部来源。
短句来源
  “internal buffering”译为未确定词的双语例句
     Increase of whey Starter Culture Activity by Internal Buffering Methd
     内缓冲法提高乳清发酵剂活力的研究
短句来源
     By combining the internal buffering technique and the float hole technique with the divide-and-conquer technique, a fast linear-time in-place 2-way merge algorithm is introduced in the paper.
     将内部缓冲技术、浮洞技术与分治技术相结合,提出了一种快速线性原地二路归并算法。
短句来源
  相似匹配句对
     Internal Control
     内部控制专题
短句来源
     ON Internal Control
     论内部控制
短句来源
     Increase of whey Starter Culture Activity by Internal Buffering Methd
     内缓冲法提高乳清发酵剂活力的研究
短句来源
     Integration,Buffering and Bridging
     整合、缓冲和桥接
短句来源
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  internal buffering
An alternative hypothesis of internal buffering is preferred to explain the carbonaceous matter in the Trois Seigneurs metasediments.
      
The anomaly of beautifully preserved internal buffering signatures and the requirement for produced fluid locally to pass across layers in a deforming rock sequence suggest that the escaping fluid did not leave any readily observable tracks.
      
Internal buffering is recognised as an important end-member process when considering the factors governing the composition of a fluid phase present in a rock during metamorphism.
      
The concentrical arrangement in the garnet segregations can be explained by the sequence in which a number of garnet- and potassium feldspar-producing reactions were met during temperature increase, with internal buffering of the activity of H2O.
      
Whereas the majority of theoretical papers assume infinite buffers, practical CIOQ implementations have a limited amount of internal buffering.
      
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The equation for estimating α CO 2 in metamorphic fluid of carbonate rocks is formulated by thermodynamic calculation for equilibrium state of decarbonation. The application of this method to marble from Jining Group in Inner Mongolia reveals that the α CO 2 value of fluid in the progressive stage of granulite facies metamorphism is higher than 0.50,which is consistent with the data from recent researches. All evidence displays that the α CO 2 value of fluid increased gradually...

The equation for estimating α CO 2 in metamorphic fluid of carbonate rocks is formulated by thermodynamic calculation for equilibrium state of decarbonation. The application of this method to marble from Jining Group in Inner Mongolia reveals that the α CO 2 value of fluid in the progressive stage of granulite facies metamorphism is higher than 0.50,which is consistent with the data from recent researches. All evidence displays that the α CO 2 value of fluid increased gradually in the progressive metamorphic process and reached 0.80 in its peak stage, which is attributed to the continuous separation of CO 2 with the intensification of decarbonation. Morever, some variations of α CO 2 among samples (from 0.537~0.643) also suggest that CO 2 in the decarbonation process is most likely derived from internal buffering rather than from the deep source. Key word:

通过脱碳反应的平衡热力学计算 ,推导出碳酸盐岩石变质流体中CO2 活度αCO2 的估算公式。将其用于内蒙古集宁群孔兹岩系的大理岩 ,得出在麻粒岩相变质峰期前进变质阶段流体已具有较高αCO2 的值 (>0 .5 )。此结果与已有研究结果吻合 ,表明在进变质过程中随脱碳反应规模加大 ,析出的CO2 使流体中αCO2 值相应增大 ,至变质峰期此值达 0 .8以上。不同样品中αCO2 值有一定变化 (0 .5 37~ 0 .6 43)也进一步表明变质过程中CO2 为内部缓冲 ,并非深部来源。

According to data of fluid inclusions within minerals and thermochemical estimation of dehydration reaction during granulite_facies metamorphism of Jining Group and Qianxi Group, the fluids existent at the peak stage must have been carbonic, with x (CO 2+CH 4)≈70%~80% and x (H 2O)≈10%~20%, the density is generally 1.0~1.1 g/cm 3. In the Jining Group, components of the metamorphic fluids and activity of H 2O seem to have been spatially inhomogeneous, and were apparently controlled by lithology. The...

According to data of fluid inclusions within minerals and thermochemical estimation of dehydration reaction during granulite_facies metamorphism of Jining Group and Qianxi Group, the fluids existent at the peak stage must have been carbonic, with x (CO 2+CH 4)≈70%~80% and x (H 2O)≈10%~20%, the density is generally 1.0~1.1 g/cm 3. In the Jining Group, components of the metamorphic fluids and activity of H 2O seem to have been spatially inhomogeneous, and were apparently controlled by lithology. The α H 2O values of Al_rich gneisses , biotite hypersthene gneisses and basic granulites are 0.1~0.2, 0.2~0.4 and 0.4~0.6 respectively. Such inhomogeneity indicates that the fluids might have experienced internal buffering, and did not permeate pervasively through rocks. They were probably developed as a result of various kinds of devolatilization and oxidation of the organic materials (now as crystalline graphite) extensively distributed in rocks, both of which must have occurred at the progressive metamorphic stage. Moreover, H 2O could escape from the system more easily than CO 2, and this might be partly related to their carbonic affinity. On the contrary, the components and physical habits of fluids during metamorphic peak of the Qianxi Group were rather homogeneous in space, being independent to lithology. In Taipingzhai district, for example, the α H 2O values of rocks of all the three types are 0.13~0.25 with X H 2O ≈0.1~0.2. These features suggest that the fluids in this region were probably of external_buffering, and had pervasively permeated through rocks. CO 2 in fluids might mostly have come from underplating mantle_source mafic magma and its crystallization process.

矿物中流体包裹体研究和脱水反应热力学计算结果表明,集宁群和迁西群麻粒岩相变质峰期流体均富碳质,x(CO2 +CH4)一般为 70 %~ 80 %,x(H2 O)≈ 10 %~ 2 0 %,密度一般为1.0~ 1.1g/cm3。集宁群中变质流体的成分和H2 O活度在空间上分布不均匀,明显受岩性控制。富铝片麻岩、黑云紫苏片麻岩和基性麻粒岩中αH2 O值分别为 0.10~ 0.2 0、0.2 0~ 0.4 0和 0.4 0~0.6 0,表明其非外源成因,未曾在岩石中均匀渗透,而可能与进变质过程原岩中普遍存在的有机质氧化和各种脱挥发分反应有关,其富碳质还与H2 O相对易于逸散有关。迁西群变质峰期流体成分在空间上分布均匀,不受岩性控制,在太平寨等地区上述 3类岩石中αH2 O值主要都在 0.13~ 0.2 5之间,XH2 O为 0.1~ 0.2,反映流体似为外源成因,并确曾在岩石中均匀渗透。本区存在幔源基性岩浆底侵的地质条件,这种富碳质流体可能与它们结晶时析出的CO2 流上升有关。

By combining the internal buffering technique and the float hole technique with the divide-and-conquer technique, a fast linear-time in-place 2-way merge algorithm is introduced in the paper. The new algorithm needs at most 2.5 m+1.5 n+4.5m+n comparisons and 7 m+6 n-m+n movements to merge two sorted sub-lists of lengths m and n(m≤n).If the coefficients can be marked down and the algorithm can be combined with other fine sort algorithms, the in-place merging algorithm must be converted from a theoretical...

By combining the internal buffering technique and the float hole technique with the divide-and-conquer technique, a fast linear-time in-place 2-way merge algorithm is introduced in the paper. The new algorithm needs at most 2.5 m+1.5 n+4.5m+n comparisons and 7 m+6 n-m+n movements to merge two sorted sub-lists of lengths m and n(m≤n).If the coefficients can be marked down and the algorithm can be combined with other fine sort algorithms, the in-place merging algorithm must be converted from a theoretical one into a more practical one than quick-sort algorithm. So the new algorithm has high value in theory and practice.

将内部缓冲技术、浮洞技术与分治技术相结合,提出了一种快速线性原地二路归并算法。归并长度分别为m和n的2个有序子表(m≤n),该算法最多需要2.5m+1.5n+4.5m+n次比较和7m+6n-m+n次移动。如进一步降低系数,并与其他好的排序算法有机结合,理论上的原地二路归并算法必将成为比快速排序更实用的算法。因此该线性原地二路归并算法具有较高的理论和实用价值。

 
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