剖面

The thermal properties and mechanical properties were analyzed by Thermogravimetric analysis and Hardness Pencil Test and Universal Test Machine, respectively. The structure of prepared PI-MWNTs was characterized by Fourier transform infrared spectrometry. The morphology of PI-MWNTs were observed by scanning electron microscopy and transmission electron microscopy. The electrical conductivity was analyzed by Super Megohmmeter.

本研究中使用能量分散光谱仪来鉴定多壁奈米碳管纯化效果，热重损失分析仪、铅笔硬度计、万能试验机分别测定材料的热稳定性质和机械性质，傅立叶转换红外光谱仪来鉴定其化学结构，扫描式电子显微镜与穿透式电子显微镜来观察材料的剖面型态与奈米碳管和基材之间的分散性，超绝缘量测仪量测材料的电性。

The author first proposed quantative correction method for the sodium metasomatism, coupled with correction method for potassium metasomatism suggested by Panahi (2000) successfully restore the profile normal composition.

首次提出了定量的Na交代作用的校正方法，与Panahi(2000)的K交代作用的校正方法联用，成功地恢复了剖面的正常组成

From momentum equation and energy equation, the ablation profile of meteoroid with different radius in different velocity is calculated, and the variation of the ablating cut-off height is analyzed.

本文从流星颗粒的动量方程和能量方程出发，计算不同半径下的流星微粒在不同的注入速度下的消融剖面，并分析了流星消融截止高度的变化趋势。

The cross-sectional scanning electron microcopy photographs of AlN films showed a high degree of alignment for the columnar structure.

剖面扫描电子显微镜照片显示AlN晶粒呈高度一致的柱状生长体制。

In transverse section, from migmatite →mylonitized migmatite →ultramylonite, phillite mylonite, the contents of Au, Ag, As, S, Cu, Bi, Se and W increase, the ratios of Au/Ag, S/Se and Cu/.

在矿床垂深剖面Au及伴生微量元素Bi、Se和S具有自上而下升高的趋势；Ag和W自160m至0m则下降，Au/Ag、S/Se和Bi/Au比值自上而下升高，这可以作为矿体延深评价及找矿地球化学的指示剂。

The thickness of the main deck was found to be the most influencing to the minimum section modulus at the main deck.

发现主甲板的最小剖面模数对主甲板处的厚度最敏感。

The benefits of deep ploughing with a moldboard could be explained by more moisture in the profile and more root volume to extract this soil moisture compared to the cultivator system.

有壁犁深耕比播种机耕的好处可解释为在土壤剖面中储存了更多水分，又有更多的根系吸取了这些水分。

The composi tional change profiles of monazite demonstrate a heterogeneous distribution of e lements La, Ce, Nd, P, Th, Si, Ca and U. This was caused by the differences in geological environments, temperatures, pressures and compositions of the hy drothermal solutions.

根据微区剖面(0.18mm)元素分布曲线，指出了La、Ce、Nd、P、Th、Si、Ca和U等元素表现出8～10个微环带成分不均匀分布的特点，并认为成矿溶液的地质环境、温压和微量元素含量变化是不均匀分布的主要原因。

Since the pressure comes mainly from southern, so the cross section of Corridor basin is dissymmetrical, it can be devided into southern fore—mountain uplift terrace, middle depressed plain and northern monocline plain.

由于挤压力主要来自南侧，因而走廊挤压断陷盆地在剖面上呈不对称状，由南向北还被进一步分为南部山前断褶丘陵台地、中央深凹陷平原和北部单斜平原。

The movability of totalP,inorganic P and Olsen-P to deeper layer was descended with soil depths.

土壤中总磷、无机磷和Olsen磷在土壤剖面中向下移动性随着土层的加深而减弱。

This one mode pays close attention to network credence foundation of the businessman very much.

这一模式非常关注商人的网络信用基础。

Cell morphology of bacterial ghost of Pasteurella multocida was observed by scanning electron microscopy and inactivation ratio was estimated by CFU analysi.

扫描电镜观察多杀性巴氏杆菌细菌幽灵和菌落形成单位评价遗传灭活率。