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变化范围

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This section shall extend to any member of any naval or marine forces not only when he is at sea but also when he is so circumstanced that if he were a soldier he would be in actual military service within the meaning of this section.

本节中的范围涵盖任何海军,船员部队的成员,不仅在海上,本节中的范围涵盖任何海军,船员部队的成员,不仅在海上,而且当条件变化其成为实际服役的军人时,也在该范围之内。

The mathematical model and optimized result indicate that the magnetic field in the inner wall of the detecting coils is of non homogeneity. At a ratio R/L .2, the magnetic field along the axial length and within the range of 90% radial direction is nearly homogeneous.

数学模型和优化结果表明:在检测传感器线圈中部范围内为非匀强磁场,且呈非线性变化,细长管磁场相对均匀;当选取 R/ L 。2 ,磁场在线圈轴向长度范围内,径向在90 %范围内可近似看作均匀磁场。

Calculating results show that variation of the propellant inlet pressure makes little impact on engine performance parameters, and the engine will transit to a new stable state. The parameter transition curves are smooth. When the engine thrust is adjusted in a small range within a short period, the parameter transition curves are also reposeful. But when the adjusting range becomes large, the parameter transition curves will fluctuate acutely. Thus, when large range adjusting is required, the time of adjusting should be lengthened or the adjusting should be divided into adequate steps.

计算结果表明,当发动机在某一个稳定工况工作时,发动机入口推进剂压强的变化对发动机性能参数的影响不大,发动机的参数都能比较平稳的过渡到一个新的稳定工况;当发动机在短时间内进行小范围的推力调节时,发动机参数的过渡过程的曲线也比较平稳,但是当在短时间内进行大范围推力调节时,参数的过渡过程的曲线振动比较剧烈,因此应当在进行大范围推力调节时,应当对调节时间进行适当延长,或者分级进行推力调节。

Results: Breast mass changing was 89.3%(42 of 47 cases). Among which, 87.5%(7 of 8 cases) round mass became irregular; 93.7%(15 of 16 cases) mass with poorly uncear margin changed into well-defined; 90.5%(19 of 21 cases) spicule around mass was shortened or disappeared; 50%(1 of 2 cases) mass surrounded with radiolucent ring was decreased 74.2%(23 of 31 cases) calcification changes variedly in range, amount, and distribution.

结果:肿块变化发生率89.3%(42/47),其中类圆形肿块变化87.5%(7/8)、形态变化趋向不规则;模糊肿块93.7%(15/16)肿块边缘趋于清晰;肿块周围毛刺90.5%(19/21)变短甚至消失;透亮环肿块(1/2)可见瘤性实体缩小;病灶钙化74.2%(23/31)出现范围、数目、分布上的变化。

Result The results showed that the substrate carbon conversion efficiency of Amygdalus mongolica Maxim. and Amygdalus pedunculata Pall. was all a constant, was 0.55, 0.57 respectively. The adapted growth temperature scope of Amygdalus mongolica Maxim. and Amygdalus pedunculata Pall. was 14-24, 13-33 ℃ respectively. The optimal growth temperature of Amygdalus mongolica Maxim. and Amygdalus pedunculata Pall.

结果]结果表明,在所测定的范围内,随温度变化蒙古扁桃和柄扁桃的底物碳转化效率为常数,分别为0.55、0.57;适宜蒙古扁桃生长的温度范围为14~34℃,最适生长温度为25℃,适宜柄扁桃生长的温度范围为13~33℃,最适生长温度为24℃。

With the rich sediments supplied by the Pearl River, under the paleogeography sedimentary background of Baiyun Sag continuously subsiding, with sedimentary sequences related to relative transgressive sea level change ,contrary to regressive eustasy, the Pearl River Deepwater Fan System has specific evolution characteristics, which left the sedimentary record controlled by peripherical significant geological events. The sharp change of deposition rate and lithologic geochemical characteristics about 23.8Ma sequence boundary demonstratesd that sediment source had changed, perhaps related to the uplift of Tibet plateau and spreading of the South China Sea, which led the paleoPearl River drainage to expand to western China plateau , maybe much broader than present.

珠江深水扇系统以珠江为沉积物源、以持续深沉降的白云凹陷为沉积古地理背景、以与全球海退型海平面相反的相对海侵型海平面变化的沉积层序构成了其发育演化的特殊性,并留下了控制沉积的周边重要事件的记录。23.8 Ma等界面沉积速率和岩石地球化学特征均有突变,反映出物源区的变化,可能折射出与青藏高原隆升、南海扩张有关的重要事件,使得古珠江骤然向西部高原拓展,甚至较今天的珠江流域范围还广阔;承载珠江深水扇系统的白云凹陷持续沉降形成了陆坡内盆地,导致21~10.5 Ma BP多个层序深水扇垂向叠置充填的特殊沉积建造;根据60多口井资料建立的相对海平面变化曲线,具有与全球海平面变化相一致的三级旋回和不一致的二级旋回。

With the rich sediments supplied by the Pearl River, under the paleogeography sedimentary background of Baiyun Sag continuously subsiding, with sedimentary sequences related to relative transgressive sea level change ,contrary to regressive eustasy, the Pearl River Deepwater Fan System has specific evolution characteristics, which left the sedimentary record controlled by peripherical significant geological events.

珠江深水扇系统以珠江为沉积物源、以持续深沉降的白云凹陷为沉积古地理背景、以与全球海退型海平面相反的相对海侵型海平面变化的沉积层序构成了其发育演化的特殊性,并留下了控制沉积的周边重要事件的记录。23.8 Ma等界面沉积速率和岩石地球化学特征均有突变,反映出物源区的变化,可能折射出与青藏高原隆升、南海扩张有关的重要事件,使得古珠江骤然向西部高原拓展,甚至较今天的珠江流域范围还广阔;承载珠江深水扇系统的白云凹陷持续沉降形成了陆坡内盆地,导致21~10.5 Ma BP多个层序深水扇垂向叠置充填的特殊沉积建造;根据60多口井资料建立的相对海平面变化曲线,具有与全球海平面变化相一致的三级旋回和不一致的二级旋回。

The observed EMF values of oxygen concentration cell coincided withtheoretical values perfectly, indicating that the ceramics were purely oxide-ionicconductors with oxygen ion transference number of 1 under oxygen atmosphere over thewhole temperature range. The electrochemical oxygen permeation rates determined were inaccordance with the theoretical rates calculated from Faradays law, verifying directexperimentally that the oxide-ionic nature of the conduction under oxygen atmosphere. Athigh oxygen partialpressure range pO_2=10~(-5~10~5 Pa, they were almost pure ionicconductors, which was consistent with the result by means of oxygen concentration cell.Whereas at low oxygen partial pressure range pO_2=10~(-5~10~(-15)Pa, the samplesexhibited mixed ionic and electronic conduction.

结果表明,氧浓差电池电动势的实测值与理论值吻合得很好,氧离子迁移数为1,表明该系列样品在该温度下氧气气氛中为纯氧离子导体;氧泵实验结果进一步证实了该系列样品在氧气气氛中为纯氧离子导体;在氧分压pO_2=10~(-5)~10~5 Pa的高氧分压气氛中,电导率与氧分压变化基本无关,表明在该氧分压范围样品为纯离子导体,这与氧浓差电池电动势测定结果相吻合:在低氧分压为10~(-5)~10~(-15) Pa范围,总电导率随氧分压降低而稍有升高,表明在该氧分压范围样品为氧离子与电子的混合导体。

Retrogressive erosion data of long-term monitoring in the typical thaw slumping indicates that expanding of the thaw slumping fluctuates along with the ground temperature's annual fluctuation, and expanding mostly takes place in 7~9 months. The maximal expanding appears at the direction of the slope tendency.

滑坡溯源侵蚀范围监测资料表明,滑塌范围的扩展随地温的周期变化波动进行,并主要集中在7~9月,最大扩展范围出现在沿坡体倾向方向。

The high-accuracy numerical simulation results by FEM indicate: the overburden deformation and failure caused by mining lead to fracture and the changes of apparent resistivity in overburden. The affected area is much larger than the actual fracture, nearly twice the fracture area. The most affected area by the apparent resistivity values is the caving zone. The changing ratio can be up to 19%. In the cracked zone, the changing ratio of the apparent resistivity is 10% to 12%.

计算结果表明:采动裂隙引起煤层上覆地层的视电阻率变化,其影响范围较实际破裂范围大得多,基本上是覆岩冒裂带范围的两倍,其视电阻率值最大影响区为冒落带,变化率可达19%;在裂隙发育带,视电阻率的变化率可达10%12%。

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