- 更多网络例句与稳定区相关的网络例句 [注：此内容来源于网络，仅供参考]
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Therefore, the moist potential vorticity analysis associated with the mesoscale convective system was researched in the paper, so as to reveal the moist potential characteristics of mesoscale convective system in typhoon circulation. The results showed that, during the generation stage, convective instability characterized by MPV1 was a favorable condition for forming MCS, while the vorticity which was caused by the slantwise isentropic surface and the vertical shear of the horizontal wind characterized by MPV2 was an inspiring mechanism. The specific process was that, the atmosphere exhibited the feature of strong convective instability at the low level of convection areas and the southeast areas, which included plenty of erratic energy. The slantwise ascended the stream transfer the erratic energy to northwest, where the stratification stability was small. As decreased, the cyclonic vorticity increased. On the other hand, the vorticity caused by the slantwise isentropic surface and the vertical shear of the horizontal wind inspired the release of convective instability and as a result that the MCS formed. During the development stage, the cyclonic vorticity increased quickly with the persistent decreasing of . Meanwhile, the inclination of isentropic linewas bigger than the absolute momentum line at middle level, which exhibited the feature of conditional symmetric instability , then the conditional symmetric instability was forced to release by the vorticity resulted from the slantwise isentropic surface and the vertical shear of horizontal wind, and the MCS developed.
结果表明，在对流形成阶段，MPV1即对流不稳定为MCS的形成提供背景不稳定条件，由MPV2即湿等熵面的倾斜和水平风的垂直切变而引起的涡旋发展作为强迫机制：MCS形成的区域及东南区域中低层是强对流不稳定层，蕴含丰富的不稳定能量，倾斜上升运动把对流不稳定区具有强不稳定能量的暖湿空气向西北中层的中性层结区输送，由于的减小，气旋性涡度增强，有利于形成对流，另一方面，由于湿等熵面倾斜和低空急流加强而引起的涡旋发展作为一种强迫机制激发对流不稳定能量得到释放，从而形成对流；在对流系统地发展阶段，由于低层的对流不稳定性进一步减弱，进一步减小，气旋性涡度进一步增强，有利于MCS的增强，中层等θe 线的倾斜度比绝对动量M 等值线的倾斜度大，对应有条件对称不稳定区域，满足条件对称不稳定条件，在湿等熵面倾斜和台风低空急流作用下引起的涡旋发展强迫对称不稳定能量释放，从而使得对流得以维持和加强。
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In this paper, the stable and unstable areas of dolomite are given by thermodynamical calculation.
文中列出了计算所得的白云石稳定区和不稳定区的范围。
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The results show that the gabion meshes present good tensile characteristics in the event of the rupture of the meshes. The larger-diameter gabion mesh shows a better mechanical performance, and the mechanical performance of 80RE geogrid is superior to that of 70RE geogrid. The revised relationship curves between the tension per unit width and unit elongation also present elastic stage, yield stage and strength stage. The constraint deformation of reinforcement is influenced by factors such as secant modulus of materials, stress levels, and the length of reinforcement in active area and stable area.
结果表明，格宾网在发生钢丝断裂之后仍呈现出较强的抗拉性能，大直径格宾网体现出优越的力学性能；80RE土工格栅的力学性能优于70RE土工格栅；修正后的格宾网的单位宽度拉伸力与伸长率的关系曲线仍呈现弹性、屈服和强化3个阶段；在约束条件下，筋带的变形量与筋带的割线模量、应力水平、筋带在加筋体中主动区和稳定区的长度等因素有关。
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We also summarized the effects of nonideal properties on thermodynamic and dynamical behaviors of B-Z reaction system.
在此基础上，对该反应体系进行了动力学稳定性分析，得到了B-Z反应体系定态的稳定区与不稳定区。
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The stick-slip region and the stable region in a parameter plane are separated by a critical parameter curve.
并在静动摩擦落差数/动摩擦系数的参数平面上划分出稳定区和粘滑运动区。
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Dated from Proterozoic to Mesozoic, they have poly-circle characteristics, found from one tectonic circle to another, which is very rare in the worldwide orogens. This reveals that the orogen and stable area of the world, the mantle and crust states of the Proterozoic and Phanerozoic are different in tectonic evolvement and dynamic process and that the rapakivi granite of the Qinling-Kunlun is a kind of orogenic granite different from the stable area of the Proterozoic.
它们出现在每一个大的造山旋回晚期，即向另一个构造旋回的转折期，这在世界造山带中是十分罕见的，反映出世界上造山带与稳定区元古宙和显生宙的地慢与地壳状态是不一样的，有着不同的构造演化历史和动力学过程，表明秦岭－昆仑地区的环斑花岗岩是一种有别于元古宙稳定区的造山型环斑花岗岩。
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We study feature of stable and existing zones of multiplecomposition natural gas hydrate in seafloor sediments.
本文研究了多组分天然气在海底沉积层中稳定区和存在区的一些特点。
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We study feature of stable and existing zones of multiple-composition natural gas hydrate in seafloor sediments.
本文研究了多组分天然气在海底沉积层中稳定区和存在区的一些特点。
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Heat flows derived from garnet, chromite/chromium-spinel and pyroxene of xenoliths, xenocrysts in Mengyin and Fuxian kimberlites are higher than 40mW/m〓 calculated from the pyroxene inclusions in diamonds, and the range of pressure is 20～40kb (equivalent to 65～130km). Metasomatism (as indicated by yimengite and lindsleyite in Mengyin) is very strong in this depth range. Lherzolite, wehrlite, and diamond-free high-Ca harzburigite around the world are derived from this depth also. The observation suggests that the low-Ca harzburigitic environment for diamond stability had been changed significantly when the kimberlitic magmas erupted. This resulted from fluid interaction with harzburigite. The geotherm of the Cenozoic lithospheric mantle beneath Eastern-North China platform is higher than oceanic one. The temperature from the interior of the Tan-Lu faults is higher than that from apart off the fault.
除金刚石中的辉石温压投点落于40m W/m〓占地温线上外，捕虏体及捕虏晶中石榴石，铬尖晶石及单斜辉石的投点均偏离该地温线，显示较高的地温特点，而且捕虏体及捕虏晶的压力范围多在20-40kb(相当于65-130km)间，该深度范围内地幔的交代作用特别发育，如蒙阴大量发育的沂蒙矿、钛钾铬石等就发育于该深度范围，世界范围内不含金刚石的高钙方辉橄榄岩、二辉橄榄岩、异剥橄榄岩也分布于该区中，一方面表明捕虏体的主要取样位置已不在金刚石稳定区中，另一方面也表明金刚石稳定的橄榄岩环境，在金伯利岩侵位并捕虏他们时已发现了明显的改造，这种改造作用主要是通过长期的熔流体与先存的橄榄岩相互作用的结果。
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Based on Darcy's law, the depth distribution of the stability zone and the deposits zone of gas hydrate is quantified, and the effective factors of their boundary conditions are identified carefully with the theoretical model.
本文以达西定律为基础，通过理论模型对水合物稳定区、沉积区的深度分布进行了量化并对各自的边界条件的影响因素做了详细的分析。
- 更多网络解释与稳定区相关的网络解释 [注：此内容来源于网络，仅供参考]
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contour zone：稳定气流区
continuous heating连续采暖 | contour zone稳定气流区 | control device控制装置
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contracted Riemann-Christoffel tensor：缩并的曲率张量
contracted responsibility system of editors 编辑承包责任制 | contracted Riemann-Christoffel tensor 缩并的曲率张量 | contracted stable region 收缩稳定区
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phase transition temperature：相变温度
相稳定区 phase stabile range | 相变温度 phase transition temperature | 相变压力 phase transition pressure
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stability region：稳定区
stability 稳定度 | stability region 稳定区 | stabilization 稳定
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stability region：稳定域
结构区:structural region | 稳定域:stability region | 调控区:control region
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transient stability region：暂态稳定区
"transient stability ","暂态稳(定)度" | "transient stability region ","暂态稳定区" | "transient state ","暂态"
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transient stability region：瞬时稳定区
transient stability power limit 瞬态稳定功率极限 | transient stability region 瞬时稳定区 | transient stage 瞬态级
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Rf stability region：射频稳定区
Rf sputtering 射频溅射 | Rf stability region 射频稳定区 | RF standard signal generator 射频标准信号发生器
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stable fixed point：(稳定区的)稳定固定点
stable fission products 稳定的裂变产物 | stable fixed point (稳定区的)稳定固定点 | stable flying 稳定飞行
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kinematically stable support：运动学稳定的支架
[25] access to the gob:采空区通路 | [26] kinematically stable support:运动学稳定的支架 | [27] seals off the gob:封闭采空区