isostatic

简明释义

英[ˌaɪsəʊˈstætɪk]美[ˌaɪsəˈstætɪk]

adj. 均衡说的；[地物] 地壳均衡的

英英释义

单词用法

同义词

反义词

例句

1.Involved in isostatic correction sometimes taken as the top of the asthenosphere.

在均衡校正中有时将其作为软流层的顶部。

2.Die pressing process and cold isostatic pressing process are the important methods of making ceramic parts.

陶瓷粉末干压成型和冷等静压成型是制备陶瓷结构部件的重要方法。

3.Advantages, and techniques of hot isostatic presses and its application in the field of magnetic material, and ceramics are introduced.

介绍了热等静压的优点和工艺技术及其在磁性材料、陶瓷等领域中的应用。

4.The glaze craze of solid core insulator fabricated by cold isostatic dry pressing is analysed. The glaze craze is attributed mainly to glazing technology.

分析了等静压干法成型棒形产品的上釉缺陷，认为釉裂缺陷的主要原因是施釉工艺问题。

5.According to Airy isostatic hypotheses, a computation of isostatic compensation has been made and a map of M surface and a map of isostatic anomaly drawn up.

根据艾利的均衡假设，进行了均衡补偿的归算，编制了莫霍界面图和均衡异常图。

6.The experiments showed that it achieved the same results as the hot isostatic compaction.

实验表明准热等静压可得到与等静压相同的结果。

7.In engineering, isostatic 等静压的 support systems are designed to distribute loads evenly across structures.

在工程中，等静压的支撑系统旨在将负载均匀分布在结构上。

8.Geologists study isostatic 等静压的 adjustments to better predict seismic activity in the region.

地质学家研究等静压的调整，以更好地预测该地区的地震活动。

9.The study of isostatic 等静压的 processes helps in understanding mountain formation.

对等静压过程的研究有助于理解山脉的形成。

10.The isostatic 等静压的 rebound after glacial melting can lead to significant geological changes.

冰川融化后的等静压的反弹可能导致显著的地质变化。

11.The concept of isostatic 等静压的 equilibrium is crucial in understanding how the Earth's crust behaves under various loads.

等静压的平衡概念对于理解地壳在不同负载下的行为至关重要。

作文

The concept of isostatic adjustment is crucial in understanding the dynamics of Earth's crust. When we think about the forces that shape our planet, it is essential to consider how different geological processes affect the stability and elevation of landforms. Isostatic adjustments occur when the Earth's crust responds to changes in surface load, such as the melting of glaciers or the accumulation of sediment. This process ensures that the crust maintains a balance, adjusting its height in response to varying weights above it.For instance, during the last Ice Age, massive ice sheets covered significant portions of North America and Europe. The immense weight of these ice sheets caused the underlying crust to sink, leading to a state of isostatic depression. As the climate warmed and the ice began to melt, the crust started to rebound, a process known as isostatic uplift. This phenomenon is still observable today, as regions formerly covered by ice continue to rise slowly, demonstrating the long-term effects of isostatic adjustments.Understanding isostatic processes is not only important for geologists but also for civil engineers and urban planners. As cities develop, they often alter the natural landscape, adding buildings, roads, and other structures that change the load on the Earth's crust. Engineers must consider isostatic principles when designing foundations and infrastructure to ensure stability over time. If the load changes significantly, it could lead to subsidence or other structural issues.Additionally, isostatic adjustments have implications for sea level rise. As glaciers melt due to climate change, the redistribution of water can impact coastal regions. Areas that were once elevated may experience flooding as the weight of the water shifts, causing an isostatic response that alters the local topography. Understanding these changes is vital for predicting future sea level scenarios and preparing for potential impacts on communities.In conclusion, the term isostatic refers to the balance and adjustments of the Earth's crust in response to changes in surface loads. This concept is fundamental in various fields, including geology, engineering, and environmental science. By studying isostatic processes, we can gain insights into the past and present dynamics of our planet, as well as prepare for future challenges related to climate change and urban development. The continued research into isostatic adjustments will undoubtedly enhance our understanding of Earth's complex systems and their interconnections.

‘等静压’（isostatic）调整的概念对于理解地球地壳的动态至关重要。当我们考虑塑造我们星球的力量时，必须考虑不同的地质过程如何影响地貌的稳定性和高度。‘等静压’（isostatic）调整发生在地壳对表面负荷变化（如冰川融化或沉积物积累）作出响应时。这个过程确保了地壳保持平衡，根据上方不同重量的变化调整其高度。例如，在上一个冰河时代，巨大的冰盖覆盖了北美和欧洲的大片地区。这些冰盖的巨大重量导致下面的地壳下沉，导致一种‘等静压’（isostatic）沉降状态。随着气候变暖，冰开始融化，地壳开始反弹，这一过程被称为‘等静压’（isostatic）抬升。今天仍然可以观察到这一现象，因为曾经被冰覆盖的地区仍在缓慢上升，展示了‘等静压’（isostatic）调整的长期影响。理解‘等静压’（isostatic）过程不仅对地质学家重要，对土木工程师和城市规划者同样重要。随着城市的发展，它们往往会改变自然景观，增加建筑物、道路和其他结构，从而改变地壳上的负载。工程师在设计基础和基础设施时必须考虑‘等静压’（isostatic）原理，以确保随着时间的推移保持稳定。如果负载发生显著变化，可能会导致沉降或其他结构问题。此外，‘等静压’（isostatic）调整对海平面上升也有影响。由于气候变化，随着冰川融化，水的重新分配可能会影响沿海地区。曾经高耸的区域可能会因水的重量转移而遭遇洪水，导致一种‘等静压’（isostatic）反应，改变当地地形。理解这些变化对于预测未来海平面情景以及为社区潜在影响做好准备至关重要。总之，‘等静压’（isostatic）一词指的是地壳在响应表面负荷变化时的平衡和调整。这个概念在地质学、工程学和环境科学等多个领域中都是基础。通过研究‘等静压’（isostatic）过程，我们可以深入了解我们星球的过去和现在动态，以及为与气候变化和城市发展相关的未来挑战做好准备。对‘等静压’（isostatic）调整的持续研究无疑将增强我们对地球复杂系统及其相互联系的理解。