概括
研究人员开发了一种分析冰架压力的新方法. 南极冰架的应变率随着偏离应力立方体的增加而增加.
科学领域:
- 冰川学的冰川学
- 固体地球地质物理学 地质物理学
背景情况:
- 冰架是南极冰盖的关键组成部分.
- 了解应力分布是预测冰架稳定性和对海平面上升的贡献的关键.
研究的目的:
- 提出一种用于计算边界冰架中应力场的新方法.
- 为了比较罗斯冰架上的应变率和偏差应力.
主要方法:
- 开发一种用于应力场计算的新计算方法.
- 该方法用于分析来自南极洲罗斯冰架的数据.
主要成果:
- 确立了延展率和偏差应力之间的定量关系.
- 延展率随着偏差应力的第三次数 (ε̇ σ̇3) 的增加而增加.
- 确定了一个比例常数 (2.3 x 10−25 s/(N/m2) 2).
结论:
- 这种新方法提供了对冰架机械行为的洞察.
- 这些发现为改善冰架动态和稳定的建模提供了基础.
更多相关视频
11:38Combining Microfluidics and Microrheology to Determine Rheological Properties of Soft Matter during Repeated Phase Transitions
Published on: April 19, 2018
08:42Challenges in Rheological Characterization of Highly Concentrated Suspensions — A Case Study for Screen-printing Silver Pastes
Published on: April 10, 2017
相关概念视频
Viscosity
When water is poured into a glass, it falls freely and quickly, whereas if honey or maple syrup is poured over a pancake, it flows slowly and sticks to the surface of the container. This difference in the flow of different kinds of liquids arises due to the fluid friction between the liquid layers and the liquid and the surrounding material. This property of fluids is called fluid viscosity. In this example, water has a lower viscosity than honey and maple syrup.
The SI unit of viscosity is...
The SI unit of viscosity is...
Phase Transitions: Melting and Freezing
Heating a crystalline solid increases the average energy of its atoms, molecules, or ions, and the solid gets hotter. At some point, the added energy becomes large enough to partially overcome the forces holding the molecules or ions of the solid in their fixed positions, and the solid begins the process of transitioning to the liquid state or melting. At this point, the temperature of the solid stops rising, despite the continual input of heat, and it remains constant until all of the solid is...
Viscosity of Fluid
Viscosity measures the resistance a fluid offers to flow and deformation. It results from internal friction between layers of fluid moving relative to one another. Dynamic viscosity, denoted by the Greek letter mu (μ), quantifies the force needed to move one fluid layer over another. For Newtonian fluids like water and air, the relationship between the shearing stress and the rate of shearing strain is linear, meaning their viscosity remains constant regardless of the applied stress.
