这是西西里岛第一个绝对重力和高度参考网络
Filippo Greco1, Giovanna Berrino2, Federica Riguzzi3
1INGV, sez. Osservatorio Etneo, Catania, Italy. filippo.greco@ingv.it.
Scientific data
|April 8, 2024
概括
在西西里建立了一个新的绝对重力和高度参考网络. 长期的重力测量证实了地理参考系统所选择的地点的稳定性.
科学领域:
- 地测和地球物理学的地质学.
- 地球科学 地球科学 地球科学
背景情况:
- 建立精确的地理测量参考网络对于科学和技术应用至关重要.
- 西西里独特的地质环境需要现代的高度系统来进行准确的监测.
研究的目的:
- 在西西里开发一个新的绝对重力和高度参考网络的方法和工具框架.
- 为更新意大利地区的参考系统做出贡献,支持重力场研究和高度系统定义.
主要方法:
- 在西西里建立一个5个站的绝对重力和高度参考网络.
- 重新占用四个站点,在20世纪90年代进行测量,以评估长期变化.
- 分析重力数据和共同定位的GPS/GNSS数据,以评估现场稳定性和地面变形.
主要成果:
- 新网络为西西里绝对重力和高度参考提供了一个强大的框架.
- 大约30年的长期重力测量表明,在选定的绝对重力站稳定.
- 对GPS/GNSS数据的分析支持对长期地形变形模式的评估.
结论:
- 已建立的网络适合定义现代高度系统并支持西西里的重力场研究.
- 这些遗址的长期稳定性证实了它们作为基本参考点的有效性.
- 这项工作为该地区未来的地理监测和研究奠定了基础.
相关概念视频
Gravimetry: Overview
5.7K
Gravimetric analysis is a quantitative method where the analyte is isolated and weighed directly or after conversion into a substance of known composition. Gravimetric analysis can be classified as precipitation, electrogravimetry, volatilization, and particulate gravimetry, based on the method used to isolate the analyte.
In precipitation gravimetry, the analyte is converted into a precipitate and weighed. For example, the silver content in a sample can be estimated by precipitating and...
In precipitation gravimetry, the analyte is converted into a precipitate and weighed. For example, the silver content in a sample can be estimated by precipitating and...
5.7K
Geoid and Ellipsoid
34
The Earth's shape is best described as an ellipsoid, a slightly flattened sphere created by rotating an ellipse around its minor axis. This flattening results in the polar axis being about 21 kilometers shorter than the equatorial axis. In contrast, the geoid represents the Earth's gravitational shape and aligns with the mean sea level (MSL). The geoid is an irregular equipotential surface where gravity is perpendicular at every point. Variations in Earth's mass distribution cause geoid...
34
Measuring Acceleration Due to Gravity
562
Consider a coffee mug hanging on a hook in a pantry. If the mug gets knocked, it oscillates back and forth like a pendulum until the oscillations die out.
A simple pendulum can be described as a point mass and a string. Meanwhile, a physical pendulum is any object whose oscillations are similar to a simple pendulum, but cannot be modeled as a point mass on a string because its mass is distributed over a larger area. The behavior of a physical pendulum can be modeled using the principles of...
A simple pendulum can be described as a point mass and a string. Meanwhile, a physical pendulum is any object whose oscillations are similar to a simple pendulum, but cannot be modeled as a point mass on a string because its mass is distributed over a larger area. The behavior of a physical pendulum can be modeled using the principles of...
562
Gravity between Spherical Bodies
8.4K
Newton's law of gravitation describes the gravitational force between any two point masses. However, for extended spherical objects like the Earth, the Moon, and other planets, the law holds with an assumption that masses of spherical objects are concentrated at their respective centers.
This assumption can be proved easily by showing that the expression for gravitational potential energy between a hollow sphere of mass (M) and a point mass (m) is the same as it would be for a pair of extended...
This assumption can be proved easily by showing that the expression for gravitational potential energy between a hollow sphere of mass (M) and a point mass (m) is the same as it would be for a pair of extended...
8.4K
Newton's Law of Gravitation
12.7K
Our everyday observation tells us that all objects close to the Earth naturally tend to fall to the ground. Early philosophers assumed that this downward force was unique to Earth. By the 16th century, Nicolaus Copernicus (1473-1543) put forward the heliocentric theory, which suggested that Earth and other planets orbited the sun, while the Moon orbited the Earth. However, it was Isaac Newton (1642-1727) who linked these two motions together in the 17th century. He reasoned that the force of...
12.7K
Influence of Earth's Curvature and Atmospheric Refraction on Leveling
92
During leveling, the Earth's curvature and atmospheric refraction introduce deviations in the line of sight from a true horizontal reference. When the line of sight is leveled, it remains perpendicular to the plumb line only at a single point. Beyond this, it deviates due to the Earth’s curvature, represented by the correction C. For a sight distance D, the deviation can be derived using the relationship:This relationship shows that the deviation increases quadratically with distance.
92


