Floor readjustment
Introduction
A land subsidence or also called sinkhole is a movement of the earth's surface in which the descending direction predominates and which takes place in areas of different characteristics and slopes. It differs from the term subsidence due to its much smaller temporal and spatial scales. This movement can be induced by different causes and can develop at very fast or very slow speeds depending on the mechanism that gives rise to such instability.
Causes
Among the main causes of land subsidence, we can mention the dissolution of limestone, which is calcium carbonate, due to the action of groundwater. Although CaCO has a relatively small solubility product constant, it is very soluble in the presence of an acid. This problem has caused many problems in many places and countries such as Prague, Mexico, Florida, Venezuela, Spain, among others.
• - Firstly, the direct action of gravity. The materials of the earth's surface that are found on steep terrain can move suddenly in response to the direct action of gravity, especially when continuous rains can contribute to the mass sliding of poorly consolidated materials from the slopes.
• - Rainwater is acidic by nature (due to the combination of carbon dioxide (CO) with atmospheric water, which is transformed into carbonic acid with a 5 to 6 and can become more acidic in contact with decomposing plant matter.
• - If the vertical movement is slow or very slow (for example, centimeters/year) and affects a large surface area (km²), it is often referred to as subsidence. If the movement is very fast (m/s) it is usually referred to as collapse.
The response of geological materials to distensional tectonic stresses, for example to the formation of tectonic trenches or which over time can give rise to fissures.
• - * The response of geological materials to locally tensional tectonic stresses in a framework of epidermal tectonics with sets of superficial faults with flexed paths, for example in pull-apart type basins.
- Lithospheric readjustments due to isostasy, for example at the end of a continental collision after the cessation of crustal uplift or the end of the formation of an orogen.
• - Variations in the water table or in the state of soil moisture, for example as a consequence of the exploitation of aquifers.