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Abstract

Abstract (AI English translation)

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In the international context, it is accepted that bone fractures heal through a prolonged process, culminating in significant regeneration that can be evaluated by X-rays approximately twelve months after the start of definitive treatment, or even at the same time if conservative treatment has been chosen. Several factors are involved in this process, among the most important being the proportion of oxygen present in the patient's blood. It is also widely recognized that the oxygen saturation in the bloodstream is proportional to the partial pressure of oxygen in the atmosphere, which varies depending on the patient's altitude above sea level.

Currently, it is accepted worldwide that altitudes greater than 2500-3000 meters above sea level (masl) reduce the rate of bone regeneration by approximately 20-30%, resulting in a similar proportion of non-union failures. Locally, in the city of Juliaca, studies on this aspect are almost nonexistent, and the few that exist focus on variables such as the stability of the fracture reduction provided by the osteosynthesis material.

Details

1010268
Title
Tiempo de aparición de signos radiológicos de consolidación ósea en medicina de altura
Alternate title
Time of Appearance of Radiological Signs of Bone Consolidation in High-Altitude Medicine
Number of pages
37
Publication year
2025
Degree date
2025
School code
2535
Source
MAI 87/6(E), Masters Abstracts International
ISBN
9798265485809
University/institution
Universidad Nacional del Altiplano de Puno (Peru)
University location
Peru
Degree
Master's
Source type
Dissertation or Thesis
Language
Spanish
Document type
Dissertation/Thesis
Dissertation/thesis number
32419287
ProQuest document ID
3288414874
Document URL
https://www.proquest.com/dissertations-theses/tiempo-de-aparición-signos-radiológicos/docview/3288414874/se-2?accountid=208611
Copyright
This work is published under https://creativecommons.org/licenses/by/4.0/ (the “License”). Notwithstanding the ProQuest Terms and Conditions, you may use this content in accordance with the terms of the License.
Database
ProQuest One Academic