Bibliographic citations
Chávez, D., (2010). Espacio disponible para la erupción del tercer molar inferior incluido según lado mandibular en pacientes de 18 a 35 años [Tesis, Universidad Nacional Mayor de San Marcos]. https://hdl.handle.net/20.500.12672/571
Chávez, D., Espacio disponible para la erupción del tercer molar inferior incluido según lado mandibular en pacientes de 18 a 35 años [Tesis]. PE: Universidad Nacional Mayor de San Marcos; 2010. https://hdl.handle.net/20.500.12672/571
@misc{renati/477476,
title = "Espacio disponible para la erupción del tercer molar inferior incluido según lado mandibular en pacientes de 18 a 35 años",
author = "Chávez Barboza, Diana",
publisher = "Universidad Nacional Mayor de San Marcos",
year = "2010"
}
--- The discharge prevalencia of third low molars not erupcionados is a constant worry for the odontologists in general for the diverse complications that he(she) carries on having remained in the jaw. It is necessary to to have knowledge of the factors that alter his(her,your) eruption but especially establish in an exact way the available space for his(her,your) eruption. An inadequate diagnosis would carry to generating patologías as(like) pericoronaritis, reabsorptions radiculares, cysts, periodontitis enclosed some studies affirm that they can aggravate the overcrowdings antero low. The unnecessary extraction of this piece carries that might not be used later as replacement of neighboring(similar) pieces or as elements protésicos which would harm the oral health of the person. The aim(lens) of this investigation(research) was to determine the available space of the third low molars. For it 50 clinical histories were examined by panoramic X-ray photographies by complete low dentition where the studied characteristics were Broad Mesio Distal of the wreath, relation of the third low molar with the ascending(rising) branch according to the analysis of Pell and Gregory, available space for the eruption of the third low molar. The results of the average for the Broad Mesio Distal of the third low molar of the sample selected for the feminine kind(genre) it(he,she) was of 11,84mm (+/-DS=1.08) and for the masculine kind(genre) 1,25 was of 12,06mm (+/-DS =), where there was no statistically significant difference. For the relation of the third low molar with the ascending(rising) pertaining to the jaw branch according to the index of Pell and Gregory there is predominance of the class the IIIrd in 60,42 % in the feminine kind(genre) and in the masculine kind(genre) it(he,she) predominates over the class the IIIrd in 62,22 %. With regard to the Available Space according to Ganns's index for the feminine kind(genre) the average was of 0,81 (+/-DS = 0,28), for the masculine kind(genre) the average was of 0,78 (+/-DS = 0,20) concluding that there were neither significant differences between kinds(genres) nor pertaining to the jaw sides. Likewise so much in the feminine population since(as,like) masculine the interval predominates with 70 % and 80 % respectively over from 0 to 0,99 according to Ganns's index and the rest of the population (30 % and 20 % respectively) they presented a major or equal index to 1, presenting both third molar included populations. Therefore one concludes that in the dimensions evaluated in the incorporation of third low molars significant difference does not exist in both kinds(genres), with regard to the index of Pell and Gregory there is predominance in both kinds(genres) of the class the IIIrd and with regard to the available space there does not exist significant difference between pertaining to the jaw sides and kinds(genres); but the interval predominates over from 0 to 0,99; this would mean according to Ganns that his(her,your) probability of eruption is 30 %, with these results the established is not fulfilled or found in other works of investigation(research) where they demonstrate a minor available space for the feminine kind(genre) and the pertaining to the jaw right(straight) side, but if there is congruity that to minor index of minor Ganns probability of eruption.
This item is licensed under a Creative Commons License