Se presentan los resultados de la investigación arqueológica del sitio inka Palacio de la Real Aduana, ubicado en el centro histórico de la ciudad de Santiago, Chile. Por medio del análisis de su contexto, se interpreta la funcionalidad del asentamiento y el rol que cumplió dentro de la estrategia de dominación inka de la población Aconcagua. Así, se lo define como el centro político del extremo austral del Tawantinsuyu. Además, a partir del estudio de las características tipológicas e iconográficas de la fragmentería alfarera se propone el contexto ideológico de los ceremoniales políticos desarrollados en este lugar y la importancia de la población diaguita en este proceso.Palabras clave: Inka, Chile central, centro político, Diaguita, Kollasuyu.These are the results of an archaeological research of the Inka site Palacio de la Real Aduana, located in the historic center of Santiago, Chile. By means of contextual analysis, there is an interpretation of the functionality of this settlement and its role as part of a strategy of Inka domination of the Aconcagua people, which lead to defining this settlement as the political center of the Austral end of the Tawantinsuyu. In addition, the study of the typological and iconographic characteristics of the pottery fragment suggests a possible ideological context of the political ceremonies developed in this place and the importance of the diaguita population in this process.
RESUMEN
Los altos porcentajes de concentración de precipitación diaria en pocos días, pueden incrementar el potencial de erosión, inestabilidad de laderas y riesgo de inundaciones
ABSTRACT
High percentages total precipitation concentration in a few very rainy days can increase the potential of erosion, instability and risks of floods, these problems are common in Peru. So it is important to know about the daily precipitation. This paper presents, an investigation of the spatial and temporal patterns of daily precipitation concentration, in central Andes of Perú, the Concentration index (CI) was evaluates measurement the varying weight of daily precipitation, the contribution of the days of greatest rainfall to the total amount. The index is applied to
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