Post on 10-Jul-2019
30/06/2011
1
PROCESOS CONSTRUCTIVOS 1 CREMASCHI-MARSILI-SAENZ
2011
EL SUELO
VEAMOS ALGUNAS IMÁGENES
CMS•CMS•CMS•CMS•CMS•CMS•CMS CMS•CMS•CMS•CMS•CMS•CMS•CMS CMS•CMS•CMS•CMS•CMS•CMS•CMS CMS•CMS•CMS•CMS•CMS•CMS•CMS CMS•CMS•CMS•CMS•CMS•CMS•CMS CMS•CMS•CMS•CMS•CMS•CMS•CMS CMS•CMS•CMS•CMS•CMS•CMS•CMS CMS•CMS•CMS•CMS•CMS•CMS•CMS CMS•CMS•CMS•CMS•CMS•CMS•CMS CMS•CMS•CMS•CMS•CMS•CMS•CMS CMS•CMS•CMS•CMS•CMS•CMS•CMS CMS•CMS•CMS•CMS•CMS•CMS•CMS CMS•CMS•CMS•CMS•CMS•CMS•CMS CMS•CMS•CMS•CMS•CMS•CMS•CMS CMS•CMS•CMS•CMS•CMS•CMS•CMS CMS•CMS•CMS•CMS•CMS•CMS•CMS CMS•CMS•CMS•CMS•CMS•CMS•CMS CMS•CMS•CMS•CMS•CMS•CMS•CMS CMS•CMS•CMS•CMS•CMS•CMS•CMS CMS•CMS•CMS•CMS•CMS•CMS•CMS CMS•CMS•CMS•CMS•CMS•CMS•CMS
30/06/2011
2
CMS•CMS•CMS•CMS•CMS•CMS•CMS CMS•CMS•CMS•CMS•CMS•CMS•CMS CMS•CMS•CMS•CMS•CMS•CMS•CMS CMS•CMS•CMS•CMS•CMS•CMS•CMS CMS•CMS•CMS•CMS•CMS•CMS•CMS CMS•CMS•CMS•CMS•CMS•CMS•CMS CMS•CMS•CMS•CMS•CMS•CMS•CMS CMS•CMS•CMS•CMS•CMS•CMS•CMS CMS•CMS•CMS•CMS•CMS•CMS•CMS CMS•CMS•CMS•CMS•CMS•CMS•CMS CMS•CMS•CMS•CMS•CMS•CMS•CMS CMS•CMS•CMS•CMS•CMS•CMS•CMS CMS•CMS•CMS•CMS•CMS•CMS•CMS CMS•CMS•CMS•CMS•CMS•CMS•CMS CMS•CMS•CMS•CMS•CMS•CMS•CMS CMS•CMS•CMS•CMS•CMS•CMS•CMS CMS•CMS•CMS•CMS•CMS•CMS•CMS CMS•CMS•CMS•CMS•CMS•CMS•CMS CMS•CMS•CMS•CMS•CMS•CMS•CMS CMS•CMS•CMS•CMS•CMS•CMS•CMS CMS•CMS•CMS•CMS•CMS•CMS•CMS
30/06/2011
3
CMS•CMS•CMS•CMS•CMS•CMS•CMS CMS•CMS•CMS•CMS•CMS•CMS•CMS CMS•CMS•CMS•CMS•CMS•CMS•CMS CMS•CMS•CMS•CMS•CMS•CMS•CMS CMS•CMS•CMS•CMS•CMS•CMS•CMS CMS•CMS•CMS•CMS•CMS•CMS•CMS CMS•CMS•CMS•CMS•CMS•CMS•CMS CMS•CMS•CMS•CMS•CMS•CMS•CMS CMS•CMS•CMS•CMS•CMS•CMS•CMS CMS•CMS•CMS•CMS•CMS•CMS•CMS CMS•CMS•CMS•CMS•CMS•CMS•CMS CMS•CMS•CMS•CMS•CMS•CMS•CMS CMS•CMS•CMS•CMS•CMS•CMS•CMS CMS•CMS•CMS•CMS•CMS•CMS•CMS CMS•CMS•CMS•CMS•CMS•CMS•CMS CMS•CMS•CMS•CMS•CMS•CMS•CMS CMS•CMS•CMS•CMS•CMS•CMS•CMS CMS•CMS•CMS•CMS•CMS•CMS•CMS CMS•CMS•CMS•CMS•CMS•CMS•CMS CMS•CMS•CMS•CMS•CMS•CMS•CMS CMS•CMS•CMS•CMS•CMS•CMS•CMS
30/06/2011
4
CMS•CMS•CMS•CMS•CMS•CMS•CMS CMS•CMS•CMS•CMS•CMS•CMS•CMS CMS•CMS•CMS•CMS•CMS•CMS•CMS CMS•CMS•CMS•CMS•CMS•CMS•CMS CMS•CMS•CMS•CMS•CMS•CMS•CMS CMS•CMS•CMS•CMS•CMS•CMS•CMS CMS•CMS•CMS•CMS•CMS•CMS•CMS CMS•CMS•CMS•CMS•CMS•CMS•CMS CMS•CMS•CMS•CMS•CMS•CMS•CMS CMS•CMS•CMS•CMS•CMS•CMS•CMS CMS•CMS•CMS•CMS•CMS•CMS•CMS CMS•CMS•CMS•CMS•CMS•CMS•CMS CMS•CMS•CMS•CMS•CMS•CMS•CMS CMS•CMS•CMS•CMS•CMS•CMS•CMS CMS•CMS•CMS•CMS•CMS•CMS•CMS CMS•CMS•CMS•CMS•CMS•CMS•CMS CMS•CMS•CMS•CMS•CMS•CMS•CMS CMS•CMS•CMS•CMS•CMS•CMS•CMS CMS•CMS•CMS•CMS•CMS•CMS•CMS CMS•CMS•CMS•CMS•CMS•CMS•CMS CMS•CMS•CMS•CMS•CMS•CMS•CMS
30/06/2011
5
CMS•CMS•CMS•CMS•CMS•CMS•CMS CMS•CMS•CMS•CMS•CMS•CMS•CMS CMS•CMS•CMS•CMS•CMS•CMS•CMS CMS•CMS•CMS•CMS•CMS•CMS•CMS CMS•CMS•CMS•CMS•CMS•CMS•CMS CMS•CMS•CMS•CMS•CMS•CMS•CMS CMS•CMS•CMS•CMS•CMS•CMS•CMS CMS•CMS•CMS•CMS•CMS•CMS•CMS CMS•CMS•CMS•CMS•CMS•CMS•CMS CMS•CMS•CMS•CMS•CMS•CMS•CMS CMS•CMS•CMS•CMS•CMS•CMS•CMS CMS•CMS•CMS•CMS•CMS•CMS•CMS CMS•CMS•CMS•CMS•CMS•CMS•CMS CMS•CMS•CMS•CMS•CMS•CMS•CMS CMS•CMS•CMS•CMS•CMS•CMS•CMS CMS•CMS•CMS•CMS•CMS•CMS•CMS CMS•CMS•CMS•CMS•CMS•CMS•CMS CMS•CMS•CMS•CMS•CMS•CMS•CMS CMS•CMS•CMS•CMS•CMS•CMS•CMS CMS•CMS•CMS•CMS•CMS•CMS•CMS CMS•CMS•CMS•CMS•CMS•CMS•CMS
30/06/2011
6
CMS•CMS•CMS•CMS•CMS•CMS•CMS CMS•CMS•CMS•CMS•CMS•CMS•CMS CMS•CMS•CMS•CMS•CMS•CMS•CMS CMS•CMS•CMS•CMS•CMS•CMS•CMS CMS•CMS•CMS•CMS•CMS•CMS•CMS CMS•CMS•CMS•CMS•CMS•CMS•CMS CMS•CMS•CMS•CMS•CMS•CMS•CMS CMS•CMS•CMS•CMS•CMS•CMS•CMS CMS•CMS•CMS•CMS•CMS•CMS•CMS CMS•CMS•CMS•CMS•CMS•CMS•CMS CMS•CMS•CMS•CMS•CMS•CMS•CMS CMS•CMS•CMS•CMS•CMS•CMS•CMS CMS•CMS•CMS•CMS•CMS•CMS•CMS CMS•CMS•CMS•CMS•CMS•CMS•CMS CMS•CMS•CMS•CMS•CMS•CMS•CMS CMS•CMS•CMS•CMS•CMS•CMS•CMS CMS•CMS•CMS•CMS•CMS•CMS•CMS CMS•CMS•CMS•CMS•CMS•CMS•CMS CMS•CMS•CMS•CMS•CMS•CMS•CMS CMS•CMS•CMS•CMS•CMS•CMS•CMS CMS•CMS•CMS•CMS•CMS•CMS•CMS
30/06/2011
7
CMS•CMS•CMS•CMS•CMS•CMS•CMS CMS•CMS•CMS•CMS•CMS•CMS•CMS CMS•CMS•CMS•CMS•CMS•CMS•CMS CMS•CMS•CMS•CMS•CMS•CMS•CMS CMS•CMS•CMS•CMS•CMS•CMS•CMS CMS•CMS•CMS•CMS•CMS•CMS•CMS CMS•CMS•CMS•CMS•CMS•CMS•CMS CMS•CMS•CMS•CMS•CMS•CMS•CMS CMS•CMS•CMS•CMS•CMS•CMS•CMS CMS•CMS•CMS•CMS•CMS•CMS•CMS CMS•CMS•CMS•CMS•CMS•CMS•CMS CMS•CMS•CMS•CMS•CMS•CMS•CMS CMS•CMS•CMS•CMS•CMS•CMS•CMS CMS•CMS•CMS•CMS•CMS•CMS•CMS CMS•CMS•CMS•CMS•CMS•CMS•CMS CMS•CMS•CMS•CMS•CMS•CMS•CMS CMS•CMS•CMS•CMS•CMS•CMS•CMS CMS•CMS•CMS•CMS•CMS•CMS•CMS CMS•CMS•CMS•CMS•CMS•CMS•CMS CMS•CMS•CMS•CMS•CMS•CMS•CMS CMS•CMS•CMS•CMS•CMS•CMS•CMS
30/06/2011
8
EL SUELO ES UN SISTEMA TRIFÁSICO
VOLÚMENES Y PESOS DE LAS FASES DEL SUELO
VOLÚMENES
Vt = Volumen Total Vs = Volumen de la fase sólida Vw = Volumen de la fase líquida (Agua) Va = Volumen de la fase gaseosa (Aire) Vv = Volumen de vacíos Vv = Vw + Va Vt = Vs + Vv = Vs + Vw + Va
PESOS
Wt = Peso Total Ws = Peso de la fase sólida Wa = Peso de la fase gaseosa Ww = Peso de la fase líquida (Agua) PESO DE LA FASE SÓLIDA (Ws) Se determina secando el suelo en estufa a 105 ºC durante 24 horas
AGUA EN EL SUELO
AGUA GRÁVICA
AGUA RETENIDA HIGROSCÓPICA
CAPILAR
CMS•CMS•CMS•CMS•CMS•CMS•CMS CMS•CMS•CMS•CMS•CMS•CMS•CMS CMS•CMS•CMS•CMS•CMS•CMS•CMS CMS•CMS•CMS•CMS•CMS•CMS•CMS CMS•CMS•CMS•CMS•CMS•CMS•CMS CMS•CMS•CMS•CMS•CMS•CMS•CMS CMS•CMS•CMS•CMS•CMS•CMS•CMS CMS•CMS•CMS•CMS•CMS•CMS•CMS CMS•CMS•CMS•CMS•CMS•CMS•CMS CMS•CMS•CMS•CMS•CMS•CMS•CMS CMS•CMS•CMS•CMS•CMS•CMS•CMS CMS•CMS•CMS•CMS•CMS•CMS•CMS CMS•CMS•CMS•CMS•CMS•CMS•CMS CMS•CMS•CMS•CMS•CMS•CMS•CMS CMS•CMS•CMS•CMS•CMS•CMS•CMS CMS•CMS•CMS•CMS•CMS•CMS•CMS CMS•CMS•CMS•CMS•CMS•CMS•CMS CMS•CMS•CMS•CMS•CMS•CMS•CMS CMS•CMS•CMS•CMS•CMS•CMS•CMS CMS•CMS•CMS•CMS•CMS•CMS•CMS CMS•CMS•CMS•CMS•CMS•CMS•CMS
30/06/2011
9
VOLÚMENES Y PESOS DE LAS FASES DEL SUELO
RELACIÓN DE PESOS Y VOLÚMENES
PESO ESPECÍFICO γS
EL PESO ESPECÍFICO O DENSIDAD REAL,
ES EL PESO VOLUMÉTRICO DE LA FASE SÓLIDA
γS DE ALGUNOS SUELOS
ARENA DE CUARZO 2,64 a 2,66 gr/cm3
LIMO 2,67 a 2,73 gr/cm3
ARCILLAS 2,70 a 2,90 gr/cm3
LOESS 2,65 a 2,75 gr/cm3
TURBA 1,30 a 1,90 gr/cm3
ES LLAMADO TAMBIÉN PESO VOLUMÉTRICO DE LOS SÓLIDOS
VOLÚMENES Y PESOS DE LAS FASES DEL SUELO
RELACIÓN DE PESOS Y VOLÚMENES
DENSIDAD APARENTE
LA DENSIDAD BRUTA O APARENTE ES EL PESO POR UNIDAD DE VOLUMEN
O PVU
INCLUYE EL PESO DE LAS FASES LÍQUIDA Y SÓLIDA
LA DENSIDAD APARENTE DEPENDE DEL CONTENIDO DE HUMEDAD
SECO SUB-SATURADO SATURADO
d sbs s
d < sbs < s
CMS•CMS•CMS•CMS•CMS•CMS•CMS CMS•CMS•CMS•CMS•CMS•CMS•CMS CMS•CMS•CMS•CMS•CMS•CMS•CMS CMS•CMS•CMS•CMS•CMS•CMS•CMS CMS•CMS•CMS•CMS•CMS•CMS•CMS CMS•CMS•CMS•CMS•CMS•CMS•CMS CMS•CMS•CMS•CMS•CMS•CMS•CMS CMS•CMS•CMS•CMS•CMS•CMS•CMS CMS•CMS•CMS•CMS•CMS•CMS•CMS CMS•CMS•CMS•CMS•CMS•CMS•CMS CMS•CMS•CMS•CMS•CMS•CMS•CMS CMS•CMS•CMS•CMS•CMS•CMS•CMS CMS•CMS•CMS•CMS•CMS•CMS•CMS CMS•CMS•CMS•CMS•CMS•CMS•CMS CMS•CMS•CMS•CMS•CMS•CMS•CMS CMS•CMS•CMS•CMS•CMS•CMS•CMS CMS•CMS•CMS•CMS•CMS•CMS•CMS CMS•CMS•CMS•CMS•CMS•CMS•CMS CMS•CMS•CMS•CMS•CMS•CMS•CMS CMS•CMS•CMS•CMS•CMS•CMS•CMS CMS•CMS•CMS•CMS•CMS•CMS•CMS
30/06/2011
10
RELACIONES FUNDAMENTALES
DENSIDAD APARENTE O PESO VOLUMÉTRICO UNITARIO PVU
Y RELACIÓN DE VACÍOS e
LA DENSIDAD APARENTE O PESO VOLUMÉTRICO UNITARIO PVU
Y LA RELACIÓN DE VACÍOS e, NO DEPENDEN DEL TAMAÑO DE LAS PARTÍCULAS SIEMPRE QUE ESTAS SEAN UNIFORMES Y MANTENGAN LA MISMA DISPOSICIÓN,
ES DECIR SIEMPRE QUE NO SE MODIFIQUE SU “EMPAQUETAMIENTO”
e1
PVU1
e2
PVU2
e1 = e2 Y PVU1 = PVU2
EN LOS DOS CASOS Vs Y Vt SON LOS MISMOS
ENTONCES:
FACTORES QUE AFECTAN e y PVU
LA DENSIDAD APARENTE O PESO VOLUMÉTRICO UNITARIO PVU
Y LA RELACIÓN DE VACÍOS e DEPENDEN DE LA DISPOSICIÓN DE LAS PARTÍCULAS
ES DECIR DEL EMPAQUETAMIENTO
e1 - PVU1 e2 - PVU2 e1 - PVU1 e2 - PVU2
PRIMER CASO SEGUNDO CASO PRIMER CASO SEGUNDO CASO
EN EL SEGUNDO CASO DE LOS DOS EJEMPLOS
PARA UN MISMO Vs SE REDUCEN Vv Y Vt
ENTONCES:
e1 > e2 Y PVU1 < PVU2
CMS•CMS•CMS•CMS•CMS•CMS•CMS CMS•CMS•CMS•CMS•CMS•CMS•CMS CMS•CMS•CMS•CMS•CMS•CMS•CMS CMS•CMS•CMS•CMS•CMS•CMS•CMS CMS•CMS•CMS•CMS•CMS•CMS•CMS CMS•CMS•CMS•CMS•CMS•CMS•CMS CMS•CMS•CMS•CMS•CMS•CMS•CMS CMS•CMS•CMS•CMS•CMS•CMS•CMS CMS•CMS•CMS•CMS•CMS•CMS•CMS CMS•CMS•CMS•CMS•CMS•CMS•CMS CMS•CMS•CMS•CMS•CMS•CMS•CMS CMS•CMS•CMS•CMS•CMS•CMS•CMS CMS•CMS•CMS•CMS•CMS•CMS•CMS CMS•CMS•CMS•CMS•CMS•CMS•CMS CMS•CMS•CMS•CMS•CMS•CMS•CMS CMS•CMS•CMS•CMS•CMS•CMS•CMS CMS•CMS•CMS•CMS•CMS•CMS•CMS CMS•CMS•CMS•CMS•CMS•CMS•CMS CMS•CMS•CMS•CMS•CMS•CMS•CMS CMS•CMS•CMS•CMS•CMS•CMS•CMS CMS•CMS•CMS•CMS•CMS•CMS•CMS
30/06/2011
11
FACTORES QUE AFECTAN e y PVU
LA DENSIDAD APARENTE O PESO VOLUMÉTRICO UNITARIO PVU
Y LA RELACIÓN DE VACÍOS e, DEPENDEN DEL EMPAQUETAMIENTO Y DE LA GRANULOMETRÍA, ES DECIR, DE LA GRADACIÓN DE LAS PARTICULAS
PRIMER CASO SEGUNDO CASO
e1 - PVU1 e2 - PVU2
PARA LA MISMA UNIDAD DE VOLUMEN
EN EL PRIMER CASO HAY DOS TAMAÑOS DE PARTÍCULAS
EN EL SEGUNDO CASO HAY TRES TAMAÑOS DE PARTÍCULAS
ENTONCES:
e1 > e2 Y PVU1 < PVU2
GRANULOMETRÍA PROCEDIMIENTO => ANÁLISIS GRANULOMÉTRICO => CURVA GRANULOMETRICA => Fracción mayor a 0,075 mm (Tamiz #200) => Análisis por vía seca => Tamizado => Fracción menor a 0,075 mm (Tamiz #200) => Análisis por vía húmeda => Método del Hidrómetro
GRANULOMETRÍA
DETERMINACIÓN DE LA DISTRIBUCIÓN DE LAS PARTÍCULAS POR
TAMAÑO EN UNA MUESTRA DE SUELO
MUESTRA DE SUELO
FRACCIÓN
GRUESA
FRACCIÓN
INTERMEDIA
FRACCIÓN
FINA
CMS•CMS•CMS•CMS•CMS•CMS•CMS CMS•CMS•CMS•CMS•CMS•CMS•CMS CMS•CMS•CMS•CMS•CMS•CMS•CMS CMS•CMS•CMS•CMS•CMS•CMS•CMS CMS•CMS•CMS•CMS•CMS•CMS•CMS CMS•CMS•CMS•CMS•CMS•CMS•CMS CMS•CMS•CMS•CMS•CMS•CMS•CMS CMS•CMS•CMS•CMS•CMS•CMS•CMS CMS•CMS•CMS•CMS•CMS•CMS•CMS CMS•CMS•CMS•CMS•CMS•CMS•CMS CMS•CMS•CMS•CMS•CMS•CMS•CMS CMS•CMS•CMS•CMS•CMS•CMS•CMS CMS•CMS•CMS•CMS•CMS•CMS•CMS CMS•CMS•CMS•CMS•CMS•CMS•CMS CMS•CMS•CMS•CMS•CMS•CMS•CMS CMS•CMS•CMS•CMS•CMS•CMS•CMS CMS•CMS•CMS•CMS•CMS•CMS•CMS CMS•CMS•CMS•CMS•CMS•CMS•CMS CMS•CMS•CMS•CMS•CMS•CMS•CMS CMS•CMS•CMS•CMS•CMS•CMS•CMS CMS•CMS•CMS•CMS•CMS•CMS•CMS
30/06/2011
12
DETERMINACIÓN GRANULOMETRÍA
POR TAMIZADO
SUELO BIEN GRADUADO EXISTE UNA GRADUACIÓN CONTINUA DE TAMAÑOS DE
PARTÍCULAS
SUELO MAL GRADUADO EXISTE UNA GRADUACIÓN UNIFORME DE TAMAÑOS DE
PARTÍCULAS
SUELO CON GRADUACIÓN DISCONTINUA EXISTE UNA GRADUACIÓN DISCONTINUA DE TAMAÑOS DE
PARTÍCULAS
GRANULOMETRÍA
GRADUACIÓN
CMS•CMS•CMS•CMS•CMS•CMS•CMS CMS•CMS•CMS•CMS•CMS•CMS•CMS CMS•CMS•CMS•CMS•CMS•CMS•CMS CMS•CMS•CMS•CMS•CMS•CMS•CMS CMS•CMS•CMS•CMS•CMS•CMS•CMS CMS•CMS•CMS•CMS•CMS•CMS•CMS CMS•CMS•CMS•CMS•CMS•CMS•CMS CMS•CMS•CMS•CMS•CMS•CMS•CMS CMS•CMS•CMS•CMS•CMS•CMS•CMS CMS•CMS•CMS•CMS•CMS•CMS•CMS CMS•CMS•CMS•CMS•CMS•CMS•CMS CMS•CMS•CMS•CMS•CMS•CMS•CMS CMS•CMS•CMS•CMS•CMS•CMS•CMS CMS•CMS•CMS•CMS•CMS•CMS•CMS CMS•CMS•CMS•CMS•CMS•CMS•CMS CMS•CMS•CMS•CMS•CMS•CMS•CMS CMS•CMS•CMS•CMS•CMS•CMS•CMS CMS•CMS•CMS•CMS•CMS•CMS•CMS CMS•CMS•CMS•CMS•CMS•CMS•CMS CMS•CMS•CMS•CMS•CMS•CMS•CMS CMS•CMS•CMS•CMS•CMS•CMS•CMS
30/06/2011
13
SUELOS DE CARACTERÍSTICAS ESPECIALES
DENTRO DE LOS SUELOS ESTRUCTURALMENTE ESTABLES SE DISTINGUEN
LOS SUELOS EXPANSIVOS SE EXPANDEN CUANDO AUMENTA EL PORCENTAJE DE HUMEDAD Y SE CONTRAEN
DURANTE LA DESECACIÓN. ALTAMENTE ACTIVOS FRENTE A CAMBIOS CÍCLICOS
EN EL CONTENIDO DE HUMEDAD.
DENTRO DE LOS SUELOS ESTRUCTURALMENTE INESTABLES SE DISTINGUEN
LOS SUELOS DISPERSIVOS O EROSIONABLES ALTA VULNERABILIDAD A LA PRESENCIA DE AGUA. REDUCEN SU VOLUMEN
POR SUSPENSIÓN Y/O ARRASTRE DE PARTÍCULAS.
SE CLASIFICAN EN EROSIONABLES Y DISPERSIVOS.
Y LOS SUELOS COLAPSABLES ALTA RESISTENCIA EN SECO, PERO ALTA VULNERABILIDAD A LA PRESENCIA DE
AGUA. SE ALTERA LA CONFORMACIÓN ESTRUCTURAL Y LOS SUELOS REDUCEN
SU VOLUMEN CON EL AUMENTO DE LA HUMEDAD Y LA SATURACIÓN.
SE CLASIFICAN EN AUTOCOLAPSABLES Y POTENCIALMENTE COLAPSABLES.
ADEMÁS, EN MECÁNICA DE SUELOS SE TAMBIÉN SE DIFERENCIAN DE ACUERDO
CON CIERTAS CARACTERÍSTICAS ESPECIALES QUE DETERMINAN SU
COMPORTAMIENTO.
CMS•CMS•CMS•CMS•CMS•CMS•CMS CMS•CMS•CMS•CMS•CMS•CMS•CMS CMS•CMS•CMS•CMS•CMS•CMS•CMS CMS•CMS•CMS•CMS•CMS•CMS•CMS CMS•CMS•CMS•CMS•CMS•CMS•CMS CMS•CMS•CMS•CMS•CMS•CMS•CMS CMS•CMS•CMS•CMS•CMS•CMS•CMS CMS•CMS•CMS•CMS•CMS•CMS•CMS CMS•CMS•CMS•CMS•CMS•CMS•CMS CMS•CMS•CMS•CMS•CMS•CMS•CMS CMS•CMS•CMS•CMS•CMS•CMS•CMS CMS•CMS•CMS•CMS•CMS•CMS•CMS CMS•CMS•CMS•CMS•CMS•CMS•CMS CMS•CMS•CMS•CMS•CMS•CMS•CMS CMS•CMS•CMS•CMS•CMS•CMS•CMS CMS•CMS•CMS•CMS•CMS•CMS•CMS CMS•CMS•CMS•CMS•CMS•CMS•CMS CMS•CMS•CMS•CMS•CMS•CMS•CMS CMS•CMS•CMS•CMS•CMS•CMS•CMS CMS•CMS•CMS•CMS•CMS•CMS•CMS CMS•CMS•CMS•CMS•CMS•CMS•CMS
30/06/2011
14
CMS•CMS•CMS•CMS•CMS•CMS•CMS CMS•CMS•CMS•CMS•CMS•CMS•CMS CMS•CMS•CMS•CMS•CMS•CMS•CMS CMS•CMS•CMS•CMS•CMS•CMS•CMS CMS•CMS•CMS•CMS•CMS•CMS•CMS CMS•CMS•CMS•CMS•CMS•CMS•CMS CMS•CMS•CMS•CMS•CMS•CMS•CMS CMS•CMS•CMS•CMS•CMS•CMS•CMS CMS•CMS•CMS•CMS•CMS•CMS•CMS CMS•CMS•CMS•CMS•CMS•CMS•CMS CMS•CMS•CMS•CMS•CMS•CMS•CMS CMS•CMS•CMS•CMS•CMS•CMS•CMS CMS•CMS•CMS•CMS•CMS•CMS•CMS CMS•CMS•CMS•CMS•CMS•CMS•CMS CMS•CMS•CMS•CMS•CMS•CMS•CMS CMS•CMS•CMS•CMS•CMS•CMS•CMS CMS•CMS•CMS•CMS•CMS•CMS•CMS CMS•CMS•CMS•CMS•CMS•CMS•CMS CMS•CMS•CMS•CMS•CMS•CMS•CMS CMS•CMS•CMS•CMS•CMS•CMS•CMS CMS•CMS•CMS•CMS•CMS•CMS•CMS
30/06/2011
15
PROCESO CÍCLICO DE EXPANSIÓN-CONTRACCIÓN
CMS•CMS•CMS•CMS•CMS•CMS•CMS CMS•CMS•CMS•CMS•CMS•CMS•CMS CMS•CMS•CMS•CMS•CMS•CMS•CMS CMS•CMS•CMS•CMS•CMS•CMS•CMS CMS•CMS•CMS•CMS•CMS•CMS•CMS CMS•CMS•CMS•CMS•CMS•CMS•CMS CMS•CMS•CMS•CMS•CMS•CMS•CMS CMS•CMS•CMS•CMS•CMS•CMS•CMS CMS•CMS•CMS•CMS•CMS•CMS•CMS CMS•CMS•CMS•CMS•CMS•CMS•CMS CMS•CMS•CMS•CMS•CMS•CMS•CMS CMS•CMS•CMS•CMS•CMS•CMS•CMS CMS•CMS•CMS•CMS•CMS•CMS•CMS CMS•CMS•CMS•CMS•CMS•CMS•CMS CMS•CMS•CMS•CMS•CMS•CMS•CMS CMS•CMS•CMS•CMS•CMS•CMS•CMS CMS•CMS•CMS•CMS•CMS•CMS•CMS CMS•CMS•CMS•CMS•CMS•CMS•CMS CMS•CMS•CMS•CMS•CMS•CMS•CMS CMS•CMS•CMS•CMS•CMS•CMS•CMS CMS•CMS•CMS•CMS•CMS•CMS•CMS
30/06/2011
16
A
Btss1
Btss2
BCk
Agregado cuneiforme o esfenoide
RASGOS MORFOLÓGICOS SUB-SUPERFICIALES
AGREGADOS CUNEIFORMES CMS•CMS•CMS•CMS•CMS•CMS•CMS CMS•CMS•CMS•CMS•CMS•CMS•CMS CMS•CMS•CMS•CMS•CMS•CMS•CMS CMS•CMS•CMS•CMS•CMS•CMS•CMS CMS•CMS•CMS•CMS•CMS•CMS•CMS CMS•CMS•CMS•CMS•CMS•CMS•CMS CMS•CMS•CMS•CMS•CMS•CMS•CMS CMS•CMS•CMS•CMS•CMS•CMS•CMS CMS•CMS•CMS•CMS•CMS•CMS•CMS CMS•CMS•CMS•CMS•CMS•CMS•CMS CMS•CMS•CMS•CMS•CMS•CMS•CMS CMS•CMS•CMS•CMS•CMS•CMS•CMS CMS•CMS•CMS•CMS•CMS•CMS•CMS CMS•CMS•CMS•CMS•CMS•CMS•CMS CMS•CMS•CMS•CMS•CMS•CMS•CMS CMS•CMS•CMS•CMS•CMS•CMS•CMS CMS•CMS•CMS•CMS•CMS•CMS•CMS CMS•CMS•CMS•CMS•CMS•CMS•CMS CMS•CMS•CMS•CMS•CMS•CMS•CMS CMS•CMS•CMS•CMS•CMS•CMS•CMS CMS•CMS•CMS•CMS•CMS•CMS•CMS
30/06/2011
17
DISTRIBUCIÓN DE TENSIONES
CMS•CMS•CMS•CMS•CMS•CMS•CMS CMS•CMS•CMS•CMS•CMS•CMS•CMS CMS•CMS•CMS•CMS•CMS•CMS•CMS CMS•CMS•CMS•CMS•CMS•CMS•CMS CMS•CMS•CMS•CMS•CMS•CMS•CMS CMS•CMS•CMS•CMS•CMS•CMS•CMS CMS•CMS•CMS•CMS•CMS•CMS•CMS CMS•CMS•CMS•CMS•CMS•CMS•CMS CMS•CMS•CMS•CMS•CMS•CMS•CMS CMS•CMS•CMS•CMS•CMS•CMS•CMS CMS•CMS•CMS•CMS•CMS•CMS•CMS CMS•CMS•CMS•CMS•CMS•CMS•CMS CMS•CMS•CMS•CMS•CMS•CMS•CMS CMS•CMS•CMS•CMS•CMS•CMS•CMS CMS•CMS•CMS•CMS•CMS•CMS•CMS CMS•CMS•CMS•CMS•CMS•CMS•CMS CMS•CMS•CMS•CMS•CMS•CMS•CMS CMS•CMS•CMS•CMS•CMS•CMS•CMS CMS•CMS•CMS•CMS•CMS•CMS•CMS CMS•CMS•CMS•CMS•CMS•CMS•CMS CMS•CMS•CMS•CMS•CMS•CMS•CMS
30/06/2011
18
CMS•CMS•CMS•CMS•CMS•CMS•CMS CMS•CMS•CMS•CMS•CMS•CMS•CMS CMS•CMS•CMS•CMS•CMS•CMS•CMS CMS•CMS•CMS•CMS•CMS•CMS•CMS CMS•CMS•CMS•CMS•CMS•CMS•CMS CMS•CMS•CMS•CMS•CMS•CMS•CMS CMS•CMS•CMS•CMS•CMS•CMS•CMS CMS•CMS•CMS•CMS•CMS•CMS•CMS CMS•CMS•CMS•CMS•CMS•CMS•CMS CMS•CMS•CMS•CMS•CMS•CMS•CMS CMS•CMS•CMS•CMS•CMS•CMS•CMS CMS•CMS•CMS•CMS•CMS•CMS•CMS CMS•CMS•CMS•CMS•CMS•CMS•CMS CMS•CMS•CMS•CMS•CMS•CMS•CMS CMS•CMS•CMS•CMS•CMS•CMS•CMS CMS•CMS•CMS•CMS•CMS•CMS•CMS CMS•CMS•CMS•CMS•CMS•CMS•CMS CMS•CMS•CMS•CMS•CMS•CMS•CMS CMS•CMS•CMS•CMS•CMS•CMS•CMS CMS•CMS•CMS•CMS•CMS•CMS•CMS CMS•CMS•CMS•CMS•CMS•CMS•CMS
30/06/2011
19
CMS•CMS•CMS•CMS•CMS•CMS•CMS CMS•CMS•CMS•CMS•CMS•CMS•CMS CMS•CMS•CMS•CMS•CMS•CMS•CMS CMS•CMS•CMS•CMS•CMS•CMS•CMS CMS•CMS•CMS•CMS•CMS•CMS•CMS CMS•CMS•CMS•CMS•CMS•CMS•CMS CMS•CMS•CMS•CMS•CMS•CMS•CMS CMS•CMS•CMS•CMS•CMS•CMS•CMS CMS•CMS•CMS•CMS•CMS•CMS•CMS CMS•CMS•CMS•CMS•CMS•CMS•CMS CMS•CMS•CMS•CMS•CMS•CMS•CMS CMS•CMS•CMS•CMS•CMS•CMS•CMS CMS•CMS•CMS•CMS•CMS•CMS•CMS CMS•CMS•CMS•CMS•CMS•CMS•CMS CMS•CMS•CMS•CMS•CMS•CMS•CMS CMS•CMS•CMS•CMS•CMS•CMS•CMS CMS•CMS•CMS•CMS•CMS•CMS•CMS CMS•CMS•CMS•CMS•CMS•CMS•CMS CMS•CMS•CMS•CMS•CMS•CMS•CMS CMS•CMS•CMS•CMS•CMS•CMS•CMS CMS•CMS•CMS•CMS•CMS•CMS•CMS
30/06/2011
20
CMS•CMS•CMS•CMS•CMS•CMS•CMS CMS•CMS•CMS•CMS•CMS•CMS•CMS CMS•CMS•CMS•CMS•CMS•CMS•CMS CMS•CMS•CMS•CMS•CMS•CMS•CMS CMS•CMS•CMS•CMS•CMS•CMS•CMS CMS•CMS•CMS•CMS•CMS•CMS•CMS CMS•CMS•CMS•CMS•CMS•CMS•CMS CMS•CMS•CMS•CMS•CMS•CMS•CMS CMS•CMS•CMS•CMS•CMS•CMS•CMS CMS•CMS•CMS•CMS•CMS•CMS•CMS CMS•CMS•CMS•CMS•CMS•CMS•CMS CMS•CMS•CMS•CMS•CMS•CMS•CMS CMS•CMS•CMS•CMS•CMS•CMS•CMS CMS•CMS•CMS•CMS•CMS•CMS•CMS CMS•CMS•CMS•CMS•CMS•CMS•CMS CMS•CMS•CMS•CMS•CMS•CMS•CMS CMS•CMS•CMS•CMS•CMS•CMS•CMS CMS•CMS•CMS•CMS•CMS•CMS•CMS CMS•CMS•CMS•CMS•CMS•CMS•CMS CMS•CMS•CMS•CMS•CMS•CMS•CMS CMS•CMS•CMS•CMS•CMS•CMS•CMS
30/06/2011
21
RECONOCIMIENTO DE SUELOS EXPANSIVOS
RASGOS MORFOLÓGICOS
LA ACTIVIDAD DE EXPANSIÓN-CONTRACCIÓN FRENTE A CAMBIOS CÍCLICOS EN
EL CONTENIDO DE HUMEDAD, PUEDE RECONOCERSE MEDIANTE LA OBSERVACIÓN
EN CAMPO DE UN CONJUNTO DE RASGOS MORFOLÓGICOS SUPERFICIALES Y
SUB-SUPERFICIALES.
PROPIEDADES ÍNDICES O PARÁMETROS DE ATTERBERG
LÍMITE LÍQUIDO: CONTENIDO DE HUMEDAD A PARTIR DEL CUAL EL SUELO SE COMPORTA COMO UN
FUIDO VISCOSO. SE EXPRESA EN % DE HUMEDAD
CMS•CMS•CMS•CMS•CMS•CMS•CMS CMS•CMS•CMS•CMS•CMS•CMS•CMS CMS•CMS•CMS•CMS•CMS•CMS•CMS CMS•CMS•CMS•CMS•CMS•CMS•CMS CMS•CMS•CMS•CMS•CMS•CMS•CMS CMS•CMS•CMS•CMS•CMS•CMS•CMS CMS•CMS•CMS•CMS•CMS•CMS•CMS CMS•CMS•CMS•CMS•CMS•CMS•CMS CMS•CMS•CMS•CMS•CMS•CMS•CMS CMS•CMS•CMS•CMS•CMS•CMS•CMS CMS•CMS•CMS•CMS•CMS•CMS•CMS CMS•CMS•CMS•CMS•CMS•CMS•CMS CMS•CMS•CMS•CMS•CMS•CMS•CMS CMS•CMS•CMS•CMS•CMS•CMS•CMS CMS•CMS•CMS•CMS•CMS•CMS•CMS CMS•CMS•CMS•CMS•CMS•CMS•CMS CMS•CMS•CMS•CMS•CMS•CMS•CMS CMS•CMS•CMS•CMS•CMS•CMS•CMS CMS•CMS•CMS•CMS•CMS•CMS•CMS CMS•CMS•CMS•CMS•CMS•CMS•CMS CMS•CMS•CMS•CMS•CMS•CMS•CMS
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PROPIEDADES ÍNDICES O PARÁMETROS DE ATTERBERG
LÍMITE PLÁSTICO: CONTENIDO DE HUMEDAD A PARTIR DEL CUAL EL SUELO DEJA DE COMPORTARSE
COMO UN MATERIAL PLÁSTICO. SE EXPRESA EN % DE HUMEDAD
PROPIEDADES ÍNDICES O PARÁMETROS DE ATTERBERG
LÍMITE DE CONTRACCIÓN: CONTENIDO DE HUMEDAD A PARTIR DEL CUAL EL SUELO YA NO REDUCE SU
VOLUMEN. SE EXPRESA EN % DE HUMEDAD
CMS•CMS•CMS•CMS•CMS•CMS•CMS CMS•CMS•CMS•CMS•CMS•CMS•CMS CMS•CMS•CMS•CMS•CMS•CMS•CMS CMS•CMS•CMS•CMS•CMS•CMS•CMS CMS•CMS•CMS•CMS•CMS•CMS•CMS CMS•CMS•CMS•CMS•CMS•CMS•CMS CMS•CMS•CMS•CMS•CMS•CMS•CMS CMS•CMS•CMS•CMS•CMS•CMS•CMS CMS•CMS•CMS•CMS•CMS•CMS•CMS CMS•CMS•CMS•CMS•CMS•CMS•CMS CMS•CMS•CMS•CMS•CMS•CMS•CMS CMS•CMS•CMS•CMS•CMS•CMS•CMS CMS•CMS•CMS•CMS•CMS•CMS•CMS CMS•CMS•CMS•CMS•CMS•CMS•CMS CMS•CMS•CMS•CMS•CMS•CMS•CMS CMS•CMS•CMS•CMS•CMS•CMS•CMS CMS•CMS•CMS•CMS•CMS•CMS•CMS CMS•CMS•CMS•CMS•CMS•CMS•CMS CMS•CMS•CMS•CMS•CMS•CMS•CMS CMS•CMS•CMS•CMS•CMS•CMS•CMS CMS•CMS•CMS•CMS•CMS•CMS•CMS
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SUELO BIEN GRADUADO EXISTE UNA GRADUACIÓN CONTINUA DE TAMAÑOS DE
PARTÍCULAS
SUELO MAL GRADUADO EXISTE UNA GRADUACIÓN UNIFORME DE TAMAÑOS DE
PARTÍCULAS
SUELO CON GRADUACIÓN DISCONTINUA EXISTE UNA GRADUACIÓN DISCONTINUA DE TAMAÑOS DE
PARTÍCULAS
GRANULOMETRÍA
GRADUACIÓN
RECONOCIMIENTO DE SUELOS EXPANSIVOS
DETERMINACIONES Y ENSAYOS DE LABORATORIO
LA ACTIVIDAD DE EXPANSIÓN-CONTRACCIÓN FRENTE A CAMBIOS CÍCLICOS EN
EL CONTENIDO DE HUMEDAD, PUEDE DETERMINARSE MEDIANTE DISTINTOS
MÉTODOS Y ENSAYOS DE LABORATORIO.
ENTRE MUCHOS OTROS:
INDIRECTOS EMPÍRICOS Y CUALITATIVOS BASADOS EN LAS PROPIEDADES ÍNDICES LÍMITE LÍQUIDO (LL)
LÍMITE PLÁSTICO (LP)
LÍMITE DE CONTRACCIÓN (LC)
INDICE PLÁSTICO (IP)
INDICE DE CONTRACCIÓN (IC)
RELACIÓN ENTRE LAS PROPIEDADES ÍNDICES Y PORCENTAJE DE FINOS < 2 ÍNDICE DE ACTIVIDAD
DIRECTOS SEMICUANTITATIVOS ENSAYO DE EXPANSIÓN LIBRE
DIRECTOS CUANTITATIVOS ENSAYO DE EXPANSIÓN POTENCIAL
RELACIÓN DE MÉTODOS DIRECTOS E INDIRECTOS
RELACIÓN ENTRE POTENCIAL DE EXPANSIÓN Y PROPIEDADES ÍNDICES
CMS•CMS•CMS•CMS•CMS•CMS•CMS CMS•CMS•CMS•CMS•CMS•CMS•CMS CMS•CMS•CMS•CMS•CMS•CMS•CMS CMS•CMS•CMS•CMS•CMS•CMS•CMS CMS•CMS•CMS•CMS•CMS•CMS•CMS CMS•CMS•CMS•CMS•CMS•CMS•CMS CMS•CMS•CMS•CMS•CMS•CMS•CMS CMS•CMS•CMS•CMS•CMS•CMS•CMS CMS•CMS•CMS•CMS•CMS•CMS•CMS CMS•CMS•CMS•CMS•CMS•CMS•CMS CMS•CMS•CMS•CMS•CMS•CMS•CMS CMS•CMS•CMS•CMS•CMS•CMS•CMS CMS•CMS•CMS•CMS•CMS•CMS•CMS CMS•CMS•CMS•CMS•CMS•CMS•CMS CMS•CMS•CMS•CMS•CMS•CMS•CMS CMS•CMS•CMS•CMS•CMS•CMS•CMS CMS•CMS•CMS•CMS•CMS•CMS•CMS CMS•CMS•CMS•CMS•CMS•CMS•CMS CMS•CMS•CMS•CMS•CMS•CMS•CMS CMS•CMS•CMS•CMS•CMS•CMS•CMS CMS•CMS•CMS•CMS•CMS•CMS•CMS
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A
Btss1
Btss2
BCk
A Btss1 Btss2 BCk
PROFUNDIDAD DE LA ZONA ACTIVA
PERFIL DE HUMEDAD, PROFUNDIDAD Y HUMEDAD DE EQUILIBRIO
CMS•CMS•CMS•CMS•CMS•CMS•CMS CMS•CMS•CMS•CMS•CMS•CMS•CMS CMS•CMS•CMS•CMS•CMS•CMS•CMS CMS•CMS•CMS•CMS•CMS•CMS•CMS CMS•CMS•CMS•CMS•CMS•CMS•CMS CMS•CMS•CMS•CMS•CMS•CMS•CMS CMS•CMS•CMS•CMS•CMS•CMS•CMS CMS•CMS•CMS•CMS•CMS•CMS•CMS CMS•CMS•CMS•CMS•CMS•CMS•CMS CMS•CMS•CMS•CMS•CMS•CMS•CMS CMS•CMS•CMS•CMS•CMS•CMS•CMS CMS•CMS•CMS•CMS•CMS•CMS•CMS CMS•CMS•CMS•CMS•CMS•CMS•CMS CMS•CMS•CMS•CMS•CMS•CMS•CMS CMS•CMS•CMS•CMS•CMS•CMS•CMS CMS•CMS•CMS•CMS•CMS•CMS•CMS CMS•CMS•CMS•CMS•CMS•CMS•CMS CMS•CMS•CMS•CMS•CMS•CMS•CMS CMS•CMS•CMS•CMS•CMS•CMS•CMS CMS•CMS•CMS•CMS•CMS•CMS•CMS CMS•CMS•CMS•CMS•CMS•CMS•CMS
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CMS•CMS•CMS•CMS•CMS•CMS•CMS CMS•CMS•CMS•CMS•CMS•CMS•CMS CMS•CMS•CMS•CMS•CMS•CMS•CMS CMS•CMS•CMS•CMS•CMS•CMS•CMS CMS•CMS•CMS•CMS•CMS•CMS•CMS CMS•CMS•CMS•CMS•CMS•CMS•CMS CMS•CMS•CMS•CMS•CMS•CMS•CMS CMS•CMS•CMS•CMS•CMS•CMS•CMS CMS•CMS•CMS•CMS•CMS•CMS•CMS CMS•CMS•CMS•CMS•CMS•CMS•CMS CMS•CMS•CMS•CMS•CMS•CMS•CMS CMS•CMS•CMS•CMS•CMS•CMS•CMS CMS•CMS•CMS•CMS•CMS•CMS•CMS CMS•CMS•CMS•CMS•CMS•CMS•CMS CMS•CMS•CMS•CMS•CMS•CMS•CMS CMS•CMS•CMS•CMS•CMS•CMS•CMS CMS•CMS•CMS•CMS•CMS•CMS•CMS CMS•CMS•CMS•CMS•CMS•CMS•CMS CMS•CMS•CMS•CMS•CMS•CMS•CMS CMS•CMS•CMS•CMS•CMS•CMS•CMS CMS•CMS•CMS•CMS•CMS•CMS•CMS
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SUELOS EROSIONABLES AMBIENTE EN EL QUE SE DESARROLLAN
SUELOS EROSIONABLES RASGOS MORFOLÓGICOS SUB-SUPERFICIALES
CMS•CMS•CMS•CMS•CMS•CMS•CMS CMS•CMS•CMS•CMS•CMS•CMS•CMS CMS•CMS•CMS•CMS•CMS•CMS•CMS CMS•CMS•CMS•CMS•CMS•CMS•CMS CMS•CMS•CMS•CMS•CMS•CMS•CMS CMS•CMS•CMS•CMS•CMS•CMS•CMS CMS•CMS•CMS•CMS•CMS•CMS•CMS CMS•CMS•CMS•CMS•CMS•CMS•CMS CMS•CMS•CMS•CMS•CMS•CMS•CMS CMS•CMS•CMS•CMS•CMS•CMS•CMS CMS•CMS•CMS•CMS•CMS•CMS•CMS CMS•CMS•CMS•CMS•CMS•CMS•CMS CMS•CMS•CMS•CMS•CMS•CMS•CMS CMS•CMS•CMS•CMS•CMS•CMS•CMS CMS•CMS•CMS•CMS•CMS•CMS•CMS CMS•CMS•CMS•CMS•CMS•CMS•CMS CMS•CMS•CMS•CMS•CMS•CMS•CMS CMS•CMS•CMS•CMS•CMS•CMS•CMS CMS•CMS•CMS•CMS•CMS•CMS•CMS CMS•CMS•CMS•CMS•CMS•CMS•CMS CMS•CMS•CMS•CMS•CMS•CMS•CMS
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Deslizamiento en Tartagal
COMO RESUMEN
• A. Los suelos tienen:
• Distinta capacidad de soporte.
• Distinto grado de cohesividad entre sus partículas
• B . • El comportamiento de
los mismos varía según el tenor de humedad.
CMS•CMS•CMS•CMS•CMS•CMS•CMS CMS•CMS•CMS•CMS•CMS•CMS•CMS CMS•CMS•CMS•CMS•CMS•CMS•CMS CMS•CMS•CMS•CMS•CMS•CMS•CMS CMS•CMS•CMS•CMS•CMS•CMS•CMS CMS•CMS•CMS•CMS•CMS•CMS•CMS CMS•CMS•CMS•CMS•CMS•CMS•CMS CMS•CMS•CMS•CMS•CMS•CMS•CMS CMS•CMS•CMS•CMS•CMS•CMS•CMS CMS•CMS•CMS•CMS•CMS•CMS•CMS CMS•CMS•CMS•CMS•CMS•CMS•CMS CMS•CMS•CMS•CMS•CMS•CMS•CMS CMS•CMS•CMS•CMS•CMS•CMS•CMS CMS•CMS•CMS•CMS•CMS•CMS•CMS CMS•CMS•CMS•CMS•CMS•CMS•CMS CMS•CMS•CMS•CMS•CMS•CMS•CMS CMS•CMS•CMS•CMS•CMS•CMS•CMS CMS•CMS•CMS•CMS•CMS•CMS•CMS CMS•CMS•CMS•CMS•CMS•CMS•CMS CMS•CMS•CMS•CMS•CMS•CMS•CMS CMS•CMS•CMS•CMS•CMS•CMS•CMS
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Conocer el suelo
• Nos permitirá planificar fundaciones más eficaces y eficientes para nuestra arquitectura.
CMS•CMS•CMS•CMS•CMS•CMS•CMS CMS•CMS•CMS•CMS•CMS•CMS•CMS CMS•CMS•CMS•CMS•CMS•CMS•CMS CMS•CMS•CMS•CMS•CMS•CMS•CMS CMS•CMS•CMS•CMS•CMS•CMS•CMS CMS•CMS•CMS•CMS•CMS•CMS•CMS CMS•CMS•CMS•CMS•CMS•CMS•CMS CMS•CMS•CMS•CMS•CMS•CMS•CMS CMS•CMS•CMS•CMS•CMS•CMS•CMS CMS•CMS•CMS•CMS•CMS•CMS•CMS CMS•CMS•CMS•CMS•CMS•CMS•CMS CMS•CMS•CMS•CMS•CMS•CMS•CMS CMS•CMS•CMS•CMS•CMS•CMS•CMS CMS•CMS•CMS•CMS•CMS•CMS•CMS CMS•CMS•CMS•CMS•CMS•CMS•CMS CMS•CMS•CMS•CMS•CMS•CMS•CMS CMS•CMS•CMS•CMS•CMS•CMS•CMS CMS•CMS•CMS•CMS•CMS•CMS•CMS CMS•CMS•CMS•CMS•CMS•CMS•CMS CMS•CMS•CMS•CMS•CMS•CMS•CMS CMS•CMS•CMS•CMS•CMS•CMS•CMS