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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

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Page 1: CMS CMS CMS CMS CMS CMS CMS - WordPress.com · la densidad bruta o aparente es el peso por unidad de volumencms cms cms cms cms cms cms o pvu incluye el peso de las fases lÍquida

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

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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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CMS•CMS•CMS•CMS•CMS•CMS•CMS CMS•CMS•CMS•CMS•CMS•CMS•CMS CMS•CMS•CMS•CMS•CMS•CMS•CMS CMS•CMS•CMS•CMS•CMS•CMS•CMS CMS•CMS•CMS•CMS•CMS•CMS•CMS CMS•CMS•CMS•CMS•CMS•CMS•CMS CMS•CMS•CMS•CMS•CMS•CMS•CMS CMS•CMS•CMS•CMS•CMS•CMS•CMS CMS•CMS•CMS•CMS•CMS•CMS•CMS CMS•CMS•CMS•CMS•CMS•CMS•CMS CMS•CMS•CMS•CMS•CMS•CMS•CMS CMS•CMS•CMS•CMS•CMS•CMS•CMS CMS•CMS•CMS•CMS•CMS•CMS•CMS CMS•CMS•CMS•CMS•CMS•CMS•CMS CMS•CMS•CMS•CMS•CMS•CMS•CMS CMS•CMS•CMS•CMS•CMS•CMS•CMS CMS•CMS•CMS•CMS•CMS•CMS•CMS CMS•CMS•CMS•CMS•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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CMS•CMS•CMS•CMS•CMS•CMS•CMS CMS•CMS•CMS•CMS•CMS•CMS•CMS CMS•CMS•CMS•CMS•CMS•CMS•CMS CMS•CMS•CMS•CMS•CMS•CMS•CMS CMS•CMS•CMS•CMS•CMS•CMS•CMS CMS•CMS•CMS•CMS•CMS•CMS•CMS CMS•CMS•CMS•CMS•CMS•CMS•CMS CMS•CMS•CMS•CMS•CMS•CMS•CMS CMS•CMS•CMS•CMS•CMS•CMS•CMS CMS•CMS•CMS•CMS•CMS•CMS•CMS CMS•CMS•CMS•CMS•CMS•CMS•CMS CMS•CMS•CMS•CMS•CMS•CMS•CMS CMS•CMS•CMS•CMS•CMS•CMS•CMS CMS•CMS•CMS•CMS•CMS•CMS•CMS CMS•CMS•CMS•CMS•CMS•CMS•CMS CMS•CMS•CMS•CMS•CMS•CMS•CMS CMS•CMS•CMS•CMS•CMS•CMS•CMS CMS•CMS•CMS•CMS•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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CMS•CMS•CMS•CMS•CMS•CMS•CMS CMS•CMS•CMS•CMS•CMS•CMS•CMS CMS•CMS•CMS•CMS•CMS•CMS•CMS CMS•CMS•CMS•CMS•CMS•CMS•CMS CMS•CMS•CMS•CMS•CMS•CMS•CMS CMS•CMS•CMS•CMS•CMS•CMS•CMS CMS•CMS•CMS•CMS•CMS•CMS•CMS CMS•CMS•CMS•CMS•CMS•CMS•CMS CMS•CMS•CMS•CMS•CMS•CMS•CMS CMS•CMS•CMS•CMS•CMS•CMS•CMS CMS•CMS•CMS•CMS•CMS•CMS•CMS CMS•CMS•CMS•CMS•CMS•CMS•CMS CMS•CMS•CMS•CMS•CMS•CMS•CMS CMS•CMS•CMS•CMS•CMS•CMS•CMS CMS•CMS•CMS•CMS•CMS•CMS•CMS CMS•CMS•CMS•CMS•CMS•CMS•CMS CMS•CMS•CMS•CMS•CMS•CMS•CMS CMS•CMS•CMS•CMS•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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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

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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

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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

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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

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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

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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

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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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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

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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

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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

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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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CMS•CMS•CMS•CMS•CMS•CMS•CMS CMS•CMS•CMS•CMS•CMS•CMS•CMS CMS•CMS•CMS•CMS•CMS•CMS•CMS CMS•CMS•CMS•CMS•CMS•CMS•CMS CMS•CMS•CMS•CMS•CMS•CMS•CMS CMS•CMS•CMS•CMS•CMS•CMS•CMS CMS•CMS•CMS•CMS•CMS•CMS•CMS CMS•CMS•CMS•CMS•CMS•CMS•CMS CMS•CMS•CMS•CMS•CMS•CMS•CMS CMS•CMS•CMS•CMS•CMS•CMS•CMS CMS•CMS•CMS•CMS•CMS•CMS•CMS CMS•CMS•CMS•CMS•CMS•CMS•CMS CMS•CMS•CMS•CMS•CMS•CMS•CMS CMS•CMS•CMS•CMS•CMS•CMS•CMS CMS•CMS•CMS•CMS•CMS•CMS•CMS CMS•CMS•CMS•CMS•CMS•CMS•CMS CMS•CMS•CMS•CMS•CMS•CMS•CMS CMS•CMS•CMS•CMS•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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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