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El Suelo: Horizontes y Formación

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El Suelo: Horizontes y Formación

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Horizontes y formación del suelo

Created by

CARLOS EDUARDO ANGUIANO GOMEZ
CARLOS EDUARDO ANGUIANO GOMEZ
Mexico

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El Suelo: Horizontes y Formación
 

El Suelo: Horizontes y FormaciónOnline version

Horizontes y formación del suelo

by CARLOS EDUARDO ANGUIANO GOMEZ
1

El horizonte E se caracteriza por lixiviación de minerales, quedando menos partículas insolubles.

2

El clima influye en la velocidad de meteorización y la formación de perfiles de suelo.

3

El horizonte R está formado por rocas desagregadas y sueltas, fundamental para la porosidad.

4

La eluviación aumenta la cantidad de arcilla en el horizonte A.

5

El horizonte A es la capa superior mineral donde se concentran nutrientes y humus ligero.

6

El horizonte B acumula materiales eluviados desde horizontes superiores, como arcillas y óxidos.

7

La formación del suelo implica procesos de meteorización, transporte y transformación del material parental.

8

En un suelo, la materia orgánica se concentra principalmente en el horizonte B.

9

El horizonte O contiene materia orgánica y residuos de plantas en descomposición.

10

El horizonte C es prácticamente una capa de roca sin haber sufrido meteorización.

 
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