Titre :	Micromorphology of a saline soils with calcrete in punjab, India
Type de document :	texte imprimé
Auteurs :	Frei, E.
Mention d'édition :	Swiss Federal Research Station for Agronomy
Editeur :	Swiss Federal Research Station for Agronomy
Année de publication :	1975
ISBN/ISSN/EAN :	CI-10581
Note générale :	Areas with imped drainage on silty deposits are often occupied by saline soils and calcrete. Their managment and reclamtion cause very difficult problems. Thin sections of the horizons of a representative soil profile show the typical phenomena of alkaline, halomorphic soils. The 40 cm clearly bordered, usual argillans. Below the calcrete a silty material with calcrete has formed under waterlogging conditions or in a small pond.
Langues :	Anglais (eng)
Mots-clés :	Gestion des sols  Sol salé  Drainage  Argile  Micromorphologie  Calcaire  Sol halomrphique
Index. décimale :	631.6 Préparation des sols et drainage
Résumé :	Areas with imped drainage on silty deposits are often occupied by saline soils and calcrete. Their managment and reclamtion cause very difficult problems. Thin sections of the horizons of a representative soil profile show the typical phenomena of alkaline, halomorphic soils. The 40 cm clearly bordered, usual argillans. Below the calcrete a silty material with calcrete has formed under waterlogging conditions or in a small pond.
Note de contenu :	Areas with imped drainage on silty deposits are often occupied by saline soils and calcrete. Their managment and reclamtion cause very difficult problems. Thin sections of the horizons of a representative soil profile show the typical phenomena of alkaline, halomorphic soils. The 40 cm clearly bordered, usual argillans. Below the calcrete a silty material with calcrete has formed under waterlogging conditions or in a small pond.

Micromorphology of a saline soils with calcrete in punjab, India [texte imprimé] / Frei, E.  . -  Swiss Federal Research Station for Agronomy . - Swiss Federal Research Station for Agronomy, 1975.
ISSN : CI-10581
Areas with imped drainage on silty deposits are often occupied by saline soils and calcrete. Their managment and reclamtion cause very difficult problems. Thin sections of the horizons of a representative soil profile show the typical phenomena of alkaline, halomorphic soils. The 40 cm clearly bordered, usual argillans. Below the calcrete a silty material with calcrete has formed under waterlogging conditions or in a small pond.
Langues : Anglais (eng)

Mots-clés :	Gestion des sols  Sol salé  Drainage  Argile  Micromorphologie  Calcaire  Sol halomrphique
Index. décimale :	631.6 Préparation des sols et drainage
Résumé :	Areas with imped drainage on silty deposits are often occupied by saline soils and calcrete. Their managment and reclamtion cause very difficult problems. Thin sections of the horizons of a representative soil profile show the typical phenomena of alkaline, halomorphic soils. The 40 cm clearly bordered, usual argillans. Below the calcrete a silty material with calcrete has formed under waterlogging conditions or in a small pond.
Note de contenu :	Areas with imped drainage on silty deposits are often occupied by saline soils and calcrete. Their managment and reclamtion cause very difficult problems. Thin sections of the horizons of a representative soil profile show the typical phenomena of alkaline, halomorphic soils. The 40 cm clearly bordered, usual argillans. Below the calcrete a silty material with calcrete has formed under waterlogging conditions or in a small pond.