Micromorphology of a saline soils with calcrete in punjab, India / Frei, E.

Public ISBD 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.

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