|
|
||||||||
| ||||||||||||||||||||||||||||||||||||||||||||||||||||||||||
ABSTRACT
The Zonal soils of New York are members of the Gray-Brown Podzolic, Brown Podzolic, and Podzol great soil groups. Each dominates the best-drained sites of extensive areas, but each is associated locally with a complete catena controlled by groundwater relationships. In addition, Brown Forest soils occupy the best-drained sites on some highly calcareous materials, and Alluvial soils occur on recent alluvium. Each of these is also associated with a complete catena.
1 Contribution from the Department of Agronomy, Cornell University Agricultural Experiment Station, Ithaca, N. Y. First received for publication September 6, 1951; publication delay due to loss of original manuscript in the mail. Presented before Section V, Soil Science Society of America, State College, Pa., August 28, 1951.
| HOME | HELP | FEEDBACK | SUBSCRIPTIONS | ARCHIVE | SEARCH | TABLE OF CONTENTS |
| The SCI Journals | Agronomy Journal | Crop Science | |||
| Vadose Zone Journal | Journal of Plant Registrations | ||||
| Journal of Natural Resources and Life Sciences Education |
Journal of Environmental Quality |
||||