THE FERTILITY OF CHERNOZEMIC SOILS ON THE MORAINE DEPOSITS
Moraine deposits in the Penza oblast were formed as a result of the destruction of the Oka-Don glacier of the lower boundary of the neo-Pleistocene during warming [6, 15, 16]. The thickness of the main moraine can be ≈ 30.0 m [8, 10]. In terms of spacing, glacial deposits of the Don horizon pre-domi...
| Main Authors: | , |
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| Format: | Article |
| Language: | English |
| Published: |
Editorial and publishing department of FSBEE HE Penza SAU
2020-10-01
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| Series: | Volga Region Farmland |
| Subjects: | |
| Online Access: | https://niva-volga.ru/file/vipuski/2020_3_56/en/2020_2_6_en_23-27.pdf |