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Bioreclamation of sodic waste land—a case study
Author(s) -
Garg V. K.
Publication year - 2000
Publication title -
land degradation and development
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 1.403
H-Index - 81
eISSN - 1099-145X
pISSN - 1085-3278
DOI - 10.1002/1099-145x(200009/10)11:5<487::aid-ldr409>3.0.co;2-c
Subject(s) - soil water , environmental science , afforestation , land reclamation , sodic soil , inceptisol , agronomy , alluvial plain , soil science , hydrology (agriculture) , agroforestry , geology , geography , biology , paleontology , geotechnical engineering , archaeology
The study reports a case of bioreclamation of a once barren sodic landscape in the middle part of Gangetic alluvial plain at Banthra Research Station (National Botanical Research Institute, Lucknow, India) (80° 45′ – 53′E and 26° 40′ – 45′N) which began about four decades ago. The investigations were carried out to ascertain the changes in soil characteristics caused by different land‐use systems adopted consistently over three decades. The results showed that the anthropogenic effect on alteration of surface texture through addition of sand in soils of Typic Natrustalfs is still distinct but persistent sodicity is retained. The soils of Inceptic Haplustalfs are markedly improved showing pH value around 8 and ESP > 4 with negligible CaCO 3 . The soils of Aeric Endoaquepts supporting stands of forest trees are now devoid of sodicity to about 0\5 m depth, whereas the soils of Aeric Halaquepts though under cultivation have mild sodicity. Soils of Typic Halaquepts occurring on a low physiographic position with aquic soil moisture regime have high sodicity. Summarizing the results of changes in the surface (0 – 15 cm) soil characteristics caused by continuous cultivation irrespective of any crop grown on any soil type reveals that there is perceptible reduction in soil pH and ESP after three decades of reclamation using organic amendments coupled with regular cultivation and afforestation in different locations. Copyright © 2000 John Wiley & Sons, Ltd.