Open Access Open Access  Restricted Access Subscription Access

Characteristics of Mangroves Substrate Sediments of Sunderbans


Affiliations
1 Department of Chemical Engineering, Jadavpur University, Calcutta-700 032, India
 

Sunderbans soil is typically a physiologically dry soil because plants cannot absorb water properly from the soil due to presence of high amount of salt. The coastal tidal forest, Sunderbans has the saline micaceous deltaic alluvium of humid region. Sunderbans has too saline humic and acid sulphate soils of humid tropical region. Acid sulphate soil has highly acidic pH, high EC, presence of humic (organic) horizon, dominance of sulphate and chloride salts. Substrate soils of different geomorphic regions like riverbank, mudflats and natural levees of Sunderbans are poor in aeration and water holding capacity.

Keywords

Saline Soils, Soil Reactions, Soil Characteristics, Acid Sulphate Soils, Micronutrients, Metal Oxides, NPK, Soil Distributions.
User
Notifications
Font Size


Abstract Views: 413

PDF Views: 134




  • Characteristics of Mangroves Substrate Sediments of Sunderbans

Abstract Views: 413  |  PDF Views: 134

Authors

Gautam Kumar Das
Department of Chemical Engineering, Jadavpur University, Calcutta-700 032, India

Abstract


Sunderbans soil is typically a physiologically dry soil because plants cannot absorb water properly from the soil due to presence of high amount of salt. The coastal tidal forest, Sunderbans has the saline micaceous deltaic alluvium of humid region. Sunderbans has too saline humic and acid sulphate soils of humid tropical region. Acid sulphate soil has highly acidic pH, high EC, presence of humic (organic) horizon, dominance of sulphate and chloride salts. Substrate soils of different geomorphic regions like riverbank, mudflats and natural levees of Sunderbans are poor in aeration and water holding capacity.

Keywords


Saline Soils, Soil Reactions, Soil Characteristics, Acid Sulphate Soils, Micronutrients, Metal Oxides, NPK, Soil Distributions.



DOI: https://doi.org/10.21843/reas%2F2013%2F7-18%2F108135